Recharge properties of the Tucson Basin aquifer as reflected by the distribution of a stable isotope
The Tucson Basin is southeastern Arizona is a semi-arid alluvial basin. Winter precipitation is derived principally from the Pacific Ocean, and summer precipitation originates mostly from the Gulf of Mexico. Previous investigations have noted that the isotopic composition of the two rainy seasons an...
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| Language: | en |
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The University of Arizona.
1979
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| Online Access: | http://hdl.handle.net/10150/191686 |