热储

热储由中生代燕山期花岗斑岩、凝灰岩组成。

Its heat reservoir is composed of Yanshanian granite-porphyry and tuff of Mesozoic .

竹海温泉浅部热储的水文地球化学问题

The hydrogeochemistry problems of the shallow heat reservoir in Zhuhai thermal spring

热储岩体的岩石成份各式各样。

The reservoir rock can be of various lithological compositions .

老第三系（E）是河南平原地热开发基底，新第三系（N）是主要热储层和开采层。

Eogene System is the fundus of terrestrial heat exploitation and Neogene System is the principal heat reservoir and exploitation bed of Henan plain .

综述了聚合物改性沥青的发展情况及路用性能，并从流变性的角度介绍了SBS改性沥青的性能，同时提出了SBS改性沥青应用过程中存在的主要问题&热储稳定性。

The rheological behavior and hot storage stability of SBS modified asphalt were reviewed .

利用SiO2温标法计算出热储温度为94.01℃；

The temperature of the geothermal reservoir , which is calculated with the SiO2 geothermometer , is 94.01 ℃ .

基于IDL的地质体真三维重构与可视化探讨&以福州市地热田热储结构为例

Three-dimensional reconstruction and visualization of geological material with IDL : a case of Fuzhou geothermal field three-dimension visualization system

得到了吸热器的能量损失、工质吸收能量、PCM的潜热储能和显热储能等重要指标，并且得到了换热管最大温度，工质出口温度等重要结果。

Heat loss , energy absorbed by gas , the latent and sensible thermal storage in PCM , tube maximum temperature , gas exit temperature and liquid PCM fraction were calculated .

以开封市埋深300～1600m孔隙地热系统为例，根据地热地质、水文地质条件的差异，以最大隔水层厚度为界，初步划分为6个热储层。

According to the differences of geological and hydrogeological characteristics , the geothermal system of Kaifeng city in the depth of 300 to 1600m is divided into six reservoirs .

根据腐蚀性，确定1000～1300m、1300～1600m热储层地热供暖时应分别采用直接和间接供暖形式。

Based on the corrosiveness , determined that geothermal heating with hot reservoirs of1000 ~ 1300m , 1300 ~ 1600m , ought to adopt separately direct and indirect heating forms .

根据地热水的水化学分析，应用SiO2和Na/K地球化学温标估算出热储温度大致为80～110℃，热储深度大致为900～1200m。

From the hydrochemical analyses of geothermal water , the temperatures and the depths of the geothermal reservoir are estimated at about 80 ~ 110 ℃ and 900 ~ 1200 m respectively by means of SiO 2 and Na / K geothermometers .

利用同位素方法得出温罗温泉来源于大气降水，补给高程507m，循环深度约3km，通过地温增温，并在有可能存在深部热源的条件下，获得较高的温度，热储温度为70-90℃范围。

Using the isotope method , we got the results : the hot spring is recharged from precipitation in the recharge area with elevation of 507 m. The depth of water circulation of the hot spring is estimated about 3 km .

另外，在1000～1300m和1300～1600m热储层均存在的地区，对两热储层的独立供暖和联合供暖模式进行了经济分析，可以看出：联合供暖显著优于独立供暖模式。

Moreover , in the area both hot reservoirs of1000 ~ 1300m and1300 ~ 1600m are all exist , economical analyses on heating models in alone and joint of both hot reservoirs , showing that joint heating model better than the alone heating model clearly .

兴城温泉热储构造与成因探讨

Discussion on the reservoir structure and formation of Xingcheng hot spring

地下含水层热储井位置选择和布置

Choice and arrangement of aquifer thermal energy storage well 's position

热储通过热传导的热损耗是无法阻挡的。

Heat losses from the reservoir by heat conduction cannot be prevented .

地热热储模型及井内换热器优化设计

Geothermal energy reservoir model and optimal design of heat-exchanger in well bore

利用地球化学温标估算热储温度150℃左右。

The thermal reservoir temperature is 150 ℃ estimated by geochemical standard .

显热储热材料的制备及性能研究

Preparation and research in g of sensible heat storage material

北京地区地热测井与热储层研究

Study of heat storage layers on the geothermal log in Beijing area

新近系热储层回灌井钻探工艺探索

The study on drilling technique of Tertiary reservoir reinjection well

热储温度数据主要通过钻探过程中温度测井来获取。

Reservoir temperature information is mainly obtained by temperature logging during drilling .

沉积盆地型层状热储可采资源量计算方法探索

The calculation of exploitable resources in the layered-geothermal reservoirs of sedimentary basin

利用测温资料判别热储流体的运动方向

Detection of geothermal fluid flow using temperature logging data

天津市塘沽低温热储回灌的水-岩相互作用地球化学模拟西安地热田地热弃水回灌数值模拟研究

Modeling water_rock interaction of geothermal reinjection in the Tanggu low_temperature field , Tianjin

中低温地热热储工程研究

Study of Geothermal Reservoir Engineering in Low-middle Temperature

开采井温度下降是热储回灌实施过程中的潜在问题之一。

The temperature decline of production wells is a potential problem induced by reinjection .

咸阳地压型热储流体基本特征及补给的研究

The Study on the Basic Characteristics and Recharge of Geopressured Geothermal Waters in Xianyang

湛江地热田热储分布规律

Thermal resource distribution law of Zhanjiang thermal field

天津市奥陶系热储层地热流体水化学特征及其主要影响因素

Hydrochemical Properties of Geothermal Fluids in Ordovician Reservoirs of Tianjin and Main Affecting Factors