Determination of Trace Metals in Sodium Dithionite‐Citrate Extracts of Soils and Sediments by Atomic Absorption
Autor: | C. Simpson, J. W. Ball, E. A. Jenne |
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Rok vydání: | 1974 |
Předmět: |
chemistry.chemical_classification
Environmental Engineering Extraction (chemistry) Management Monitoring Policy and Law Dithionite Pollution law.invention Sodium dithionite Solvent Methyl isobutyl ketone chemistry.chemical_compound chemistry law Atomic absorption spectroscopy Dithiocarbamate Waste Management and Disposal Dissolution Water Science and Technology Nuclear chemistry |
Zdroj: | Journal of Environmental Quality. 3:281-287 |
ISSN: | 1537-2537 0047-2425 |
DOI: | 10.2134/jeq1974.00472425000300030021x |
Popis: | A general method has been developed for the analysis of Co, Cu, Ni, Mo, and Zn in dithionite-citrate extracts of soils and sediments. Because of the high Zn content of dithionite, it is necessary to preclean the dithionite-citrate solution before it is used to extract soils or sediments. This precleaning lowers the detection level significantly for other trace elements as well. Since Fe causes flame interferences in the determination of several first transition series elements by atomic absorption, the size of the individual sample aliquot taken to chelation-solvent concentration is varied to provide a constant quantity of Fe (5,000 µg). The standards and blanks are adjusted to the same Fe content. This approach is necessitated by the wide differences in the Fe concentrations of the dithionitecitrate extracts. Following pH adjustments and addition of ammonium-1-pyrrolidine dithiocarbamate, the trace metals (and Fe) are concentrated via two successive 10-ml methyl isobutyl ketone extractions. Quantities of Fe much greater than 5,000 µg interfere in the solvent concentration step. Natural organics released by the dissolution of free-Fe and -Mn oxides, to the extent that they are represented by fulvic acids, do not cause any significant interference in the ammonium-1-pyrrolidine dithiocarbamate methyl isobutyl ketone extraction of the trace metals due to the releasing effect of the Fe present. |
Databáze: | OpenAIRE |
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