Titlebook: Geothermics; An Introduction Günter Buntebarth Textbook 1984 Springer-Verlag, Berlin Heidelberg 1984 Geothermik.energy.energy consumption.e

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書目名稱Geothermics影響因子(影響力)




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書目名稱Geothermics網(wǎng)絡(luò)公開度




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Climate

Analytical Treatment of Conductive Cooling in the Crust,such as magmatic intrusions or volcanic events, as thermal equilibration processes based on heat conduction. Whereas tectonic events can hardly by treated without convective heat transport, intrusions or volcanic events can be modelled with thermal equilibration based on conduction only. In geologic

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Geothermal Heat as an Energy Source, broadest sense of the term, is relatively evenly distributed in the earth. But it is economically feasible to harness this energy only when conditions are favorable. This is only true for volcanically young areas where hot steam can be found close to the surface and can be economically converted in

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,Marshall’s ‘Economic Biology’,such as magmatic intrusions or volcanic events, as thermal equilibration processes based on heat conduction. Whereas tectonic events can hardly by treated without convective heat transport, intrusions or volcanic events can be modelled with thermal equilibration based on conduction only. In geologic

方舟

B. Harte,D. R. M. Pattison,C. M. Linklatercontinuous thermal evolution. The thermal state which it has now reached can be estimated by direct and indirect means. However the difficulties in estimating temperature increase rapidly with depth. At present it is difficult to plot an accurate temperature map for crustal depths of only 10 km even

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Survival under Production Uncertainty,Temperature is one of the most important physical properties of the earth. It is both spacially variable and time-dependent, on a variety of time scales, from the variation of surface temperature in the course of a year to the thermal evolution of the entire planet, which takes billions of years.

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Competition and Increasing Returns,Thermal conductivity K is an important physical quantity in the transport of heat. It both controls temperature gradients in individual layers of the earth’s crust under stationary conditions and determines the time scale for transient processes such as the cooling of intrusive bodies.