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Last modified
1/26/2010 2:58:36 PM
Creation date
10/12/2006 4:17:37 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8111.805
Description
Arkansas River Compact Administration - Keesee Ditch
Basin
Arkansas
Date
1/1/1986
Author
HRS Engineering
Title
Keesee Ditch Change of Water Rights Vol 1 - Historical Operation of Kessee Ditch
Water Supply Pro - Doc Type
Publication
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<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 /> <br />Effective precipitation is the amount of precipitation falling during the growing <br />season which supplies water for evapotranspiration, or in essence, reduces the <br />irrigation requirements. It was calculated using Lamar precipitation data and <br />a commonly used analysis method outlined in Technical Release No. 21 (U.S. Soil <br />Conservation Service, 1970). This method incorporates monthly rates of potential <br />evapotranspiration and monthly precipitation to estimate the amount of <br />precipitation which becomes available for consumptive use after accounting for <br />surface runoff and deep soil percolation losses. Precipitation data for Lamar <br />used in the analysis are included in Appendix B and estimates of effective <br />precipitation for each of the crops are included in Appendix C. <br /> <br />Irrigation water requirements for each of the crops were calculated as potential <br />evapotranspirlltion less effective precipitation and are included in Appendix C. <br />The average annual crop irrigation water requirements in acre-feet per acre for <br />the study period were 2.48 for alfalfa, 1.78 for grain corn, 1.51 for grain sorghum <br />and 1.22 for winter grains. <br /> <br />In addition to crop irrigation water requirements, estimates of potential <br />evaporation from wet soils irrigated during the winter months of November to <br />March were made. Soil evaporation takes place at rates dependent on climatic <br />factors until the top few inches of soil dry out. Potential rates of soil evaporation <br />were calculated using the Modified Blaney-Criddle Method and an assumed crop <br />coefficient to represent wet soil conditions. Effective precipitation was determined <br />and irrigation water requirements calculated using the same methods as for crops. <br />Results of this analysis are included in Appendix C. This analysis resulted in an <br />average annual winter irrigation water requirement of 0.08 acre-feet per acre <br />or about one~inch of potential water loss. This estimate appears realistic when <br />factors of low temperatures, intermittant snow cover, and frozen soils are <br />considered. It also correpsonds to the approximate water holding capacity in <br />the top three to six inches of soil, or the expected depth to which drying would <br />occur during an average winter. <br /> <br />Irrigation water requirement rates for the four crops and winter irrigation <br />were combined with acreages and weighted to determine overall monthly and <br />annual irrigation water requirements. Table IV includes these weighted irrigation <br />water requirements in acre-feet per acre. The average annual irrigation water <br /> <br />-9- <br /> <br />~ <br /> <br />)(' <br />
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