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Wiley InterScience

Ground Water

Ground Water

Volume 39 Issue 6, Pages 831 - 840

Published Online: 13 Dec 2005

Journal compilation © 2010 National Ground Water Association



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Potential Artifacts in Interpretation of Differential Breakthrough of Colloids and Dissolved Tracers in the Context of Transport in a Zero-Valent Iron Permeable Reactive Barrier
Pengfei Zhang 1 5 , William P. Johnson 1 4 , Michael J. Piana 2 , Christopher C. Fuller 2 David L. Naftz 3
  1 University of Utah, Department of Geology and Geophysics, 135 South 1460 East, Salt Lake City, UT 84112   2 U.S. Geological Survey, Water Resources Division, 345 Middlefield Rd., Menlo Park, CA 94025   3 U.S. Geological Survey, Water Resources Division, 2329 West Orton Circle, West Valley City, UT 84119
  4 Corresponding author: (801) 581–5033; fax (801) 581–7065; wjohnson@mines.utah.edu
 

5 Current address: New Mexico Institute of Mining and Technology, Department of Earth and Environmental Science, 801 Leroy Pl., Socorro, NM 87801

Copyright 2001 National Ground Water Association

Abstract

AbstractReferences

Many published studies have used visual comparison of the timing of peak breakthrough of colloids versus conservative dissolved tracers (hereafter referred to as dissolved tracers or tracers) in subsurface media to determine whether they are advected differently, and to elucidate the mechanisms of differential advection. This purely visual approach of determining differential advec-tion may have artifacts, however, due to the attachment of colloids to subsurface media. The attachment of colloids to subsurface media may shift the colloidal peak breakthrough to earlier times, causing an apparent "faster" peak breakthrough of colloids relative to dissolve tracers even though the transport velocities for the colloids and the dissolved tracers may actually be equivalent. In this paper, a peak shift analysis was presented to illustrate the artifacts associated with the purely visual approach in determining differential advection, and to quantify the peak shift due to colloid attachment. This peak shift analysis was described within the context of microsphere and bromide transport within a zero-valent iron (ZVI) permeable reactive barrier (PRB) located in Fry Canyon, Utah. Application of the peak shift analysis to the field microsphere and bromide breakthrough data indicated that differential advection of the microspheres relative to the bromide occurred in the monitoring wells closest to the injection well in the PRB. It was hypothesized that the physical heterogeneity at the grain scale, presumably arising from differences in inter- versus intra-particle porosity, contributed to the differential advection of the microspheres versus the bromide in the PRB. The relative breakthrough (RB) of microspheres at different wells was inversely related to the ionic strength of ground water at these wells, in agreement with numerous studies showing that colloid attachment is directly related to solution ionic strength.


Received September 2000, accepted April 2001.

DIGITAL OBJECT IDENTIFIER (DOI)
10.1111/j.1745-6584.2001.tb02471.x About DOI

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