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geothermal     
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  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
短句来源
    Mechanism of Deep Circulation Heat Exchange of Artificial Recharge Water in Fuzhou Geothermal Field
    福州地热田人工补给深循环热交换机理分析
短句来源
    A STUDY ON GEOTHERMAL RESOURCE IN DAQNG-HARBIN REGION
    大庆-哈尔滨地段地热资源研究
短句来源
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  地温
    Geotemperature Field Feature and Distribution Law of Geothermal Anomaly and Their Control Conditions
    江苏地温水温场特征及地热异常分布规律与控制条件探讨
短句来源
    The heat flow values of the South Huabei Basins are between 30 mW/m2 and 89.6mW/m2,with an average value of 53.7mW/m2.The South Huabei Basins can be described as a " mild " basin in a whole,compared with the geothermal fields of the basins in eastern and western China.
    大地热流值在30~89.6 mW/m2之间,平均热流值为53.7mW/m2.和中国东、西部盆地现今地温相比,整体表现为一温盆.
短句来源
    The paper has discussed the pressure gradient of lithosphere form the theory and indicated that the pressure gradient in the lithosphere is no-linear, and its minimum is the hydrostatic pressure gradient, and that the pressure gradient of the lithosphere will increase obviously from the contribution of both geothermal and weight of rocks, can be more than twice times as the hydrostatic pressure gradient.
    与地温梯度一样,岩石圈中的地压梯度在空间和时间上也应是复杂多变的。 本文从理论方面论述,岩石圈中的地压梯度是非线性的,静岩压力梯度(the lithostatic gradient——the pressure resulting from the weight of the overburden)是岩石圈中地压梯度的最小值,受地温梯度的影响岩石圈中地压梯度明显增加,可达到静岩压力梯度的2倍以上。
    THE CHARACTERISTICS OF HEAT FLOW AND GEOTHERMAL FIELDS IN JUNGGAR BASIN
    准噶尔盆地热流及地温场特征
短句来源
    A study of geothermal information management system for Pingdingshan Mine Area
    平顶山矿区地温信息管理系统研究
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    Study of the Tectonic-thermal Evolution of the Songliao Basin and Quantitative Assessment of Its Geothermal Resource: A Case Study on the Dumeng District
    松辽盆地构造演化及地资源定量评价研究——以杜蒙地区为例
短句来源
    Characteristics of the Geothermal Field in Northern Beijing and the Influence of Its Exploitation on Seismic Ground Fluid Behaviour
    京北地田特征及其开发对地震地下流体动态的影响
短句来源
    GEOTHERMAL FIELD STUDY AND ITS SIGNIFICANCES IN EASTERN ZHEJIANG,FUJIAN AND GUANGDONG PROVINCES
    浙闽粤东部地场研究及其意义
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
    Characteristics of Geothermal Field in Bonan Depression of Shengli Oil Field
    胜利油田渤南洼陷古地场特征
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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
    Development of Geothermal Pool Deduced from Old Thermal Current Values and Denudation Quantity——By the Example of Well 100 at Chuanhe in Sichuan Basin
    从古热流值和剥蚀量的研究来判断地热的发育——以四川盆地川合100井为例
短句来源
    According to the standpoint of the systematic theory, the thesis regards the whole procedure of low enthalpy geothermal as a consecutive organic whole.
    本文根据系统论的观点,将低焓地热的整个利用流程作为一个前后关联的有机整体。
短句来源
    The paper focuses on the introduction of the geological conditions and the characteristics of geothermal resources in Tantou,Lianchen County and on the discussion of the genesis of geothermal water in the surveyed area. Finally,the author presented a proposal about the exploitation and utilization of the geothermal resources.
    简要介绍了连城县汤头地热的地质概况及地下热水资源特征,探讨了该区地下热水的成因,并提出合理开发利用的建议。
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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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    The Zhangzhou Geothermal Field is one of the highest temperature geothermal fields so far discovered on SE coast of China. Geological, geochemical and temperature pattern studies indicate that the Zhangzhou Geothermal Field belongs to a deep circulating thermal water field of convective type. For calculating the circulation depth of thermal water, a cylinder model was applied in the study. Firstly, the upwelling flow rate of thermal water along the cylinder was calculated from the temperature measurements...

    The Zhangzhou Geothermal Field is one of the highest temperature geothermal fields so far discovered on SE coast of China. Geological, geochemical and temperature pattern studies indicate that the Zhangzhou Geothermal Field belongs to a deep circulating thermal water field of convective type. For calculating the circulation depth of thermal water, a cylinder model was applied in the study. Firstly, the upwelling flow rate of thermal water along the cylinder was calculated from the temperature measurements in boreholes located in the central part of the field. Secondly, reservoir temperature was determined from the geochemical parameters of the thermal water. Finally, a value of about 3.5 to 4.0km for thermal water circulation depth in the Zhangzhou Geothermal Field was obtained by using a plot method. This value is used for genetic analysis and thermal water resource assessment in the Zhangzhou Geothermal Field.

