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<br />j <br />1 <br />I ,. <br />.. \ .) <br />.1 <br /> <br />calcium-bicarbonate-type water. Moving downstrea~~ chemical <br /> <br />characteristics change, indicating greater proportions of <br /> <br />sodium, m~gnesium. sulfate, and chloride leached from <br /> <br />the geological formations by preci~itation and irrigation <br /> <br />return flow waters. <br /> <br />Tabulated below are ty~ical dissolved solids ranges <br /> <br />for streams within the six subbasins studied in the <br /> <br />Colorado River Basin. <br /> <br /> Subbasin Typical diss01 ved soUds <br /> concentr-atio:1 <br /> Yampa 40 mRIl - 774 m~/l <br /> I-Ihi te 1/ 144 mg/l - 439 r.:g/l <br /> Upper Colorado 25 mg/l - 647 mg/l <br />. I Gunnison 83 " - 1,u10 m~/J. <br />mV/J. <br />\...: " <br />Dolores 200 mg/l 6,0(1) Mgil <br /> San Juan 41 mgll - 5,000 r.:g/l <br /> <br />(b) Biological - For many years the coliform group of <br /> <br />bacteria has been used as a bacterial indicator cf pollution. <br /> <br />High coliform countsID water supplies are presumed to <br /> <br />indicate pres~nce of pathogenic or~~nisms if contamination <br /> <br />from sewage or animal wastes is likely. <br /> <br />In recent years ffilalytical procedures have been <br /> <br />developed whereby coiiform bacteria of fecal origin can be <br /> <br />identified. Fecal coliform tests measure bacteria from <br /> <br />both man and animal. <br /> <br />Typical total coliform data available ..ithin the <br /> <br />Colorado River Bdsin for the period 1953 to 1970 from troe <br /> <br />. <br /> <br />I <br />,--- <br /> <br />11 <br /> <br />Upper .r~aches to lowel~ reaches of ~.~nite River. <br /> <br />J3-I. <br />8 <br /> <br />r- <br /> <br />4~'~ <br /> <br />, , <br /> <br />~ <br />