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- W2017637462 abstract "Measurements of pH and A1 concentration were made on 10-2 M CaCl2, suspensions of a number of acid soils that had been limed to give 3 range of pH values, and exchangeable A1 and Ca+Mg were determined in 1.0 M NH4Cl extracts. The variation of pH with A1 concentration did not support the theory that pH is controlled by the solubility of Al(OH)3. For some of the soils, proton release on hydrolysis of A13+ions in solution accounted for the pH values, and explained quantitatively the variation of pH with the Ca:Al balance of the exchange complex, taking account of the selectivity coefficient for exchange, Kca→A1 Although Kca→A1 was smaller for soils containing more humus, their pH values were also less than those predicted by the hydrolysis of A13+ in solution, indicating that they contained other sources of protons, presumably the carboxyl groups in humus." @default.
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- W2017637462 date "1974-09-01" @default.
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- W2017637462 title "SOLUBLE ALUMINIUM AND CALCIUM-ALUMINIUM EXCHANGE IN RELATION TO THE pH OF DILUTE CALCIUM CHLORIDE SUSPENSIONS OF ACID SOILS" @default.
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- W2017637462 doi "https://doi.org/10.1111/j.1365-2389.1974.tb01128.x" @default.
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