爱尔兰岩石的导热性

Q4 Earth and Planetary Sciences Irish Journal of Earth Sciences Pub Date : 2022-01-01 DOI:10.3318/IJES.2018.36.63
M. Long, S. Murray, R. Pasquali
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引用次数: 2

摘要

摘要:本文建立了爱尔兰50个岩层的导热系数数据库。所有的测试都是在都柏林大学学院(UCD)的一个单隔板装置上进行的。这项工作的目的是为爱尔兰未来中小型地热项目的设计提供导热系数输入参数。为了证明UCD分棒装置的可靠性和可重复性,在另外两台独立装置上进行了重复试验和附加试验。结果之间的误差通常在±5%以内。所得的热导率值在一个狭窄的范围内,与世界上公布的其他地方发现的类似岩石的值一致。岩石孔隙度和矿物成分的相对丰度是影响热导率的主要因素。热导率随深度和岩石密度没有变化。对一些岩性的1.8毫米至5毫米大小的岩屑进行了进一步的导热性测试;建议这可能是一个可行的测量技术,虽然需要进一步的测试来验证这一点。
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Thermal conductivity of Irish rocks
Abstract:A database of thermal conductivity values for 50 formations of Irish rock has been established and is presented here. All of the testing was carried out on a single divided bar apparatus at University College Dublin (UCD). The aim of this work is to provide thermal conductivity input parameters for the design of future small to medium-scale geothermal projects in Ireland. Some tests were repeated and additional tests were carried out on two other independent devices in order to prove the reliability and repeatability of the UCD divided bar device. Results were generally found to be within ±5% of one another. The resulting thermal conductivity values are in a narrow range and are consistent with worldwide published values for similar rocks found elsewhere. Rock porosity and the relative abundances of the mineral compositions were found to be the main controlling factors on the thermal conductivity values. No variation with thermal conductivity with depth or rock density was found. Further thermal conductivity tests carried out on rock chippings, 1.8mm to 5mm in size, of some of the lithologies; suggest that this may be a viable measurement technique, though further testing is required to verify this.
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来源期刊
Irish Journal of Earth Sciences
Irish Journal of Earth Sciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
0.90
自引率
0.00%
发文量
2
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