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WSP11669
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Last modified
1/26/2010 3:18:27 PM
Creation date
10/12/2006 5:06:03 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8149.100
Description
Miscellaneous Small Projects and Project Studies - NRCS-Ft Lyon Canal Co Limestone Graveyard Creeks
State
CO
Basin
Arkansas
Water Division
2
Date
9/1/1996
Author
Bent Soil Conservati
Title
Limestone-Graveyard Creeks Watershed Bent County Colorado Prowers County Colorado Watershed Plan and Environmental Assessment
Water Supply Pro - Doc Type
EIS
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<br />0553 <br /> <br />aqu~=ic life standard. The increase in dissolved selenium is similar <br />to =ie total selenium concentration trend. <br /> <br />The ~aximum selenium concentration detected in fish from the stream <br />sites was 18.5 micrograms/gram in a sample of common acarp from the <br />Arka~sas River near Lamar, Colorado guaging station. 2/ Five species <br />of :ish in the Arkansas River had selenium concentrations ranging from <br />2.1 co 18.5 micrograms/gram. Three species in the tributaries had <br />sele~ium concentrations ranging from 3.6 to 16.9 micrograms/gram. All <br />but 3 of the 59 total fish samples exceeded the 85th percentile <br />nat~onal baseline for selenium in fish (2.45 micrograms/gram dry <br />weiqit), and 21 of the samples had concentrations exceeding the range <br />asscciated with reproductive failure in bluegill. About one-half of <br />the samples had selenium concentrations that exceeded the dietary <br />concentration known to increase the rate of mortalities and deformities <br />in ~allard embryos. Selenium levels in aquatic plants exceeded <br />accs?table dietary limits of avion species. <br /> <br />Sele~ium concentrations in surface water was 1 microgram/liter in <br />Pue~lo Reservoir upstream from the project area. Data from EPA, STORET <br />dataoase, indicates that the stretch of the Arkansas River from below <br />Joh~ Martin Reservoir to Lamar, Colorado, has significant higher levels <br />of selenium. 117 Samples taken indicated average total selenium <br />concentration increases from 7.2 micrograms/liter to 19.7 <br />mic~ograms/liter between the two gage stations. The mean value of 19.7 <br />mic~ograms/liter total selenium was determined using 96 values from <br />1962 to 1994. <br /> <br />Add~tional USGS outflow data from John Martin Reservoir indicates a <br />tre~d in increased selenium concentrations. Data from 1980 and 1981 <br />tha= was used with comparison data from 1988 through 1993 indicates <br />tha= dissolved selenium is increasing by .2 micrograms/liter annually. <br />The trend indicates that selenium standards for agriculture use, 20 <br />mic~ograms/liter, will be exceeded in the near future. <br /> <br />Alt~ough the project was not formulated to reduce other toxic trace <br />ele~ents or heavy metals, project action will help reduce those <br />proclems and improve water quality. Dissolved uranium levels of the <br />Arkansas River are also increasing. Uranium ingested by humans and <br />wildlife goes to both the kidneys and bone. It is a chemical poison to <br />the kidneys. Kidney inflammation and failure can occur. <br /> <br />Sam~ling of the Arkansas River from Manzanola to Lamar found that <br />dissolved uranium increases at a much higher rate than in the upper <br />reaches. An abrupt increase in dissolved uranium is observed along the <br />sec=~on of river where flow is greatly reduced because of extensive <br />dive=sions for irrigation and the remaining flow is largely composed of <br />irr~gation return water. Water samples in this section of river are <br />more enriched in dissolved uranium compared to the average <br />concentration found in water outside the irrigated areas. <br /> <br />The mean concentration of uranium in ground water was 19.4 micro <br />gra~s/liter for uranium in the Lamar Quadrangle of Southeastern <br />Colorado (825 samples). Wells of less than 100 feet depth were' <br /> <br />15 <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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