Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geosphere Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geosphere; June 2006; v. 2; no. 4; p. 220-235; DOI: 10.1130/GES00029.1
© 2006 Geological Society of America
This Article
Free via Open Access: OA
Right arrow Figures Only
Right arrow OA Full Text
Right arrow Full Text (PDF)
Right arrow Animations
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Scheibe, T. D.
Right arrow Articles by Hubbard, S. S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

ARTICLES

Transport and biogeochemical reaction of metals in a physically and chemically heterogeneous aquifer

Timothy D. Scheibe1, Yilin Fang1, Christopher J. Murray1, Eric E. Roden2, Jinsong Chen3, Yi-Ju Chien4, Scott C. Brooks5 and Susan S. Hubbard6

1 Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington 99352, USA
2 University of Wisconsin, Department of Geology and Geophysics, 1215 W. Dayton Street, Madison, Wisconsin 53706, USA
3 Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS 90-1116, Berkeley, California 94720, USA
4 Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington 99352, USA
5 Oak Ridge National Laboratory, P.O. Box 2008, MS 6038, Oak Ridge, Tennessee 37831-6038, USA
6 Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS 90-1116, Berkeley, California 94720, USA

Biologically mediated reductive dissolution and precipitation of metals and radionuclides play key roles in their subsurface transport. Physical and chemical properties of natural aquifer systems, such as reactive iron-oxide surface area and hydraulic conductivity, are often highly heterogeneous in complex ways that can exert significant control on transport, natural attenuation, and active remediation processes. Typically, however, few data on the detailed distribution of these properties are available for incorporation into predictive models. In this study, we integrate field-scale geophysical, hydrologic, and geochemical data from a well-characterized site with the results of laboratory batch-reaction studies to formulate two-dimensional numerical models of reactive transport in a heterogeneous granular aquifer. The models incorporate several levels of coupling, including effects of ferrous iron sorption onto (and associated reduction of reactive surface area of) ferric iron surfaces, microbial growth and transport dynamics, and cross-correlation between hydraulic conductivity and initial ferric iron surface area. These models are then used to evaluate the impacts of physical and chemical heterogeneity on transport of trace levels of uranium under natural conditions, as well as the effectiveness of uranium reduction and immobilization upon introduction of a soluble electron donor (a potential biostimulation remedial strategy).

Keywords: reactive transport • heterogeneity • modeling • groundwater • uranium







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of America