Redox reaction along a ground water conducting fracture and secondary elemental migration in granitic rock:—Analogue of long-term contaminant migration and fixation in geological environment

Redox reaction along a ground water conducting fracture and secondary elemental migration in granitic rock:—Analogue of long-term contaminant migration and fixation in geological environment—

Published:2004 Issue:11 Volume:110 Page:671-685
ISSN:0016-7630
Container-title:The Journal of the Geological Society of Japan
language:en
Short-container-title:Jour. Geol. Soc. Japan

Author:

Akagawa Fuminori¹,Yoshida Hidekazu²,Yogo Setuo³,Yamamoto Koshi¹

Affiliation:

1. Nagoya University, Graduate School of Environmental Studies

2. The Nagoya University Museum, Material Research Section

3. Nagoya University, School of Science

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Link

https://www.jstage.jst.go.jp/article/geosoc/110/11/110_11_671/_pdf

Reference39 articles.

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2. Berner, R.A., 1981, A new geochemical classification of sedimentary environments. Jour. Sediment. Petrol., 51, 359-365.

3. Cochran, J.K., Carey, A.E., Sholkovitz, E. and Suprenant, L.D., 1986, The geochemistry of uranium and thorium in coastal mareine sediments and sediment porewaters. Geochim. Cosmochim. Acta, 50, 663-680.

4. Compton, J.S., White, R.A. and Smith, M., 2003, Rare earth element behavior in soils and salt pan sediments of a semi-arid granitic terrain in the Western Cape, South Africa. Chem. Geol., 201, 239-255.

5. De Carlo, E.H. and Wen, X., 1998, The influence of redox reactions on the uptake of dissolved Ce by suspended Fe and Mn oxide particles. Aquatic Geochem., 3, 357-389.

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