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Geologic And Hydrologic Factors Governing ... - Gunnison County

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<strong>Geologic</strong> <strong>And</strong> <strong>Hydrologic</strong> <strong>Factors</strong> <strong>Governing</strong> Impacts Of Development<br />

On The Crystal River Near Marble, Colorado<br />

<strong>Gunnison</strong> <strong>County</strong>, Colorado<br />

5.4 million pounds x<br />

7<br />

1, 000, 000<br />

= 37.8 pounds of N/day<br />

3. With 1 EQR contributing 0.10 lbs of N per day, the allowable pollution load for leaching<br />

fields inflow would be 378 EQR. In the event the creek flow was at 2 cfs, the allowable<br />

number of EQR contributing pollutants to Carbonate Creek would be 756, twice that for a 1<br />

cfs flow.<br />

Taking into consideration the effluent from leaching fields, the cumulative pollutant impact<br />

of NO3-N would impact Carbonate Creek surface flows at a relatively high level of leaching<br />

field density in the Carbonate Creek basin. Direct discharge of effluent to Carbonate Creek<br />

would have a numerically somewhat lower, but similar impact on the quality of Carbonate<br />

Creek. However, with a surface discharge, the impact would also relate to questions of<br />

harmful organisms, such as fecal coliform bacteria and viruses, during times that the sewage<br />

treatment plant malfunctioned.<br />

This example provides a simplified approximate procedure for computing the carrying ca-<br />

pacity of a basin under steady-state future conditions after pollutant inflow become equal to<br />

pollutant outflow.<br />

5.10.4 Impact on the Shale Bedrock<br />

Shale bedrock is characterized as having secondary permeability created by cracks and joints ex-<br />

tending downward with varying distances, but generally no more than about 50 feet. The following<br />

approximate procedure provides a method of estimating the pollutional impact on a bedrock aquifer.<br />

Assuming one such crack or fissure per 10 feet on the average and each crack or joint having a rate<br />

of flow capability of 0.5 gpm, a 209-foot-wide section of the aquifer would have a groundwater flow<br />

capability of approximately 10 gpm, or 14,400 gpd.<br />

951-110.000 Wright Water Engineers, Inc. Page 54

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