Sato Energy Holdings - SRK Consulting Africa
Sato Energy Holdings - SRK Consulting Africa
Sato Energy Holdings - SRK Consulting Africa
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Preliminary Desktop Surface<br />
Water and Geotechnical Study<br />
for the proposed SATO holdings<br />
Photovoltaic project, near<br />
Aggeneys, Northern Cape<br />
Report Prepared for<br />
<strong>Sato</strong> <strong>Energy</strong> <strong>Holdings</strong> (Pty) Ltd<br />
Report Number 435209_SurfaceWater<br />
Report Prepared by<br />
January 2012
<strong>SRK</strong> <strong>Consulting</strong>: 435209: Desktop Surface Water & Geotechnical Page i<br />
Preliminary Desktop Surface Water and<br />
Geotechnical Study for the proposed SATO<br />
holdings Photovoltaic project, near Aggeneys,<br />
Northern Cape<br />
<strong>Sato</strong> <strong>Energy</strong> <strong>Holdings</strong> (Pty) Ltd<br />
111 John Adamson Drive<br />
Montgomery Park<br />
Johannesburg<br />
<strong>SRK</strong> <strong>Consulting</strong> (South <strong>Africa</strong>) (Pty) Ltd<br />
Section A Second Floor<br />
IBM House<br />
54 Norfolk Terrace<br />
Westville 3630<br />
South <strong>Africa</strong><br />
e-mail: Durban@srk.co.za<br />
website: www.srk.co.za<br />
Tel: +27 (0) 31 279 1200<br />
Fax:+27 (0) 31 279 1204<br />
<strong>SRK</strong> Project Number 435209/SurfaceWater<br />
January 2012<br />
Compiled by: Peer Reviewed by:<br />
Murray Sim<br />
Associate Partner<br />
Peter Shepherd<br />
Director<br />
Email: msim@srk.co.za Email: pshepherd@srk.co.za<br />
Authors:<br />
Murray Sim; Colin Wessels; Sagadevan Kisten;<br />
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Table of Contents<br />
Disclaimer .................................................................................................................................................... iv<br />
1 Introduction and Scope of Report ............................................................................... 5<br />
2 Background and Brief .................................................................................................. 5<br />
2.1 Background of the project ................................................................................................................... 5<br />
3 Program Objectives and Work Program ..................................................................... 6<br />
3.1 Program objectives ............................................................................................................................. 6<br />
3.2 Work Program ..................................................................................................................................... 6<br />
3.3 Project Team ....................................................................................................................................... 6<br />
4 Legal Framework .......................................................................................................... 7<br />
4.1 National Water Act (36 of 1998) .......................................................................................................... 7<br />
4.2 National Environmental Management Act No. 107 of 1998 ................................................................ 8<br />
4.3 Best Practise Guideline (G1) Storm Water Management DWA 2006 ................................................ 8<br />
5 Hydrological evaluation ............................................................................................. 13<br />
5.1 Surface water .................................................................................................................................... 13<br />
5.1.1 Description ............................................................................................................................ 13<br />
5.1.2 Rainfall................................................................................................................................... 13<br />
5.1.3 Evaporation ........................................................................................................................... 14<br />
5.1.4 Extreme events ..................................................................................................................... 14<br />
5.1.5 Development considerations ................................................................................................. 15<br />
5.2 Hydrogeology .................................................................................................................................... 15<br />
5.2.1 Description ............................................................................................................................ 15<br />
5.2.2 Development considerations ................................................................................................. 16<br />
5.3 Surface water resources ................................................................................................................... 16<br />
6 Geotechnical evaluation ............................................................................................ 17<br />
6.1 Geology ............................................................................................................................................. 17<br />
6.2 Founding conditions .......................................................................................................................... 18<br />
6.3 Development considerations ............................................................................................................. 18<br />
7 Impact Assessment .................................................................................................... 19<br />
7.1 Construction / Operational Phase ..................................................................................................... 19<br />
7.1.1 Decrease in surface water quality ......................................................................................... 19<br />
7.1.2 Increase in surface water quantity ........................................................................................ 21<br />
7.1.3 Increase in erosion potential ................................................................................................. 22<br />
7.1.4 Increase in flooding potential and change in flow regime ..................................................... 23<br />
7.2 Mitigation measures .......................................................................................................................... 24<br />
8 Conclusions and Recommendations ........................................................................ 24<br />
8.1 Hydrological ...................................................................................................................................... 24<br />
8.2 Geotechnical ..................................................................................................................................... 25<br />
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8.3 Impact Assessment ........................................................................................................................... 26<br />
8.4 Mitigation Measures .......................................................................................................................... 26<br />
9 Final Remarks ............................................................................................................. 28<br />
10 References .................................................................................................................. 29<br />
Appendices ...................................................................................................................... 30<br />
Appendix A: Impact Assessment Methodology .......................................................... 31<br />
Appendix B: Figures ..................................................................................................... 38<br />
435209/1.1 Regional drainage map ...................................................................... 38<br />
435209/1.2 Study area ........................................................................................... 38<br />
435209/1.3 Catchment boundaries and surface water features ........................ 38<br />
435209/1.4 Surface water runoff potential .......................................................... 38<br />
435209/1.5 Hydro geological map ........................................................................ 38<br />
435209/1.6 Geology map ...................................................................................... 38<br />
List of Tables<br />
Table 3-1: Project Team ................................................................................................................................ 6<br />
Table 5-1: Overview/Strategies of Storm Water Management ..................................................................... 9<br />
Table 6-1: Percentage of time rainfall amount is exceeded and average monthly rainfall ......................... 14<br />
Table 6-2: Average monthly S-pan evaporation (mm) ................................................................................ 14<br />
Table 6-3: 24-hour design rainfall depths (mm) .......................................................................................... 14<br />
Table 8-1: Impact assessment (deterioration in water quality) ................................................................... 20<br />
Table 8-2: Impact assessment (increase in surface water quantity) ........................................................... 21<br />
Table 8-3: Impact assessment (increase in erosion potential) .................................................................... 22<br />
Table 8-4: Impact assessment (increase in flooding potential and change in flow regime)........................ 23<br />
Table 9-1: Mitigation measures (deterioration in water quality) .................................................................. 26<br />
Table 9-2: Mitigation measures (increase in surface water quantity) .......................................................... 27<br />
Table 9-3: Mitigation measures (increase in erosion potential) .................................................................. 27<br />
Table 9-4: Mitigation measures (increase in flooding potential and change in flow regime) ...................... 27<br />
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Disclaimer<br />
The opinions expressed in this Report have been based on the information supplied to <strong>SRK</strong><br />
<strong>Consulting</strong> (South <strong>Africa</strong>) (Pty) Ltd (<strong>SRK</strong>) by <strong>Sato</strong> <strong>Energy</strong> <strong>Holdings</strong> Pty (Ltd) (SATO). The opinions<br />
in this Report are provided in response to a specific request from SATO to do so. <strong>SRK</strong> has<br />
exercised all due care in reviewing the supplied information. Whilst <strong>SRK</strong> has compared key supplied<br />
data with expected values, the accuracy of the results and conclusions from the review are entirely<br />
reliant on the accuracy and completeness of the supplied data. <strong>SRK</strong> does not accept responsibility<br />
for any errors or omissions in the supplied information and does not accept any consequential<br />
liability arising from commercial decisions or actions resulting from them. Opinions presented in this<br />
report apply to the site conditions and features as they existed at the time of <strong>SRK</strong>’s investigations,<br />
and those reasonably foreseeable. These opinions do not necessarily apply to conditions and<br />
features that may arise after the date of this Report, about which <strong>SRK</strong> had no prior knowledge nor<br />
had the opportunity to evaluate.<br />
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1 Introduction and Scope of Report<br />
<strong>Sato</strong> <strong>Energy</strong> <strong>Holdings</strong> (Pty) Ltd (<strong>Sato</strong>) proposes to develop a solar energy facility using photovoltaic<br />
(PV) panels near Aggeneys in the Northern Cape. The farm is located adjacent to the N14 between<br />
Springbok and Pofadder, in close proximity to the Namibian border. The PV plant is anticipated to<br />
have an array of photovoltaic panels covering just less than 900 hectares, with 500MW power<br />
generating capacity.<br />
<strong>SRK</strong> <strong>Consulting</strong> (Pty) Ltd (<strong>SRK</strong>) has been appointed by <strong>Sato</strong> as an independent environmental<br />
consultant to carry out an Environmental Impact Assessment (EIA) as required by the National<br />
Environmental Management Act (NEMA) Act 107 of 1998. As such, <strong>SRK</strong> is fulfilling the role of<br />
environmental assessment practitioner (EAP) as specified in the EIA regulations. Included in the EIA<br />
process is the need to develop draft and final scoping reports, as well as draft and final EIA reports.<br />
Subsequent to submission of the Draft Scoping Report (DSR), motivation for splitting the project into<br />
seven EIAs has been provided to DEA based on Department of <strong>Energy</strong> (DoE) requirements of<br />
restricting the capacity per application and environmental authorisation to 75 MW. The format of the<br />
development is thus now as follows: 6 x 75 MW units and 1 x 50 MW unit; together they comprise<br />
the original 500 MW project.<br />
The approach for the <strong>Sato</strong> PV EIA process will be through the production of a consolidated Final<br />
Scoping Report (FSR) and environmental impact assessment report (EIR) which includes all seven<br />
of the PV projects, but which will also allow individual authorisations to be provided for each of the<br />
projects (reference 12/12/20/2334/1 to 12/12/20/2334/7).<br />
