期刊
PLANT AND SOIL
卷 279, 期 1-2, 页码 107-117出版社
SPRINGER
DOI: 10.1007/s11104-005-0437-2
关键词
K-d; nutrient uptake modeling; partition coe. cient; phosphorus bioavailability; tropical soil
Developing desorption isotherms for inorganic phosphorus (P) is a time-consuming and non-standardized procedure. Anion exchange membranes (AEMs) have been successfully used in studies of P desorption kinetics and total membrane-desorbable P, but rarely have they been used for developing P desorption isotherms. Our study had two objectives: (1) to evaluate the suitability of using multiple strips of AEMs (termed the Multiple AEM Method) to develop P desorption isotherms; and (2) to compare the Multiple AEM Method with a sequential-extraction approach using AEMs (termed the Sequential AEM Method) to determine if the manner in which AEMs were used would influence the slope of the desorption isotherm, i.e. the partition coefficient. Both methods yielded well-defined, but numerically different desorption isotherms for all levels of sorbed P. However, estimated K-d values among methods were equivalent in the low and medium levels of P sorbed. The Multiple AEM method was quicker than the Sequential AEM method, but both gave similar K-d values in an agriculturally significant range of soil solution concentrations. These methods should be tested on a range of soil type to determine their suitability in developing P desorption isotherms and to move toward method standardization for desorption isotherms.
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