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Titlebook: Geysers and Geothermal Energy; John S. Rinehart Book 1980 Springer-Verlag New York Inc. 1980 Energy.Fundament.Geothermische Energie.Geysir

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書目名稱Geysers and Geothermal Energy
編輯John S. Rinehart
視頻videohttp://file.papertrans.cn/386/385671/385671.mp4
圖書封面Titlebook: Geysers and Geothermal Energy;  John S. Rinehart Book 1980 Springer-Verlag New York Inc. 1980 Energy.Fundament.Geothermische Energie.Geysir
描述Geysers. What makes them work? Many who have seen a geyser in action know only that it spouts hot water into the air. Many others have never seen one. Chapter 1, Geysers of the World, delineates their distinguishing features, locates the geyser regions of the world, and places investigations by world travelers and scientists in historic perspective. One of the quickest ways to become acquainted with a geyser is to observe it. The descriptions of several well known geysers, some based on past observations by others, but frequently by me, do not neces- sarily portray current behavior. They do, however, represent general features. Geysers exist as a result of a delicate and unique interplay among the heat, the water, and the rocks of the earth. In essence, heat and water must be available, transported, distributed, stored, and finally released. Chapter 2, The Geologic, Thermal, and Hydrologic State of the Earth, especially that close to its surface, sets the stage for Chapter 3, Fundamentals of Geyser Operation. The geyser is treated here as a simple system consisting of three major interacting elements: a source of water, a source of heat, and a reservoir for storing water. The discu
出版日期Book 1980
關(guān)鍵詞Energy; Fundament; Geothermische Energie; Geysir; Reservoir; earthquake; seismic
版次1
doihttps://doi.org/10.1007/978-1-4612-6084-4
isbn_softcover978-1-4612-6086-8
isbn_ebook978-1-4612-6084-4
copyrightSpringer-Verlag New York Inc. 1980
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Maureen Bricker,Vasant Thakkar,John Petrill less dense crust varying in thickness from 5 to 70 km, overlies the mantle, the thinnest parts of which lie under the ocean. Thicker sections form the continents and the thickest parts lie beneath the mountains (see Fig. 2–1).
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Daniel Day,Stephen Weber,Min Guural geysers whose detailed plumbing systems are unknown, and except in the uppermost reaches of the vent, inaccessible for making temperature and other measurements. Besides this, wells can in most cases be freely regulated and tampered with.
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