Arsenic in Ground Water

Arsenic in Ground Water PDF Author: Alan H. Welch
Publisher: Springer Science & Business Media
ISBN: 0306479567
Category : Science
Languages : en
Pages : 476

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Book Description
Interest in arsenic in ground water has greatly increased in the past decade because of the increased awareness of human health effects and the costs of avoidance or treatment of ground water supplies used for consumption. The goal of this book is to provide a description of the basic processes that affect arsenic occurrence and transport by providing sufficient background information on arsenic geochemistry and descriptions of hi- arsenic ground water, both affected and unaffected by human activity. An understanding of thermodynamics, adsorption, and the speciation of arsenic in solid phases, which are described in first three chapters, is needed to predict the fate of arsenic in ground water systems. Large-scale and deep movement of ground water can and has redistributed arsenic in the near surface environment, as described in the next two chapters. These large-scale systems can affect large volumes of both ground water and surface water, such as in the Yellowstone system, and can produce mineralised zones that subsequently release arsenic to ground water supplies. Regional identification of high-arsenic ground water and its consumption as described in the next three chapters clearly demonstrates a need for increased wat- quality monitoring, particularly in south and southeast Asia. Chapters 9-11 provide examples of high arsenic ground water associated with sulfide mineral oxidation and alkaline conditions. Finally, smaller scale studies of the effects of human activities that have produced high-arsenic ground water and methods for attenuation of ground water are presented.

Arsenic in Ground Water

Arsenic in Ground Water PDF Author: Alan H. Welch
Publisher: Springer Science & Business Media
ISBN: 0306479567
Category : Science
Languages : en
Pages : 476

Get Book Here

Book Description
Interest in arsenic in ground water has greatly increased in the past decade because of the increased awareness of human health effects and the costs of avoidance or treatment of ground water supplies used for consumption. The goal of this book is to provide a description of the basic processes that affect arsenic occurrence and transport by providing sufficient background information on arsenic geochemistry and descriptions of hi- arsenic ground water, both affected and unaffected by human activity. An understanding of thermodynamics, adsorption, and the speciation of arsenic in solid phases, which are described in first three chapters, is needed to predict the fate of arsenic in ground water systems. Large-scale and deep movement of ground water can and has redistributed arsenic in the near surface environment, as described in the next two chapters. These large-scale systems can affect large volumes of both ground water and surface water, such as in the Yellowstone system, and can produce mineralised zones that subsequently release arsenic to ground water supplies. Regional identification of high-arsenic ground water and its consumption as described in the next three chapters clearly demonstrates a need for increased wat- quality monitoring, particularly in south and southeast Asia. Chapters 9-11 provide examples of high arsenic ground water associated with sulfide mineral oxidation and alkaline conditions. Finally, smaller scale studies of the effects of human activities that have produced high-arsenic ground water and methods for attenuation of ground water are presented.

Ground-water Resources of Catron County, New Mexico

Ground-water Resources of Catron County, New Mexico PDF Author: George Taylor Basabilvazo
Publisher:
ISBN:
Category : Aquifers
Languages : en
Pages : 156

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Book Description


Ground-water Levels in the United States

Ground-water Levels in the United States PDF Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 172

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Book Description


Hydrogeology of Cibola County, New Mexico

Hydrogeology of Cibola County, New Mexico PDF Author: Joe A. Baldwin
Publisher:
ISBN:
Category : Aquifers
Languages : en
Pages : 116

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Book Description


Ground-water Levels in the United States, 1971-74

Ground-water Levels in the United States, 1971-74 PDF Author:
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 362

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Book Description


Geological Survey Water-supply Paper

Geological Survey Water-supply Paper PDF Author:
Publisher:
ISBN:
Category : Floods
Languages : en
Pages : 676

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Book Description


Scientific Investigations Report

Scientific Investigations Report PDF Author:
Publisher:
ISBN:
Category : Earth sciences
Languages : en
Pages : 294

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Book Description


National Water Summary

National Water Summary PDF Author:
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 572

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Book Description


Effects of Uranium-mining Releases on Ground-water Quality in the Puerco River Basin, Arizona and New Mexico

Effects of Uranium-mining Releases on Ground-water Quality in the Puerco River Basin, Arizona and New Mexico PDF Author:
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 84

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Book Description


Bulletin 162

Bulletin 162 PDF Author: Geoffrey C. Rawling
Publisher:
ISBN: 9781883905453
Category :
Languages : en
Pages : 48

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Book Description
Several thousand water-level measurements spanning over 50 years, from over a thousand wells, were used to create aquifer lifetime projections for the High Plains Aquifer in east-central New Mexico. Lifetime projections were made based on past water-level decline rates calculated over ten- and twenty-year intervals. Projected lifetimes were calculated for two scenarios. One scenario is the time until total dewatering of the full saturated thickness of the aquifer, and the other scenario is the time until a 30-ft saturated thickness threshold is reached, which is the minimum necessary to sustain high-capacity irrigation wells. Agricultural water use has largely determined water-level decline rates in the past - assuming future decline rates match those of the past ten to twenty years, the two scenarios may be viewed as the usable aquifer lifetime for domestic and low-intensity municipal and industrial uses, and the usable lifetime for large-scale irrigated agriculture.