Thermal Properties of Rocks and Density of Fluids
Thermal Properties of Rocks and Density of Fluids
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DOI：
10.1007/978-3-642-34023-9_2
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发表时间：
2014-01-01
期刊：
影响因子：
--
通讯作者：
Pilchin, Arkady
中科院分区：
文献类型：
--
作者：
Eppelbaum, Lev;Kutasov, Izzy;Pilchin, Arkady
本章描述了最重要的热学参数，如电导率、容量、磁导率以及这些参数之间的相互关系。在某些情况下，热各向异性的影响可能会显著改变所研究的地热模式。研究岩石和矿物的熔点、温度和压力对岩石和矿物的热物性和流体密度的影响在深部地热模型的发展中起着重要的作用。结果表明，早期地球大气的分析对于探测现代地球地热状况的某些特征具有重要意义。
This Chapter describes the most important thermal parameters such as conductivity, capacity, duffusivity and interrelation of these parameters between themselves. Effect of thermal anisotropy in some cases may significantly change the studied geothermal pattern. Investigation of melting points of rocks and minerals, and temperature and pressure influence to thermal properties of rocks and minerals and fluid density play an important role in development of deep geothermal models. It is shown that analysis of the early Earth atmosphere is significant for detecting some peculiarities of the modern geothermal regime of the Earth.