As part of the EIA process a desktop surface water and geotechnical assessment is required and<br />
this forms the basis of this report. The study area can be found in Appendix B, Figure 1.2<br />
2 Background and Brief<br />
2.1 Background of the project<br />
<strong>SRK</strong> has been appointed by <strong>Sato</strong> as an independent environmental consultant to carry out an<br />
Environmental Impact Assessment (EIA) and this specialist surface water and geotechnical<br />
assessment will be incorporated into the final EIA’s.<br />
The PV Array is proposed to cover approximately 900 ha, divided into seven areas and is anticipated<br />
to produce 500 MW when developed in its entirety. The aboveground designed footings (strip<br />
foundation) will be 0.51 m in height, 4.8 m in length and 0.8 m wide. The PV plant will comprise<br />
seven units (6x 75 MW plus 1x 50 MW). Each of the six 75 MW units will have 15 adjacent sites,<br />
each of which will produce 5 MW (thus totalling 75 MW for each unit). The seventh unit will have 3.3<br />
adjacent sites each of which will generate 15 MW (totalling 50 for the unit). The total proposed<br />
development will comprise about 26 adjacent sites each of 19.23 MW. Each table will in turn consist<br />
of 85 panels.<br />
The final number of rows and panels depends on the configuration of the array and power rating of<br />
the panels.<br />
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3 Program Objectives and Work Program<br />
3.1 Program objectives<br />
The main objectives of the specialist study are to assess potential impacts due to the proposed<br />
development and assist in providing information to enable the project team and authorities in<br />
decision making.<br />
3.2 Work Program<br />
The activities undertaken in the work program have been divided into a hydrological and<br />
geotechnical desktop evaluation based on the available data at hand.<br />
3.3 Project Team<br />
The project team is presented in Table 3-1.<br />
Table 3-1: Project Team<br />
Team Member Role Specialist Area<br />
Peter Shepherd Project Reviewer Water regulation and strategic water management<br />
Murray Sim Project Manager Water engineering<br />
Sagadevan Kisten Principal Scientist Hydrogeological specialist<br />
Colin Wessels Senior Geologist Geotechnical specialist<br />
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4 Legal Framework<br />
Only those relevant to surface water have been included and there are many other legal<br />
requirements which would be covered in the other disciplines.<br />
4.1 National Water Act (36 of 1998)<br />
The surface water management for the proposed development and related infrastructure falls under<br />
legislation contained in, amongst others, the National Water Act (No 36 of 1998) (NWA). Section 4<br />
deals with prevention of contamination: The person who owns and/or controls, occupies or uses the<br />
land in question is responsible for taking measures to prevent pollution of water resources. If these<br />
measures are not taken, the catchment management agency concerned may itself do whatever is<br />
necessary to prevent the pollution or to remedy its effects, and to recover all reasonable costs from<br />
the persons responsible for the pollution. This can be broadly summarised as follows:<br />
• Separate “clean” and “dirty water”;<br />
• Water contaminated by activities / infrastructure may not be discharged to surface or<br />
groundwater resources; and<br />
• Prevention of erosion.<br />
Extracts from National Water Act No 36 of 1998, Section 4<br />
(1) An owner of land, a person in control of land or a person who occupies or uses the land on which -<br />
(a) any activity or process is or was performed or undertaken; or<br />
(b) any other situation exists, which causes, has caused or is likely to cause pollution of a water<br />
resource, must take all reasonable measures to prevent any such pollution from occurring, continuing<br />
or recurring.<br />
(2) The measures referred to (above) may include measures to -<br />
(a) cease, modify or control any act or process causing the pollution;<br />
(b) comply with any prescribed waste standard or management practice;<br />
(c) contain or prevent the movement of pollutants;<br />
(d) eliminate any source of the pollution;<br />
(e) remedy the effects of the pollution; and<br />
(f) remedy the effects of any disturbance to the bed and banks of a watercourse.<br />
Regulations relating to capacity requirements of “clean” and “dirty” water systems<br />
Every person in control of an activity must-<br />
a) confine any unpolluted water to a clean water system, away from any dirty area;<br />
b) collect the water arising within any dirty area, into a dirty water system;<br />
c) design, construct, maintain and operate any dirty water system so that it is not likely to spill into<br />
any clean water system more than once in 50 years;<br />
The following water use activities will require authorisation and possibly licensing from the DWA prior<br />
to commencement of said activities:<br />
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Extract from the National Water Act, Section 21<br />
For the purposes of this Act, water use includes -<br />
(a) taking water from a water resource;<br />
(b) storing water;<br />
(c) impeding or diverting the flow of water in a watercourse;<br />
(d) engaging in a stream flow reduction activity contemplated in section 36;<br />
(e) engaging in a controlled activity identified as such in section 37 (1) or declared under section<br />
38 (1);<br />
(f) discharging waste or water containing waste into a water resource through a pipe, canal, sewer, sea<br />
outfall or other conduit;<br />
(g) disposing of waste in a manner which may detrimentally impact on a water resource;<br />
(h) disposing in any manner of water which contains waste from, or which has been heated in, any<br />
industrial or power generation process;<br />
(i) altering the bed, banks, course or characteristics of a watercourse;<br />
(j) removing, discharging or disposing of water found underground if it is necessary for the efficient<br />
continuation of an activity or for the safety of people; and<br />
(k) using water for recreational purposes<br />
4.2 National Environmental Management Act No. 107 of 1998<br />
Chapter 7 of the National Environmental Management Act deals with compliance, enforcement and<br />
protection and Section 28 deals specifically with duty of care and remediation of environmental<br />
damage.<br />
Extract from the National Environmental Management Act no 107 of 1998<br />
(1) Every person who causes, has caused or may cause significant pollution or degradation of the<br />
environment must take reasonable measures to prevent such pollution or degradation from<br />
occurring, continuing or recurring, or, in so far as such harm to the environment is authorised by<br />
law or cannot reasonably be avoided or stopped, to minimise and rectify such pollution or<br />
degradation of the environment.<br />
(2) Without limiting the generality of the duty in subsection (1), the persons on whom subsection (1)<br />
imposes an obligation to take reasonable measures, include an owner of land or premises, a<br />
person in control of land or premises or a person who has a right to use the land or premises on<br />
which or in which -<br />
(a) any activity or process is or was performed or undertaken; or<br />
(b) any other situation exists, which causes, has caused or is likely to cause significant pollution<br />
or degradation of the environment.<br />
(3) The measures required in terms of subsection (1) may include measures to -<br />
(a) investigate, assess and evaluate the impact on the environment;<br />
(b) inform and educate employees about the environmental risks of their work and the manner<br />
khkkhkh in which their tasks must be performed in order to avoid causing significant pollution or<br />
degradation of the environment;<br />
(c) cease, modify or control any act, activity or process causing the pollution or degradation;<br />
(d) contain or prevent the movement of pollutants or the causant of degradation;<br />
(e) eliminate any source of the pollution or degradation; or<br />
(f) remedy the effects of the pollution or degradation.<br />
4.3 Best Practise Guideline (G1) Storm Water Management DWA 2006<br />
The Storm Water Management DWA 2006 guidelines are geared towards the mining industry but<br />
there are definite similarities which need to be incorporated where relevant.<br />
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Table 4-1: Overview/Strategies of Storm Water Management<br />
Section Guidelines (BPG G2) Measures (combination of BPG G2<br />
and Reg. 704)<br />
General<br />
objectives<br />
Primary<br />
principles<br />
Protection of life (prevent loss of<br />
life) and property (reduce damage<br />
to infrastructure) from flood<br />
hazards<br />
Planning for drought periods during<br />
operation<br />
Ensuring continuous operation and<br />
production through different<br />
hydrological cycles<br />
Prevention of land and<br />
watercourse (bed and banks)<br />
erosion (especially during storm<br />
events)<br />
Minimising the impact of<br />
operations on downstream users<br />
by maintaining the downstream<br />
water quantity and quality<br />
requirements.<br />
Preservation and protection of the<br />
natural environment in terms of<br />
quality, quantity and ecological<br />
integrity (water courses and their<br />
ecosystems)<br />
‘Clean’ water must be kept clean<br />
and routed to the natural water<br />
course<br />
All storm water management<br />
infrastructures are designed to<br />
withstand a 1:50 year flood.<br />
<strong>Energy</strong> dissipaters and erosion<br />
protection measures are in place,<br />
including along roads and at<br />
culvert/channel outlets.<br />
The quality and quantity<br />
requirements of downstream users<br />
will be assessed. Dirty areas will be<br />
minimised and all dirty water will be<br />
contained up to the 1:50 year event.<br />
Operating levels of containment<br />
facilities will be set to ensure<br />
adequate capacity for a 1:50 year<br />
event. ‘Clean’ water will be diverted<br />
back to the catchment but will be<br />
contained for controlled release after<br />
the storm event if the volume of the<br />
runoff poses a risk.<br />
‘Dirty’ areas will be minimised and all<br />
‘dirty’ water will be contained up to<br />
the 1:50 year event. Clean water will<br />
be diverted back to the catchment.<br />
The definition of 'dirty' for the site will<br />
be negotiated with DWA in terms of<br />
the water quality objectives set for<br />
the catchment.<br />
‘Clean’ areas will be maximised and<br />
‘clean’ runoff will be returned to the<br />
receiving water<br />
environment/catchment; maximize<br />
reuse of dirty water where feasible<br />
e.g. through separation of less dirty<br />
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Section Guidelines (BPG G2) Measures (combination of BPG G2<br />
and Reg. 704)<br />
‘Dirty’ water must be collected and<br />
contained<br />
water, and minimize seepage and<br />
overflows from containment facilities;<br />
separate less dirty water where<br />
feasible<br />
‘Dirty’ areas will be minimised and<br />
reuse of dirty water will be<br />
maximised where feasible. Specific<br />
measures include separation of less<br />
dirty water for reuse in<br />
operations/areas where a better<br />
quality water is required and<br />
minimising seepage and overflows<br />
from containment facilities<br />
Sustainability over life cycle Sustainability over the development<br />
life cycle and over different<br />
hydrological cycles will incorporate<br />
principles of risk management<br />
including the consideration of the<br />
consequences of extreme events<br />
(extreme rainfall and emergency<br />
events), as well as potential water<br />
shortfalls in areas subject to drought.<br />
The SWMP has full commitment from<br />
management and staff and will be<br />
regularly reviewed and revised<br />
accordingly.<br />
Consideration of regulations and<br />
stakeholders<br />
Other principles Precautionary approach and being<br />
proactive<br />
Consideration of a range of<br />
management measures and<br />
options<br />
All stormwater management<br />
measures are in compliance with<br />
Regulation 704 under the National<br />
Water Act, Act 36 of 1998 and<br />
Regulation 527 under the MPRDA.<br />
The interests of stakeholders will be<br />
considered and incorporated and<br />
communication channels will be<br />
established with the Catchment<br />
Management Agency once these are<br />
up and running.<br />
Regular auditing is required to<br />
develop such an approach.<br />
Investigations are required to<br />
identify potential management<br />
measures and options specific for the<br />
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Section Guidelines (BPG G2) Measures (combination of BPG G2<br />
and Reg. 704)<br />
Issues that<br />
need to be<br />
taken into<br />
account<br />
Implementation, operation,<br />
monitoring and auditing<br />
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site.<br />
Management support, resources and<br />
adequately trained staff will be<br />
provided. Performance of the SWMP<br />
will be reviewed regularly (including<br />
design performance validation,<br />
operational and environmental<br />
considerations) and where necessary<br />
modified.<br />
Statutory requirements All stormwater management<br />
measures are in compliance with<br />
Regulation 704 under the National<br />
Water Act, Act 36 of 1998 and<br />
Regulation 527 under the MPRDA.<br />
Catchment objectives that need to<br />
be met or protected<br />
Management of risk, precipitation<br />
event or recurrence interval<br />
