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HYDERAULIC/CHEMICAL CHANGES DURING GROUND-WATER RECHARGE BY INJECTION.

Ground Water

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Abstract

Ground-water recharge by injection of reclaimed water is a feasible method of improving ground-water quality in the shallow aquifer system in the Palo Alto Baylands along the San Franciso Bay. Ground water was initially more saline than sea water. Reclaimed water was injected at a rate of 10 gallons per minute from June 5, 1980, to July 1, 1980. At the completion of injection, water from an observation well 31 feet from the injection well was 98 percent injected water - in essence, fresh water. An abrupt rise in the water level in the injection well of about 1. 5 feet during the initial injection test was the result of a 3. 5 percent density difference between injected fresh water and saline ground water. The arrival of injected water at observation wells showed the same effect, allowing monitoring of chemical and hydraulic changes entirely through water-level data. Prior to injection the saline ground water was super-saturated withn calcite. Dilution, as injection proceeded, eventually produced an undersaturation of calcite. An increase in well specific capacity indicates that calcite dissolved from the aquifer matrix, improving hydraulic conductivity.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
HYDERAULIC/CHEMICAL CHANGES DURING GROUND-WATER RECHARGE BY INJECTION.
Series title:
Ground Water
Volume
25
Issue:
3
Year Published:
1987
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
First page:
267
Last page:
274
Number of Pages:
8