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|  | | 为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。 | |
Combined with the sedimentary burial history and basin geothermal history, the modeling of carbon isotope kinetics provides a new and effective means for the determination of the origin and accumulation history of natural gas pools.
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The carbon isotopic characteristics of natural gas are not only affected by the gas source and maturity of the source rock, but also are related to the accumulation condition and geothermal gradient in a basin.
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Several natural associations composed of thermophilic anaerobic bacteria capable of utilizing various cellulose materials at 60 ± 2°C and pH 6.0-7.0 were isolated from the sludge of Kamchatka geothermal springs.
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The yeast grown in a medium containing geothermal water was shown to accumulate more amino acids.
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Mathematical model of water injection into a geothermal steam-saturated reservoir
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It is assumed that a layer of mantle matter, rising up or going down, enters a region of decompression (in which for a number of reasons the geotherm passes above the temperature of the solidus) and is subjected to partial fusion there.
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These results have been used to modify the previously constructed lower crust-upper mantle geotherm for the studied area.
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In this paper we focus on two kinds of problems generating the variational stress field, which is related to geotherm.
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In basaltic composition, CaCO3 (calcite and aragonite), the major carbonate phase in marine sediments, is altered into MgCO3 (magnesite) via reactions with Mg-bearing silicates under conditions that are 200-300°C colder than the mantle geotherm.
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Furthermore, CO2 itself breaks down to diamond and oxygen under geotherm conditions over 70?GPa, which might imply a possible mechanism for diamond formation in the lower mantle.
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Besides, greenhouses with a total area of 465?000 m2 use terrestrial heat in some regions of Russia.
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Terrestrial heat flow in Junggar Basin, Northwest China
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Temperature is an important factor affecting seismic velocity, and terrestrial heat flow is the most direct indication of temperature distribution of the lithosphere.
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Thermal energy transported by volcanic materials is compared with the terrestrial heat flow in the belt.
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Terrestrial heat flow, Q=K×ΔT/ΔZ cal/cm2 sec has been determined at 51 localities (39 on land and 12 in the sea) in and around the Japanese Islands.
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The use of geothermal energy: A reliable, cheap, and environmentally friendly method for generating electricity and heat
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It has higher resolution and greater depth penetration than the direct current method and is especially fit for geothermal energy exploration and low-and mid-level groundwater detection.
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Several variants of heat pipes for utilization of geothermal energy and underground rock heat are studied.
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Analysis of the exploitation of existing deep production wells for acquiring geothermal energy
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The aim of the work is to assess the possibility and usefulness of acquiring geothermal energy from the existing production well Jachówka K-2.
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