Solubility and Redox Equilibria of Iron Compounds in Soils

Author:

Lindsay Willard L.

Publisher

Springer Netherlands

Reference23 articles.

1. Back, W., and I. Barnes. 1965. Relation of electrochemical potentials and iron content to groundwater flow patterns. U.S. Geol. Survey Prof. Paper 398-C. U.S. Government Printing Office, Washington, DC.

2. Barnes, I., and W. Back. 1964. Geochemistry of iron-rich groundwater of southern Maryland. J. Geol. 72:435–447.

3. Breemen, N. van. 1976. Genesis and Solution Chemistry of Acid Sulfate Soils in Thailand. Agric. Res. Rept. (Versl. landbouwk. Onderz.) 848. Center for Agric. Pub. and Documentation, Wageningen, The Netherlands.

4. Chukhrov, F. V., B. B. Zvyagin, L. P. Ermilova, and A. I. Gorshkov. 1972. New data on iron oxides in the weathering zone. p. 397–404. In J. M. Serratosa (ed.)Proc. Int. Clay Conf., Madrid, 1972. Div. Ciencias C.S.I.C., Madrid.

5. Cline, G. R., P. E. Powell, P. J. Szaniszlo, and C. P. P. Reid. 1982. Comparison of the abilities of hydroxamic, synthetic, and other natural organic acids to chelate iron and other ions in nutrient solution. Soil Sci. Soc. Am. J. 46:1158–1164.

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