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ABSTRACT
Saturation extract, hot water-soluble, acid-soluble, and total B fractions were determined in soil samples from profiles representing six geographically diverse areas in Egypt. Saturation extract and hot water-soluble B averaged 0.6 µg/ml and 1.3 µg/g. Acid-soluble and total B averaged 10.2 and 113 µg/g. The acid fraction showed a curvilinear relationship with CaCO3 content of the soil, and averaged 12.5% of the total B. Total B, on the average, was twice as high in clay samples as in sandy samples, and decreased by about 32% beyond the 60-cm depth of the soil profile. Concentrations of saturation extract B were either similar to or a reasonable multiple of Nile-Water B, indicating that the latter is a direct source of at least water soluble B in these soils. Concentrations of water and acid-soluble B suggest that B status in soils of Egypt is above the sufficiency level, and that under proper soil and water management the incidence of toxicity is unlikely.
1 Contribution from the Dept. Soil and Water Science, Faculty of Agriculture, Alexandria Univ., Alexandria, Egypt, and the Dept. of Soil and Environmental Sciences, Univ. of California, Riverside, CA 92521.
2 Formerly Associate Professor of Soil Science and Graduate Student, respectively, Dept. of Soil and Water Science, Faculty of Agriculture, Alexandria Univ., Alexandria, Egypt. Present address of the senior author is Dept. of Soil and Environmental Sciences, Univ. of California, Riverside, CA 92521.
Received for publication March 20, 1978. Accepted for publication November 7, 1978.
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