Water infiltration and percolation at the University of Arizona radioactive waste burial site, Pinal County, Arizona
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azu_td_hy_e9791_1984_87_sip1_w.pdf
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azu_td_hy_e9791_1984_87_sip1_w.pdf
Author
Salvetti, Joseph Peter.Issue Date
1984Keywords
Hydrology.Groundwater flow -- Arizona -- Oracle Region.
Groundwater flow -- Arizona -- Pinal County.
Hazardous waste sites -- Environmental aspects -- Arizona -- Oracle Region.
Hazardous waste sites -- Environmental aspects -- Arizona -- Pinal County.
Radioactive waste disposal -- Environmental aspects -- Arizona -- Oracle Region.
Radioactive waste disposal -- Environmental aspects -- Arizona -- Pinal County.
Radioactive waste disposal in the ground -- Environmental aspects -- Arizona -- Oracle Region.
Radioactive waste disposal in the ground -- Environmental aspects -- Arizona -- Pinal County.
Groundwater -- Pollution -- Arizona -- Oracle Region.
Groundwater -- Pollution -- Arizona -- Pinal County.
Committee Chair
Dutt, Gordon R.
Metadata
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The University of Arizona.Rights
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.Abstract
The University of Arizona produces different types of radioactively contaminated waste. It is shipped to a burial site located on the Oracle Agricultural Center in Pinal County, Arizona and disposed of in shallow pits. This study dealt with water movement at the disposal site. Monitoring of water movement through young pits was accomplished with a neutron probe. It was found that due to slumping and cracking of the pit cap, the younger pits were very susceptible to greater than normal water infiltration. Further data were gathered around the older pits by deep soil sampling for tritium activity. Water fluxes and travel times to the major aquifer were calculated from these data. Estimates of travel times range from 40 to 230,000 years to reach the principal aquifer at 150 m.Type
Thesis-Reproduction (electronic)text
Degree Name
M.S.Degree Level
mastersDegree Program
Soils, Water and EngineeringGraduate College