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Removal of Fixed Ammonium from Clay Minerals by Cation Exchange Resins

Abstract

AMMONIUM in clay minerals that is not replaceable by K+ has been defined as fixed NH4 +. This fixed NH4 + is replaceable to some extent by Na+ and H+, but the amount that can be replaced depends upon the extraction method used. Recent work1,2 has shown that small amounts of K+ or NH4 + in the extracting solution block the replacement of fixed NH4 +. Thus, the efficiency of an equilibrium extraction of fixed NH4 + is decreased by the accumulation of displaced NH4 + in the extracting solution2. If a clay mineral containing fixed NH4 + were equilibrated with a cation exchange resin instead of a soluble salt, there would be less soluble K+ or NH4 + in the system. A comparison of these extraction methods was made, therefore, to determine if there was also less blocking and thus more fixed NH4 + removed in a resin extraction.

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References

  1. Hanway, J. J., et al., Soil Sci. Soc. Amer. Proc., 21, 29 (1957).

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  2. Scott, A. D., et al., Soil Sci. Soc. Amer. Proc., 22, 388 (1958).

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  3. Hanway, J. J., Iowa State Coll. J. Sci., 30, 374 (1956).

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SCOTT, A., EDWARDS, A. & BREMNER, J. Removal of Fixed Ammonium from Clay Minerals by Cation Exchange Resins. Nature 185, 792 (1960). https://doi.org/10.1038/185792a0

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