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geothermal     
相关语句
  地热
     Study of the Tectonic-thermal Evolution of the Songliao Basin and Quantitative Assessment of Its Geothermal Resource: A Case Study on the Dumeng District
     松辽盆地构造热演化及地热资源定量评价研究——以杜蒙地区为例
短句来源
     Study on Generating Mechanism and Evaluation of Low-Medium Temperature Geothermal System
     中低温地热系统形成机制及评价研究
短句来源
     Perspective Prognosis on Geothermal Resource in Synthetic Information in Shandong Province
     山东省地热资源综合信息远景预测
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     BACKGROUND ANALYSES OF CHEMICAL THERMOMECHA- NICS OF A STRONG AFTERSHOCK IN GEOTHERMAL ANOMALY AREA
     地热异常区一次强余震的化学热力学背景分析
短句来源
     SURVEY OF RADIONUCLIDES IN GEOTHERMAL WATER IN BEIJING
     北京地热水中放射性核素初步调查
短句来源
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  地温
     the geothermal gradient is 4. 0~4. 8℃/100m, the average is 4. 26℃/100m, the temperature is of abnormality.
     地温梯度4.0~4.8℃/100m,平均4.26C/100m,属温度异常。
短句来源
     The results show that the heat flow values range from 44.8 mW/m~2 to 101.8mW/m~2, with the average 62.7±15.2 mW/m~2, and that the present geothermal gradient varies from 20.9 ℃/km to 47.6 ℃/km with the mean value of 28.2±10.3 ℃/km in the basin.
     结果表明:沁水盆地具有偏高的大地热流背景,现今热流变化于44·8~101·8mW/m2之间,平均62·7±15·2mW/m2,现今地温梯度介于20·9~47·6℃/km之间,平均地温梯度28·2±10·3℃/km.
短句来源
     Statistical analysis of the geothermal gradient data show that the geothermal gradients in South China range from 7.82 to 162.5℃/km with a mean of 24.1℃/km.
     结果显示,中国南方地温梯度介于7.82~162.5℃/km,平均24.1℃/km;
短句来源
     from Triassic to Jurassic, geothermal gradients was in range of 3.38℃ /100m-3.93℃/100m, 3.12℃/100m-3.59℃/100m respectively in the north andsouth of Tiaohu depression, and about 2.56℃/100m-3.86℃/100m in Malang depression.
     三叠纪-侏罗纪的地温梯度在条湖凹陷西部、东部依次为3.38℃/100m~3.93℃/100m、3.12℃/100m~3.59℃/100m,在马朗凹陷约为2.56℃/100m~3.86℃/100m。
短句来源
     Geothermal gradient was higher before Nantun Formation was deposited, it is (4.0~5.8)×10~(-2)℃/m.
     海拉尔盆地古地温高于今地温,南屯组沉积前具有较高的地温梯度,可达(4.0~5.8)×10-2℃/m。
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     They are respectively the cold water aquifer (depth < 2.2 km ), up per, middle and deep-seated geothermal water (depths are separately 2.2-3. 4 km, 3. 5 - 3. 9 km, > 4. 0km).
     2.2km以上为冷水层,2.2—3.4km、3.5—3.9km、4km以下分别为上部、中部和深部水层。
短句来源
     whereas in the downwarped area they are relatively low, with G=2.7—3.5℃/100m and Q=46-59mW/m~2. The geothermal background values are relatively high in the whole region, with =3.58℃/100 m and =62.5±13.4mW/m~2, and geothermal anomalies occur in some areas.
     而凹陷区则较低,G=2.7—3.5℃/100m,Q=46—59mW/m~2。 全区=3.58℃/100m,=61.5±13.4mW/m~2,这说明全区具有较高的地背景值和局部异常。
短句来源
     The temperature of the geothermal reservoir, which is calculated with the SiO2 geothermometer, is 94.01℃.
     利用SiO2温标法计算出储温度为94.01℃;
短句来源
     Yecheng depression is believed that it may be in where thegeothermal field is the lowest of the Basin,being less than 16℃/km in geothermal degree and 34.42mW/m~2 in heatflow value, which is consistent with those of the foreland depression.
     叶城凹陷地温梯度小于16℃/km,大地流值为34.42mW/m~2,是盆内地场最低之处,与前陆坳陷低地场之特点一致。
短句来源
     The temperatures and depths of the geothermal reservoir are estimatedat 80 ̄ 110 ℃ and 850 ̄950 m, respectively, using SiO2, Na/K and 18 O(SO4/H2O)geothermometers.
     应用SiO2、Na/K及 O(SO4/H2O)地温标,估算出储温度大致为80~110℃,储深度大致为850~950m。
短句来源
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  地热的
     Effect of Application of Line Source TEM to Geothermal Exploration
     线源TEM在腾冲热水塘寻找地热的应用效果
短句来源
     The hottest geothermal well in Beijing was drilled in Baolong Garden in 1998. The depth of this well is 3608.88 m, the temperature 88℃ and the quantity of water is 2163 m~3/d. The geothermal development is very important for the study of the bedrock geology of the plain area in Beijing and the development of capital economy.
     井深3608.88m,出水温度88℃,水量2163m~3/d。 北京地热的开发对填补平原区基岩地质研究的空白和促进首都经济的发展意义重大。
短句来源
     This paper presented two methods of loop heat pipe: shower ring nozzle and the geothermal convector, and compared with other methods.
     本文介绍了两种回路热管采集地热的方法:喷流(shower ring nozzle)强化液膜蒸发和井下地热转换器(the geothermal convector)法。
     It is suggested that the overall action of the out-going stress heating effect and the geothermal and the greenhouse effect initiated and amplified by the movement and concentration of crustal stress field in the seismogenic zone is the chief mechanism of satellite thermal anomaly before Hengchun earthquake.
     利用已有遥感-岩石力学基础实验结果,对震前红外异常的产生机制进行了讨论,提出震前构造应力场的迁移与集中活动所激发与加剧的应力热与地热的传递,及其与孕震区温室效应的叠加,是此次地震卫星热红外异常产生的主要机理。
短句来源
     A system combined with solar energy, geothermal and heat pump is proposed.
     并与其它两种低温地热的采集方法作了比较,提出太阳能、地热和热泵组合可再生能利用系统。
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      geothermal
    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.
          
