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Published online 27 October 2006
Published in J Environ Qual 35:2261-2272 (2006)
DOI: 10.2134/jeq2005.0401
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Sorption and Transport of 17ß-Estradiol and Testosterone in Undisturbed Soil Columns

H. A. Sangsupan, D. E. Radcliffe*, P. G. Hartel, M. B. Jenkins, W. K. Vencill and M. L. Cabrera

Dep. of Crop and Soil Sciences, 3111 Plant Sciences Bldg., Univ. of Georgia, Athens, GA 30602-7272


Figure 1
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Fig. 1. Kinetic sorption of (a) estradiol and (b) testosterone to soil from the 0- to 10-cm (closed symbol) and 20- to 30-cm (open symbol) soil depths. Error bars indicate one standard error.

 

Figure 2
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Fig. 2. Distribution of measured (a) estradiol and (b) testosterone within conventionally tilled (CT; closed symbol) and no-till (NT; open symbol) soil columns and the quasi-combined model predictions of sorbed hormones (differences between tillages were too small to show separate curves) . Error bars indicate one standard error.

 

Figure 3
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Fig. 3. Breakthrough curve of Cl (+), estradiol (o), and testosterone ({Delta}) through columns of conventionally tilled (CT) and no-till (NT) Cecil sandy loam. Each graph possesses two y-axes. The left y axis represents the relative concentration of hormones (C C0–1). The right y axis represents the relative concentration of Cl (C C0–1). Solid lines indicate the fitted model generated by HYDRUS-1D. A physical nonequilibrium model was fit to the Cl data and a quasi-combined physical and chemical nonequilibrium model was fit to the hormone data.

 





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Journal of Natural Resources
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Copyright © 2006 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.