Deuterium content of water from wells and perennial springs, southeastern California

Cover of: Deuterium content of water from wells and perennial springs, southeastern California |

Published by U.S. Geological Survey, Open-file Reports Section [distributor] in Sacramento, Calif, Denver, CO .

Written in English

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  • Groundwater -- California, Southern -- Quality,
  • Deuterium -- Environmental aspects

Edition Notes

Book details

Statementby Jim D. Gleason ... [et al.]
SeriesRegional aquifer-system analysis, U.S. Geological Survey open-file report -- 91-470
ContributionsGleason, James D, Geological Survey (U.S.)
The Physical Object
Paginationiii, 22 p.
Number of Pages22
ID Numbers
Open LibraryOL14442199M

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Get this from a library. Deuterium content of water from wells and perennial springs, southeastern California. [Jim D Gleason; Geological Survey (U.S.);]. Owens Valley Hydrogeology. Welcome to the U.S. Geological Survey (USGS) Owens Valley Hydrogeology website.

Deuterium content of water from wells and perennial springs, southeastern California: U.S. Geological Survey Hydrologic Investigations Atlas1 sheet.

Owens Valley Hydrogeology. Welcome to the U.S. Geological Survey (USGS) Owens Valley Hydrogeology website. Deuterium content of water from wells and perennial springs, southeastern California: U.S.

Geological Survey Hydrologic Investigations Atlas1 sheet. Gorelick, S.M., Islands of California: their history, romance and physical characteristics.

/ With many illus. by the a Extracts from the speech of the Rev. Father Gleason at Central Theatre, San Francisco, [mic Deuterium content of water from wells and perennial springs, southeastern California [microform] / by. George I. Smith's 25 research works with 1, citations and 1, reads, including: Stable isotope composition of waters in the Great Basin, United States 1.

The ground-water data collected as part of this study include major- and minor-element chemistry (30 elements), oxygen and deuterium content of water, carbon content and carbon activity.

The unique combination of evaporative concentration and bicarbonate-rich water compositions in saline, alkaline lakes leads to conditions favoring rapid hydrolysis of labile silicate minerals and volcanic glass ().The resulting high pH water (pH commonly >9) leads to solubilization of silica and aluminum from relatively unstable mineral phases, which subsequently drives chemical oversaturation Cited by: The Groundwater Ambient Monitoring and Assessment program (Belitz et al.,Belitz et al., ) aims to assess the quality and vulnerability of groundwater resources in California.A large proportion of the monitoring effort is dedicated to the collection and analysis of water quality samples (Deeds et al.,Fram and Belitz, a, Jurgens et al.,Fram and Belitz, b, Landon Cited by: While the desert ecosystem is highly dependent on the water resources that sustain it, the Fish Slough spring complex is an arid, spring-dependent wetland undergoing a multidecadal decline in spring outflow.

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and Veatch,p. Most production wells to the west of Cheyenne withdraw water primarily from wells completed in permeable zones of the Ogallala Formation, although some contribution from the underlying White River Group or Formation is likely where screens penetrate the unit. In contrast, production wells to the northwest of Cheyenne Author: Timothy T.

Bartos, Sharon F. Diehl, Laura L. Hallberg, Daniel M. Webster. Distribution of wells in the central part of the western San Joaquin Valley, California U.S. Geological Survey Water-Resources Investigations Report51 p.

Hull, L.C. Geochemistry of ground water in the Sacramento Valley, California U.S. Geological Survey Professional Paper B, 36 p. Laudon, Julie, and Belitz, Kenneth. Ground Water Management Book 10 of the Series Proceedings of the Third Conference on Hydrogeology, Ecology, Monitoring and Management of Ground Water in Karst Terranes December 4- 6, Maxwell House Clarion Nashville, Tennessee Abstract The Karst Conference was comprised of 2 days of technical presentations, and a day-long field trip.

water from these wells range from to mg/L (table 4). Water from wells perforated in the regional aqui­ fer in the vicinity of the Nebo and Yermo Annexes gen­ erally has high dissolved-solids concentrations (greater than mg/L; fig. 13). Wells 9N/1W-4M5, K13,N5, and 9N/1E-4K2, and Q3 perforated in theCited by: 3.

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BLM ). Ground water development can reduce spring flow, change springs from 41 perennial to intermittent, or eliminate springs altogether. Full text of "Haiwee Geothermal Leasing Area: draft environmental impact statement and draft proposed amendment to the California Desert Conservation Area plan" See other formats.

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Key characteristics of California groundwater systems related to aquifer vulnerability, sustainability, recharge locations and mechanisms, and anthropogenic impact on recharge are revealed in a spatial geostatistical analysis of a unique data set of tritium, noble gases and other isotopic analyses unprecedented in size at nearly correlation length of key groundwater residence.

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