globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-012-0820-1
Scopus记录号: 2-s2.0-84874019310
论文题名:
Thermal conductivity of short sequences of rock
作者: Jessop A.M.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2013
卷: 102, 期:2
起始页码: 483
结束页码: 491
语种: 英语
英文关键词: Measurement ; Mineral content ; Sample size ; Simulation ; Thermal conductivity
Scopus关键词: computer simulation ; error analysis ; igneous rock ; numerical model ; quartz ; thermal conductivity
英文摘要: Numerical models of igneous rock samples provide estimates of the variation in conductivity of discs cut from lengths of core. Ten discs cut from a piece of core have a root mean squared deviation of up to 6 %, depending on quartz content and crystal size. Greater crystal size increases the apparent conductivity of a disc by up to 3. 2 % when quartz content is 49 %, but less when quartz content is 30 % or less. Measured conductivity depends on the thickness of the measured disc. When quartz content is low, this difference is well within the normal limits of experimental error, but when quartz content is high, the apparent conductivity will be within the normal limits of experimental error only when the disc is at least 8 mm thick. The estimation of contact resistance between the sample and the bar by using sets of discs of different thickness is unreliable because of variation in mineral content between contiguous discs. Better representation of the conductivity profile is obtained by measuring single discs with an estimation of the contact resistance. © 2012 Her Majesty the Queen in Right of Canada.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84874019310&doi=10.1007%2fs00531-012-0820-1&partnerID=40&md5=034b956e2e924a55f0b33c8ae5043e19
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70576
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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作者单位: 333 Silver Ridge Crescent NW, Calgary, AB, T3B 3T6, Canada; Geological Survey of Canada, 3303, 33 Street NW, Calgary, AB, T2L 2A7, Canada

Recommended Citation:
Jessop A.M.. Thermal conductivity of short sequences of rock[J]. International Journal of Earth Sciences,2013-01-01,102(2)
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