Water levels in continuously monitored wells in the Yucca Mountain area, Nevada, 1985--88

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Water levels have been monitored hourly in 15 wells completed in 23 depth intervals in the Yucca Mountain area, Nevada. Water levels were monitored using pressure transducers and were recorded by data loggers. The pressure transducers were periodically calibrated by raising and lowering them in the wells. The water levels were normally measured at approximately the same time that the transducers were calibrated. Where the transducer output appeared reasonable, it was converted to water levels using the calibrations and manual water- level measurements. The amount of transducer output that was converted to water levels ranged from zero for several intervals … continued below

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252 p.

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Luckey, Richard R.; Lobmeyer, David H. & Burkhardt, Douglas J. July 1, 1993.

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This report is part of the collection entitled: Office of Scientific & Technical Information Technical Reports and was provided by the UNT Libraries Government Documents Department to the UNT Digital Library, a digital repository hosted by the UNT Libraries. It has been viewed 17 times. More information about this report can be viewed below.

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Description

Water levels have been monitored hourly in 15 wells completed in 23 depth intervals in the Yucca Mountain area, Nevada. Water levels were monitored using pressure transducers and were recorded by data loggers. The pressure transducers were periodically calibrated by raising and lowering them in the wells. The water levels were normally measured at approximately the same time that the transducers were calibrated. Where the transducer output appeared reasonable, it was converted to water levels using the calibrations and manual water- level measurements. The amount of transducer output that was converted to water levels ranged from zero for several intervals to about 98 percent for one interval. Fourteen of the wells were completed in Tertiary volcanic rocks and one well was completed in Paleozoic carbonate rocks. Each well monitored from one to four depth intervals. Water-level fluctuation caused by barometric pressure changes and earth tides were observed.

Physical Description

252 p.

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US Geological Survey, Books and Open-File Reports Section, Box 25425, Mail Stop 517, Federal Center, Denver, CO 80225-0425; OSTI as DE93017415

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  • Other Information: PBD: 1993

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Office of Scientific & Technical Information Technical Reports

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  • July 1, 1993

Added to The UNT Digital Library

  • June 16, 2015, 7:43 a.m.

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  • March 24, 2022, 11:15 a.m.

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Luckey, Richard R.; Lobmeyer, David H. & Burkhardt, Douglas J. Water levels in continuously monitored wells in the Yucca Mountain area, Nevada, 1985--88, report, July 1, 1993; Denver, Colorado. (https://digital.library.unt.edu/ark:/67531/metadc628535/: accessed July 16, 2024), University of North Texas Libraries, UNT Digital Library, https://digital.library.unt.edu; crediting UNT Libraries Government Documents Department.

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