    漳州热田是我国东南沿海地区目前所见温度(121.5℃)最高的一个。热田地热地质、地球化学以及地温场的研究结果表明,漳州热田属于深循环对流型热田。为了计算热田的热水循环深度,本文采用管道模型的方法,利用热田中心钻孔的测温资料计算地下热水上涌的流速,利用热田内水化学资料计算热储温度,然后用图解法求出漳州热田热水的循环深度为3.4—4.0 km,为漳州热田的成因分析和热水资源的评价提供了依据。

    Based on the data obtained from the study and tests oft the geophysical and geochemical methods applied to the prospecting for geothermal resources and the related reconnaissance surveys conducted around the Hongshuilan Hot Spring in Wenden County, Wenquan Village in Anqiu County and the Ji'nan Area in recent years,the author outlines the prerequisites for reconnaissance survey of geothermal resources by geophysical and geochemical methods and affirms the good results achieved in the course. The...

    Based on the data obtained from the study and tests oft the geophysical and geochemical methods applied to the prospecting for geothermal resources and the related reconnaissance surveys conducted around the Hongshuilan Hot Spring in Wenden County, Wenquan Village in Anqiu County and the Ji'nan Area in recent years,the author outlines the prerequisites for reconnaissance survey of geothermal resources by geophysical and geochemical methods and affirms the good results achieved in the course. The author has further worked out a set of operational procedures for exploring subsurface hot water by geophysical and geochemical methods.

    本文以近几年开展地热物化探试验研究和地热物化探普查所取得的资料为基础,以文登县洪水岚温泉外围,济南地区和安丘县温泉乡为例,概述了应用物化探方法开展地热普查的前提,分析并肯定了应用物化探方法进行地热普查所取得的地质效果。根据自己的体会,总结出一套应用物化探方法寻找地下热水的工作程序。

    The paper presents the analyzing results of recharge tests in Fuzhou Geothermal Field. Based on the structural setting of the fissure-type granite thermal reservoirs and the principles of the gravity-differentiation driving force caused by water temperature difference and of injection water column pressure and downward inertia force of water columns, we used the new technique of deep circulation heat exchange by force in the thermal center of Fuzhou Geothermal Field at the short distance to turn the 17℃ injection...

    The paper presents the analyzing results of recharge tests in Fuzhou Geothermal Field. Based on the structural setting of the fissure-type granite thermal reservoirs and the principles of the gravity-differentiation driving force caused by water temperature difference and of injection water column pressure and downward inertia force of water columns, we used the new technique of deep circulation heat exchange by force in the thermal center of Fuzhou Geothermal Field at the short distance to turn the 17℃ injection water into the about 90℃ hot water and to faciliate the water level rising greatly again. The technique can be widely applicable for artificial recharge of the geothermal fields characterized by the thermal reservoirs of steep fault-fissure type, which is an efficient method of resolving the shortage of underground hotwater in this type of geothermal fields. All three recharge contratests in Fuzhou Geothermal Field obtained good results and prove that the technique possesses many advantages, such as quick temperature rising, high recovery of the recharge water and great rising of the underground water level. Therfore, it is a reliable measure of enlarging the production of geothermal field, rising the groundwater level. avoiding the ground subsidence and improving water quality , which has obvious economic and social-environmental effects in improvement of the investment environment of Fuzhou City. Its freshening is of great application value to protection from the production well jamming and for resistance to corrosion and incrustation of the equipments used in saline-water hotsprings of the coastal areas and high-temperature and mineralized geothermal belts in Tibet and Yunnan Provinces.

    根据花岗岩裂隙型热储的构造条件,以及冷热水温差所引起的重力分异驱动力、注水水柱压力和水柱向下运动的惯性冲力等原理,采用热中心近距离强迫对流深循环热交换新技术,把约17℃的冷水加温成90℃左右的热水,促使地下水位大幅度回升。通过三次对比试验,取得圆满结果。该成果普遍适甩于以陡倾断层裂隙为热储的地热田人工补给回灌,它是解决这类热田地下热水资源不足的最经济方法之一。通过三次回灌对比试验,证明采用人工补给深循环热交换技术具有升温快、回收率高及水位回升大等优点,因此它是增大地热田的开采量、促使地下水位回升、防止地面下沉、改善水质等促使地热田“复生”,防止衰退的可靠保护措施。其经济效益、社会环境效益显著,且有利于改善福州市区对外开放的投资环境。同时,对沿海咸水温泉带及西藏、云南高温高矿化地热带的开发利用、设备的防腐蚀、防结垢及防止开采井堵塞等也具有一定的推广应用价值。

     
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