Water balance management (refer<br />
to BPG G2)<br />
Interaction with regulators and the<br />
community.<br />
Operational and emergency<br />
monitoring and documentation<br />
The Catchment Management<br />
Strategy has not yet been developed<br />
but a catchment-based approach will<br />
be followed to identify current and<br />
potential water management issues<br />
in the catchment.<br />
Risks associated with stormwater<br />
management have been minimised<br />
as follows: all dirty and clean water<br />
facilities will be capable of handling<br />
the 1:50 year event or sequential<br />
events that have the cumulative<br />
impact of a 1:50 year event;<br />
maximum storage of water for reuse<br />
will take place prior to the start of dry<br />
periods; etc.<br />
The water balance has been<br />
optimised to maximise reuse of water<br />
and ensure maximum returns of<br />
clean water runoff to the catchment<br />
in accordance with BPG G2 to<br />
minimise the loss of catchment yield.<br />
Suitable forums should be<br />
established.<br />
Reference the Emergency<br />
Preparedness and Response
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Section Guidelines (BPG G2) Measures (combination of BPG G2<br />
and Reg. 704)<br />
Integration with<br />
other water<br />
management<br />
aspects<br />
(refer to BPG G3) Procedure and the Aspects and<br />
Impact Register as maintained in<br />
terms of ISO140001.<br />
Provide for incidents and<br />
accidents, and contingencies<br />
associated with incidents and other<br />
emergencies<br />
Water quality: downstream<br />
contamination of natural<br />
watercourses due to runoff or<br />
spillage of contaminated storm<br />
water.<br />
Reference the Emergency<br />
Preparedness and Response<br />
Procedure and the Aspects and<br />
Impact Register as maintained in<br />
terms of ISO140001.<br />
‘Dirty’ areas will be minimised and all<br />
dirty water will be contained up to the<br />
1:50 year event. Where feasible, less<br />
polluted water will be separated from<br />
more polluted water to maximise<br />
reuse of water (BPG H3). ‘Clean’<br />
water will be diverted back to the<br />
catchment. Materials and waste<br />
handling will be in designated areas<br />
to prevent spillages in clean areas<br />
and the subsequent potential<br />
pollution of clean water runoff.<br />
<strong>Energy</strong> dissipaters and erosion<br />
protection measures are in place to<br />
minimise sediment loads entering the<br />
catchment.<br />
Performance indicators Suitable performance indicators will<br />
be developed.<br />
Training and research All contractors and personnel<br />
responsible for the stormwater<br />
management systems will undergo<br />
suitable training, which will be<br />
reinforced on a regular basis. Where<br />
new technology is employed,<br />
experiences and findings will be<br />
captured and disseminated via<br />
published articles/presentations.<br />
Water reuse and reclamation (see<br />
BPG H3)<br />
Impact prediction (see BPG G4)<br />
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Section Guidelines (BPG G2) Measures (combination of BPG G2<br />
and Reg. 704)<br />
Water and salt balances (see BPG<br />
G2)<br />
Water monitoring systems (see<br />
BPG G3)<br />
5 Hydrological evaluation<br />
5.1 Surface water<br />
5.1.1 Description<br />
The preferred site is located between the Windhoek se Berge in the south, Skelmberg in the west<br />
and the low lying pans in the north. The catchment starts in the south and drains towards Windhoek<br />
se Poort, east of the Skelmberg and down to the low lying pans in the north. The slopes are<br />
extremely flat with the majority of the surface water runoff flowing as sheet wash. There are various<br />
localised drainage lines around Skelmberg and any runoff rapidly dissipates and infiltrates on<br />
reaching the flat open sandy soils. There is one defined watercourse towards the north which drains<br />
under the N14 and gravel roads, also discharging into the pans but does not cross the preferred site<br />
location. The regional drainage map and the catchment boundaries including surface water features<br />
can be found in Appendix B, Figures 1.1 and 1.3 respectively.<br />
There is little evidence of erosion occurring around the flat open sandy soils due to the low velocities<br />
but there is more evidence of erosion along the slopes of the Skelmberg and Windhoek se Berge.<br />
The site can be summarized into two distinct hydrological soil groups which give an indication of the<br />
runoff potential:<br />
• Group A: Low stormflow potential (Infiltration rate is high and permeability is rapid in this group);<br />
and<br />
• Group D: High stormflow potential (Soils in this group are characterized by very slow infiltration<br />
rates and severely restricted permeability. Very shallow soils and those of high shrink-swell<br />
potential are included in this group).<br />
Group A consists of the sands characterized by a low runoff and erosion potential whereas Group D<br />
consists of Skelmberg and the Windhoek se Berge with high runoff and erosion potential. The map<br />
indicating surface water runoff potential can be found in Appendix B, Figure 1.4<br />
5.1.2 Rainfall<br />
Monthly rainfall depths were extracted from the closest weather station (approximately 10 km from<br />
the site) from 1950 - 2000. The selection of Aggeneys station 0246555_W is based on the fact that<br />
this is the closest weather station to the study area, with a good reliable record, and little patching of<br />
data was required (patching of rainfall requires filling in the missing data with data from nearby<br />
stations based on statistical rainfall parameters). As more reliable data becomes available the<br />
above data set can be refined and updated but 50 years of data is deemed adequate for this desktop<br />
investigation.<br />
The rainfall in the area is low with an average annual rainfall of approximately 107 mm. The monthly<br />
rainfall data was obtained from SAWS (South <strong>Africa</strong>n Weather Services) and the period of data was<br />
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from 1950 to 2000. The maximum and minimum MAP (Mean Annual Precipitation) was 272 mm<br />
(1976) and 8 mm (1999) respectively. A statistical analysis for the rainfall period was undertaken and<br />
the results are presented in Table 6-1. The table should be read as follows: - “Approximately 10% of<br />
the time 24 mm or more rainfall falls during October”.<br />
Table 5-1: Percentage of time rainfall amount is exceeded and average monthly rainfall<br />
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Annual<br />
Maximum 52 49 83 79 122 91 122 67 58 86 39 46 272<br />
10% 24 17 21 27 34 45 29 18 15 16 12 19 194<br />
30% 5 3 2 6 19 25 13 8 7 6 7 4 126<br />
50% 2 1 0 1 4 8 7 4 4 3 3 2 99<br />
Average 7 6 7 8 14 18 14 8 7 8 5 6 107<br />
70% 1 0 0 0 0 3 2 1 1 2 1 0 72<br />
90% 0 0 0 0 0 0 0 0 0 0 0 0 43<br />
98% 0 0 0 0 0 0 0 0 0 0 0 0 21<br />
Minimum 0 0 0 0 0 0 0 0 0 0 0 5 8<br />
5.1.3 Evaporation<br />
WRSM2000<br />
Region<br />
14A<br />
The S-Pan evaporation was abstracted from the WRSM2000 (Water Research Commission (2005),<br />
Water Resources of South <strong>Africa</strong>) reports and is presented in Table 6-2<br />
Table 5-2: Average monthly S-pan evaporation (mm)<br />
5.1.4 Extreme events<br />
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Annual<br />
252 297 340 346 291 273 196 131 99 97 136 192 2650<br />
The 24 hour design rainfall depths for the area were taken from "Rainfall Statistics for Design Flood<br />
Estimation in South <strong>Africa</strong>" (WRC Project K5/1060), by JC Smithers and RE Schulze. The 24 hour<br />
design rainfall depths are indicated in Table 6-3.<br />
Table 5-3: 24-hour design rainfall depths (mm)<br />
Return Period (Years) 1:2 1:5 1:10 1:20 1:50 1:100 1:200<br />
Rainfall depth (mm) 24 41 55 70 93 114 138<br />
These values are to be used for determining the peak flows and volumes when designing any of the<br />
relevant infrastructures. This would also be used for determining any floodlines on the site if and<br />
where required.<br />
The 1:100 year peak flows were generated using TR137 (Regional Maximum Flood Peaks) which is<br />
an empirical method based on historical data. The SDF (Standard Design Flood Method) was also<br />
used which is a numerically regionally calibrated version of the Rational method. These methods are<br />
more commonly used on large regional catchments but there are no applicable site-specific methods<br />
or gauging data available for the area.<br />
The main catchment commands a catchment area of 690 km 2 and drains from the south towards<br />
Windhoek se Poort, east of the Skelmberg and across the proposed site into the low lying pans in<br />
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the north. This catchment does not have an outlet (endoreic) and the surface water reaching the<br />
pans during a storm event temporarily ponds and evaporates or infiltrates within the catchment<br />
before even reaching the pans.<br />
The 1:100 year peak flow is estimated to be between 150 – 200 m 3 /s using the above empirical and<br />
calibrated rational methods. There is no well defined channel and the surface water flows as sheet<br />
flow across the site to a depth of approximately 200 mm – 300 mm during an extreme event (1:100<br />
year storm event). These flows are not expected to cause any significant damage due to the low<br />
velocities (less than 1 m/s) associated with flat gradients and wide open plains.<br />
There will be some significant localised run-off at the foot of the Skelmberg but this will rapidly<br />
dissipate on reaching the flat sandy gradients, resulting in sheet wash across the site.<br />
5.1.5 Development considerations<br />
The following should be considered during the development of the site:<br />
• There is a well defined watercourse located north of the proposed site which drains under the<br />
N14 and the old gravel road before discharging into the low lying pans. The only large catchment<br />
which may have an impact on the site has its watershed south of the proposed site and drains<br />
east of the Skelmberg from south to north across the proposed site at sheet wash. There are,<br />
however, small erosion gullies along the steep slopes which would need to be taken into account<br />
during the detailed design;<br />
• Although it is difficult to demarcate the 1:100 year floodlines due to the terrain, the proposed<br />
development would still need to manage the sheet flow and/or drainage lines crossing the site<br />
and may require minor diversion channel/berms/culverts to protect the relevant infrastructure;<br />
• Depending on the layouts, any hard surface areas create by the new development would need<br />
to adequately drain and dissipate prior to discharging back into the environment to prevent<br />
downstream erosion potential;<br />
• All clean and dirty water needs to be separated;<br />
• Any water being used to wash the panels and discharging as surface water back into the natural<br />
environment needs to comply with relevant authorities water quality standards; and<br />
• Any waste/ water treatment discharging as surface water back into the natural environment<br />
needs to comply with the relevant authorities water quality standards.<br />
5.2 Hydrogeology<br />
5.2.1 Description<br />
The surface geology at the site comprises Quaternary Age Kalahari Sands (Qs) which is likely to be<br />
underlain by Tertiary Age calcrete deposits. Lithologies at greater depth are likely to comprise an<br />
assemblage of low to medium grade metamorphic rocks ranging from pelitic schist to sillimanite<br />
bodies. Typically the aquifers associated with these lithologies are integranular and fractured and<br />
according to the 1:500 000 hydrogeological map sheet (2718, Upington) has yields ranging from 0.1-<br />
0.5 L/s. The hydro geological map can be found in Appendix B, Figure 1.5<br />
The Mean Annual Precipitation (MAP) for the area is 107 mm (WRSM 2000, Region 14A) and<br />
recharge is expected to be at negligible levels. Due to the site’s location in a quaternary catchment<br />
that displays characteristics of an endoreic pan, which does not appear to be in continuity with<br />
surface drainage in adjacent quaternaries, shallow groundwater flow (if any) is expected to mimic the<br />
surface water drainage patterns towards the topographic low which is located to the north of the site.<br />
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According to the Groundwater Resources Map of the Republic of South <strong>Africa</strong>, Sheet 2, recharge<br />
occurs in the range of 1-5 mm/annum which can be considered low, implying that the baseflow<br />
contributed by groundwater to rivers is negligible. Groundwater levels are at an approximate depth of<br />
45 metres below ground level (mbgl) and the regional groundwater flow direction is northwest<br />
towards the Orange River.<br />
Groundwater analytical data received from the National Groundwater Archives (NGA) is summarised<br />
below:<br />
• The nearest groundwater user (Site I.D. 89747) is located >10 km north of the site. The average<br />
Total Dissolved Solids (TDS) is 845 mg/L, chloride (Cl) is 296 mg/l, sodium (Na) is 113 mg/L and<br />
sulphate (SO4) is 237 mg/L;<br />
• In comparison, groundwater users located to the north (>15 km from the site) indicate the<br />
average Total Dissolved Solids (TDS) at 1599 mg/L, chloride (Cl) at 602 mg/l, sodium (Na) at<br />
330 mg/L and sulphate (SO4) at 237 mg/L; and<br />
• The elevated TDS and chloride levels recorded can relate to a groundwater system<br />
characterised by low recharge and longer residence time.<br />
5.2.2 Development considerations<br />
