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geothermal groundwater
相关语句
  地下热水
     NUMERICAL SIMULATION FOR SOLUTE TRANSPORT IN KARST GEOTHERMAL GROUNDWATER AQUIFER SYSTEM IN KUNMING GEOTHERMAL FIELD
     昆明地热田岩溶地下热水系统中溶质运移的模拟
短句来源
     Application of Integrated Exploration Method in Geothermal Groundwater Seeking
     综合勘探方法寻找地下热水
短句来源
     Space-time distribution of geothermal groundwater exploitation in thermal spring area of Fuzhou
     福州温泉区地下热水开采时空分布特征分析
短句来源
     Through analyzing the geological, hydrogeological and extractive conditions of the geothermal groundwater in Kunming Geothermal Field, a hydrogeological concept model and a quasi-three dimensional numerical model with temperature and pressure variation for the leaky karst geothermal aquifer system are set up in this paper, which is coupled with a groundwater flow model and a heat transfer model and a solute (contaminant) transport model.
     通过对昆明地热田深层基岩地下热水系统的地质、水文地质条件和开采现状的分析,建立了考虑温压变化和越流条件的岩溶热储层中地下热水的水流和溶质(污染物)运移的准三维非稳定流数学模型。
短句来源
     That is, the present model is reliable and practical, and can be used to simulate and predict the groundwater flow and solute (or contaminant) transport in the geothermal groundwater system under different conditions and to provide the appropriate corresponding counter-measures for the sustainable exploitation and utilization for the geothermal groundwater resources.
     模型可预测不同条件下地热田地下热水的流场和溶质浓度的动态变化趋势,为防治地下热水环境的进一步恶化提供参考。
短句来源
  地下热水的
     NUMERICAL SIMULATION OF GEOTHERMAL GROUNDWATER IN LEAKY AQUIFER SYSTEM,IN KUNMING CITY GEOTHERMAL FIELD
     昆明市地热田越流含水系统中地下热水的数值模拟
短句来源
     Through analyzing the geological, hydrogeological and extractive conditions of the geothermal groundwater in Kunming Geothermal Field, a hydrogeological concept model and a quasi-three dimensional numerical model with temperature and pressure variation for the leaky karst geothermal aquifer system are set up in this paper, which is coupled with a groundwater flow model and a heat transfer model and a solute (contaminant) transport model.
     通过对昆明地热田深层基岩地下热水系统的地质、水文地质条件和开采现状的分析,建立了考虑温压变化和越流条件的岩溶热储层中地下热水的水流和溶质(污染物)运移的准三维非稳定流数学模型。
短句来源
  “geothermal groundwater”译为未确定词的双语例句
     URANIUM MINERALIZATION OF GEOTHERMAL GROUNDWATER AND DISSIPATIVE STRUCTURE
     热水铀成矿作用的耗散结构
短句来源
     The F1 fault belt is the first area for the geothermal groundwater exploration, the second is the area confined by F1 , F41 and HF3. This conclusion has been proved by the exploration.
     北部、北西部,F1断层带、F41断层带、滑动构造(HF3)分布区均是温热水赋存的有利地段.
短句来源
     The formation of geothermal groundwater in the Longmen geothermal field
     龙门地热田温热水成因探讨
短句来源
     The age,the circulating rate and the recharge area of geothermal groundwater are determined based on the radioactive isotope 14C content.
     利用放射性同位素14 C法 ,估算了各热储层地热水的年龄和循环速率并确定了补给源
短句来源
     According to field investigation and exploration, the characteristics of tectonics, the distribution and the chemical composition of geothermal groundwater in the Longmen geothermal field are analyzed in this paper.
     根据地面调查和勘探资料,作者系统地分析了龙门地热田的构造特点、温热水的分布及水化学特征,指出龙门地热田温热水的分布具有两个特点:一是在地热田的南部主要受F1断层的控制呈线状分布;
短句来源
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  geothermal groundwater
To investigate the biomass and phylogenetic diversity of the microbial community inhabiting the deep aquifer of the Great Artesian Basin (GAB), geothermal groundwater gushing out from the aquifer was sampled and analyzed.
      
Numerical modeling of geothermal groundwater flow in karst aquifer system in eastern Weibei, Shaanxi Province, China
      
Effects of geothermal groundwater on nutrient dynamics of a lowland Costa Rican stream.
      


WT5BZ]The geothermal groundwater resources are very abundant in Tongjing scenic spot, north Chongqing district, Chongqing city. The water yield per well may reach 1000~7200 m 3/d, the highest temperature of the water may get 60℃. Investigation and study show that the major heat storage reservoir is carbonate rocks of the Jialingjiang Group, Lower Triassic system. The heat insulation layers are mainly the red sandstone rock, coal layer, mudstone rock of the Xujiahe Group, the Jura Upper Trias System....

