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一种用于测定油页岩及相关岩石中硫形态的分析方案。

An analytical scheme for determining forms of sulphur in oil shales and associated rocks.

作者信息

Tuttle M L, Goldhaber M B, Williamson D L

机构信息

U.S. Geological Survey, MS 916, Box 25046, Denver Federal Center, Denver, CO 80225, U.S.A.

出版信息

Talanta. 1986 Dec;33(12):953-61. doi: 10.1016/0039-9140(86)80234-x.

DOI:10.1016/0039-9140(86)80234-x
PMID:18964237
Abstract

An analytical scheme for determining various forms of sulphur in oil shales and associated rocks is presented. Acid-soluble sulphate, sulphur contained in monosulphide and in disulphide minerals, and organically-bound sulphur are all quantitatively recovered as separate fractions. Finely-ground oil-shale samples are treated in an inert atmosphere with 6M hydrochloric acid to dissolve the acid-soluble sulphate minerals and form H(2)S from the decomposition of monosulphide minerals. The acid-soluble sulphate is precipitated as barium sulphate and the H(2)S is collected and weighed as silver sulphide. Disulphide minerals in the solid residue from the acid treatment are reduced by an acidified Cr(II) solution in an inert atmosphere, releasing the sulphide as H(2)S. The H(2)S is collected as silver sulphide. An Eschka fusion oxidizes and solubilizes all sulphur remaining within the Cr(II)-treated residue. This sulphate represents organically-bound sulphur and is collected as barium sulphate. The analytical procedures have been verified by using (57)Fe Mössbauer spectroscopy. Good agreement between the chemical and Mössbauer data substantiated the sequential removal of the forms of sulphur and also demonstrated the ability of Mössbauer spectroscopy to determine the absolute quantities of iron present in specific minerals.

摘要

本文提出了一种测定油页岩及相关岩石中各种硫形态的分析方案。酸溶性硫酸盐、单硫化物和二硫化物矿物中所含的硫以及有机结合硫都能作为单独的馏分进行定量回收。将细磨的油页岩样品在惰性气氛中用6M盐酸处理,以溶解酸溶性硫酸盐矿物,并使单硫化物矿物分解生成H₂S。酸溶性硫酸盐以硫酸钡形式沉淀,H₂S收集后以硫化银形式称重。酸处理后固体残渣中的二硫化物矿物在惰性气氛中用酸化的Cr(II)溶液还原,释放出的硫化物以H₂S形式存在。H₂S以硫化银形式收集。艾氏熔剂法可氧化并溶解Cr(II)处理后残渣中剩余的所有硫。该硫酸盐代表有机结合硫,以硫酸钡形式收集。分析程序已通过使用⁵⁷Fe穆斯堡尔光谱法进行了验证。化学数据和穆斯堡尔数据之间的良好一致性证实了硫形态的顺序去除,同时也证明了穆斯堡尔光谱法测定特定矿物中存在的铁绝对量的能力。

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