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Chemical Properties
Chemical measurements include a
wide range of chemicals and chemical properties. Most water chemistry tests
measure concentration, defined as milligrams of chemical per liter of water
(mg/l).
Even the purest water
contains countless chemicals, and it would be impossible to measure all of them.
Water quality studies therefore focus on the chemicals that are most important
for the problem at hand. In agricultural areas, studies measure chemicals found
in manure, fertilizers, and pesticides. In an industrial area studies focus on
measuring chemicals used by the nearby industries.
The following basic parameters
are measured in nearly all studies; petroleum products, metals, industrial
chemicals, pesticides, and herbicides are added when needed.
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Dissolved Oxygen (DO)
Dissolved Oxygen is the
concentration of oxygen dissolved in the water, expressed as milligrams oxygen
per liter water (mg/l). DO is an important measurement of aquatic health, since
aquatic organisms must get all of their oxygen from water. Healthy water bodies
usually have DO levels of 8 mg/l or higher.
Many fish and
macroinvertebrate species are sensitive to low DO levels. For
example, salmonids suffer when the DO drops below 2 to 4 mg/L.
Larval and juvenile fish are even more susceptible to low DO levels (USEPA
1997).
Low DO levels can
have more negative effects than just suffocating fish. Low DO can
cause declines in macroinvertebrate populations which leads to the
starvation of organisms higher in the food chain. Also, low DO
increase anaerobic bacteria that produce gases often associated with
polluted streams.
Oxygen
is introduced into water by two primary mechanisms; transfer from air or
photosynthesis by aquatic macrophtyes.
The transfer of oxygen from the air to water can occur by the following
means:
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Internal
mixing and turbulence
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Wind
mixing
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Waterfalls,
dams, and rapids
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Consumption of DO,
on the other hand, occurs by several mechanisms:
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Carbonaceous
deoxygenation
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Nitrification
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Biological
Oxygen Demand (BOD)
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Sediment
Oxygen Demand
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Respiration
of plants and animals
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Biological Oxygen
Demand (BOD) measures how much oxygen is
consumed by bacteria as they break down pollution and organic matter in the
water. It is measured by observing how much dissolved oxygen levels decrease in
a sealed sample over a 5-day period.
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Nitrate (NO3) and Phosphate
(PO4)
Nitrates and phosphates are nutrients that
come from both natural sources and human activities (fertilizers, detergents,
wastewater). These nutrients determine the productivity of a water body, and are
needed at some level to provide good aquatic habitat. However, pollution from
manure, fertilizer, and wastewater can cause excessive nutrient levels. Too much
nitrate or phosphate causes algae to grow out of control, reducing light and
oxygen for fish.
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pH
pH
is a measure of the acidity of water, and is important in understanding the
chemical balance of the water. pHs below 7 indicate acid conditions, while pHs
above 7 indicate alkaline conditions. pH is a strong determinant of the
solubility and availability of both nutrients and pollutants. Most natural water
bodies will have pHs close to 7, depending on the local geochemistry. Very low
pHs (less than about 6) can come from acid rain, industrial sources, or mine
drainage. Stream organisms cannot tolerate extreme pH values or large
fluctuations in pH. Deviations from close to neutral (7) increase stress
levels and will ultimately decrease species diversity.
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