Based on the available desktop groundwater data for the site, the following characteristics should be<br />
considered towards identifying sensitivities around the proposed development:<br />
• The aquifer type is integranular and fractured with yields ranging from 0.1 to 0.5 L/s;<br />
• Regional groundwater level is at 45 mbgl;<br />
• The site is located in an endoreic pan which does not appear to be in continuity with surface<br />
drainage in adjacent quaternaries. Shallow groundwater flow (if any) is likely to mimic<br />
topography and flow to the north;<br />
• The nearest groundwater user is located >10 km to the north of the site; and<br />
• The elevated TDS and chloride levels are indicative of a groundwater system receiving low<br />
recharge and having a longer residence time.<br />
Based on these characteristics, the impact to the groundwater environment due to the proposed<br />
development is expected to be low but falls outside of the current scope of works.<br />
5.3 Surface water resources<br />
The proposed site falls within drainage region D, quaternary sub-catchment D82C which was taken<br />
from WRSM2000 water resource reports.The WRSM2000 model is a “mathematical model, which<br />
simulates the movement of water through an interlinked system of catchments, river reaches,<br />
reservoirs and irrigation areas” (Midgley, Pitman and Middleton, 1994). WRSM2000 has its origin in<br />
the Stanford Watershed Model developed in the United States of America by Crawford and Linsley<br />
(1966).<br />
Sub-catchment D82C is considered to be an endoreic area which means that the rivers terminate in<br />
inland lakes or pans and the surface runoff does not contribute to any of the surrounding drainage<br />
systems which eventually end up at the ocean. The degree of endoreism is clearly a function of the<br />
rainfall and normally located in arid, semi-arid and dry sub-humid drylands.<br />
The low lying pans towards the north remain dry most of the time and the pans temporarily pond only<br />
when enough surface runoff is generated.<br />
Due to the low rainfall and high evaporation, surface water abstraction from any of the rivers, pans<br />
and/or open storage areas is not a viable option. Therefore, the majority of water in the vicinity is<br />
currently obtained from the ground water system via boreholes or piped to the site from the nearby<br />
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town. At this stage it is our understanding that the water would be obtained from the local<br />
municipality which forms part of the original water supply for the Black Mountain mining operations.<br />
If water is not available from the Municipality and a borehole is required, then a yield and water<br />
quality test on any existing boreholes would need to be carried out. If this does not meet the required<br />
water demand and water quality standards, then additional boreholes may be required which may<br />
also require a small desalination plant.<br />
Other options which are being considered would be to truck the water in from neighbouring<br />
municipalities or sourcing directly from the Orange River. The viability of these two options needs to<br />
be investigated further. A feasibility study has been completed by JIS Environmental Engineers<br />
(2012) on the water requirements and demands.<br />
A significant volume of water would normally be required for washing of the panels but it is our<br />
understanding that an option of cleaning the panels with compressed air will decrease the water<br />
demand significantly. The viability of this option needs to be investigated further.<br />
6 Geotechnical evaluation<br />
6.1 Geology<br />
The proposed site is underlain by the following sands and rock:<br />
• Quaternary deposits (Q-s1) – Red windblown sand and dunes;<br />
• Quaternary deposits (Q-s2) – Sand, scree, rubble and sandy soil;<br />
• Tertiary deposits (T-c) – Calcrete;<br />
• Wortel formation rocks (Kwr) – A layered sequence of medium to thick bedded, white quartzite<br />
and pelitic schist with interbedded sillimanite bodies. Contains minor lenses of quartzite, biotite<br />
gneiss, and massive amphibolite/calc-silicate gneiss; and<br />
• Konkyp gneiss formation (Nky) – Grey, megacrystic biotite augen gneiss (occurs over a<br />
relatively small area in the south western corner of the study area).<br />
The site is generally flat, with outcrop of metamorphic rock across the area and forming<br />
approximately 200 m high hills in the north western corner. The flatter areas are mainly overlain by<br />
Quaternary red windblown sands and Quaternary sand, scree and rubble. These sands generally<br />
have a loose consistency and exhibit a collapsible fabric. It may be possible to found light structures<br />
on these sands using various foundation techniques/treatments, but for heavy structures it may be<br />
necessary to found on rock below these sands.<br />
Hardpan and/or gravel calcrete often lies beneath these sands and over underlying rock. The<br />
consistency of calcrete may indicate suitable founding material, however, as it is a calcium<br />
carbonate it may become weaker over time and founding below the calcrete on rock is<br />
recommended. The depth to rock in this area is generally expected to vary between 1.0 m and<br />
3.0 m, but this depends on the structure of the underlying rock formations and topography. The<br />
sands can be in excess of 6.0 m deep in places where they have filled up paleo channels. Quartzite<br />
and schist of the Wortel formation is expected to underlie most of the sands in the area. The geology<br />
for the area can be found in Appendix B, Figure 1.6<br />
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6.2 Founding conditions<br />
Rock is the ideal founding medium, but the topography of the outcrop where it occurs in the area is<br />
not expected to provide a suitable foundation solution (this would be verified during the detailed<br />
investigation), and it is likely that excessive hard rock excavation (blasting) may be necessary.<br />
The far south west corner intersects a very small area of surface calcrete (Nky) (probably where the<br />
sands have been eroded away). These areas consist of sandy calcrete gravel often over relatively<br />
shallow rock.<br />
For founding the solar panels, we suggest investigating the northern half of the area (Q-sands).<br />
During the detailed investigation one would need to verify the depth of the rock as this can have a<br />
major impact on the type of foundation required, which is normally the highest civil cost on the<br />
project.<br />
The estimated guidelines for maximum safe bearing capacity (shallow footings) for vertical loadings<br />
have been included below:<br />
Cohesive Soils<br />
Very soft clays, sandy clays, silty clays, clayey silts, clayey sands 0 – 50 kPa<br />
Soft clays, sandy clays, sandy silts, silty sands 50 – 100 kPa<br />
Firm clays, sandy clays, sandy silts, silty sands 100 – 200 kPa<br />
Stiff clays, sandy clays, silts, silty sands 195 – 390 kPa<br />
Very stiff clays, sandy clays, silty clays, sandy silts, silty sands 390 – 490 kPa<br />
Non-cohesive soils<br />
Compact, well graded gravels, sands and gravel mixtures (dry) 390 – 490 kPa<br />
Compact, well graded gravels, sands and gravel mixtures (wet) 200 – 250 kPa<br />
Compact, poorly graded gravels, sands and gravel mixtures (dry) 200 – 390 kPa<br />
Loose sands by test only<br />
Rock<br />
Fresh rock, massively bedded, intact, igneous, metamorphic sedimentary 4900 kPa<br />
Fresh rock, fractured or jointed 980 kPa<br />
These values are typical values and would depend on various other site specific conditions.<br />
There are a number of founding options available depending on the above infrastructure which could<br />
include strip footings, large bored piles/ drilled anchors, augured piles and mini-piles/anchors. The<br />
adopted foundation has a significant cost implication and would depend on the depth to bedrock and<br />
the above infrastructure to be constructed. This would be confirmed during a detailed geotechnical<br />
investigation.<br />
6.3 Development considerations<br />
As previously discussed the ground conditions will influence the choice of foundation for the<br />
infrastructure which has a major impact on the civil construction costs. It is recommended that the<br />
detailed geotechnical assessment for the preferred site be looked at in correlation to the proposed<br />
layouts to establish the most economical founding option.<br />
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The following should be considered during the development of the site:<br />
• Determine the depth to bedrock across the proposed site and demarcate appropriate zones;<br />
• Assign the correct founding for the appropriate depth zone; and<br />
• Consider where the nearest suitable borrow pit and quarry is located (sand and stone) for the<br />
concrete foundations as importing the concrete would be an expensive option.<br />
7 Impact Assessment<br />
The impacts posed to the surface water by the solar operations were assessed based on criteria<br />
explained in the impact methodology in Appendix A. Potential water management impacts that may<br />
arise from the proposed activities and associated infrastructure relate to both the quantity and quality<br />
entering or leaving water resources. These include the following:<br />
• Altered availability to downstream water users due to changes in water quantity or flow regime;<br />
• Reduced availability of water to downstream water users due to changes in water quality;<br />
• Reduced availability of water to surrounding water users due to physical obstruction of flow from<br />
infrastructure;<br />
• Damage to the aquatic ecosystem due to substances contained in releases from the proposed<br />
activities;<br />
• Scouring effect on drainage lines due to run-off from hard surface areas; and<br />
• Increased erosion from areas of exposed soils.<br />
The potential impacts listed above are normally assessed for each stage of the development:<br />
• Pre-construction;<br />
• Construction;<br />
• Operation; and<br />
• Decommissioning and Post-closure.<br />
The Decommissioning and Post-closure will be rehabilitation back to pre-construction conditions<br />
(farmlands) according to legislation requirements and, therefore, the impact assessment has been<br />
done on the construction and operational phases only.<br />
Due to the phased construction over a seven year period, the construction and the operational phase<br />
will be occurring simultaneously and have, therefore, been assessed accordingly.<br />
7.1 Construction / Operational Phase<br />
Project construction is anticipated to be undertaken using a phased approach, initially with 75 MW<br />
being constructed following authorisation, where after further units of approximately 80 MW units is<br />
to be completed over 5 to 7 years in all.<br />
7.1.1 Decrease in surface water quality<br />
Water quality, required by downstream users and in particular the aquatic ecology can be impacted<br />
in two main ways: point sources discharging and diffuse pollution. The two point sources would be<br />
the outlet from the water/waste water treatment plant and the discharge during the washing of the<br />
panels. In both instances these are very small volumes and would not remain at the surface, rapidly<br />
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infiltrating into the sand soils. These points would also need to comply with the authorities’ water<br />
quality guidelines.<br />
Potential impacts will also arise from accidental point sources and diffuse sources. Accidental point<br />
source pollution can arise from the following activities, which are more difficult to detect and control<br />
than intentional point source discharges, but this can be managed with appropriate systems in place:<br />
• Spills from any pipelines and vehicles (fuel, oil or grease);<br />
• Uncontrolled discharges (burst pipes, overflows or pump failures); and<br />
• Flooding causing mixing of any clean and dirty water areas.<br />
Diffuse pollution, which is often more difficult to manage, can arise from:<br />
• Seepage of any dirty water containment areas (parking areas, sewage and water/waste<br />
treatment works); and<br />
• Run-off from exposed areas carrying increased sediment load.<br />
Sediment in any runoff will potentially come from exposed areas during construction but higher<br />
sediment loads may naturally be introduced along the drainage lines (low lying areas) due to<br />
increased frequency and intensity of flooding, large-scale erosion and sediment movement. Table 8-<br />
1 below indicates the impact assessment for the potential decrease in surface water quality.<br />
Table 7-1: Impact assessment (deterioration in water quality)<br />
Deterioration in surface water quality due to proposed activities<br />
Construction<br />
Impact<br />
before<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Moderate Medium -<br />
term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Medium<br />
Minimum disturbance to existing topography during implementation and incorporate into construction program.<br />
Any surface water discharging to environment during washing of panels to comply with authorities water quality standards.<br />
Any surface water discharging to environment from water/waste treatment works to comply with authorities water quality<br />
standards.<br />
Separate clean and dirty water at point source.<br />
Strategically placed hessian/geo-fabric attached to rows of stakes to prevent sediment washing downstream of the site during<br />
construction.<br />
Impact<br />
after<br />
Operational<br />
Impact<br />
before<br />
Moderate Medium -<br />
term<br />
