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- W3022142854 abstract "Publisher SummaryThis chapter discusses the determination of carbon dioxide in silicate rocks. Most silicate rocks contain small amounts of carbon dioxide. The presence of carbonate minerals in silicate rocks is indicated by the effervescence that is obtained by warming with dilute acid. Shapiro and Brannock's apparatus is used for the determination of carbon dioxide in silicate rocks. The simplest procedures for determining carbon dioxide are based upon a measurement of the volume of gas liberated on heating the rock material with mineral acid. These procedures are not the most accurate and gravimetric procedures are to be preferred generally. A gas chromatographic procedure can be used for the rocks containing only traces of carbon dioxide. The chapter describes the Schrotter's apparatus used for the determination of carbon dioxide. It also discusses the determination of carbon dioxide using titrimetric method and gas chromatography. The chapter also discusses the determination of organic matter in silicate rocks. The separation of organic matter from both consolidated and unconsolidated sediments by extraction with organic solvents is an empirical procedure. Factors such as the weight of the sample in relation to the volume of solvent, the grain size to which the sample has been crushed or ground, the length of time during which the sample is extracted, and the particular solvent used can all materially affect the results." @default.
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- W3022142854 date "1981-01-01" @default.
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- W3022142854 title "Carbon" @default.
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- W3022142854 doi "https://doi.org/10.1016/b978-0-08-023806-7.50020-8" @default.
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