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Titlebook: Geothermal Fluids; Chemistry and Explor Keith Nicholson Book 1993 Springer-Verlag Berlin Heidelberg 1993 Gas.Geochemie.Geothermal.Geothermi

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發(fā)表于 2025-3-21 17:45:27 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Geothermal Fluids
副標(biāo)題Chemistry and Explor
編輯Keith Nicholson
視頻videohttp://file.papertrans.cn/385/384170/384170.mp4
圖書封面Titlebook: Geothermal Fluids; Chemistry and Explor Keith Nicholson Book 1993 Springer-Verlag Berlin Heidelberg 1993 Gas.Geochemie.Geothermal.Geothermi
描述This book introduces aqueous geochemistry applied to geothermal systems. It is specifically designed for readers first entering into the world of geothermal energy from a variety of scientific and engineering backgrounds, and consequently is not intended to be the last word on geothermal chemistry. Instead it is intended to provide readers with sufficient background knowledge to permit them to subsequently understand more complex texts and scientific papers on geothermal energy. The book is structured into two parts. The first explains how geothermal fluids and their associated chemistry evolve, and shows how the chemistry of these fluids can be used to, deduce information about the resource. The second part concentrates on survey techniques explaining how these should be performed and the procedures which need to be adopted to ensure reliable sampling and analytical data are obtained. A geothermal system requires a heat source and a fluid which transfers the heat towards the surface. The fluid could be molten rock (magma) or water. This book concentrates on the chemistry of the water, or hydrothermal, systems. Consequently, magma-energy systems are not considered. Hot-dry rock (HD
出版日期Book 1993
關(guān)鍵詞Gas; Geochemie; Geothermal; Geothermie; Isotope; Reservoir; Wasser; Water; geochemistry; geothermal energy
版次1
doihttps://doi.org/10.1007/978-3-642-77844-5
isbn_softcover978-3-642-77846-9
isbn_ebook978-3-642-77844-5
copyrightSpringer-Verlag Berlin Heidelberg 1993
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發(fā)表于 2025-3-21 22:09:27 | 只看該作者
Water Chemistrywaters encountered within the profile of a geothermal field are commonly derived from this deep fluid as a consequence of chemical or physical processes. These waters, the characteristics of which are described below, are classified according to the dominant anions. Although not a formal genetic sch
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發(fā)表于 2025-3-22 02:13:58 | 只看該作者
地板
發(fā)表于 2025-3-22 06:59:02 | 只看該作者
Isotope Chemistrymic number, but are distinguished on the basis of different atomic masses (mass number, A = number of protons + number of neutrons). These differences in atomic mass are caused by the gain or loss of neutrons. Isotopes of an element display slight differences in their chemical and physical behaviour
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發(fā)表于 2025-3-22 12:43:40 | 只看該作者
Water Surveysassodated sources of error. However, before a sample can be analysed it must be collected, and it is this aspect of the analytical programme than can be neglected; Bad sampling techniques can invalidate a survey and are far more costly to correct than analytical errors. Laboratory errors or mistakes
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發(fā)表于 2025-3-22 14:16:43 | 只看該作者
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發(fā)表于 2025-3-22 17:13:48 | 只看該作者
Soil and Soil-Gas Surveysw and where the extent of the field is not known, soil and soil-gas surveys can prove helpful. These surveys can identify permeable regions in a field and possible upflow or boiling zones. They can also delineate the margins of a geothermal system, and therefore often complement geophysical surveys
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https://doi.org/10.1007/978-3-642-77844-5Gas; Geochemie; Geothermal; Geothermie; Isotope; Reservoir; Wasser; Water; geochemistry; geothermal energy
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發(fā)表于 2025-3-23 07:24:31 | 只看該作者
Evolutionism and the Africanist Project,the different types of geothermal system has distinct characteristics which are reflected in the chemistry of the geothermal fluids and their potential applications. However, they all have in common a heat source at a few kilometres depth, and it is this which sets water, present in the upper sectio
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