The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona

The occurrence of dissolved oxygen concentrations of 4.4 to 7.3 milligrams per liter in ground waters from artesian aquifers within the semi-arid Upper San Pedro basin, Arizona, supports recent research documenting the occurrence of oxygenated ground waters. These findings are in conflict with earli...

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Main Author: DeWald, Lloyd Brian.
Other Authors: Davis, Stanley N.
Language:en
Published: The University of Arizona. 1984
Online Access:http://hdl.handle.net/10150/191815
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-1918152015-10-23T04:37:46Z The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona DeWald, Lloyd Brian. Davis, Stanley N. The occurrence of dissolved oxygen concentrations of 4.4 to 7.3 milligrams per liter in ground waters from artesian aquifers within the semi-arid Upper San Pedro basin, Arizona, supports recent research documenting the occurrence of oxygenated ground waters. These findings are in conflict with earlier hypotheses postulating that dissolved oxygen in recharge waters is rapidly reduced to negligible concentrations by chemical and biochemical processes in the soil and aquifer environments. However, the reported concentrations of dissolved oxygen become theoretically plausible upon consideration of the physical, chemical, and biological processes occurring within the water-soil-aquifer complex of the study area. These processes may also be dominant factors controlling the chemistry of dissolved oxygen in the ground waters of other semi-arid basins similar to the Upper San Pedro basin. 1984 Thesis-Reproduction (electronic) text http://hdl.handle.net/10150/191815 213296788 en Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. The University of Arizona.
collection NDLTD
language en
sources NDLTD
description The occurrence of dissolved oxygen concentrations of 4.4 to 7.3 milligrams per liter in ground waters from artesian aquifers within the semi-arid Upper San Pedro basin, Arizona, supports recent research documenting the occurrence of oxygenated ground waters. These findings are in conflict with earlier hypotheses postulating that dissolved oxygen in recharge waters is rapidly reduced to negligible concentrations by chemical and biochemical processes in the soil and aquifer environments. However, the reported concentrations of dissolved oxygen become theoretically plausible upon consideration of the physical, chemical, and biological processes occurring within the water-soil-aquifer complex of the study area. These processes may also be dominant factors controlling the chemistry of dissolved oxygen in the ground waters of other semi-arid basins similar to the Upper San Pedro basin.
author2 Davis, Stanley N.
author_facet Davis, Stanley N.
DeWald, Lloyd Brian.
author DeWald, Lloyd Brian.
spellingShingle DeWald, Lloyd Brian.
The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
author_sort DeWald, Lloyd Brian.
title The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
title_short The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
title_full The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
title_fullStr The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
title_full_unstemmed The occurrence of dissolved oxygen in ground waters of the Upper San Pedro Basin, Cochise County, Arizona
title_sort occurrence of dissolved oxygen in ground waters of the upper san pedro basin, cochise county, arizona
publisher The University of Arizona.
publishDate 1984
url http://hdl.handle.net/10150/191815
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