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Last modified
1/26/2010 12:27:05 PM
Creation date
10/11/2006 9:52:03 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8143
Description
John Martin Reservoir
State
CO
Basin
Arkansas
Water Division
2
Date
1/1/1966
Title
Available Data at Colorado State University for the Arkansas Valley of Colorado
Water Supply Pro - Doc Type
Data
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<br />" <br /> <br />o <br />, .~) <br /> <br />,..'-. <br />..-' <br /> <br />~ <br />.... <br />N <br /> <br />STUDIES OR ANALYSES CONDUCTED BY COLORADO STATE <br />UNIVERSITY ON 'tHE ARKANSAS VALLEY OF COLORADO <br /> <br />Physical Relationship Between Surface and Ground Water - In 1961 <br />a cooperative study with USGS and Colorado State University <br />personnel was initiated and funded by the Colorado Natural Resources <br />Department under the direction of Dr. Clark. The purpose of the <br />study was to determine physical relationship between surface and <br />ground water for a hydraulically connected stream-aquifer system <br />such as the South Platte or Arkansas River valleys, The La Junta to <br />Las Animas reach of the Arkansas was selected as a pilot sturly area <br />because the physical system appeared to contain most of the variables <br />and had fairly good records. The multiple I'egression,crop consump- <br />ti ve use, phreatophyte use, and water exchange analyses as described <br />below were all developed as part of the overall study. Funding in <br />1963 was transferred to the Colorado Water Consel"vation Board. <br /> <br />Multiple Regression Analyses - Over 40 regression analyses were <br />made using river gain between La Junta and Las ,\nimas as the depen- <br />dent variable and prf'cipitation, applied irrigation water, pumped <br />water, eonsurnptive US" by phreatophytes, and combinations of these <br />parameters as independent variables. It wa;; hoped that the regression <br />coefficients would indicat.' the physical significance of each variable <br />but the high correlation betwL'cn independent variables often caused <br />the regression coefficient to havc a value that could not be explained <br />physically. This technique did indicate some valuable guidelines in <br />the overall hydrologic anlyses, but was disappointing as a tool to <br />determine Just how much each independent variable affected river <br />gain. River gaIn was defined as outflow from a reach plus diversions <br />in the reach minus inflow and had both positive and negative values. <br /> <br />Consumptive Use Analyses - Estimates of the consumptive use by <br />crops and the nonbeneficial use by phreatophytes were made using the <br />Colorado Agricultural Statistics data for historic county acreages for <br />individual crops, the windshield survey data for 19/,1, and phreatophyte <br />data from the respective field study. The Blaney-Criddle technique <br />was used to compute the consumptive use. Monthly values of the <br />consumptive use were computed for the period 10 39-1962. <br /> <br />Time Series Analyses of Hiver' Flows - An extensive effort was made <br />to determine if there was a time series relationshil' for river flows at <br />Canyon City, Pueblo, Nepesta or La Junta WIth the river gain. Of <br />course, the annual runoff cycle was quiet evident and there was some <br />indication of a fi ve year cycle. Cycles of greater length or ha ving a <br />period less than twelve months were not core lusive although there <br />appeared to be a time lag relationship between river flow and river <br />gain. <br />
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