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<br />third resistor-capacitor network. Thus, 1nthe Yuma Valley area <br />the model includes a three layer network so that the effects of <br />water level declines on the gravity drains can be evaluated in <br />the overlying fine-grained sediments. The effect of any pumping <br />regimen imposed on the grounw\ater system can be readily de- <br />termined; such as, regional water level decline, changes in <br />ground,mter storage (including Yuma Valley), depletion of flo" <br />in the gravity drains. It was assumed that both the ~ravity <br />drainage and wa~er from Dumped drainage wells would be potentially <br />salvageable. <br /> <br />The southern boundary of the model, more than 30 miles south <br />of Sall Luis, is simulated by taking account of the ability of <br />the sediments to transmit ,"ater in response to changes ,in 'vater <br />level. The fault zone, passing through the Yuma Hesa across <br />which head differences of about 30 feet occur, is modeled as <br />a zone of greatly reduced transmissivity., <br /> <br />? <br /> <br />.....; <br /> <br /> <br />, <br />; <br />, , <br />,I <br /> <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />i <br />I <br />, <br />I <br />I <br />