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WSP06567
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Last modified
1/26/2010 2:23:21 PM
Creation date
10/12/2006 1:43:10 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.750
Description
San Juan River General
State
CO
Basin
San Juan/Dolores
Water Division
7
Date
5/1/1986
Author
Wheeler and Assoc
Title
Documentation for Mancos River Hydrology Analysis - Historic and Virgin Flow Conditions - May 1986
Water Supply Pro - Doc Type
Report/Study
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<br />DOD378 <br /> <br />. <br /> <br />Water Requirements in New Mexico," New Mexico State Engineer - Techni- <br /> <br /> <br />cal Report 32, 1965. The net potential consumptive use of alluvial ground- <br /> <br /> <br />water, corrected for effective precipitation, was estimated and is summa- <br /> <br />rized below: <br /> <br />Reach <br /> <br />West, Middle & East Mancos <br />Rivers to Weber Canyon <br /> <br />Net <br />Potential <br />Consumptive <br />Use <br />(ac-ft! ac ) <br /> <br />Area <br />( acres) <br /> <br />Potential <br />Stream <br />Loss <br />(ac-ft!yr ) <br /> <br />3.2 <br /> <br />280 <br /> <br />900 <br /> <br />Weber Canyon to Navajo Canyon <br /> <br />3.4 <br /> <br />520 <br /> <br />1,800 <br /> <br />Navajo Canyon to Highway 666 <br /> <br />3.5 <br /> <br />590 <br /> <br />2,100 <br /> <br />Highway 666 to Aztec Wash <br /> <br />3.6 <br /> <br />690 <br /> <br />2,500 <br /> <br />Totals <br /> <br />2,080 <br /> <br />7,300 <br /> <br />Johnson Canyon to Highway 666 <br /> <br />3.5 <br /> <br />800 <br /> <br />2,800 <br /> <br />. <br /> <br />C. <br /> <br />Estimated Stream Losses. <br /> <br />Stream losses for the reach between Johnson Canyon and Highway 666 <br /> <br /> <br />were estimated by two separate methods as described above. In the first <br /> <br /> <br />method, a comparison was made between gaged flows at Johnson Canyon <br /> <br /> <br />versus gaged flows at Highway 666. By this method it appears that the <br /> <br /> <br />average stream loss is about 2,100 acre-feet per year. Tributary inflow <br /> <br /> <br />between the two gages may have been significant during the spring months, <br /> <br />resulting in a stream loss estimate that is too low. <br /> <br />In the second method, evapotranspiration losses were estimated through <br /> <br /> <br />use of aerial photographs of the riparian phreatophyte areas, together <br /> <br /> <br />with calculations of potential consumptive use by the phreatophytes. By <br /> <br /> <br />this method, the stream loss for this reach was estimated to be 2,800 <br /> <br /> <br />acre-feet per year. The use of potential consumptive use calculations <br /> <br />. <br /> <br />-32- <br /> <br />j; _'c. <br />
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