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Titlebook: Geothermics; Heat Flow in the Lit Vincenzo Pasquale,Massimo Verdoya,Paolo Chiozzi Book 2014 The Author(s) 2014 Conductive Heat.Geothermal F

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發(fā)表于 2025-3-21 17:12:01 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Geothermics
副標(biāo)題Heat Flow in the Lit
編輯Vincenzo Pasquale,Massimo Verdoya,Paolo Chiozzi
視頻videohttp://file.papertrans.cn/385/384175/384175.mp4
概述Offers a clear overview of the thermal structure of the Earth.Gives an insight into the formation processes and upwelling mechanisms of magma.Presents an interdisciplinary approach to the analysis of
叢書名稱SpringerBriefs in Earth Sciences
圖書封面Titlebook: Geothermics; Heat Flow in the Lit Vincenzo Pasquale,Massimo Verdoya,Paolo Chiozzi Book 2014 The Author(s) 2014 Conductive Heat.Geothermal F
描述After a brief review of global tectonics and the structure of the crust and upper mantle, the basic relations of conductive heat transport and the rock thermal properties are introduced as well as the various methods for measuring thermal conductivity and heat generation due to the decay of radioactive elements. The authors analyze geothermal flow and the thermal state of the lithosphere and deep interior and discuss the fundamental problems related to the formation, upwelling mechanisms, solidification and cooling of magmas. The text presents analytical methods that allow us to gain information on heat and groundwater flow from the analyses of temperature–depth data. It also provides ample data and examples to facilitate understanding of the different topics. This book is useful to researchers and graduate students interested in pure and applied geothermics.
出版日期Book 2014
關(guān)鍵詞Conductive Heat; Geothermal Flow; Heat in the Groundwater Flow; Lithosphere Thermal State; Magma Formati
版次1
doihttps://doi.org/10.1007/978-3-319-02511-7
isbn_softcover978-3-319-02510-0
isbn_ebook978-3-319-02511-7Series ISSN 2191-5369 Series E-ISSN 2191-5377
issn_series 2191-5369
copyrightThe Author(s) 2014
The information of publication is updating

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發(fā)表于 2025-3-22 00:01:43 | 只看該作者
https://doi.org/10.1007/978-3-658-29859-3operties. It is shown how the lithospheric thickness can be inferred from the elevation of the Earth’s surface in regions in isostatic equilibrium. The fundamentals of plate tectonics, the mechanisms which provide the energy dissipated in earthquakes, volcanic eruptions and orogenesis, and the force
板凳
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https://doi.org/10.1007/978-3-642-46511-6ivity and radiogenic heat. Also, it outlines the most commonly used techniques for estimating these parameters. Models involving the application of mixing laws for a mineral aggregate are discussed together with techniques for estimating the in situ thermal conductivity and volumetric heat capacity.
地板
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An Introduction to Phase Diagrams, of the lithosphere. Changes in surface temperature can cause fluctuations in the temperature of the uppermost crustal layers. The geothermal flow can be envisaged as a combination of the heat generated from the rock radioactive elements, a transient component caused by tectothermal processes, and t
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307 Towards Vibrational Models,ilibrium with the surrounding rocks. The magmatic fluid attempts to find an equilibrium condition through energy and mass transfer from the bottom upwards. The volcanic activity is therefore the surface expression of a redistribution of the internal energy of the Earth through an advection mechanism
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發(fā)表于 2025-3-22 13:37:38 | 只看該作者
Heavy Ion Spherical Optical Model, the heat transport associated with water flow. This chapter presents some analytical methods and shows how subsurface temperatures can provide a quantitative tool for inferring water flow in permeable layers and heat advection in hydrothermal systems. Thermal convection in deep aquifers and its pot
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Geothermics978-3-319-02511-7Series ISSN 2191-5369 Series E-ISSN 2191-5377
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