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Published online 6 January 2006
Published in Soil Sci Soc Am J 70:297-304 (2006)
DOI: 10.2136/sssaj2005.0200
© 2006 Soil Science Society of America
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Adsorption of Polyacrylamide on Smectite, Illite, and Kaolinite

Youjun Dengb,*, Joe B. Dixona and G. Norman Whitea

a Dep. of Soil and Crop Sciences, Texas A&M Univ., College Station, TX 77843-2474
b current address: Dep. of Crop and Soil Sciences, Washington State Univ., Pullman, WA 99164-6420



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Fig. 1. Settlement of smectite in the presence of (a) anionic PAM 836A, (b) nonionic PAM 903N, and (c) cationic PAM 494C. Six hours after mixing the polymers and clay suspension. Illite and kaolinite suspensions had similar responses to the polymer solutions as smectite suspension had.

 


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Fig. 2. Concentration of clay remained in suspension after settling for 6 h in the presence of (a) anionic PAM 836A, (b) nonionic PAM 903N, and (c) cationic PAM 494C.

 


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Fig. 3. Effect of pH on the adsorption of (a) anionic PAM 836A, (b) nonionic PAM 903N, and (c) cationic PAM 494C on smectite, illite, and kaolinite.

 


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Fig. 4. Adsorption isotherms of (a) anionic PAM 836A, (b) nonionic PAM 903N, and (c) cationic PAM 494C on smectite, illite, and kaolinite.

 


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Fig. 5. Accumulative amount of desorbed polymers from clays by four consecutive water washing: (a) anionic PAM 836A, (b) nonionic PAM 903N, and (c) cationic PAM 494C.

 


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Fig. 6. X-ray diffraction patterns of (a) Ca-smectite, (b) anionic PAM 836A-smectite, (c) nonionic PAM 903N-Smectite, and (d) cationic PAM 494C-smectite after 4-h heating at each sequentially increased temperature.

 


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Fig. 7. Cation exchange capacities of smectite, illite, kaolinite, and their PAM complexes; and the amount of adsorbed Cu and Cr on the clays and complexes.

 


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Fig. 8. X-ray diffraction patterns of glycerol solvated (a) Ca-smectite, (b) anionic PAM 836A-smectite, (c) nonionic PAM 903N-smectite, and (d) cationic PAM 494C-smectite.

 





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