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ABSTRACT
Soil-sulfur in Volcanic-ash derived soils was determined in soil extracts. The sulfur extracted was transformed into sulfate ions and organic matter destroyed by means of a 30% H2O2 solution. Sulfate ions were precipitated with a 15% BaCl2 solution and the precipitate then dissolved in (NH4)2 EDTA, and Barium determined by Atomic Absorption Spectrophotometry. Sulfur recovery was ascertained using an internal standard.
1 Contribution from the Department of Chemistry, Facultad de Química y Farmacia, Universidad de Chile, Santiago, Chile.
2 Assistant Professors and Professor of Analytical Chemistry respectively.
Received for publication April 29, 1969. Accepted for publication June 25, 1969.
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