Stream Water Quality Monitoring at Wind Cave
Since December of 1998, Resource Management staff have been collecting monthly water quality parameters on the three perennial park streams (Beaver, Highland, and Cold Spring Creeks.) The parameters gathered include dissolved oxygen, oxygen saturation, temperature, pH, conductivity, specific conductivity, salinity, and turbidity. These parameters are indicators to monitor the condition of the water. Having many years worth of data provides us with a baseline of stream condition, and will enable us to determine if there are any changes in the quality of the water. Currently the overall heath of the park streams is good, with no parameter being suspect.
|
Stream
|
Oxygen (mg/L)
|
Temp (F)
|
pH
|
Conductivity (uhos/cm)
|
Turbidity (ntu)
|
| Beaver |
11.25
|
46.2
|
8.7
|
334.6
|
7.22
|
| Highland |
10.95
|
49.9
|
8.7
|
197.7
|
3.88
|
| Cold Spring |
10.74
|
47.3
|
8.4
|
395.8
|
2.64
|
|
|
|
|
|
|
Average parameters of park streams
In an attempt to keep this short, a description of only five of the eight parameters is included.
Oxygen is measured in its dissolved form in milligrams per liter (mg/L), which is the amount of oxygen in a liter of water. Sources of oxygen-consuming pollutants include wastewater from sewage treatment plants, storm water runoff from farmland or urban streets, feedlots, and failing septic systems.
Temperature affects the oxygen content of the water; the rate of photosynthesis by aquatic plants; the metabolic rates of aquatic organisms; and the sensitivity of organisms to toxic wastes, parasites, and diseases. Unnatural causes of temperature change include removal of shading stream bank vegetation, impoundments, and storm water.
Water Quality Monitoring at Cold Spring Creek
pH is a term used to indicate the alkalinity or acidity of a substance as ranked on a scale from 1.0 to 14.0. Acidity of water increases as pH gets lower. pH affects many chemical and biological processes in the water. Causes of acid change include atmospheric deposition (acid rain), surrounding rock, and wastewater discharges.
Conductivity is a measure of the ability of water to pass an electrical current, and is useful as a general measure of stream water quality. Each stream tends to have a relatively constant range of conductivity that, once established, can be used as a baseline for comparison with regular conductivity measurements. Significant changes in conductivity could then be an indicator that a discharge or some other source of pollution has entered a stream.
Turbidity is a measure of water clarity. Higher turbidity increases water temperatures because suspended particles absorb more heat. This, in turn, reduces the concentration of dissolved oxygen because warm water holds less oxygen than cold. Higher turbidity also reduces the amount of light penetrating the water, which reduces photosynthesis and the production of oxygen. Regular monitoring of turbidity can help detect trends that might indicate increasing erosion in the watershed.