Abstract
As part of a series of experiments in this laboratory to evaluate pyrophosphate as a source of phosphorus for plants1,2, attention has been given to the comparative rates of movement of orthophosphate and pyrophosphate in soil and to their adsorption isotherms.
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References
Sutton, C. D., and Larsen, S., Soil Sci., 97, 196 (1964).
Sutton, C. D., Gunary, D., and Larsen, S., Soil Sci., 101, 199 (1966).
Olsen, S. R., and Watanabe, F. S., Soil Sci. Soc. Amer. Proc., 21, 144 (1957).
Gunary, D., Hallsworth, E. G., and Crawford, D. V., Exp. Pedol. Proc. Univ. Nottingham Easter School Agric. Sci., 1964, 149 (1965).
Bodman, G. B., and Coleman, E. A., Soil Sci. Soc. Amer. Proc., 8, 116 (1943).
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GUNARY, D. Pyrophosphate in Soil; some Physico-chemical Aspects. Nature 210, 1297–1298 (1966). https://doi.org/10.1038/2101297a0
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DOI: https://doi.org/10.1038/2101297a0
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