Water levels in the Yucca Mountain area, Nevada, 1994
Author(s) -
R.P. Graves,
P. Tucci,
Robert L. Goemaat
Publication year - 1996
Publication title -
osti oai (u.s. department of energy office of scientific and technical information)
Language(s) - English
Resource type - Reports
DOI - 10.2172/426987
Subject(s) - sea level , geology , carbonate rock , water level , altitude (triangle) , paleozoic , volcano , carbonate , hydrology (agriculture) , water quality , geochemistry , sedimentary rock , oceanography , geotechnical engineering , geography , ecology , materials science , geometry , cartography , mathematics , metallurgy , biology
Water levels were monitored in 28 wells in the Yucca Mountain area, Nevada, during 1994. Twelve wells representing 13 intervals were monitored periodically, generally on a monthly basis, 6 wells representing 10 intervals were monitored hourly, and 10 wells representing 13 intervals were monitored both periodically and hourly. All wells monitor water levels in Tertiary volcanic rocks, except one, that monitors water levels in Paleozoic carbonate rocks. Water levels were measured using calibrated steel tapes, a multiconductor cable unit, and pressure transducers. Water-level altitudes in the Tertiary volcanic rocks ranged from about 728 to about 1,034 meters above sea level during 1994. The mean-annual water-level altitude in the well monitoring the Paleozoic carbonate rocks was about 753 meters above sea level during 1994. Water levels were only an average of about 0.01 meters lower than 1993 water levels. All data were acquired in accordance with a quality-assurance program to support the reliability of the data
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