Thermal properties of rocks and density of fluids

Lev Eppelbaum*, Izzy Kutasov, Arkady Pilchin

*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

119 Scopus citations

Abstract

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.

Original languageEnglish
Title of host publicationLecture Notes in Earth System Sciences
PublisherSpringer International Publishing
Pages99-149
Number of pages51
Edition9783642340222
DOIs
StatePublished - 2014

Publication series

NameLecture Notes in Earth System Sciences
Number9783642340222
Volume0
ISSN (Print)2193-8571
ISSN (Electronic)2193-858X

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