
High concentrations of sediment in a river cause water-quality problems. Fine sediments (clays and silts) increase the turbidity of the water. Turbidity is a measure of the clarity of the water: the more turbid water is, the less clear it is. Turbidity may be a problem for fish and other aquatic life, such as sight-feeding fish and mussels. If fish spawning beds are covered with sediment, populations may be reduced. Chemical contaminants from human activities can also be bound to sediments, including heavy metals, polychlorinated biphenyls (PCBs), and other organic chemicals.
Nutrients tend to build up within an impounded system more quickly than in free-flowing systems. High nutrient levels in impoundments can lead to eutrophication of the impoundment. This means that the water contains enough nutrients to support nuisance growths of aquatic plants and algae blooms. When these algae blooms die, the decay process uses up oxygen dissolved in the water, reducing the amount of oxygen available to fish and other aquatic life. The turbidity caused by decaying algae and suspended sediment can cause problems for other plants. Plants rely on sunlight reaching them to carry out photosynthesis. Turbidity causes problems for fish, not allowing them to be able to see their prey and predators. Turbidity also promotes typically undesirable species, such as carp, which can tolerate lower dissolved oxygen conditions and exacerbate turbidity problems themselves by stirring up the bottom sediments.
The upper layer of the still water in an impoundment also tends to have
higher temperatures than in a free-flowing system. This increase in temperature
decreases the amount of dissolved oxygen present in the water. Also, the
still water of an impoundment mixes less with the air above than free-flowing
rivers, reducing the amount of oxygen added by contact with the air. This
increase in temperature and decrease in dissolved oxygen affects the quality
of the water in the impoundment and also affects the quality of the river
downstream. Similarly, water–quality problems caused by any other dissolved
chemical in the water will affect the impoundment and the river downstream
of the impoundment.
Increases in the sediment load of a river can lead to increases in the
amounts of nutrients, such as nitrogen and phosphorous because these nutrients
are commonly bound to sediments. Higher levels of nutrients may allow greater
biological productivity, but eventually these organisms die, and their
decay uses up some of the available dissolved oxygen. If all the oxygen
is used up, the decay continues through other biological mechanisms that
give off unpleasant chemicals, such as methane (rotten egg smell) and hydrogen
sulfide (sewer gas smell). Some of these gases can cause organic sediments
to rise to the surface and form unsightly scum, which also reduces light
penetration. High nutrient levels can lead to poor water quality.
The removal of a dam may lead to improvements in the water quality of the former impounded area and to the river downstream. Removing the dam will flush out the warm, low dissolved oxygen, high nutrient water from the impoundment. The water quality in the restored area should return to that of the river upstream from the impoundment. The initial drawdown of the impoundment (prior to the physical removal of the dam), however, may cause temporary water–quality problems downstream until the flushing is complete.
URL: http://www.ies.wisc.edu/research/wrm00/educqual.htm