Site/Local Medium Unlikely Low - Medium<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Minor Long -<br />
term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Medium<br />
Any surface water discharging to environment during washing of panels to comply with authorities water quality standards.<br />
Any surface water discharging to environment from water/waste treatment works to comply with authorities water quality<br />
standards.<br />
Separate clean and dirty water at point source.<br />
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Impact<br />
after<br />
Minor Long -<br />
term<br />
7.1.2 Increase in surface water quantity<br />
There are three potential areas where there will be an increase in the surface water quantity:<br />
• Increase in surface water run-off during a storm event due to additional hard surface areas<br />
(panels, roads, buildings etc). During minor storm events this would only occur for a short period<br />
of time before rapidly infiltrating into the sandy soils;<br />
• Increase in surface run-off during washing of the panels (assumes the water quality meets the<br />
authorities’ water quality standards). These volumes are relatively small (approximately 7 m 3 per<br />
day) which rapidly dissipates and infiltrates into the sandy soils. This may fall away if a<br />
compressed air system is installed to clean the panels; and<br />
• Increase in surface run-off when discharging from waste water plant, sewer soak-away<br />
(assumes the water quality meets the authorities’ water quality standards). These volumes are<br />
relatively small which would more than likely not even daylight (soak-away system) or if used for<br />
irrigation would dissipate and infiltrate into the sandy soils. This may be reduced or fall away if a<br />
dry sanitation system is installed for the sewer system.<br />
Due to the current low surface water run-off at the site any clean additional surface water would<br />
improve conditions for any local surface water uses within the site or directly downstream of the<br />
proposed development. Table 8-2 below indicates the impact assessment for the increase in surface<br />
water quantity.<br />
Table 7-2: Impact assessment (increase in surface water quantity)<br />
Increase in surface water quantity due to proposed activities<br />
Construction<br />
Impact<br />
before<br />
Site/Local Medium Unlikely Low - Medium<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Minor Medium<br />
- term<br />
Management measures:<br />
Site/Local Low Possible Low + Medium<br />
Local surface water run-off will increase due to hard surfaces created during construction and would need to be<br />
dissipated back to sheet flow (see erosion protection).<br />
Impact<br />
after<br />
Operational<br />
Impact<br />
before<br />
Minor Medium<br />
- term<br />
Site/Local Low Possible Low + Medium<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Moderate Long -<br />
term<br />
Management measures:<br />
Site/Local Medium Definite Medium + Medium<br />
Local surface water run-off will increase due to hard surfaces (panels, roads, infrastructure, etc) and would need<br />
to be dissipated back to sheet flow (see erosion protection).<br />
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Impact<br />
after<br />
Moderate Long -<br />
term<br />
7.1.3 Increase in erosion potential<br />
There are two areas where there will be an increase in the erosion potential due to higher surface<br />
water flows:<br />
• During a storm event the hard surface areas will generate higher surface water flows resulting in<br />
higher velocities and erosion potential. This would occur locally, directly downstream of the hard<br />
surface areas (discharge from panels, roads, buildings, etc.). During the construction period<br />
exposed areas will also have a higher erosion potential; and<br />
• During washing of the panels there will be a small chance of erosion occurring when flowing off<br />
the panels but this would be insignificant when compared to the storm flows;<br />
High erosion may naturally be introduced along the drainage lines (low lying areas) due to increased<br />
frequency and intensity of flooding, large-scale erosion and sediment movement. Table 8-3 below<br />
indicates the impact assessment for the increase in erosion potential.<br />
Table 7-3: Impact assessment (increase in erosion potential)<br />
Increase in erosion potential from proposed activities<br />
Construction<br />
Impact<br />
before<br />
Site/Local Medium Definite Medium + Medium<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Moderate Medium<br />
- term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Medium<br />
Minimum disturbance to existing topography during implementation and incorporate into construction program.<br />
Any surface water discharging to environment during washing of panels to be adequately dissipated back to sheet flow.<br />
Any surface water discharging to environment from water/waste treatment works needs to be adequately dissipated.<br />
Increased peaks due to hard surfaces requires adequate dissipation and erosion protection to ensure concentrated flows<br />
back to sheet flow, minimising erosion potential. This can be achieved by strategically placing appropriate sized stone<br />
downstream of the hardened surface areas (including panels).<br />
Strategically placed hessian/geo-fabric attached to rows of stakes to decrease the velocities during construction.<br />
Impact<br />
after<br />
Operational<br />
Impact<br />
before<br />
Moderate Medium<br />
- term<br />
Site/Local Medium Unlikely Low - Medium<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Minor Long -<br />
term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Medium<br />
Any surface water discharging to environment during washing of panels to be adequately dissipated back to sheet flow.<br />
Any surface water discharging to environment from water/waste treatment works needs to be adequately dissipated.<br />
Increased peaks due to hard surfaces requires adequate dissipation and erosion protection to ensure concentrated flows<br />
back to sheet flow, minimising erosion potential. This can be achieved by strategically placing appropriate sized stone<br />
downstream of the hardened surface areas (including panels).<br />
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Impact<br />
after<br />
Minor Long -<br />
term<br />
Site/Local Medium Unlikely Low - Medium<br />
7.1.4 Increase in flooding potential and change in flow regime<br />
There are two areas which may impact on the flooding potential and the change to the flow regime:<br />
• From a regional perspective there may be an increase in the flooding potential due to the<br />
infrastructure changing the original flow path during an extreme storm event. There is no<br />
evidence of a defined watercourse channel and, therefore, the surface water flows as sheet flow<br />
across a wide floodplain. The maximum flow depth would be approximately 200 mm – 300 mm<br />
and would flow between and below the panels across the site; and<br />
• From a local perspective there may be an increase in flooding potential just downstream of the<br />
hard surface areas but this is expected to reach original flow regime just downstream of the site;<br />
Flooding may naturally occur along the drainage lines (low lying areas) due to increased frequency<br />
and intensity of storms, large-scale erosion and sediment movement.<br />
It should be noted that with the proposed development in place there will be no increase in flooding<br />
potential to neighbouring properties but one still needs to manage the flooding potential on the<br />
proposed infrastructure. Table 8-4 below indicates the impact assessment for the increase in<br />
flooding potential.<br />
Table 7-4: Impact assessment (increase in flooding potential and change in flow regime)<br />
Increase in flooding potential and change in flow characteristics from proposed activities<br />
Construction<br />
Impact<br />
before<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Moderate Medium<br />
- term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Low<br />
From a regional perspective ensure all the relevant infrastructure is constructed outside of the envisaged flood plain<br />
assumed a potential flow depth of 200 mm – 300 mm during an extreme flood event. This can be achieved by raising the<br />
floor level of the affected infrastructure or relocating some of the buildings.<br />
From a local perspective any concentrated surface water discharging from Skelmberg would need to be adequately diverted<br />
away from any relevant infrastructure. This can be achieved by constructing earth berms to divert the surface water away<br />
from the infrastructure and back to original sheet flow path.<br />
Any local surface water flowing towards the N14 would also need to be managed by diverting along the side of the road in<br />
the form of an earth channel/berm, until an appropriate crossing under the N14.<br />
Impact<br />
after<br />
Operational<br />
Impact<br />
before<br />
Moderate Medium<br />
- term<br />
Site/Local Medium Possible Medium - Low<br />
Magnitude Duration Scale Consequence Probability SIGNIFICANCE +/- Confidence<br />
Moderate Long -<br />
term<br />
Management measures:<br />
Site/Local Medium Definite Medium - Low<br />
From a regional perspective ensure all the relevant infrastructure is constructed outside of the envisaged flood plain<br />
assumed a potential flow depth of 200 mm – 300 mm during an extreme flood event. This can be achieved by raising the<br />
floor level of the affected infrastructure or relocating some of the buildings.<br />
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From a local perspective any concentrated surface water discharging from Skelmberg would need to be adequately diverted<br />
away from any relevant infrastructure. This can be achieved by constructing earth berms to divert the surface water away<br />
from the infrastructure and back to original sheet flow path.<br />
Any local surface water flowing towards the N14 would also need to be managed by diverting along the side of the road in<br />
the form of an earth channel/berm, until an appropriate crossing under the N14.<br />
Impact<br />
after<br />
Moderate Long -<br />
term<br />
7.2 Mitigation measures<br />
The suggested mitigation measures have been covered in the above impact assessment. These<br />
mitigation measures are based on standard engineering approaches but there are alternative options<br />
available to achieve the same result.<br />
8 Conclusions and Recommendations<br />
The conclusions and recommendations for the desktop study have been divided into hydrological,<br />
geotechnical and the impact assessment including relevant mitigation measures.<br />
8.1 Hydrological<br />
Site/Local Medium Possible Medium - Low<br />
The following pertinent issues have been summarised below:<br />
• The site is located in a low rainfall zone (MAP 107 mm) with the majority of the site having a low<br />
run-off potential with a high Infiltration rate and rapid permeability;<br />
• Nearly 50% of the average monthly rainfall occurs between February and March;<br />
• Besides the local runoff from Skelmberg there is only one major catchment of 690 km 2 draining<br />
from the south to Skelmberg and into the low lying pan north of the proposed site;<br />
• The catchment is considered to be an endoreic area which means that the rivers terminate in<br />
inland lakes or pans and the surface runoff does not contribute to any of the surrounding<br />
drainage systems which normally ends up at the ocean. The degree of endoreism is clearly a<br />
function of the rainfall and normally located in arid, semi-arid and dry sub-humid drylands;<br />
• The 1:100 year peak flow was generated using TR137 and SDF. These methods are normally<br />
used on regional catchments but there are no applicable site-specific methods available for this<br />
area. Due to the locality, terrain and climate there is a high possibility that most of the surface<br />
water draining from the upper catchments would not even reach the site;<br />
• The following development considerations need to be considered:<br />
I. There is a well defined watercourse located north of the proposed site which drains<br />
under the N14 and the old gravel road before discharging into the low lying pans. The<br />
only large catchment which may have an impact on the site is the catchment which has<br />
its watershed south of the proposed site flowing towards Skelmberg from south to north<br />
across the proposed site at sheet flow. There are, however, small erosion gullies at the<br />
foot of the Skelmberg which would need to be taken into account during the detailed<br />
design;<br />
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II. Although it is difficult to demarcate the 1:100 year floodlines due to the terrain, the<br />
proposed development would still need to manage the sheet flow/drainage lines<br />
(approximately 200 mm – 300 mm) crossing the site and may require minor diversion<br />
channel/berms/culverts to protect the relevant infrastructure. In addition, any of the<br />
operational buildings needs to be constructed on the higher ground;<br />
III. All clean and dirty water needs to be separated;<br />
IV. Depending on the layouts, any hard surface areas created by the new development<br />
would need to adequately drain and dissipate prior to discharging into the existing<br />
drainage lines to prevent downstream erosion;<br />
V. Any water being used to wash the panels and discharging back into the natural<br />
environment as surface water needs to comply with authorities water quality standards;<br />
and<br />
VI. Any waste/ water treatment discharging as surface water back into the natural<br />
environment needs to comply with authorities water quality standards.<br />
