Lakes and Watercourses

Lakes and Watercourses Lakes and Watercourses

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concentrations. Using accepted terminology, the classes correspond to oligotrophy (1), mesotrophy (2), eutrophy (3 and 4) and hypertrophy (5). There is good reason to define a further characteristic sub-group with concentrations below 6 µg/l within the oligotrophic range. This group represents ultra-oligotrophy. Total nitrogen is more variable during the season than total phospho- TABLE 3. CURRENT CONDITIONS: concentration of total nitrogen in lakes (µg/l) Class Description Concentration May – October 1 Low concentrations ≤ 300 2 Moderately high concentrations 300 – 625 3 High concentrations 625 – 1.250 4 Very high concentrations 1.250 – 5.000 5 Extremely high concentrations > 5.000 rus and is therefore unsuitable for assessments based on concentrations in August. Inorganic nitrogen (nitrate + ammonium) peaks markedly in late winter and organic nitrogen reaches a peak in the summer. It is therefore difficult to describe a general pattern of variation for total nitrogen. TABLE 4. CURRENT CONDITIONS: ratio of total nitrogen/ total phosphorus in lakes Class Description Ratio June – September 1 Nitrogen surplus ≥ 30 2 Nitrogen – phosphorus balance 15 – 30 3 Moderate nitrogen deficit 10 – 15 4 Large nitrogen deficit 5 – 10 5 Extreme nitrogen deficit < 5 The assessment scale is intended to group concentrations that are typical of Swedish lakes and is not related to biological/microbial effects. The scale refers to the mean value during June – September over one year based on monthly readings taken in the epilimnion or, if only one sample is taken, surface water (0.5 m). The ratios are weight-based and 21

show the availability of nitrogen in relation to phosphorus in lakes. In class 1 the availability of phosphorus alone governs production; in class 2 there is a tendency for accumulation of cyanobacteria (”bluegreen algae”) in general; in class 3 the occurrence of nitrogen fixation and specific nitrogen-fixing cyanobacteria is likely; in class 4 nitrogen fixation is highly likely but cannot fully compensate for the nitrogen deficit, and in class 5 the nitrogen deficit is extreme and fixation is unable to compensate. TABLE 5. CURRENT CONDITIONS: area-specific loss of total nitrogen, watercourses (kg N/ha, year) Class Description Area-specific loss 1 Very low losses ≤ 1.0 2 Low losses 1.0 – 2.0 3 Moderately high losses 2.0 – 4.0 4 High losses 4.0 – 16.0 5 Very high losses > 16 Area-specific losses refer to the monitoring of concentrations 12 times a year over three years and recorded or modelled water flow per 24-hour period. It may be necessary to monitor concentrations more frequently in small watercourses. 24-hour water flow figures are multiplied by the corresponding concentrations obtained using linear interpolation between readings. The 24-hour transport figures thus obtained are accumulated to give annual figures and show area-specific losses after division by the area of the catchment. Nitrogen loss includes input from all sources upstream of the monitoring point, which classifies the total area-specific input from the catchment to lakes and seas, for example. The scale is also intended to be used to assess losses from all types of soil in comparison with normal losses from different types of land use. Known input from point sources can be deducted to gain a better picture of diffuse nitrogen losses. Class 1 represents normal leaching from mountain heaths and the poorest forest soils. Class 2 shows normal leaching from non-nitrogensaturated forest soils in northern and central Sweden. Class 3 contains losses from unaffected bog/peat land and affected forest soils (eg, leaching from certain clear-cut areas), as well as leaching from arable soils (unfertilised seeded grassland). Class 4 shows common leaching 22

show the availability of nitrogen in relation to phosphorus in lakes.<br />

In class 1 the availability of phosphorus alone governs production; in<br />

class 2 there is a tendency for accumulation of cyanobacteria (”bluegreen<br />

algae”) in general; in class 3 the occurrence of nitrogen fixation <strong>and</strong><br />

specific nitrogen-fixing cyanobacteria is likely; in class 4 nitrogen fixation<br />

is highly likely but cannot fully compensate for the nitrogen deficit, <strong>and</strong><br />

in class 5 the nitrogen deficit is extreme <strong>and</strong> fixation is unable to<br />

compensate.<br />

TABLE 5.<br />

CURRENT CONDITIONS: area-specific loss of total nitrogen,<br />

watercourses (kg N/ha, year)<br />

Class Description Area-specific loss<br />

1 Very low losses ≤ 1.0<br />

2 Low losses 1.0 – 2.0<br />

3 Moderately high losses 2.0 – 4.0<br />

4 High losses 4.0 – 16.0<br />

5 Very high losses > 16<br />

Area-specific losses refer to the monitoring of concentrations 12 times<br />

a year over three years <strong>and</strong> recorded or modelled water flow per 24-hour<br />

period. It may be necessary to monitor concentrations more frequently in<br />

small watercourses. 24-hour water flow figures are multiplied by the<br />

corresponding concentrations obtained using linear interpolation between<br />

readings. The 24-hour transport figures thus obtained are accumulated<br />

to give annual figures <strong>and</strong> show area-specific losses after division by<br />

the area of the catchment.<br />

Nitrogen loss includes input from all sources upstream of the monitoring<br />

point, which classifies the total area-specific input from the catchment<br />

to lakes <strong>and</strong> seas, for example. The scale is also intended to be used<br />

to assess losses from all types of soil in comparison with normal losses<br />

from different types of l<strong>and</strong> use. Known input from point sources can be<br />

deducted to gain a better picture of diffuse nitrogen losses.<br />

Class 1 represents normal leaching from mountain heaths <strong>and</strong> the<br />

poorest forest soils. Class 2 shows normal leaching from non-nitrogensaturated<br />

forest soils in northern <strong>and</strong> central Sweden. Class 3 contains<br />

losses from unaffected bog/peat l<strong>and</strong> <strong>and</strong> affected forest soils (eg,<br />

leaching from certain clear-cut areas), as well as leaching from arable<br />

soils (unfertilised seeded grassl<strong>and</strong>). Class 4 shows common leaching<br />

22

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