Total cations in the size‐fractions of some british and malayan soils and their release to H+‐resins

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Abstract
Total K, Na, Ca and Mg in the sand, silt and clay of six British and four Malayan soils and the proportions released to H+‐resins in 1 h, 3, 10, 23 and 43 days were measured. The clays contained and released to the resins more K and Mg than coarser fractions. The release was continuous except from the acid Malayan soils which stopped releasing K after 3 days.More Mg was released to the resins than K, although no non‐exchangeable Mg but much non‐exchangeable K was released to ryegrass grown in the soils (after liming). This suggests that H+‐resins caused structural decomposition of the clay minerals which, together with the anomolous K release from acid soils, would limit their usefulness for measuring soil cations available to crops.