What controls the apparent timescale of solute mass transfer in aquifers and soils? A comparison of experimental results
- Oregon State Univ., Corvallis, OR (United States). Dept. of Geosciences
- Massachusetts Inst. of Technology (MIT), Cambridge, MA (United States). Ralph Parsons Lab.
- Oregon State Univ., Corvallis, OR (United States). Dept. of Geosciences; John Shomaker and Associates, Inc., Albuquerque, NM (United States)
- Sandia National Lab. (SNL-NM), Albuquerque, NM (United States). Geohydrology Dept.
We compare estimates of mass transfer timescales from 316 solute transport experiments reported in 35 publications to the pore-water velocities and residence times, as well as the experimental durations. We also conducted new tracer experiments in columns of different lengths so that the velocity and the advective residence time could be varied independently. In both the experiments reported in the literature and the new experiments, the estimated mass transfer timescale (inverse of the mass-transfer rate coefficient) is better correlated to residence time and the experimental duration than to velocity. Of the measures considered, the experimental duration multiplied by 1 + β (where β is the capacity coefficient, defined as the ratio of masses in the immobile and mobile domains at equilibrium) best predicted the estimated mass transfer timescale. This relation is consistent with other work showing that aquifer and soil material commonly produce multiple timescales of mass transfer.
- Research Organization:
- Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
- Sponsoring Organization:
- USDOE
- DOE Contract Number:
- AC04-94AL85000
- OSTI ID:
- 889012
- Report Number(s):
- SAND2003--0138J
- Journal Information:
- Water Resources Research, Journal Name: Water Resources Research Journal Issue: 1 Vol. 40; ISSN 0043-1397
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
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