• Based on the available desktop groundwater data for the site, the following should be<br />
considered towards identifying sensitivities around the proposed development:<br />
I. The aquifer type is integranular and fractured with yields ranging from 0.1 to 0.5 L/s;<br />
II. Regional groundwater level is at 45 mbgl;<br />
III. The site is located in an endoreic pan which does not appear to be in continuity with<br />
surface drainage in adjacent quaternaries. Shallow groundwater flow (if any) is likely to<br />
mimic topography and flow to the north;<br />
IV. The nearest groundwater user is located >10 km to the north of the site;<br />
V. The elevated TDS and chloride levels are indicative of a groundwater system receiving<br />
low recharge and having a longer residence time; and<br />
VI. Based on these characteristics, the impact to the groundwater environment due to the<br />
proposed development is expected to be low.<br />
8.2 Geotechnical<br />
Although the geotechnical assessment does not have a direct input into the impact assessment it is<br />
important to be aware of the issues as it can have a major financial implication which could modify<br />
the layout of the proposed development. The following pertinent issues have been summarised<br />
below:<br />
• The area is generally flat, with outcrop of metamorphic rock across the area and forming<br />
approximately 200 m high hills in the north western corner. The flatter areas are mainly overlain<br />
by Quaternary red windblown sands and Quaternary sand, scree and rubble. These sands<br />
generally have a loose consistency and exhibit a collapsible fabric. It may be possible to found<br />
light structures on these sands using various foundation techniques/treatments, but for heavy<br />
structures (solar masks assuming they are heavy) it is necessary to found on rock below these<br />
sands. Hardpan and/or gravel calcrete often lies beneath these sands and over underlying rock.<br />
The consistency of calcrete may indicate suitable founding material, however, as it is a calcium<br />
carbonate it may become weaker over time and founding below the calcrete on rock is<br />
recommended. The depth to rock in this area is generally expected to vary between 1.0 m and<br />
3.0 m, but this depends on the structure of the underlying rock formations and topography. The<br />
sands can be in excess of 6.0 m deep in places where they have filled up paleo channels.<br />
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Quartzite and schist of the Wortel formation is expected to underlie most of the sands in the<br />
area.<br />
• The following development considerations need to be considered:<br />
I. Determine the depth to bedrock across the preferred site and demarcate appropriate<br />
zones;<br />
II. Assign the correct founding for the appropriate depth zone; and<br />
III. Consider where the nearest suitable borrow pit and quarry is located (sand and stone)<br />
for the concrete foundations as importing the concrete would be an expensive option.<br />
8.3 Impact Assessment<br />
The following pertinent issues have been summarised below:<br />
I. The impact assessment (negative) for deterioration in water quality changes from a<br />
medium to a low with management measures in place during construction and during<br />
the operational phase;<br />
II. The impact assessment (positive) for increase in water quantity remains low with<br />
management measures in place during construction and changes to medium during<br />
operational phase;<br />
III. The impact assessment (negative) for increase in erosion potential changes from a<br />
medium to a low with management measures in place during construction and during<br />
the operational phase;<br />
IV. The impact assessment (negative) for increase in flooding potential remains medium<br />
with management measures in place during construction and operational phase.<br />
8.4 Mitigation Measures<br />
The surface water management measures have been summarised below:<br />
Table 8-1: Mitigation measures (deterioration in water quality)<br />
Deterioration in surface water quality due to proposed activities<br />
Construction<br />
Management measures:<br />
Minimum disturbance to existing topography during implementation and incorporate into construction program.<br />
Any surface water discharging to environment during washing of panels to comply with authorities water quality standards.<br />
Any surface water discharging to environment from water/waste treatment works to comply with authorities water quality<br />
standards.<br />
Separate clean and dirty water areas.<br />
Strategically placed hessian/geo-fabric attached to rows of stakes to prevent sediment washing downstream of the site<br />
during construction.<br />
Operational<br />
Management measures:<br />
Any surface water discharging to environment during washing of panels to comply with authorities water quality standards.<br />
Any surface water discharging to environment from water/waste treatment works to comply with authorities water quality<br />
standards.<br />
Separate clean and dirty water areas.<br />
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Table 8-2: Mitigation measures (increase in surface water quantity)<br />
Increase in surface water quantity due to proposed activities<br />
Construction<br />
Management measures:<br />
Local surface water run-off will increase due to hard surfaces created during construction and would need to be<br />
dissipated back to sheet flow (see erosion protection).<br />
Operational<br />
Management measures:<br />
Local surface water run-off will increase due to hard surfaces (panels, roads, infrastructure etc) and would need to be<br />
dissipated back to sheet flow (see erosion protection).<br />
Table 8-3: Mitigation measures (increase in erosion potential)<br />
Increase in erosion potential from proposed activities<br />
Construction<br />
Management measures:<br />
Minimum disturbance to existing topography during implementation and incorporate into construction program.<br />
Any surface water discharging to environment during washing of panels to be adequately dissipated back to sheet flow.<br />
Any surface water discharging to environment from water/waste treatment works needs to be adequately dissipated.<br />
Increased peaks due to hard surfaces requires adequate dissipation and erosion protection to ensure concentrated flows<br />
back to sheet flow, minimising erosion potential. This can be achieved by strategically placing appropriate sized stone<br />
downstream of the hardened surface areas (including panels).<br />
Strategically placed hessian/geo-fabric attached to rows of stakes to decrease the velocities during construction.<br />
Operational<br />
Management measures:<br />
Any surface water discharging to environment during washing of panels to be adequately dissipated back to sheet flow.<br />
Any surface water discharging to environment from water/waste treatment works needs to be adequately dissipated.<br />
Increased peaks due to hard surfaces requires adequate dissipation and erosion protection to ensure concentrated flows<br />
back to sheet flow, minimising erosion potential. This can be achieved by strategically placing appropriate sized stone<br />
downstream of the hardened surface areas (including panels).<br />
Table 8-4: Mitigation measures (increase in flooding potential and change in flow regime)<br />
Increase in flooding potential and change in flow characteristics from proposed activities<br />
Construction<br />
Management measures:<br />
From a regional perspective ensure all the relevant infrastructure is constructed outside of the envisaged flood plain<br />
assumed a potential flow depth of 200 mm – 300 mm during an extreme flood event. This can be achieved by raising<br />
the floor level of the affected infrastructure or relocating some of the buildings.<br />
From a local perspective any concentrated surface water discharging from Skelmberg would need to be adequately<br />
diverted away from any relevant infrastructure. This can be achieved by constructing earth berms to divert the surface<br />
water away from the infrastructure and back to original sheet flow path.<br />
Any local surface water flowing towards the N14 would also need to be managed by diverting along the side of the road<br />
in the form of an earth channel/berm, until an appropriate crossing under the N14.<br />
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Operational<br />
Management measures:<br />
From a regional perspective ensure all the relevant infrastructure is constructed outside of the envisaged flood plain<br />
assumed a potential flow depth of 200 mm – 300 mm during an extreme flood event. This can be achieved by raising<br />
the floor level of the affected infrastructure or relocating some of the buildings.<br />
From a local perspective any concentrated surface water discharging from Skelmberg would need to be adequately<br />
diverted away from any relevant infrastructure. This can be achieved by constructing earth berms to divert the surface<br />
water away from the infrastructure and back to original sheet flow path.<br />
Any local surface water flowing towards the N14 would also need to be managed by diverting along the side of the road<br />
in the form of an earth channel/berm, until an appropriate crossing under the N14.<br />
9 Final Remarks<br />
Due to the nature of the proposed development, the locality of the site and assuming all the relevant<br />
surface water management measures are in place, the potential negative impact on the surrounding<br />
environment is expected to be minimal.<br />
Prepared by<br />
Murray Sim<br />
Associate Partner<br />
Reviewed by<br />
Peter Shepherd<br />
Director<br />
All data used as source material plus the text, tables, figures, and attachments of this document<br />
have been reviewed and prepared in accordance with generally accepted professional engineering<br />
and environmental practices.<br />
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10 References<br />
Alexander WJR, (2001), Flood Risk Reduction Measures incorporating Flood Hydrology for Southern<br />
<strong>Africa</strong>;<br />
Dent, M.C., Lynch, S.D. and Schulze, R.E. (1989). Mapping mean annual and other rainfall statistics<br />
over Southern <strong>Africa</strong>. Water Research Commission, Pretoria. Report 109/1/89;<br />
Department of Water Affairs and Forestry (1998). The National Water Act, Act 36 of 1998. Pretoria;<br />
Department of Water Affairs and Forestry (1988). Regional Maximum Flood Peaks in Southern<br />
<strong>Africa</strong>, TR137;<br />
Department of Water Affairs and Forestry (2006). Best Practise Guideline (G1) Storm Water<br />
Management;<br />
Hamlin, M.J., 1983. The significance of rainfall in the study of hydrological processes at basin scale.<br />
Journal of Hydrology, 65, 73-94;<br />
Institute for Commercial Forestry Research, Daily Rainfall Data Extraction Utility KwaZulu-Natal<br />
University, User Manual Version 1.2;<br />
Magagula S JIS Environmental Engineers 2012, Feasibility Study on the Water Requirements for<br />
SATO PV Project: Zuurwater Farm, Northern Cape Province. Report JIS/R/2012/01/18;<br />
Midley DC, Pitman, WV and Middleton, BJ (1981) Surface water resources of South <strong>Africa</strong> Volumes I<br />
to VI. Hydrological Research unit Report Nos 8/81 to 13/81, University of Witwatersrand,<br />
Johannesburg;<br />
Midley DC, Pitman, WV and Middleton, BJ (1994) Surface water resources of South <strong>Africa</strong> 1990<br />
Water Research Commission Report Nos. WRC 298/1/94 to 298/6.2/94, Pretoria;<br />
Pitman WC (1973). A mathematical model for generating monthly river flow from the<br />
Hydrometeological data in South <strong>Africa</strong>. Hydrological Research Unit Report No. 2/73, University of<br />
the Witwatersrand , Johannesburg;<br />
Schulze, R.E., 1995. Hydrology and Agrohydrology. A theory text to accompany the ACRU 3.00<br />
Agrohydrological Modelling System. Water Research Commission, Pretoria. Report TT69/95;<br />
Schulze, R.E., 1995. Hydrology and Agrohydrology. A practical text to accompany the ACRU 3.00<br />
Agrohydrological Modelling System. Water Research Commission, Pretoria. Report TT70/95;<br />
Schulze, R.E., 1997. South <strong>Africa</strong>n Atlas of Agrohydrology and Climatology, Water Research<br />
Commission Report. School of Bio Resources Engineering and Environmental Hydrology;<br />
SCS-SA (1992). User, Flood estimation for small Catchments in Southern <strong>Africa</strong>, Manual, PC-Based<br />
SCS Design;<br />
Smithers JC and Schulze RE (2000), Long duration design rainfall estimates for South <strong>Africa</strong>, WRC<br />
Report No. 811/1/00;<br />
Smithers JC and Schulze RE (2000), Rainfall Statistics for Design Flood Estimation in South <strong>Africa</strong>"<br />
(WRC Project K5/1060); and<br />
Water Research Commission (2005), WRSM2005 Water Resources of South <strong>Africa</strong>, Report<br />
numbers: 380/08, 381/08, 382/08. Pretoria.<br />
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Appendices<br />
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Appendix A: Impact Assessment Methodology<br />
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Impact Assessment Methodology<br />
The environmental impact assessment has been undertaken according to <strong>SRK</strong><br />
<strong>Consulting</strong>’s standard criteria for impact assessment which are detailed below. This<br />
methodology is compliant with the NEMA regulations.<br />
All specialists working on the EIA have been asked to use a common, systematic and<br />
defensible method of assessing significance that will enable comparisons to be made<br />
between impacts across different disciplines. It will also enable all relevant parties to<br />
