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Lakes and Watercourses

Lakes and Watercourses

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Light conditions<br />

Introduction<br />

Light conditions are crucial for the survival of many organisms. Water<br />

quality in this respect is assessed on the basis of absorbency readings<br />

taken from filtered water at a wavelength of 420 nm in a photometer or<br />

equivalent readings taken using a colour comparator, using brownishyellow<br />

platinum chloride as a reference. A high water table, eg, in bogs<br />

<strong>and</strong> marshes, results in run-off with a high humus content <strong>and</strong> hence a<br />

higher colour figure. Various chemical, photochemical <strong>and</strong> biological<br />

processes cause a certain amount of discoloration. This means that lakes<br />

with a long retention time are less discoloured than those with rapid<br />

turnover. From some points of view, a high concentration of humic<br />

matter is advantageous, since it provides scope for complexing, which<br />

reduces the toxicity of metals.<br />

The turbidity of the water is assessed by analysing light dispersion<br />

measured according to the FNU scale. These readings quantify the<br />

particulate content of the water in the form of clayey matter as well as<br />

organic matter such as humus floccules, plankton etc.<br />

Turbidity is determined electronically using a turbidimeter in<br />

accordance with the Swedish st<strong>and</strong>ard. Particles in the water scatter light<br />

<strong>and</strong>, after calibration, the intensity of this light is used as a measure of<br />

turbidity. One complication is that readings are affected by the concentration<br />

as well as the nature of the particles. The turbidity of natural<br />

running water is mainly caused by inorganic particles. The main source<br />

of material like this, which causes turbidity, is probably erosion.<br />

Inorganic matter has a high density <strong>and</strong> therefore sediments fairly<br />

quickly. <strong>Lakes</strong> thus serve as clarification basins, where the predominant<br />

cause of turbidity is usually organic matter.<br />

Measuring the Secchi depth of lakes gives an indication of the optical<br />

characteristics of the water. Secchi depth readings are taken using a<br />

Secchi dish in situ, which indicates the overall effects of water colour <strong>and</strong><br />

turbidity on light penetration. The Secchi depth thus gives a direct,<br />

simple measure of the optical characteristics of the water. It is generally<br />

considered that the Secchi depth represents the depth reached by<br />

approximately 10 per cent of natural light. A Secchi depth figure can be<br />

32

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