Biogeochemical processes during the infiltration of river water into an alluvial aquifer

A field investigation of hydrogeochemical processes occurring during the infiltration of river water into an alluvial aquifer through river bank sediments is presented. Chloride was used as a natural tracer of water mixing.

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Bibliographic Details
Published inEnvironmental science & technology Vol. 27; no. 4; pp. 661 - 666
Main Authors Bourg, Alain C. M, Bertin, Clotilde
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 01.04.1993
Subjects
Aquifers
Chemistry
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geochemistry
Hydrology
Hydrology. Hydrogeology
Mineralogy
Silicates
Water
Water geochemistry
Lot
Aquitaine Basin
France
Europe
chlorides
rivers
calcium
bacteria
tracers
magnesium
carbonates
infiltration
drainage basins
solution
hydrochemistry
aquifers
recharge
organic materials
alteration
dissolved materials
biogenic effects
fresh water
organic carbon
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Summary:A field investigation of hydrogeochemical processes occurring during the infiltration of river water into an alluvial aquifer through river bank sediments is presented. Chloride was used as a natural tracer of water mixing.
Bibliography:ark:/67375/TPS-M9DPHX9N-8
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ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0013-936X
1520-5851
DOI:10.1021/es00041a009