understand the process and rationale upon which impacts have been assessed.<br />
The following section contains the methodology to be used by specialists to assist them in<br />
identifying, defining and evaluating the impacts.<br />
A. Method<br />
Generally, impact assessment is divided into three parts:<br />
• Issue identification<br />
• Impact definition<br />
• Impact evaluation<br />
Iteration of these parts occurs in each stage of an EIA process (screening, scoping, impact<br />
studies, reporting etc) to a varying degree. As the study progresses through the EIA<br />
stages, the main emphasis shifts from issue identification, through impact definition, then to<br />
impact evaluation.<br />
Identification of issues<br />
Each specialist was asked to evaluate the ‘aspects’ arising from the project description and<br />
ensure that all issues in their area of expertise have been identified. ‘Aspects’ is a term for<br />
the “mechanisms” by which project activities impact on receptors (people, economy,<br />
infrastructure, institutions and natural environment).<br />
Impact Definition<br />
Positive and negative impacts associated with these issues (and any others not included)<br />
then need to be defined – the definition statement should include the activity (source of<br />
impact), aspect and receptor. Impacts are identified and defined where there is a plausible<br />
pathway between the activities and receptors.<br />
Specialists will be asked to ensure that the suite of potential direct, indirect and cumulative<br />
impacts 1 are clearly defined. Direct impacts require a quantitative assessment wherever<br />
1 An indirect impact is an effect that is related to but removed from a proposed action by an intermediate step or process. An<br />
example would be increased hunting and illegal logging in the concession area (following mining) as a result of inmigration<br />
and improved access. Cumulative impacts occur when: a) Different impacts of one activity or impacts of different activities<br />
on the natural and social environment take place so frequently in time or so densely in space that they cannot be assimilated;<br />
or b) Impacts of one activity combine with the impacts of the same or other activities in a synergistic manner. Specialists<br />
should consider areas/stakeholders potentially affected by reasonably foreseeable further planned development of the project<br />
and other activities that may result in cumulative impacts.<br />
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possible. Indirect and cumulative impacts should be described qualitatively, but where data<br />
exist these should be quantified.<br />
Specialists will also be asked to identify fatal flaws i.e. very significant adverse impacts<br />
which cannot be avoided or mitigated and which will jeopardise the project and/or activities.<br />
All conclusions need to be backed up by scientific, economic and technical evidence or<br />
where this is not possible, based on specialist experience.<br />
Impact evaluation<br />
The last step is to evaluate the impact significance. Impact evaluation is not a purely<br />
objective and quantitative exercise. It has a subjective element, often using judgement and<br />
values as much as science-based criteria and standards. The need therefore exists to<br />
clearly explain how impacts have been interpreted so that others can see the weight<br />
attached to different factors and can understand the rationale of the assessment.<br />
With recognition that impact evaluation is generally relative, there is a need to set it in<br />
context. To achieve this it is important to:<br />
clearly describe the sensitivity of the receiving environment/ receptors;<br />
define the impact – the effect on the receiving environment/ receptors;<br />
explain the level of stakeholder 2 concern;<br />
explain the significance of impacts in a logical and justifiable way.<br />
There are many ways in which significance can be determined. Impacts are likely to be<br />
significant if they:<br />
are extensive over space or time;<br />
are intensive in concentration or in relation to assimilative capacity;<br />
exceed or approximate to standards or thresholds;<br />
do not comply with policies, land use plans, sustainability strategy;<br />
affect ecologically sensitive areas and heritage resources; and<br />
affect community lifestyle, traditional land uses and values.<br />
The basic elements used in the evaluation of impact significance are described in Table 1<br />
and the characteristics that specialists should use to describe the consequence of an<br />
impact are outlined in Table 2.<br />
2 Stakeholders are workers, affected stakeholders and other stakeholders. Affected Stakeholders are people, groups or<br />
communities who are subject to actual or potential project-related risks and /or adverse impacts on their physical environment,<br />
health or livelihoods and who are often located in the project’s near geographical proximity. Note that workers are defined as<br />
employees and other workers directly contracted by AGA to carry out work on the project.<br />
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Table 1: Key elements in the evaluation of impact significance<br />
Element Description Questions applied to<br />
the test of<br />
significance<br />
Consequence An impact or effect can be described as the change in an<br />
environmental parameter, which results from a particular<br />
project activity or intervention. Here, the term “consequence”<br />
refers to:<br />
• The sensitivity of the receiving environment, including its<br />
capacity to accommodate the kinds of changes the project<br />
may bring about;<br />
• The type of change and the key characteristics of the<br />
change (these are magnitude, extent and duration);<br />
• The importance of the change (the level of public concern/<br />
value attached to environment by the stakeholders and the<br />
change effected by the project).<br />
• The following should be considered in the determination of<br />
impact consequence:<br />
• standards and guidelines (e.g. pollution and emissions<br />
thresholds);<br />
• scientific evidence and professional judgement;<br />
• points of reference from comparable cases;<br />
• levels of stakeholder concern.<br />
Will there be a change in<br />
the biophysical and/or<br />
social environment?<br />
Is the change of<br />
consequence (of any<br />
importance)?<br />
Probability Likelihood/ chances of an impact occurring Is the change likely to<br />
occur?<br />
Effectiveness of the<br />
management<br />
measures<br />
Uncertainty/<br />
Confidence<br />
Significance of the impact needs to be determined both<br />
without management measures and with management<br />
measures.<br />
The significance of the unmanaged impact needs to be<br />
determined so there is an appreciation of what could occur in<br />
the absence of management measures and of the<br />
effectiveness of the proposed management measures.<br />
Uncertainty in impact prediction and the effectiveness of the<br />
proposed management measures. Sources of uncertainty in<br />
impact prediction include:<br />
• scientific uncertainty – limited understanding of an<br />
ecosystem or affected stakeholder and the processes that<br />
govern change;<br />
• data uncertainty – restrictions introduced by incomplete,<br />
contradictory or incomparable information, or by insufficient<br />
measurement techniques; and<br />
• policy uncertainty – unclear or disputed objectives,<br />
standards or guidelines.<br />
Will the management<br />
measures reduce impact<br />
to an acceptable level?<br />
What is the degree of<br />
confidence in the<br />
significance ascribed to<br />
the impact?<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012
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Table 2: Characteristics to be used in impact description<br />
Characteristics<br />
used to describe<br />
consequence<br />
Sub-components Terms used to describe the characteristic<br />
Type Biophysical, social or economic<br />
Nature Direct or indirect, cumulative etc<br />
Status Positive (a benefit), negative (a cost) or neutral<br />
Phase of project<br />
Timing Immediate, delayed<br />
Magnitude<br />
Sensitivity of the receiving<br />
environment/ receptors<br />
Severity/ intensity (degree of<br />
change measured against thresholds<br />
and/or professional judgment)<br />
Level of stakeholder concern<br />
Spatial extent or population affected<br />
The area/population affected by the impact<br />
The boundaries at local and regional extents will be<br />
different for biophysical and social impacts.<br />
Duration (and reversibility)<br />
Length of time over which an impact occurs and potential<br />
for recovery of the endpoint from the impact<br />
During pre-construction (if applicable e.g.<br />
resettlement), construction, operation,<br />
decommissioning/post closure<br />
High, medium or low sensitivity<br />
Low capacity to accommodate the change (impact)/<br />
tolerant of the proposed change<br />
Gravity/ seriousness of the impact<br />
Intensity/ influence/ power/ strength<br />
High, medium or low levels of concern<br />
All or some stakeholders are concerned about the<br />
change<br />
Area/ volume covered, distribution, population<br />
Site/Local (social impacts should distinguish<br />
between site and local), regional, national or<br />
international<br />
Short term, long term<br />
Intermittent, continuous<br />
Reversible/ irreversibility<br />
Temporary, permanent<br />
Confidence High, Medium, Low<br />
B. Management recommendations<br />
Specialists will be asked to recommend practicable management measures in as much<br />
detail as possible and should focus on avoidance, and if avoidance is not possible, then to<br />
reduce, restore, compensate/offset negative impacts, enhance positive impacts and assist<br />
project design. The significance of impacts must be assessed both without and with<br />
assumed management measures in place. Unsubstantiated recommendations for further<br />
studies should be avoided. Specialists should also recommend and describe appropriate<br />
monitoring and review programmes to track the efficacy of management measures.<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012
<strong>SRK</strong> <strong>Consulting</strong>: 435209: Desktop Surface Water & Geotechnical Page 36<br />
C. Impact significance rating<br />
The impact significance rating process serves two purposes: firstly, it helps to highlight the<br />
critical impacts requiring consideration in the management and approval process; secondly,<br />
it serves to show the primary impact characteristics, as defined above, used to evaluate<br />
impact significance.<br />
The impact significance rating system is presented in Table 3 and involves three parts:<br />
Part A: Define impact consequence using the three primary impact characteristics of<br />
magnitude, spatial scale/population and duration;<br />
Part B: Use the matrix to determine a rating for impact consequence based on the<br />
definitions identified in Part A; and<br />
Part C: Use the matrix to determine the impact significance rating, which is a function of<br />
the impact consequence rating (from Part B) and the probability of occurrence.<br />
Part D: Define the Confidence level.<br />
Table 3: Method for rating the significance of impacts<br />
PART A: DEFINING CONSEQUENCE IN TERMS OF MAGNITUDE, DURATION AND SPATIAL<br />
SCALE<br />
Impact<br />
characteristics<br />
MAGNITUDE<br />
SPATIAL<br />
SCALE OR<br />
POPULATION<br />
DURATION<br />
Use these definitions to define the consequence in Part B<br />
Definition Criteria<br />
Major<br />
Moderate<br />
Minor<br />
Minor+<br />
Moderate+<br />
Major+<br />
Substantial deterioration or harm to receptors; receiving environment has<br />
an inherent value to stakeholders; receptors of impact are of conservation<br />
importance; or identified threshold often exceeded<br />
Moderate/measurable deterioration or harm to receptors; receiving<br />
environment moderately sensitive; or identified threshold occasionally<br />
exceeded<br />
Minor deterioration (nuisance or minor deterioration) or harm to receptors;<br />
change to receiving environment not measurable; or identified threshold<br />
never exceeded<br />
Minor improvement; change not measurable; or threshold never<br />
exceeded<br />
Moderate improvement; within or better than the threshold; or no<br />
observed reaction<br />
Substantial improvement; within or better than the threshold; or<br />
favourable publicity<br />
Site or local Site specific or confined to the immediate project area<br />
Regional May be defined in various ways, e.g. cadastral, catchment, topographic<br />
National/<br />
International<br />
Nationally or beyond<br />
Short term Less than 18 months<br />
Medium term 18 months to 5 years<br />
Long term >5 years<br />
PART B: DETERMINING CONSEQUENCE RATING<br />
Rate consequence based on definition of magnitude, spatial extent and duration<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012
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MAGNITUDE<br />
Minor DURATION<br />
Moderate DURATION<br />
Major DURATION<br />
PROBABILITY<br />
(of exposure to<br />
impacts)<br />
SPATIAL SCALE/ POPULATION<br />
Site or Local Regional National/<br />
international<br />
Long term Medium Medium High<br />
Medium<br />
term<br />
Low Low Medium<br />
Short term Low Low Medium<br />
Long term Medium High High<br />
Medium<br />
term<br />
Medium Medium High<br />
Short term Low Medium Medium<br />
Long term High High High<br />
Medium<br />
term<br />
Medium Medium High<br />
Short term Medium Medium High<br />
PART C: DETERMINING SIGNIFICANCE RATING<br />
Rate significance based on consequence and probability<br />
CONSEQUENCE<br />
Low Medium High<br />
