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深层热水
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  deep thermal water
     Shallow cold water recharges deep thermal water.
     浅层常温水对深层热水亦有补给。
短句来源
  “深层热水”译为未确定词的双语例句
     In some fault zones bounded the uplifts, there are heat sources caused by upward hot water, which are superposed on the heat conduction, and the gradients are up to 5-8℃/100m, showing apparently positive thermal anomalies.
     某些控制凸起区的边界断裂,当深层热水沿其上涌,造成附加热源,和传导传热相叠加,盖层地温梯度可高达5—8℃/100m,形成更鲜明的地热正异常。
短句来源
     おhe cold and hot waters in the Yangbajing geothermal field could be classified into CaHCO3, NaHCO3Cl, (Ca, Mg)SO4 and NaCl types. Thermal waters in the shallow and deep reservoirs are of NaCl types both with the same B/Cl ratio. There is distinct difference on chemical and isotopic compositions between the thermal waters and the water of Lake Nam Co.
     羊八井地热田深、浅层热水都是Cl-Na类型,具有相同的B/Cl比值,说明深层热水在上升通道中与冷水相混合形成了浅层热水。
短句来源
     This paper introduces the whole procedure that a 1500-meter geothermal well is investigated, designed
     本文报道了云南某地体育中心成功建造1500m深层热水井工程的勘察、设计、施工全过程的概况,可供同类工程参考。
  相似匹配句对
     An Analysis of the Exploitation Regime of Thermal Groundwater in Deep-seated Aquifers in the Tianjin Area
     天津地区深层地下热水开采动态分析
短句来源
     A PRELIMINARY STUDY OF THE PHYSICAL CHEMISTRY MECHANISM OF WATER LEVEL CHANGE OF DEEP THERMO-GROUNDWATER
     深层地下热水水位变化的物理化学机理初步探讨
短句来源
     the Atlantic layer waters are in the deep water;
     深层为大西洋源水 ;
短句来源
     Energy-efficiency Type Hot Water Heating System
     节能型热水系统
短句来源
     Deep Reaction of Coke
     焦炭的深层反应
短句来源
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  deep thermal water
The fractions of deep thermal water in the total discharge of admixed groundwaters were estimated and the elevations of recharge zones for the Paleogene aquifer were determined.
      
Instead, vent and pore water data define a trend that intersects the boiling curves for deep thermal water at the 220C mark.
      


Leizhou Peninsula as a land part of Beibuwan Basin is located on the northern continental shelf of South China Sea. According to the geologic structures, the basin is a stretch faul-ting-depression basin, most of the Cenozoic strata developed on the basement of the Paleozoic groups and the Yenshanian granites. The geohermal field is controlled mainly by the pattern of basement tectonics and influcened by ground water activity, but it cannot be ignored that the heat generation of radioactive elements in blind...

Leizhou Peninsula as a land part of Beibuwan Basin is located on the northern continental shelf of South China Sea. According to the geologic structures, the basin is a stretch faul-ting-depression basin, most of the Cenozoic strata developed on the basement of the Paleozoic groups and the Yenshanian granites. The geohermal field is controlled mainly by the pattern of basement tectonics and influcened by ground water activity, but it cannot be ignored that the heat generation of radioactive elements in blind granites played a part here. The remained heat of the Pleistocene volcanic activities seems to be disappeared and thus a temperature balance is reached between magmatic rocks and their country rocks. The volcanic eruptions formed both the southern (Luogangling) and the northern (Shimoling) basaltic terraces, which are the intflow areas of groundwater. By the effect of downward cold water flow, the geothermal gradients are below 3℃/100m in the shallow part of the Conozoic cover, showing negative thermal anomalies. In the areas dominated by heat conduction, the geothermal field is similar to that in North China Basin, and the gradient of the Cenozoic cover is closely related to the depth of the bedrock roof. Because the uniform heat flow from the deeper crust was redistributed in the shallower Crust, the gradients in the cover on the several basement uplifts are in a range of 4-5℃/100m, showing positive thermal anomalies. In some fault zones bounded the uplifts, there are heat sources caused by upward hot water, which are superposed on the heat conduction, and the gradients are up to 5-8℃/100m, showing apparently positive thermal anomalies.

