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The area is underlain by the C aquifer and Redwall-Muav aquifer. The C aquifer is a water-table aquifer, with a depth of up to 1500 feet to the water table and is dry in the west, except for perched water-bearing zones. It is underlain by the Redwall-Muav, confined and up to 3200 feet below the land surface.
In geotechnical engineering, watertable control is the practice of controlling the height of the water table by drainage.Its main applications are in agricultural land (to improve the crop yield using agricultural drainage systems) and in cities to manage the extensive underground infrastructure that includes the foundations of large buildings, underground transit systems, and extensive ...
A study in an arid agricultural region of Arizona [3] showed that, even with a water level recovery of 100 ft after groundwater pumping was stopped, the land surface continued to subside for decades. This is a result of the continued dewatering of aquitards (fine-grain layers that slow the movement of groundwater) from stresses mentioned in the ...
Today, the national forest land in the heart of Arizona’s “Copper Corridor” is scattered with 20 rustic campsites a Historic Arizona mining town backs copper project on land that Native ...
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The lake was initially filled with one billion US gallons (3,800,000 m 3) of water purchased from the Central Arizona Project. Evaporation and other water losses of 1.7 million US gallons (6,400 m 3) per day are compensated through additional purchase of CAP water, exchanges of reclaimed water, and long-term storage credits. Seepage losses are ...
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