4.2 Article

Boron fractionation in some Saskatchewan soils

期刊

CANADIAN JOURNAL OF SOIL SCIENCE
卷 82, 期 2, 页码 173-179

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AGRICULTURAL INST CANADA
DOI: 10.4141/S01-027

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boron fractionation; exchangeable B; extractable B; organically bound B; soil; soluble B

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Raza, M., Mermut, A. R., Schoenau, J. J. and Malhi, S. S. 2002. Boron fractionation in some Saskatchewan soils. Can. J. Soil Sci. 82: 173-179. Knowledge of B fractions is essential for understanding its chemistry and potential contribution to plant uptake. Four different extraction methodologies to determine readily available B were compared, using a four-step sequential B fractionation procedure, to reveal the nature of soil B in nine selected soils from the Brown and Gray Luvisol zones with different textures and management histories. The four soil extraction techniques were: hot water (HW), 0.01M CaCl2, 1 M NH4-acetate and anion exchange membranes (AEM). The other four fractions, specifically adsorbed, oxide bound, organically bound, and residual B were determined sequentially on the same soil samples. On average, HW extracted more B than 0.01M CaCl2, 1 M NH4-acetate, and AEM. In almost every soil, readily soluble B represented only a small proportion of the total B content, regardless of the extraction method used. Most soil B existed in the residual or occluded form, which accounted for between 92 and 99%, with an average of 97%, of the total soil B. The concentration of organically bound B was higher than that of oxide bound B and specifically adsorbed B, irrespective of the readily soluble B extracting solution used. Cation exchange capacity (CEC) appeared to be an important characteristic to predict the B pools. No significant correlation was found between soil organic carbon content and the different B pools, except for hot water soluble (HWS) B. Correlation coefficients between the B pools and particle size distribution were poor and correlation between carbonates and B pools were insignificant. The findings suggest that in Saskatchewan soils, readily soluble B is only a small proportion of the total B, and the majority of B exists as residual or occluded form. Hot water soluble B appears to be a good method to estimate available B. We found this method rather simple, efficient, and consistent.

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