Hydrology and Land Surface Studies
Pore-scale analysis of permeability reduction resulting from colloid deposition
Version of Record online: 4 APR 2008
Copyright 2008 by the American Geophysical Union.
Geophysical Research Letters
Volume 35, Issue 7, April 2008
How to Cite
2008), Pore-scale analysis of permeability reduction resulting from colloid deposition, Geophys. Res. Lett., 35, L07404, doi:10.1029/2007GL033077., , and (
- Issue online: 4 APR 2008
- Version of Record online: 4 APR 2008
- Manuscript Accepted: 3 MAR 2008
- Manuscript Revised: 6 FEB 2008
- Manuscript Received: 26 DEC 2007
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|grl24324-sup-0001-readme.txt||plain text document||2K||readme.txt|
|grl24324-sup-0002-txts01.tex||application/x-tex||999||Text S1. Descriptions of approach and results.|
|grl24324-sup-0003-txts01.pdf||PDF document||64K||Text S1. Descriptions of approach and results.|
|grl24324-sup-0004-fs01.tif||TIFF image||904K||Figure S1. The 2D vertical cross sections of 299 × 598 pixels (1.79 × 3.58 mm).|
|grl24324-sup-0005-fs02.tif||TIFF image||121K||Figure S2. Scale dependency of (a) porosity, (b) specific surface area, and (c) permeability from sample 1-B before deposition.|
|grl24324-sup-0006-fs03.tif||TIFF image||37K||Figure S3. Specific surface area vs. porosity.|
|grl24324-sup-0007-fs04.tif||TIFF image||37K||Figure S4. Values of the Kozeny-Carman geometric parameter “b” found by fitting Equation 1 to the local permeabilities obtained from lattice Boltzmann simulations based on measured values of porosity and specific surface area, as well as the ensemble average tortuosity obtained from particle tracking simulations.|
|grl24324-sup-0008-fs05.tif||TIFF image||38K||Figure S5. Normalized head loss increase vs. specific deposit.|
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