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Published online 17 May 2007
Published in Vadose Zone J 6:363-372 (2007)
DOI: 10.2136/vzj2006.0048
© 2007 Soil Science Society of America
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Spatial and Temporal Variability in Colloid Dispersion as a Function of Groundwater Injection Rate within Atlantic Coastal Plain Sediments

J. C. Seamana,*, P. M. Bertscha and D. I. Kaplanb

a Savannah River Ecology Lab., The Univ. of Georgia, Drawer E, Aiken, SC 29802
b Savannah River National Lab., Aiken, SC 29808

Figure 1
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  		FIG. 1. Relative location of the injection well (IW) and various sampling wells (S1–S6) at the injection test site (ITS).

 

Figure 2
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  		FIG. 2. Well construction diagram for the injection well (IW), sampling wells (S1–S6 and Obs-1–Obs-3), and modified multidepth Waterloo sampling system.

 

Figure 3
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  		FIG. 3. Sample turbidity at various depths within (A) Well S3 and (B) Well S6 during groundwater injection ranging from 19 to 132 L min–1 (Zone 1, deepest; Zone 3, shallowest; the location of wells is presented in Fig. 1).

 

Figure 4
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  		FIG. 4. (A) Sample turbidity (NTU) at three depths within Well S1, and (B) groundwater mounding in injection well, IW, as a function of injection rate.

 




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