Definite Medium Medium High<br />
Possible Low Medium High<br />
Unlikely Low Low Medium<br />
PART D: CONFIDENCE LEVEL<br />
High Medium Low<br />
+ denotes a positive impact.<br />
Using the matrix, the significance of each described impact is initially rated. This rating assumes the<br />
management measures inherent in the Project design are in place.<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012
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Appendix B: Figures<br />
435209/1.1 Regional drainage map<br />
435209/1.2 Study area<br />
435209/1.3 Catchment boundaries and surface water features<br />
435209/1.4 Surface water runoff potential<br />
435209/1.5 Hydro geological map<br />
435209/1.6 Geology map<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012
29°0'0"S<br />
29°30'0"S<br />
D82E<br />
F30C<br />
Brak River<br />
D82D<br />
F30B<br />
18°30'0"E<br />
18°30'0"E<br />
Orange River<br />
Path: G:\435209_SATO_PV_JHB\8GIS\GISPROJ\MXD\Water&Geotech\Updated January 2012\435209_F_1_1_SATO_Regional Drainage_A3L_C_02022012.mxd<br />
D82C<br />
D82A<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Regional Drainage Map<br />
19°0'0"E<br />
19°0'0"E<br />
D82B<br />
D81G<br />
Legend<br />
Water Features<br />
Site Boundary<br />
Dams D81F<br />
D81E<br />
Internal Site Boundaries<br />
Non-Perennial Pans<br />
Rivers<br />
Quaternary catchments<br />
Sub-catchment<br />
D53F<br />
0 3.5 7 14 21 28<br />
Kilometers<br />
29°0'0"S<br />
29°30'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:465,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
01/02/2012<br />
Project No:<br />
435209<br />
MURA<br />
Fig No:<br />
1.1<br />
Revision: A Date: 01 02 2012
29°20'0"S<br />
To Springbok<br />
18°40'0"E<br />
18°40'0"E<br />
Bobbejaangat<br />
Hoedkop<br />
Windhoek se Berg<br />
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Skelmberg<br />
Windhoek se Berg<br />
Swartberg<br />
Platjiesvlei se Kop<br />
Kranskop<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Aerial photograph showing the study area<br />
N14<br />
18°50'0"E<br />
18°50'0"E<br />
Legend<br />
Project Area<br />
To Kakamas<br />
Internal Site Boundaries<br />
0 0.5 1 2 3 4<br />
Kilometers<br />
29°20'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:70,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
01/02/2012<br />
Project No:<br />
435209<br />
MURA<br />
Fig No:<br />
1.2<br />
Revision: A Date: 01 02 2012
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
18°20'0"E<br />
740<br />
1120<br />
1080<br />
900<br />
940<br />
1000<br />
860<br />
920<br />
1080<br />
900<br />
1100<br />
880<br />
1060<br />
1000<br />
18°20'0"E<br />
940<br />
920<br />
1040<br />
840<br />
820<br />
1020<br />
1060<br />
800<br />
1060<br />
940<br />
1040<br />
760<br />
1060<br />
1020<br />
800<br />
960<br />
980<br />
860<br />
780<br />
840<br />
860<br />
960<br />
860<br />
820<br />
820<br />
840<br />
900<br />
840<br />
880<br />
840<br />
840<br />
840<br />
860<br />
860<br />
840<br />
840<br />
840<br />
860<br />
880<br />
1000<br />
1080<br />
880<br />
940<br />
F30B<br />
880<br />
880<br />
1040<br />
820<br />
880<br />
900<br />
1020<br />
1040<br />
800<br />
920<br />
1060<br />
920<br />
1080<br />
1120<br />
18°30'0"E<br />
920<br />
920<br />
980<br />
1060<br />
1100<br />
960<br />
D82C<br />
1060<br />
940<br />
1060<br />
1040<br />
1040<br />
1060<br />
760<br />
740<br />
18°40'0"E<br />
900<br />
980<br />
780<br />
860<br />
980<br />
1020<br />
840<br />
780<br />
840<br />
980<br />
760<br />
940<br />
960<br />
1040<br />
820<br />
800<br />
760<br />
880<br />
1000<br />
840<br />
900<br />
880<br />
1000<br />
820<br />
100019°0'0"E<br />
2.5<br />
18°30'0"E<br />
18°40'0"E<br />
18°50'0"E<br />
Path: G:\435209_SATO_PV_JHB\8GIS\GISPROJ\MXD\Water&Geotech\Updated January 2012\435209_F_1_3_SATO_Catchments_A3L_C_01022012.mxd<br />
760<br />
800<br />
900<br />
780<br />
820<br />
1020<br />
980<br />
780<br />
840<br />
780<br />
920<br />
820<br />
820<br />
880<br />
820<br />
820<br />
760<br />
840<br />
980<br />
820<br />
820<br />
980<br />
840<br />
780<br />
820<br />
880<br />
840<br />
960<br />
980<br />
980<br />
980<br />
960<br />
980<br />
1000<br />
18°50'0"E<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Catchment boundaries and surface water features<br />
800<br />
900<br />
900<br />
1020<br />
980<br />
960<br />
860<br />
980<br />
940<br />
840<br />
920<br />
980<br />
980<br />
900<br />
1000<br />
880<br />
940<br />
920<br />
900<br />
980<br />
D82B<br />
960<br />
880<br />
880<br />
19°0'0"E<br />
900<br />
940<br />
900<br />
860<br />
1000<br />
1020<br />
900<br />
840<br />
880<br />
920<br />
880<br />
Legend<br />
900<br />
Site Boundary<br />
880<br />
860<br />
880<br />
900<br />
900<br />
900<br />
920<br />
900<br />
920<br />
920<br />
920<br />
980<br />
Internal Site Boundaries<br />
Contours<br />
Rivers<br />
Water Features<br />
Dams<br />
Non-Perennial Pans<br />
Quaternary catchments<br />
Sub-catchment<br />
0 5 10 15 20<br />
Kilometers<br />
940<br />
940<br />
960<br />
900<br />
940<br />
960<br />
940<br />
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:250,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
28/11/2011<br />
Project No:<br />
435209<br />
MURA<br />
Fig No:<br />
1.3<br />
Revision: C Date: 01 02 2012
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
18°20'0"E<br />
740<br />
1120<br />
1080<br />
900<br />
940<br />
D<br />
1000<br />
860<br />
920<br />
1080<br />
900<br />
D<br />
1100<br />
880<br />
1060<br />
1000<br />
18°20'0"E<br />
940<br />
840<br />
C<br />
920<br />
1040<br />
820<br />
1020<br />
1060<br />
800<br />
1060<br />
940<br />
1040<br />
760<br />
1060<br />
1020<br />
800<br />
C<br />
960<br />
980<br />
860<br />
780<br />
840<br />
860<br />
960<br />
860<br />
820<br />
820<br />
840<br />
A<br />
840<br />
900<br />
880<br />
840<br />
840<br />
840<br />
860<br />
860<br />
840<br />
840<br />
840<br />
860<br />
880<br />
1000<br />
1080<br />
880<br />
940<br />
880<br />
880<br />
1040<br />
820<br />
880<br />
900<br />
1020<br />
1040<br />
800<br />
920<br />
1060<br />
920<br />
1080<br />
1120<br />
18°30'0"E<br />
920<br />
920<br />
980<br />
1060<br />
1100<br />
1060<br />
940<br />
960<br />
1060<br />
1040<br />
1040<br />
1060<br />
760<br />
740<br />
18°40'0"E<br />
900<br />
980<br />
780<br />
860<br />
980<br />
1020<br />
840<br />
780<br />
840<br />
980<br />
760<br />
940<br />
960<br />
1040<br />
820<br />
800<br />
760<br />
880<br />
1000<br />
840<br />
900<br />
880<br />
1000<br />
820<br />
100019°0'0"E<br />
2.5<br />
18°30'0"E<br />
18°40'0"E<br />
18°50'0"E<br />
Path: G:\435209_SATO_PV_JHB\8GIS\GISPROJ\MXD\Water&Geotech\Updated January 2012\435209_F_1_4_SATO_Pot_Runoff_A3L_C_01022012.mxd<br />
A<br />
C<br />
D<br />
760<br />
800<br />
900<br />
780<br />
820<br />
1020<br />
980<br />
780<br />
840<br />
780<br />
920<br />
820<br />
820<br />
880<br />
820<br />
820<br />
760<br />
840<br />
980<br />
820<br />
820<br />
980<br />
840<br />
780<br />
820<br />
880<br />
840<br />
960<br />
980<br />
980<br />
980<br />
960<br />
980<br />
1000<br />
18°50'0"E<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Runoff potential<br />
C<br />
800<br />
900<br />
900<br />
1020<br />
980<br />
960<br />
860<br />
980<br />
940<br />
840<br />
920<br />
980<br />
980<br />
A<br />
900<br />
1000<br />
880<br />
940<br />
C<br />
920<br />
900<br />
980<br />
960<br />
880<br />
880<br />
19°0'0"E<br />
900<br />
940<br />
900<br />
860<br />
1000<br />
1020<br />
900<br />
840<br />
880<br />
Legend<br />
920<br />
880<br />
900<br />
Site Boundary<br />
0 5 10 15 20<br />
Kilometers<br />
880<br />
860<br />
880<br />
900<br />
900<br />
900<br />
920<br />
900<br />
A<br />
920<br />
920<br />
920<br />
D<br />
980<br />
Internal Site Boundaries<br />
Sub-catchment<br />
Contours<br />
Run-off Potential<br />
Soil Group<br />
Soil Group A<br />
Low stormwater potential:<br />
Infiltration is high and<br />
permeability is rapid in this<br />
group. Overall drainage<br />
is excessive to well-drained<br />
Soil Group B<br />
Moderately low stormwater<br />
potential:<br />
Moderate Infiltration rates,<br />
effective depth and drainage.<br />
Permeability is slightly<br />
restricted<br />
Soil Group C<br />
Moderately high stormflow<br />
potential:<br />
Infiltration is slow or<br />
deteriorates rapidly.<br />
permeability restricted. Soil<br />
depth tends to be shallow<br />
Soil Group D<br />
High stormflow potential:<br />
Infiltration is slow and<br />
permeability is severely<br />
restricted.Very shallow soils,<br />
and soils with a high<br />
shrink-swell potential<br />
940<br />
940<br />
960<br />
900<br />
940<br />
960<br />
940<br />
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:250,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
28/11/2011<br />
Project No:<br />
435209<br />
MURA<br />
Fig No:<br />
1.4<br />
Revision: C Date: 01 02 2012
29°10'0"S<br />
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
F30B<br />
18°30'0"E<br />
18°30'0"E<br />
182289<br />
D82C<br />
!H !H<br />
182291<br />
!H<br />
18°40'0"E<br />
182275<br />
18°40'0"E<br />
Path: G:\435209_SATO_PV_JHB\8GIS\GISPROJ\MXD\Water&Geotech\Updated January 2012\435209_F_1_5_SATO_Hyrdogeological_A3L_C_01022012.mxd<br />
!H<br />
182281<br />
!H<br />
89747<br />
!H 180620 !H<br />
18°50'0"E<br />
180622<br />
18°50'0"E<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Hydrogeological map<br />
D82B<br />
19°0'0"E<br />
Hydrogeology<br />
19°0'0"E<br />
Legend<br />
Site Boundary<br />
Internal Site Boundaries<br />
Sub-catchment<br />
!H Boreholes<br />
Quaternary catchments<br />
Water Features<br />
Dams<br />
Non-Perennial Pans<br />
Rivers<br />
Groundwater Quality as Electrical Conductivity<br />
Fractured<br />
70 - 300 mS/m<br />
300 - 1 000 mS/m<br />
> 1 000 mS/m<br />
0.1 - 0.5 l/s<br />
Intergranular and Fractured<br />
Intergranular and fractured 0.0 - 0.1 l/s<br />
Intergranular and fractured 0.1 - 0.5 l/s<br />
D82B<br />
0 2.5 5 10 15 20<br />
Kilometers<br />
29°10'0"S<br />
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:250,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
28/11/2011 MURA<br />
Project No: Fig No:<br />
435209<br />
1.5<br />
Revision: C Date: 01 02 2012
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
18°20'0"E<br />
740<br />
1120<br />
1080<br />
900<br />
940<br />
1000<br />
860<br />
920<br />
1080<br />
900<br />
1100<br />
880<br />
1060<br />
1000<br />
18°20'0"E<br />
940<br />
920<br />
1040<br />
840<br />
820<br />
1020<br />
1060<br />
800<br />
1060<br />
940<br />
1040<br />
760<br />
1060<br />
1020<br />
800<br />
960<br />
980<br />
860<br />
780<br />
840<br />
860<br />
960<br />
860<br />
820<br />
820<br />
840<br />
900<br />
840<br />
880<br />
840<br />
840<br />
840<br />
860<br />
860<br />
840<br />
840<br />
840<br />
860<br />
880<br />
1000<br />
1080<br />
880<br />
940<br />
880<br />
880<br />
1040<br />
820<br />
880<br />
900<br />
1020<br />
1040<br />
800<br />
920<br />
1060<br />
920<br />
1080<br />
1120<br />
18°30'0"E<br />
920<br />
920<br />
980<br />
1060<br />
1100<br />
1060<br />
940<br />
960<br />
1060<br />
1040<br />
1040<br />
1060<br />
760<br />
740<br />
18°40'0"E<br />
900<br />
980<br />
780<br />
860<br />
980<br />
1020<br />
840<br />
780<br />
840<br />
980<br />
760<br />
940<br />
960<br />
1040<br />
820<br />
800<br />
760<br />
880<br />
1000<br />
840<br />
900<br />
880<br />
1000<br />
820<br />
100019°0'0"E<br />
2.5<br />
18°30'0"E<br />
18°40'0"E<br />
18°50'0"E<br />
Path: G:\435209_SATO_PV_JHB\8GIS\GISPROJ\MXD\Water&Geotech\Updated January 2012\435209_F_1_6_SATO_Geology_A3L_C_01022012.mxd<br />
760<br />
800<br />
900<br />
780<br />
820<br />
1020<br />
980<br />
780<br />
840<br />
780<br />
920<br />
820<br />
820<br />
880<br />
820<br />
820<br />
760<br />
840<br />
980<br />
820<br />
820<br />
980<br />
840<br />
780<br />
820<br />
880<br />
840<br />
960<br />
980<br />
980<br />
980<br />
960<br />
980<br />
1000<br />
18°50'0"E<br />
SATO PV: DESKTOP SURFACE WATER AND GEOTECHNICAL STUDY<br />
Geology map<br />
800<br />
900<br />
900<br />
1020<br />
N14<br />
980<br />
960<br />
860<br />
980<br />
940<br />
840<br />
920<br />
980<br />
980<br />
900<br />
1000<br />
880<br />
940<br />
920<br />
900<br />
980<br />
960<br />
880<br />
880<br />
19°0'0"E<br />
900<br />
940<br />
900<br />
860<br />
1000<br />
1020<br />
900<br />
840<br />
880<br />
Legend<br />
920<br />
880<br />
900<br />
Site Boundary<br />
880<br />
860<br />
880<br />
900<br />
900<br />
900<br />
920<br />
900<br />
920<br />
920<br />
920<br />
980<br />
Internal Site Boundaries<br />
Contours<br />
Sub-catchment<br />
0 5 10 15 20<br />
Kilometers<br />
940<br />
940<br />
960<br />
900<br />
940<br />
960<br />
940<br />
29°20'0"S<br />
29°30'0"S<br />
29°40'0"S<br />
¯<br />
Data Source:<br />
Scale:<br />
1:250,000<br />
Projection: Datum:<br />
TM<br />
HH94<br />
Central Meridian/Zone:<br />
Lo19<br />
Date: Compiled by:<br />
28/11/2011 MURA<br />
Project No: Fig No:<br />
435209<br />
1.6<br />
Revision: C Date: 01 02 2012
<strong>SRK</strong> <strong>Consulting</strong>: 435209: Desktop Surface Water & Geotechnical Page 39<br />
Report No.<br />
Copy No.<br />
<strong>SRK</strong> Report Distribution Record<br />
Name/Title Company Copy Date Authorised by<br />
Approval Signature:<br />
This report is protected by copyright vested in <strong>SRK</strong> (SA) (Pty) Ltd. It may not be reproduced or<br />
transmitted in any form or by any means whatsoever to any person without the written permission of<br />
the copyright holder, <strong>SRK</strong>.<br />
SIMM/SHEP 435209_SATO_SurfaceWater_GW_Geotechnical_Preliminary_Jan2012_FinalDraft.docx January 2012