雷州半岛地热场主要受基底构造格局的控制和地下水活动的影响,隐伏花岗岩体放射性元素生热对盖层地温的贡献不可忽视,第四纪更新世火山喷发活动的岩浆余热已几乎完全散失,岩浆体和围岩温度已趋于平衡。由火山喷发而形成的雷北螺岗岭和雷南石峁岭两个玄武岩台地,为半岛地下水的主要补给区,由于冷水流下渗的地温效应,新生界盖层浅部地温梯度<3℃/100m,呈现地热负异常。在以传导传热为主的区域,地热场特点与华北盆地相似,新生界盖层地温梯度与基底岩面的埋深密切相关。由于地壳深部较均一的热流在地壳表部再分配的结果,若干凸起区盖层地温梯度为4—5℃/100m,呈现地热正异常。某些控制凸起区的边界断裂,当深层热水沿其上涌,造成附加热源,和传导传热相叠加,盖层地温梯度可高达5—8℃/100m,形成更鲜明的地热正异常。

Based on observition data of Xiaozhai ground fissure and Xiying well's water level, the characteristics of quasi -synchroneity and relationship to phase are analyzed. Combining with the data of ground subsidence rate and seismic activity nearby, we have studied the cause of interrelation between ground fissure and Tertiary deep water, and the effect of water - pumping ground subsidence on the ground fissure.

本文根据西安小寨地裂缝与西影井第三系深层热水水位的观测资料,分析了二者变化周期的准同步和相位的滞后性特征,并结合地面沉降速率和周围地震活动性,探讨了地裂缝与第三系深层承压水位之间存在内在联系的原因,以及抽水—地面沉降对地裂缝影响的构造动态调制作用.

おhe cold and hot waters in the Yangbajing geothermal field could be classified into CaHCO3, NaHCO3Cl, (Ca, Mg)SO4 and NaCl types. Thermal waters in the shallow and deep reservoirs are of NaCl types both with the same B/Cl ratio. There is distinct difference on chemical and isotopic compositions between the thermal waters and the water of Lake Nam Co. It suggests that Lake Nam Co is not a recharge area of the Yangbajing geothermal field. The shallow thermal water is a mixture of the deep thermal fluid...

おhe cold and hot waters in the Yangbajing geothermal field could be classified into CaHCO3, NaHCO3Cl, (Ca, Mg)SO4 and NaCl types. Thermal waters in the shallow and deep reservoirs are of NaCl types both with the same B/Cl ratio. There is distinct difference on chemical and isotopic compositions between the thermal waters and the water of Lake Nam Co. It suggests that Lake Nam Co is not a recharge area of the Yangbajing geothermal field. The shallow thermal water is a mixture of the deep thermal fluid and the shallow cold ground water. Its movement is controlled mainly by faults in the region. It flows with a decreasing in temperature from northwest to southeast. Exploitation of the deep thermal water would accelerate the shallow resource exhaustion. Some minerals reach or approach chemical equilibrium in the shallow reservoir. Waterrock interaction results in the Na/K ratio increasing in the shallow thermal water. The calculated temperatures of Na/K geothermometer are between those in the deep and shallow reservoirs. Quartz and chalcedony geothermometers are applicable for the deep and shallow reservoirs respectively in the Yangbajing geothermal field. The CO2 and H2S contents in the steam of well ZK4001 are much higher than that of the shallow fluid. Anticorrosive measures should be paid attention to during exploitation of the deep geothermal resources. When the deep thermal water adiabatically boils down to 125℃, silica scaling will become very serious. The tail water could not be used to inject directly in order to prevent silica deposit lowering rock permeability. The CaCO3 saturation index of the deep thermal water is lower than that of the shallow one and its calcite scaling is not serious. it needs a longterm discharge to verify, whether there is no calcite deposit on the wellbore. The chemical monitoring of the thermal water is of benefit to understand the state of the reservoirs. 

羊八井地热田深、浅层热水都是Cl-Na类型,具有相同的B/Cl比值,说明深层热水在上升通道中与冷水相混合形成了浅层热水。浅层流体自西北向东南流动,温度逐渐降低。浅层热储内普遍存在着水岩交换反应,对热水的化学组成有一定的影响。石英和玉髓地热温度计分别适用于计算深、浅层的热储温度。纳木错(湖)不是羊八井地热田的补给区。深层热水在井筒内绝热汽化时不会出现SiO2结垢,CaCO3是否会在井筒壁沉淀需要放喷较长时间来检验。文中还阐述了对热水的化学组分进行监测的必要性。

 
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