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Stormwater
Problems Here is how the Federal Highway Administration described the problem in Klingle in 1991:
The problem in Klingle Valley is largely about stormwater runoff. Klingle Creek is a stream about 1/2 mile long which discharges into Rock Creek near Porter Street. The Klingle watershed is about 320 acres, much of it impervious surfaces. This means that when there are heavy rains, the water goes into the valley almost immediately, flash flooding the creek, causing massive erosion of the creek and the roadbed. Although this is a big deal for Klingle Stream - each time there are big rains it scours the stream - it is a far bigger deal for Rock Creek. This water is hotter than the natural stream water, and depleted of oxygen, and comes down way to fast, carrying all sorts of sediment and other junk with it. |
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The chief pollutants are dirt (which has an
enormous impact on biological oxygen demand in streams, which causes
eutrophication), pollen and other organic stuff (ditto), bird and other
animal waste (ditto); heat (drives down the ability of water to carry
dissoved oxygen), deposited air pollution (e.g., sulfates, acid rain, misc
toxics), and then auto-related oils and gunk.
Klingle is different from other DC stream valleys in that it is too narrow to provide for a generous buffer area to filter and slow this road stormwater runoff. A typical city block generates 9 times more runoff than a woodland area of the same size. See more about the urban runoff problem from the EPA http://www.epa.gov/OWOW/NPS/facts/point7.htm |
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