WT5BZ]The geothermal groundwater resources are very abundant in Tongjing scenic spot, north Chongqing district, Chongqing city. The water yield per well may reach 1000~7200 m 3/d, the highest temperature of the water may get 60℃. Investigation and study show that the major heat storage reservoir is carbonate rocks of the Jialingjiang Group, Lower Triassic system. The heat insulation layers are mainly the red sandstone rock, coal layer, mudstone rock of the Xujiahe Group, the Jura Upper Trias System. Precipitation sinks to the heat storage reservoir via karst trough valley,then the groundwater flows in the depth along fault structure line from north to south and discharges to the earth surface in maximum deressurization area, such as river valley, to form the geothermal spring.

重庆渝北区统景风景旅游区地下热水资源十分丰富 ,井泉流量可达 10 0 0~ 72 0 0 m3 / d,水温最高可达 6 2℃。调查研究表明 ,热水以下三叠统嘉陵江组碳酸盐岩为主要储热介质 ,以上三叠统须家河组至侏罗系的红色砂页岩、煤层、泥岩为隔热保温盖层。大气降水通过岩溶槽谷下渗至热储层 ,在深部沿断裂构造线由北向南迳流 ,并在地表减压最大处 ,如河谷地段等 ,排出地表而形成温泉。

This paper studies the distributing characteristics and the controlling factors of ground temperature, geothermal gradient and surface geothermal current value by using the data of 28 geothermal wells in the Kaifeng geothermal field. Dividing the reservoir (depth 300~1600 m) into 6 sub-reservoirs, the hydraulic-connection among sub-reservoir is researched also. The hydro-geological characteristics and hydro-chemical characteristics of 6 sub-reservoirs are assessed.The age,the circulating rate and the recharge...

This paper studies the distributing characteristics and the controlling factors of ground temperature, geothermal gradient and surface geothermal current value by using the data of 28 geothermal wells in the Kaifeng geothermal field. Dividing the reservoir (depth 300~1600 m) into 6 sub-reservoirs, the hydraulic-connection among sub-reservoir is researched also. The hydro-geological characteristics and hydro-chemical characteristics of 6 sub-reservoirs are assessed.The age,the circulating rate and the recharge area of geothermal groundwater are determined based on the radioactive isotope 14C content.

以 2 8眼地热井水温资料为基础 ,研究了开封市地热系统的地温、地温梯度及地表热流值的分布特征及控制因素。结合钻孔柱状和地热水动态资料 ,划分了亚热储层 ,并说明了各亚热储层地热水之间的相互关系及水文地质特征。依据地热水水质化验结果 ,评价了各亚热储层地热水的水化学特征。利用放射性同位素14 C法 ,估算了各热储层地热水的年龄和循环速率并确定了补给源

With the increasing seriousness of groundwater(or geothermal groundwater) pollution,the need for modeling and predicting groundwater flow and solute mass(or contaminants) transport in groundwater system of the basement rock aquifers under the condition of nature and human activity has imposed extraordinary demands on the field of groundwater modeling, which has been brought to the great notice of experts at home and abroad. In accordance with the geological and hydrogeologic conditions...

With the increasing seriousness of groundwater(or geothermal groundwater) pollution,the need for modeling and predicting groundwater flow and solute mass(or contaminants) transport in groundwater system of the basement rock aquifers under the condition of nature and human activity has imposed extraordinary demands on the field of groundwater modeling, which has been brought to the great notice of experts at home and abroad. In accordance with the geological and hydrogeologic conditions of Kunming city geothermal field,which is a large low temperature geothermal groundwater field, a quasithree dimensional numerical model with temperature and pressure variation in the geothermal leaky aquifers system is presented based on the authors' recent years' research in this paper. It is coupled with the wellknown groundwater flow model and a heat transfer model and a mass(contaminant) transport model. The above model is applied to describe the geothermal groundwater hydrauliclevel and concentration of the simulated mass factor(contaminant) versus time of Z2dn aquifer in II block under the situation of exploitation.The simulated results agree well with the observed facts.The average error of geothermal water hydraulic-level is less than 1.5 meter,and the average error of chlorin ion and vitriol ion are both less than 3 to 5 percent. It is revealed that the present model is reliable and practical. Finally, the changes of the geothermal water seepage field and the mass(contaminant) concentration is evaluated and predicted quantitatively under the current scale of exploitation. The appropriate corresponding countermeasures to sustainable exploitation and utilization have been proposed.

深层基岩地下(热)水水化学污染问题日趋严重,急需定量而仿真地模拟和预报天然状态和各种人为工程经济活动下地下(热)水流动及溶质(或污染物)的运移。在充分认识地质、水文地质条件的基础上,建立了考虑温压变化和越流条件的昆明市地热田深层基岩地下热水系统中水流和溶质运移的准三维非稳定流数学模型。模型用于开采条件下地热田地下热水水位及F-、Cl-浓度的模拟,模拟结果具有较高的仿真性,拟合误差一般小于2%~5%,表明模型合理、可靠。应用所建模型预测了开采条件下昆明市地热田II块段地下热水流场和溶质浓度动态的变化趋势,并提出了控制地下热水环境进一步恶化的措施。

 
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