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Volumn 112, Issue 27, 2008, Pages 9980-9982

High pressure pair distribution function studies of Green River oil shale

Author keywords

[No Author keywords available]

Indexed keywords

AMBIENT PRESSURE; BULK MODULUS; COMPRESSION BEHAVIOR; CRYSTALLINE QUARTZ; GREEN RIVER; HIGH PRESSURE; IN-SITU; PAIR DISTRIBUTION FUNCTION; PARIS-EDINBURGH CELL; PRESSURE RANGES; REAL-SPACE; SINGLE-PHASE MODEL; STRUCTURAL INFORMATIONS; STRUCTURAL MODEL; THREE PHASE;

EID: 48249093100     PISSN: 19327447     EISSN: 19327455     Source Type: Journal    
DOI: 10.1021/jp803900s     Document Type: Article
Times cited : (2)

References (29)
  • 2
    • 49249118879 scopus 로고    scopus 로고
    • Andrews, A. Oil Shale: History, Incentives, and Policy; Congress Research Service, The Library of Congress: Washington, DC, 2006, RL33359.
    • Andrews, A. Oil Shale: History, Incentives, and Policy; Congress Research Service, The Library of Congress: Washington, DC, 2006, RL33359.
  • 22
  • 27
    • 48249151756 scopus 로고
    • Saxby, J. D. Fuel 1981, 60, 994-996.
    • (1981) Fuel , vol.60 , pp. 994-996
    • Saxby, J.D.1
  • 28
    • 0023981644 scopus 로고    scopus 로고
    • Kerogens are known to exhibit glass-rubber transitions (see Parks, T. J.; Lynch, L. J.; Webster, D. S.; Barrett, D. Energy Fuels 1988, 2, 185-190.). Although such transitions have been found to occur at temperatures above that of the present study, the processes used to isolate the kerogen from the mineral matrix in those studies also eliminates the smaller organic molecules. Consequently, the glass transition temperature for the organic material within the raw oil shale is likely to be systematically lower than for the isolated kerogen and the present sample is likely to contain a greater fraction of rubber-like organic component than found in isolated kerogen.
    • Kerogens are known to exhibit glass-rubber transitions (see Parks, T. J.; Lynch, L. J.; Webster, D. S.; Barrett, D. Energy Fuels 1988, 2, 185-190.). Although such transitions have been found to occur at temperatures above that of the present study, the processes used to isolate the kerogen from the mineral matrix in those studies also eliminates the smaller organic molecules. Consequently, the glass transition temperature for the organic material within the raw oil shale is likely to be systematically lower than for the isolated kerogen and the present sample is likely to contain a greater fraction of rubber-like organic component than found in isolated kerogen.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.