A review of the organic geochemistry of shales
Shale formations have been suggested as a potential site for a high level nuclear waste repository. As a first step in the study of the possible interaction of nuclides with the organic components of the shales, literature on the identification of organic compounds from various shales of the continent of the United States has been reviewed. The Green River shale of the Cenozoic era is the most studied shale followed by the Pierre shale of the Mesozoic era and the Devonian black shale of the Paleozoic era. Organic compounds that have been identified from these shales are hydrocarbons, fatty acids, fatty alcohols, steranes, terpanes, carotenes, carbohydrates, amino acids, and porphyrins. However, these organic compounds constitute only a small fraction of the organics in shales and the majority of the organic compounds in shales are still unidentified.
- Research Organization:
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
- DOE Contract Number:
- AC05-84OR21400
- OSTI ID:
- 6338030
- Report Number(s):
- ORNL/TM-10474; ON: DE87011889; TRN: 87-025453
- Resource Relation:
- Other Information: Portions of this document are illegible in microfiche products
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
58 GEOSCIENCES
SHALES
CHEMICAL COMPOSITION
ALCOHOLS
AMINO ACIDS
CARBOHYDRATES
CARBOXYLIC ACIDS
CAROTENOIDS
HIGH-LEVEL RADIOACTIVE WASTES
HYDROCARBONS
ORGANIC COMPOUNDS
PORPHYRINS
RADIOACTIVE WASTE DISPOSAL
HETEROCYCLIC ACIDS
HETEROCYCLIC COMPOUNDS
HYDROXY COMPOUNDS
MANAGEMENT
MATERIALS
ORGANIC ACIDS
ORGANIC NITROGEN COMPOUNDS
PIGMENTS
RADIOACTIVE MATERIALS
RADIOACTIVE WASTES
ROCKS
SEDIMENTARY ROCKS
TERPENES
WASTE DISPOSAL
WASTE MANAGEMENT
WASTES
052002* - Nuclear Fuels- Waste Disposal & Storage
580400 - Geochemistry- (-1989)