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Phosphorus Retention Mechanisms of a Water Treatment Residual

J. A. Ippolito*,a, K. A. Barbaricka, D. M. Heila, J. P. Chandlerb and E. F. Redenteb

a Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523-1170
b Department of Forest, Rangeland, and Watershed Stewardship, Colorado State University, Fort Collins, CO 80523-1170



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Fig. 1. The influence of shaking time on P-loaded water treatment residual (WTR) solution pH.

 


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Fig. 2. The influence of shaking time on Ca desorption from P-loaded water treatment residual (WTR).

 


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Fig. 3. The influence of shaking time on Al desorption from P-loaded water treatment residual (WTR).

 


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Fig. 4. The influence of shaking time on P desorption from P-loaded water treatment residual (WTR).

 


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Fig. 5. The influence of shaking time on P mineral solubility from P-loaded water treatment residual (WTR). Adapted from Lindsay (1979). DCP, dicalcium phosphate (CaHPO4); DCPD, dicalcium phosphate dibasic (CaHPO4·2H2O); OCP, octacalcium phosphate [Ca4H(PO4)3·2.5H2O]; TCP, tricalcium phosphate [Ca3(PO4)2].

 


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Fig. 6. Backscattered electron (BSE) image and wavelength dispersive spectroscopy dot maps of Ca, P, and Al of sample Day 1. The light-colored portions on the dot maps indicate the presence of Ca, P, or Al.

 


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Fig. 7. Backscattered electron (BSE) image and wavelength dispersive spectroscopy dot maps of Ca, P, and Al of sample Day 211. The light-colored portions on the dot maps indicate the presence of Ca, P, or Al.

 





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