36C1 measurements and the hydrology of an acid injection site

G. Vourvopoulos; J. V. Brahana; E. Nolte; G. Korschinek; A. Priller; B. Dockhorn

doi:10.1016/0168-583X(90)90456-5

³⁶C1 measurements and the hydrology of an acid injection site

G. Vourvopoulos, J. V. Brahana, E. Nolte, G. Korschinek, A. Priller, B. Dockhorn

Lehrstuhl für Experimentelle Astroteilchenphysik

Publikation: Beitrag in Fachzeitschrift › Artikel › Begutachtung

2 Zitate (Scopus)

Abstract

In an area in western Tennessee (United States), an industrial firm is injecting acidic (pH = 0.1) iron chloride into permeable zones of carbonate rocks at depths ranging from 1000 to 2200 m below land surface. Overlying the injection zone at a depth of approximately 500 m below land surface is a regional fresh-water aquifer, the Knox aquifer. A study is currently underway to investigate whether the injection wells are hydraulically isolated from the fresh-water aquifer. Drilling of a test well that will reach a total depth of 2700 m has been initiated. The ³⁶Cl content of 15 samples from the Knox aquifer, from monitor wells in the vicinity of the injection site, and from the test well have been analyzed.

Originalsprache	Englisch
Seiten (von - bis)	451-454
Seitenumfang	4
Fachzeitschrift	Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms
Jahrgang	52
Ausgabenummer	3-4
DOIs	https://doi.org/10.1016/0168-583X(90)90456-5
Publikationsstatus	Veröffentlicht - 2 Dez. 1990

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10.1016/0168-583X(90)90456-5

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title = "36C1 measurements and the hydrology of an acid injection site",

abstract = "In an area in western Tennessee (United States), an industrial firm is injecting acidic (pH = 0.1) iron chloride into permeable zones of carbonate rocks at depths ranging from 1000 to 2200 m below land surface. Overlying the injection zone at a depth of approximately 500 m below land surface is a regional fresh-water aquifer, the Knox aquifer. A study is currently underway to investigate whether the injection wells are hydraulically isolated from the fresh-water aquifer. Drilling of a test well that will reach a total depth of 2700 m has been initiated. The 36Cl content of 15 samples from the Knox aquifer, from monitor wells in the vicinity of the injection site, and from the test well have been analyzed.",

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T1 - 36C1 measurements and the hydrology of an acid injection site

AU - Vourvopoulos, G.

AU - Brahana, J. V.

AU - Nolte, E.

AU - Korschinek, G.

AU - Priller, A.

AU - Dockhorn, B.

PY - 1990/12/2

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N2 - In an area in western Tennessee (United States), an industrial firm is injecting acidic (pH = 0.1) iron chloride into permeable zones of carbonate rocks at depths ranging from 1000 to 2200 m below land surface. Overlying the injection zone at a depth of approximately 500 m below land surface is a regional fresh-water aquifer, the Knox aquifer. A study is currently underway to investigate whether the injection wells are hydraulically isolated from the fresh-water aquifer. Drilling of a test well that will reach a total depth of 2700 m has been initiated. The 36Cl content of 15 samples from the Knox aquifer, from monitor wells in the vicinity of the injection site, and from the test well have been analyzed.

AB - In an area in western Tennessee (United States), an industrial firm is injecting acidic (pH = 0.1) iron chloride into permeable zones of carbonate rocks at depths ranging from 1000 to 2200 m below land surface. Overlying the injection zone at a depth of approximately 500 m below land surface is a regional fresh-water aquifer, the Knox aquifer. A study is currently underway to investigate whether the injection wells are hydraulically isolated from the fresh-water aquifer. Drilling of a test well that will reach a total depth of 2700 m has been initiated. The 36Cl content of 15 samples from the Knox aquifer, from monitor wells in the vicinity of the injection site, and from the test well have been analyzed.

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