List of Parameters
Parameter |
Potential
Impacts |
Potential
Causes |
Ammonia-N (NH3-N) |
Elevated levels
of ammonia can injure or kill aquatic life,
such as fish and invertebrates. In fish,
even low concentrations of ammonia can
damage sensitive tissues such as gills,
deplete natural resistances to bacterial
infections, and hinder reproductive
capacities and growth. |
Ammonia occurs
naturally as a by-product of protein
metabolism and decomposition. Ammonia can
also enter a water body from runoff of
fertilizers, livestock waste, and discharges
of untreated sewage and industrial
wastewater. |
Chloride (Cl-) |
Although small
amounts of chlorides are essential to proper
cell function in plants and animals, large
concentrations of chlorides can damage
aquatic life physiology and hinder
reproductive fertility and growth. |
Chlorides occur
naturally from the weathering and erosion of
sedimentary rocks. Agricultural runoff,
industrial wastewater, petroleum industrial
activities, salt water intrusions, and
effluent from wastewater treatment
facilities are sources of chlorides. |
Chlorophyll-a |
Chlorophyll-a,
a photosynthetic pigment found in green
plants, is an indicator of the presence of
algae in water. It is used to monitor the
biological productivity of lakes and
streams. |
Elevated levels
of nutrients could result in an
overabundance of algae. |
Dioxin |
Dioxin is a
family of polychlorinated chemicals. a
carcinogen, it is detrimental to animal and
human health. |
Dioxin is present
in the waste from the paper bleaching
process and from the combustion of
chlorinated compounds. |
Dissolved
Oxygen (DO) |
Oxygen is the
most important component for the survival of
aquatic life. Dissolved Oxygen is
essentially the amount of oxygen available
in water. Low dissolved oxygen can suffocate
aquatic species. |
Elevated levels
of organic nutrients can cause an
overabundance of bacteria and algae, which
depletes oxygen from water. Human-caused
increases in water temperature industrial
discharges can also lower the capacity for
water to hold oxygen. |
E. coli
and Enterococci Bacteria |
Escherichia
coli (E. coli)
and enterococci are bacterial indicator
species for the presence of fecal matter,
pathogenic bacteria, and viruses. E. coli
is the indicator bacteria for
freshwater, while enterococci are used as an
indicator in saltwater. |
Malfunctioning or
failing on-site sewage facilities (OSSFs),
untreated domestic sewage, improper disposal
of grease, and runoff from agricultural and
livestock activities can cause an
overabundance of bacteria and other
pathogenic organisms. |
Flow Instantaneous
Flow (Quantitative) Flow Severity
(Qualitative) |
Flow conditions
affect water quality. Aquatic species are
adapted to specific instream flow patterns.
Low flow events, associated with hot summer
months, can severely alter a stream habitat.
High flow events, such as those associated
with heavy rain, can also disrupt an aquatic
habitat. |
Drought or heavy
rain events can disrupt normal flow
patterns. Impediments such as fallen trees,
beaver dams, or man-made dams can disrupt or
alter in-stream flow. |
Nitrogen Nitrate-N (NO3-N) Nitrite-N (NO2-N) |
An abundance of
nutrients can increase plant and algal
growth. Bacteria use oxygen in the
decomposition of plant matter, which can
reduce dissolved oxygen. Nitrites are an
intermediate form of Nitrogen can cause
brown blood disease in fish by preventing
the transfer of oxygen by hemoglobin.
Nitrites can also adversely affect human
health. |
Nutrient sources
are usually found in runoff from fertilizers
and livestock facilities. They are also
present in the effluent of wastewater
treatment facilities. |
pH |
Aquatic organisms
have evolved to live in a specific range of
pH. Biological and chemical processes can be
altered or affected if the pH drops or rises
over certain thresholds. Fish species cannot
survive if the pH drops below 4 or rises
above 12. |
Runoff from
mining operations and discharges of
industrial wastewater can alter the pH of a
water body. |
Phosphorus Total Phosphate-P |
Most phosphorus
compounds found in water are phosphates.
Orthophosphate is consumed by aquatic plants
and organisms and is considered the limiting
factor for aquatic plant growth. High or
excessive levels of orthophosphate results
in higher yield in growth. Excessive plant
growth can cause eutrophication, (the
natural aging progression of a water body)
which can decrease dissolved oxygen. |
Phosphates occur
naturally from the decomposition of
organisms and the weathering of rock
material. It can also result from fertilizer
runoff. |
Polychlorinated biphenyls (PCBs) |
PCBs are acutely
toxic, and can disrupt endocrine and neural
processes in aquatic life and humans. |
PCBs are found in
dielectric fluids used in transformers,
capacitors, and coolants. |
Salinity |
Salinity is the
measurement of conductive ions in the water.
High levels of sodium sulfate and magnesium
sulfate produce a laxative effect in
drinking water. High levels of total
dissolved solids can cause an unpleasant
taste in potable water. |
Weathering or
erosion of rocks, salt mining, and salt
water intrusions are sources of increased
salinity. |
Secchi
Transparency |
Secchi
transparency is used to calculate the depth
at which natural light can penetrate the
water column. It also used as a measurement
of eutrophication. |
An abundance of
algae and plants or excessive levels of
total suspended solids can decrease the
ability for light to transmit through the
water column. |
Specific
Conductance |
Specific
conductance is the measure of the water’s
capacity to carry an electrical current. It
is indicative of the amounts of total solids
present in a water body. |
The conductivity
of water is increased by the presence of
salt-forming substances such as sulfate,
chloride, and sodium. |
Sulfate (SO42-) |
In the absence of
oxygen and with a pH below 8, bacteria can
reduce sulfate ions to sulfide ions. Sulfide
ions can cause serious and unpleasant odor
problems. Sulfates in sediment can also
alter soil composition and hinder or prevent
growth of native plants. |
Sulfate is
derived from rocks and soils containing
gypsum, iron sulfides, and organic
compounds. Sulfur-containing fossil fuels,
heavy industrial activities, and some
fertilizers are also potential sources for
sulfates. |
Temperature |
The types of
aquatic life that can survive in a water
body are dependent upon water temperature.
Water temperature can affect levels of
dissolved oxygen. Water with a high
temperature has less capacity to hold
oxygen. As the water temperature drops,
cold-blooded animals such as fish can become
more susceptible to pathogenic stress or
shock, which can lead to infections or
death. |
Releases of water
from reservoirs can contribute to drops in
temperature. Temperatures can increase with
the removal of flora from riparian areas or
from the release of heated water from
industrial activities. |
Total
Dissolved Solids (TDS) |
Elevated amounts
of total dissolved solids can be corrosive
to sewer and plumbing fixtures. High TDS may
also affect the aesthetic quality of water. |
Elevated amounts
of TDS occur naturally from salt deposits,
salt water intrusions, and sedimentary rock
high in carbonate. Salt mining, petroleum
exploration, potable water treatments,
wastewater discharges, and chemical,
stormwater, or fertilizer runoff can
increase the amounts of TDS. |
Total
Suspended Solids (TSS) |
An increase in
the amount of total suspended solids can
decrease the ability for light to penetrate
through the water column. This can decrease
the productivity of aquatic plants. As
excessive amounts of TSS settle and become
sediment, benthic habitats can be altered or
destroyed. |
High erosion
events, usually coinciding with the removal
of riparian floral species and severe flow
events, can create excess levels of total
suspended solids. Unsound agricultural
practices can also contribute to soil
erosion into waterways. |