    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.
          
    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.
          
    The yeast grown in a medium containing geothermal water was shown to accumulate more amino acids.
          
    Mathematical model of water injection into a geothermal steam-saturated reservoir
          
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    Under the assumption that before the occurrence of earthquakes the variations of the stress field in the crust can induce corresponding geothermal variations, the em-pirical relations between the daily geothermal variations in 1973 at Yangjiang County measured by thermo-electric couples buried 3 meters underground and the times and space distributions as well as magnitudes of earthquakes greater than magnitude 2 are discussed. The work presents some data on the premonitory phenomena of earth-quakes....

    Under the assumption that before the occurrence of earthquakes the variations of the stress field in the crust can induce corresponding geothermal variations, the em-pirical relations between the daily geothermal variations in 1973 at Yangjiang County measured by thermo-electric couples buried 3 meters underground and the times and space distributions as well as magnitudes of earthquakes greater than magnitude 2 are discussed. The work presents some data on the premonitory phenomena of earth-quakes.

    本文根据地震前地壳中由于地应力场的变化而会引起地温变化的想法,阐述了对埋在地下三米深处的温差电偶用电桥所测出的阳江县1973年地温日变化曲线与当地二级以上小地震在时间、地点及震级方面的经验关系。为寻找前兆现象提供一点资料。

    In this paper, the characteristic features of the short period geomagnetic variations observed in the eastern part of the Kansu Province have been studied. It can be inferred that an east-west belt of high electrical conductivity exists underneath this region. With reference to geothermal and earthquake activity of the same region, the question of the origin of the conductivity belt was examined and a preliminary explanation made. . It has also been attempted to relate the conductivity anomaly with earthquakes....

    In this paper, the characteristic features of the short period geomagnetic variations observed in the eastern part of the Kansu Province have been studied. It can be inferred that an east-west belt of high electrical conductivity exists underneath this region. With reference to geothermal and earthquake activity of the same region, the question of the origin of the conductivity belt was examined and a preliminary explanation made. . It has also been attempted to relate the conductivity anomaly with earthquakes.

    本文研究甘肃省东部地区的短周期地磁变化的特点,由此推测地下存在东西方向的一条电导率异常带.结合地热和地震活动现象,对高电导率异常的成因提出了初步解释,最后,试图探索电导率异常与地磁发生的关系.

    In this paper, the distribution of geothermal activities in China in relation to tectonic structures, are discussed. Prospecting of geothermal resources and their utili-zation and the present state of theoretical, observational and experimental work in geo-thermic studies are reviewed.Finally, the future tasks are suggested and the prospects of geothermie research in this cuntry are proposed.

    本文对中国地热分布与大地构造,地热资源的勘探与利用,地热的理论研究以及地热的观测与实验等研究成果进行了论述。最后提出了我国当前地热研究的任务和展望。

     
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