What controls the apparent timescale of solute mass transfer in aquifers and soils? A comparison of experimental results-Reference-Cited by-同舟云学术

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What controls the apparent timescale of solute mass transfer in aquifers and soils? A comparison of experimental results

Published:2004-01 Issue:1 Volume:40 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Haggerty Roy¹,Harvey Charles F.²,Freiherr von Schwerin Claudius¹,Meigs Lucy C.³

Affiliation:

1. Department of Geosciences; Oregon State University; Corvallis Oregon USA

2. Ralph Parsons Laboratory; Massachusetts Institute of Technology; Cambridge Massachusetts USA

3. Geohydrology Department; Sandia National Laboratories; Albuquerque New Mexico USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2002WR001716/fullpdf

Reference93 articles.

1. Nonequilibrium sorption and aerobic biodegradation of dissolved alkylbenzenes during transport in aquifer material: Column experiments and evaluation of a coupled-process model;Angley;Environ. Sci. Technol.,1992

2. Kinetics of cadmium and cobalt desorption from iron and manganese oxides;Backes;Soil Sci. Soc. Am. J.,1995

3. Direct comparison of kinetic and local equilibrium formulations for solute transport affected by surface reactions;Bahr;Water Resour. Res.,1987

4. Nonequilibrium solute transport parameters and their physical significance: Numerical and experimental results;Bajracharya;J. Contam. Hydrol.,1997

5. Long-term sorption of halogenated organic chemicals by aquifer material, 2, Intraparticle diffusion;Ball;Environ. Sci. Technol.,1991

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