environmental impact statement kilmainhamwood compost facility ...
environmental impact statement kilmainhamwood compost facility ... environmental impact statement kilmainhamwood compost facility ...
5361- Kilmainhamwood Compost Facility Extension- EIS At the composting facility area, approximately 56% of the total annual rainfall is recorded during the winter period (October – March). This amount of precipitation (including snow) will normally be associated with more prolonged Atlantic frontal weather depressions passing over the region compared to the summer. 9.4.2.4 Evapotranspiration and Effective Rainfall The nearest meteorological station with evapotranspiration measuring equipment is located at the Clones Synoptic Station. Evapotranspiration is the return of water vapour to the atmosphere by evaporation from land and by the transpiration of plants, generally measured from a short-grass covered surface (such as a permanent pasture) adequately supplied with water. Evaporation is the return of water vapour to the atmosphere by evaporation from a free water surface such as a pan of water, known as a “Class A Pan”, fitted with a depth measuring gauge. The evapotranspiration figures for the Clones Synoptic Station are detailed in Table 9.10. It can be noted that evapotranspiration is very low during winter months, when plant growth is minimal. The vast majority of evapotranspiration during winter months is attributable to direct evaporation from ground surfaces. During summer months the rate of evapotranspiration increases and often exceeds the monthly rainfall. This is due to increased free evaporation from the surface and from transpiration from leaves and plants. Using the rainfall data calculated for the site in Table 9.9 and the potential evapotranspiration data for the nearest synoptic station, i.e. Clones Synoptic Station, the effective rainfall for the subject site can be calculated. Table 9.10 also shows the effective rainfall to the site. Any rain falling on the site will infiltrate to the ground, evaporate from the surface or become surface water runoff. Table 9.10 Hydrological Data for the Development Site Month Rainfall (mm) For inspection purposes only. Consent of copyright owner required for any other use. Potential Evapo- transpiration (mm) Actual Evapo- transpiration (mm) (PE x 0.92) Effective Rainfall (mm) January 108 2.4 2.2 105.8 February 74 14.6 13.4 60.9 March 78 29.9 27.5 50.9 April 65 51.7 47.6 17.6 May 70 72.1 66.3 3.9 June 67 79.8 73.4 -6.2 July 64 74.1 68.2 -4.0 August 86 58.5 53.8 31.7 September 89 35.9 33.0 55.6 October 99 16.8 15.5 83.3 November 90 3 2.8 86.9 December 102 -0.5 -0.5 102.3 Total 1032 438.3 403.2 588.8 147 EPA Export 01-06-2010:03:55:59
5361- Kilmainhamwood Compost Facility Extension- EIS The surface water runoff drainage system is discussed in more detail in Section 8.3 of the water section of this report. 9.4.2.5 Wind The closest synoptic weather station with the capability of measuring wind and that has been in operation for at least 30 years is the Clones Synoptic Station, which is approximately 50km northwest of the existing development site. The wind rose for the Clones Synoptic Station shows that the prevailing winds are from the southwest (See Appendix 9.2). The mean wind speed at Clones Synoptic Station is 7.9 knots. This value is also applied to the existing composting facility site. 9.4.3 Potential Impacts On a local scale, the climate will not be altered by the proposed development of an extension to the existing composting facility. Composting is a degradation process that would occur naturally and therefore the production of carbon dioxide from this process is not considered to contribute to global greenhouse gas levels. Also the composting of these materials will ensure that these materials are not sent to landfill thereby reducing methane generation due to anaerobic decomposition. 9.4.4 Mitigation Measures As there will be no significant impact on the local or global climate, there are no mitigation measures proposed other than the operation of the facility to BAT guidelines. For inspection purposes only. Consent of copyright owner required for any other use. 148 EPA Export 01-06-2010:03:55:59
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5361- Kilmainhamwood Compost Facility Extension- EIS<br />
At the <strong>compost</strong>ing <strong>facility</strong> area, approximately 56% of the total annual rainfall is recorded during the<br />
winter period (October – March). This amount of precipitation (including snow) will normally be<br />
associated with more prolonged Atlantic frontal weather depressions passing over the region compared<br />
to the summer.<br />
9.4.2.4 Evapotranspiration and Effective Rainfall<br />
The nearest meteorological station with evapotranspiration measuring equipment is located at the<br />
Clones Synoptic Station. Evapotranspiration is the return of water vapour to the atmosphere by<br />
evaporation from land and by the transpiration of plants, generally measured from a short-grass<br />
covered surface (such as a permanent pasture) adequately supplied with water. Evaporation is the<br />
return of water vapour to the atmosphere by evaporation from a free water surface such as a pan of<br />
water, known as a “Class A Pan”, fitted with a depth measuring gauge. The evapotranspiration figures<br />
for the Clones Synoptic Station are detailed in Table 9.10.<br />
It can be noted that evapotranspiration is very low during winter months, when plant growth is minimal.<br />
The vast majority of evapotranspiration during winter months is attributable to direct evaporation from<br />
ground surfaces. During summer months the rate of evapotranspiration increases and often exceeds<br />
the monthly rainfall. This is due to increased free evaporation from the surface and from transpiration<br />
from leaves and plants.<br />
Using the rainfall data calculated for the site in Table 9.9 and the potential evapotranspiration data for<br />
the nearest synoptic station, i.e. Clones Synoptic Station, the effective rainfall for the subject site can be<br />
calculated. Table 9.10 also shows the effective rainfall to the site. Any rain falling on the site will<br />
infiltrate to the ground, evaporate from the surface or become surface water runoff.<br />
Table 9.10 Hydrological Data for the Development Site<br />
Month Rainfall (mm)<br />
For inspection purposes only.<br />
Consent of copyright owner required for any other use.<br />
Potential Evapo-<br />
transpiration (mm)<br />
Actual Evapo-<br />
transpiration (mm)<br />
(PE x 0.92)<br />
Effective Rainfall<br />
(mm)<br />
January 108 2.4 2.2 105.8<br />
February 74 14.6 13.4 60.9<br />
March 78 29.9 27.5 50.9<br />
April 65 51.7 47.6 17.6<br />
May 70 72.1 66.3 3.9<br />
June 67 79.8 73.4 -6.2<br />
July 64 74.1 68.2 -4.0<br />
August 86 58.5 53.8 31.7<br />
September 89 35.9 33.0 55.6<br />
October 99 16.8 15.5 83.3<br />
November 90 3 2.8 86.9<br />
December 102 -0.5 -0.5 102.3<br />
Total 1032 438.3 403.2 588.8<br />
147<br />
EPA Export 01-06-2010:03:55:59