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Temperature:
Temperature changes can affect all aquatic life. For example, warmer
water holds less dissolved oxygen (D.O.) than cold water and triggers
higher plant growth and respiration rates. The lowered oxygen levels
of warmer waters are further reduced when more plants die and decay.
Although most aquatic life has adapted to survive within a range
of water temperatures, some fish species (trout, for example), require
cooler waters. Temperatures over 78 degrees F, for example, are
usually fatal to brook trout, which need waters in the range of
55-65 degrees F. The metabolic rate of organisms, or the rate at
which they convert food into energy, also increases with higher
water temperatures, resulting in even greater demands on oxygen.
Turbidity:
Water clarity is one of the most obvious measures of water quality.
Turbidity can be a useful indicator of runoff from construction
sites, fields, logging activity, industrial discharges, stream bank
erosion, and other sources. All streams have background turbidity,
or a baseline standard for a natural amount of turbidity. Fish and
aquatic life that are native to streams have evolved over time to
adapt to varying levels of background turbidity. Turbidity is measured
in NTU's or Nephelometeric Turbidity Units, which is a measure of
the amount of light scattered by suspended material in the sample.
The more turbid the water is the higher the turbidity level and
NTU's will be. For example, many of our local streams will run on
the average of <10 NTU or > 21.5" of visibility. A water
sample having visibility of 9.6" will have a value of 30 NTU's.
Very turbid water with visibility of 2.5" would have a value
of 240 NTU.
Relational Trends of Freshwater
Fish Activity to Turbidity Values and Time: With values exceeding
10 NTUs for a few hours, fish start to show signs of stress. For
a few days, we see reduced feeding rates and coughing rates. For
a few weeks, long-term reduction in feeding success. With values
exceeding 100 NTUs for a few hours, fish begin to show stress. For
a few days, we see reduced feeding rates and increased respiration.
For a few weeks, delayed hatching rates and long term reduction
in feeding success. For a few months, death usually occurs.

Dissolved
Oxygen and Percent Oxygen Saturation: Both aquatic plants
and animals depend on dissolved oxygen (D.O.) for survival. D.O.
concentrations are influenced by many factors including water temperature,
the rate of photosynthesis, the degree of water turbulence or wave
action, and the amount of oxygen used by respiration and decay of
organic matter. Both plants and animals depend on dissolved oxygen
for survival. Lack of dissolved oxygen can cause aquatic animals
to quickly leave the area or face death. Under low-oxygen conditions,
the aquatic animal community changes quickly. Under extreme conditions,
lack of oxygen can kill aquatic plants and animals. Measuring dissolved
oxygen is probably the most significant water quality test to determine
the suitability of a stream for fish and many other aquatic organisms.
Factors affecting
oxygen levels: Oxygen is removed from the water by respirations
of living organisms including fish, bacteria, fungi, and protozoans;
by the decay process of organic matter; and by chemical reactions.
Water temperature and atmospheric pressure affect the capacity of
water to hold dissolved oxygen. Cold water at high atmospheric pressure
holds more dissolved oxygen than warm water at low atmospheric pressure.
Oxygen levels also are affected by the degree of light penetration
(turbidity, color, and water depth) and the degree of water turbulence
or wave action. D.O. is reported as milligrams of oxygen per liter
of water (mg/L) which can be called parts by weight per million
(ppm). Different aquatic organisms have different oxygen needs.
Trout and stoneflies, for example, require high oxygen levels. Trout
need water with at least 6 mg/L D.O. Warm water fish like bass and
bluegills survive nicely at 5 mg/L D.O. and carp and bloodworms
can survive on less than 1 mg/L D.O.
Oxygen Saturation:
Saturation is the limit of how much oxygen water can hold under
certain conditions.
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