Feng J, Gao Z, Zhu R, Luo Z, Zhang L. The application of thermal conductivity measurements to the Kuqa River profile, China, and implications for petrochemical generation.
SPRINGERPLUS 2013;
2:580. [PMID:
24255869 PMCID:
PMC3824696 DOI:
10.1186/2193-1801-2-580]
[Citation(s) in RCA: 6] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 05/20/2013] [Accepted: 09/30/2013] [Indexed: 11/10/2022]
Abstract
Measurement of thermal conductivity of rocks is important to understand the thermal properties of earth materials, the characteristics of terrestrial heat flow, and the formation of oil. In this paper we report thermal conductivity, thermal diffusivity, and heat capacity data for 12 conglomerate, sandstone, and gypsum-bearing samples from the Paleogene Kuqa River profile in Kuqa, China. Samples were measured via the hot disk technique, yielding thermal conductivity values of 0.436 to 0.998 W/mK, thermal diffusivity measurements of 0.395 to 1.314 mm(2)/s, and heat capacity values of 0.439 to 1.717 MJ/m(3)K. These analyses reveal that gypsum-bearing rocks, with their low thermal conductivity, can act as excellent insulators over oil and gas reservoirs, aiding the formation and thermal maturation of petroleum.
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