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ISFAPPC04246
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Instream Flow Appropriations
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ISFAPPC04246
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Last modified
3/28/2017 2:32:54 PM
Creation date
10/5/2006 11:15:18 PM
Metadata
Fields
Template:
Instream Flow Appropriations
Case Number
00CW0101
Stream Name
Fourmile Creek
Watershed
Fourmile Creek
Water Division
2
Water District
12
County
Fremont
Instream Flow App - Doc Type
Supplemental Data
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<br />of the time of day the measurement was conducted, and thus do not have a spatial pattern, <br /> <br />'. <br /> <br />The pH in Fourmile Creek was relatively basic, reflecting the geology and <br />morphology of the basin. In the smaller, colder headwater reaches of Fourmile Creek <br />above the town of Cripple Creek, the pH is closer to a neutral pH of 7. As the stream <br />travels downstream, COllecting more ground water and surface runoff, the pH increases to <br />around 8.3 to 8,5. <br /> <br />Hardness (calcium and magnesium). mitigates metal toxicity, As hardness <br />increases, the toxicity of a metal concentration usually decreases. The hardness in the <br />Fourmile Creek Drainage was increased by Ariqua Gulch (via Cripple Creek) and the <br />Carlton Tunnel. The hardness levels of Ariqua Gulch and the Carlton Tunnel are higher <br />than in most Colorado mountain streams. <br /> <br />~,..) <br />;;. <br /> <br />Metal concentrations in Fourmile Creek upstream of Cripple Creek were at or less <br />than detection limits, although iron and manganese were present in the Fourmile Creek <br />headwater reaches, Both Cripple Creek a'nd Carlton Tunnel increased the metal <br />concentrations in Fourmile Creek (Table 3), The highest metal concentrations were found <br />downstream of the Carlton Tunnel. Fourmile Creek metal concentrations were not at <br />levels toxic to fish or macroinvertebrates. <br /> <br />3.1.2 Cripple Creek <br />Cripple Creek and Ariqua Gulch were sampled for the first time in 1995. Ariqua <br />Gulch influenced the water chemistry of Cripple: Creek (Table 4), For example, upstream <br />of Ariqua Gulch, the pH of Cripple Creek was basic, 8.28 and downstream of Ariqua Gulch <br />pH was 7,71. Ariqua Gulch was acidic (pH = 6,33) with a very low alkalinity (6mg/1 CaC03) <br />indicating a low buffering capacity, Hardness and sulfate were very high in Ariqua Gulch <br />compared to a "typical" Colorado mountain stream, Cripple Creek hardness and sulfate <br />concentrations increased downstream, with the largest increase just downstream of Ariqua <br />Gulch. <br /> <br />Metals in Cripple Creek were higher d~wnstream of Ariqua Gl.Jlch compared to <br />upstream (Table 5). However, metal levels decreased as Cripple Creek flowed <br />downstream to the confluence with Fourmile Creek due to dilution and/or precipitation. <br />Cripple Creek metal concentrations were lower at the confluence with Fourmile Creek than <br />upstream of Ariqua Gulch, The copper concentration in Cripple Creek upstream of Ariqua <br />Gulch (18 ugll) exceeded a level of 17.4 ugll known to cause 100% chronic (long term) <br />mortality to brook trout (McKim and Benoit 1974). Downstream of Ariqua Gulch, the <br />copper concentration of 14 ugll approached the ~rook trout chronic value for low hardness <br />waters, However, hardness levels were elevateq so that copper was not toxic. Brook trout <br />are the most sensitive trout species to copper. ' <br /> <br />'''4'\'''' <br /> <br />Metal concentrations in Ariqua Gulch were higher than any other location sampled <br />in the Fourmile Creek Basin by the DOW in' 1995. Cadmium, ml'lnganese and zinc <br /> <br />4 <br /> <br />I <br />I <br />I <br />I <br />I <br />'I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />
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