Adsorption strength of zinc for soil humus
Open Access
- 1 July 1969
- journal article
- research article
- Published by Taylor & Francis in Soil Science and Plant Nutrition
- Vol. 15 (4) , 169-174
- https://doi.org/10.1080/00380768.1969.10432797
Abstract
Soil humus plays a significant role in the cation exchange of a soil. YOSHIDA (1) showed that, as a general rule, divalent ions such as calcium and magnesium were adsorbed more strongly onto humus than monovalent ions such as ammonium and potassium in an ion-exchange reaction. He did not, however, describe the behavior of heavy metal ions. BREMNER et al. (2) first suggested that soil organic matter forms complexes with polyvalent cations. HIMES and BARBER (3) found that soil organic matter reacts with divalent metal ions in a manner similar to the chelation reaction. Reviews of the soil organic matter-metal complex have been written by BREMNER et al. (2) and KAWAGUCHI, MATSUO and KYUMA (4).Keywords
This publication has 3 references indexed in Scilit:
- Chelating Ability of Soil Organic MatterSoil Science Society of America Journal, 1957
- Metal complexes in soils.Australian Journal of Agricultural Research, 1955
- Metallo-organic Complexes in SoilNature, 1946