Fe(II)−Fe(III)-Bearing Phases As a Mineralogical Control on the Heterogeneity of Arsenic in Southeast Asian Groundwater-Reference-Cited by-同舟云学术

Fe(II)−Fe(III)-Bearing Phases As a Mineralogical Control on the Heterogeneity of Arsenic in Southeast Asian Groundwater

Published:2010-09-10 Issue:19 Volume:44 Page:7541-7547
ISSN:0013-936X
Container-title:Environmental Science & Technology
language:en
Short-container-title:Environ. Sci. Technol.

Author:

Burnol Andre¹,Charlet Laurent¹

Affiliation:

1. LGIT-OSUG, University of Grenoble-I, BP 53, 38041 Grenoble Cedex 9, France, and Environment and Process Division, BRGM, Bureau de Recherches Géologiques et Minières, BP 36009, 45060 Orléans Cedex 2, France

Publisher

American Chemical Society (ACS)

Subject

Environmental Chemistry,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/es100280h

Reference41 articles.

1. Mechanism of arsenic release to groundwater, Bangladesh and West Bengal

2. Role of metal-reducing bacteria in arsenic release from Bengal delta sediments

3. Decoupling of As and Fe release to Bangladesh groundwater under reducing conditions. Part II: Evidence from sediment incubations

4. Decoupling of arsenic and iron release from ferrihydrite suspension under reducing conditions: a biogeochemical model

5. Decoupling of As and Fe release to Bangladesh groundwater under reducing conditions. Part I: Evidence from sediment profiles

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