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2014 | OriginalPaper | Buchkapitel

2. Thermal Properties of Rocks and Density of Fluids

verfasst von : Lev Eppelbaum, Izzy Kutasov, Arkady Pilchin

Erschienen in: Applied Geothermics

Verlag: Springer Berlin Heidelberg

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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.

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Vorheriges Kapitel The Thermal Field of the Earth

Nächstes Kapitel Methods of Thermal Field Measurements

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Titel: Thermal Properties of Rocks and Density of Fluids
verfasst von: Lev Eppelbaum
Izzy Kutasov
Arkady Pilchin
Verlag: Springer Berlin Heidelberg
Buch: Applied Geothermics
Print ISBN: 978-3-642-34022-2

Electronic ISBN: 978-3-642-34023-9

Copyright-Jahr: 2014
DOI: https://doi.org/10.1007/978-3-642-34023-9_2

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Abstract

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