The origins of high concentrations of iron, sodium, bicarbonate, and arsenic in the Lower Mississippi River Alluvial Aquifer

Author:

Borrok David M.ORCID,Lenz Rebecca M.,Jennings John E.,Gentry Mary L.,Steensma Julie,Vinson David S.ORCID

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference44 articles.

1. Hydrology of the Mississippi River Valley Alluvial Aquifer, South-central United States; a Preliminary Assessment of the Regional Flow System. U.S. Geological Survey Water Resources Investigations Report 88-4028;Ackerman,1989

2. Arsenic enrichment in groundwater of the alluvial aquifers in Bangladesh: an overview;Ahmed;Appl. Geochem.,2004

3. Geochemical occurrence of arsenic in groundwater of Bangladesh: sources and mobilization processes;Anawar;J. Geochem. Explor.,2003

4. Hydrogeology, Model Description, and Flow Analysis of the Mississippi River Alluvial Aquifer in Northwestern Mississippi. U.S. Geological Survey Water Resources Investigations Report 01-4035;Arthur,2001

5. Evolution of the Holocene Mississippi River floodplain, Ferriday, Louisiana: insights on the origin of fine-grained floodplains;Aslan;J. Sediment. Res.,1999

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