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Last modified
1/26/2010 2:19:31 PM
Creation date
10/12/2006 1:12:01 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8278.400
Description
Title I - Mexican Treaty
Basin
Colorado Mainstem
Date
2/17/1973
Author
IWBC by Harshbager
Title
Memorandum Report MR-73-1 Appendices, A - Groundwater Conditions in the Colorado River Delta Area, United States and Mexico and Appendix B - Pumping Regimens, Effects and Prediction Analysis
Water Supply Pro - Doc Type
Publication
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<br />APPENDIX B <br /> <br />. <br /> <br />PillIPING REGINENS ,EFFECTS, AND PREDICTION ANALYSIS <br /> <br />INTRODUCTION <br /> <br />In order to assess the effects of pumping from wells now <br />installed and proposed well field plans in Nexico and United <br />States, a series of analog model runs have been conducted by the <br />U. S. Geological Survey Analog ~lodel Laboratory, Phoenix, Arizona. <br />The singular effects for each existing and proposed pumping <br />regimen in United States and Nexico have been studied. Pertinent <br />aspects of these results are reviewed in this Appendix B. <br /> <br />I <br />, <br />, <br />I <br />I <br />I <br />i <br />I <br />, <br />, <br /> <br />,Specifically, the study was to determine the effects of <br />1) United States groundwater pumpage and 2) !--lexican groundwater <br />pumpage, on the magnitude and direetion of underground flol.s <br />across the international boundary in the limitrophe section of <br />the Colorado River and in the Arizona-Sonora boundary seetion <br />(Figure B-1). <br /> <br />Description of Electric Analog Hodel <br /> <br />The geologic and hydrologic features of the groundwater basin <br />have been modeled in an electric analog eovering about <br />2,860 square miles at scales ranging from one node equals <br />1,500 feet to one node equals 6,000 feet and ineludes a total <br />of 16,500 nodes. Two resi stor-capaei tor networl(s are inter- <br />connected at corresponding nodes by resistors that represent <br />the average vertical permeability and distance along the flo1{ <br />path between the wedge and coarse-gravel aquifers. For the <br />current model, the upper layer of fine-grained sediments <br />(shallow aquifer) in the Yuma Vallcy has been simulated with a <br />
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