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Published online 9 April 2007
Published in Vadose Zone J 6:221-232 (2007)
DOI: 10.2136/vzj2006.0064
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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The Impact of Clay Mineralogy on Nitrate Mobility under Unsaturated Flow Conditions

Barry J. Allreda,*, Jerry M. Bighamb and Glenn O. Brownc

a USDA-ARS Soil Drainage Research Unit, 590 Woody Hayes Dr., Rm. 234, Columbus, OH 43210
b School of Natural Resources, Ohio State Univ., 2021 Coffey Rd., 210 Kottman Hall, Columbus, OH 43210
c Biosystems and Agricultural Engineering Dep., Oklahoma State Univ., 109 Agricultural Hall, Stillwater, OK 74078


Figure 1
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FIG. 1. Pore-scale conceptualization of anion adsorption and anion exclusion processes under unsaturated flow conditions.

 

Figure 2
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FIG. 2. (a) Schematic of the computer-controlled syringe pump apparatus, (b) the computer-controlled syringe pump apparatus, (c) syringe pump and horizontal soil column with controller in background, and (d) syringes inserted into column inlet.

 

Figure 3
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FIG. 3. Ideal transient unsaturated horizontal column water content and soil solution NO3–N concentration profiles for an initially dry soil with no NO3–N initially present.

 

Figure 4
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FIG. 4. Experimental data profiles for (a) 100% sand, water content, (b) 100% sand, NO3-N concentration, (c) 25% kaolinite, 75% sand, water content, (d) 25% kaolinite, 75% sand, NO3-N concentration, (e) 25% illite, 75% sand, water content, (f) 25% illite, 75% sand, NO3-N concentration, (g) 25% montmorillonite, 75% sand, water content, and (h) 25% montmorillonite, 75% sand, NO3-N concentration.

 

Figure 5
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FIG. 5. Experimental data profiles for (a) 15% kaolinite, 7.5% illite, 7.5% montmorillonite, 70% sand, water content, (b) 15% kaolinite, 7.5% illite, 7.5% montmorillonite, 70% sand, NO3–N concentration, (c) Slaughterville, water content, (d) Slaughterville, NO3–N concentration, (e) Teller, water content, and (f) Teller, NO3–N concentration. Organic matter was removed from the Slaughterville and Teller soils before testing.

 





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