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geothermal fluid
相关语句
  地热流体
     AN ANALYSIS OF GEOTHERMAL FLUID MINERALIZATION
     地热流体成矿作用分析
短句来源
     The content of some components of geothermal fluid are highly dependent on temperature.
     地热流体中一些组分的浓度依赖于热流体温度的高低。
短句来源
     Features and origin of geothermal fluid in the new district of Hebi, Henan
     河南省鹤壁市新区地热流体特征及成因分析
短句来源
     Gold mineralization is related to metallogeneses of transmis-sive hot brine geothermal fluid and of supergene weathering.
     金矿化与地热流体渗流热卤水成矿作用和表生风化成矿作用有关。
短句来源
     These may provide a geological basis for the proper development and utilization of the geothermal fluid in this district.
     从而为合理开发利用地热流体资源提供了地质依据。
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  “geothermal fluid”译为未确定词的双语例句
     It is held that silver mainly migrated in the form of [Ag(S_2O_3)_2]~(3-) complex under the shallow alkaline environment,and that geothermal fluid and its circulation and alteration action led to the formation of a series of mineral resources such as silver deposits and bentonite deposits.
     认为Ag在浅部碱性环境下主要呈[Ag(S2O3)2]3-络合物的形式迁移;
短句来源
     In 1988 a geothermal borehole with a measured temperature of 202℃ at a depth of 970m was drilled in the north hydrothermal alteration area of the Yangbajain geothermal field, which proved that the Yangbajain geothermal system is characterized by lateral geothermal fluid migration from NW to SE.
     在1988年,羊八井地热田的北部水热蚀变区的一个地热孔在970m深度上测得温度为202℃此事实证明了羊八片地热系统具有从西北往东南的侧向地热流体的运移。
短句来源
     GEOLOGICAL FEATURES AND GENESES OF GEOTHERMAL FLUID LEACHING TYPE GOLD DEPOSITS IN NORTHERN GUANGXI
     桂北地下热水溶滤金矿床地质特征及成因
短句来源
     GEOCHEMICAL CHARACTERISTICS OF GEOTHERMAL FLUID IN THE ACTIVE AREA OF THE TENGCHONGMODERN VOLCANOES
     腾冲现代火山活动区地热流体的地球化学特征
短句来源
     Therefore, chemical monitoring of geothermal fluid may give important information about the changes of geothermal systems.
     因此 ,地热流体的化学监测可以提供许多有关地热系统变化的宝贵信息。
短句来源
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  相似匹配句对
     AN ANALYSIS OF GEOTHERMAL FLUID MINERALIZATION
     地热流体成矿作用分析
短句来源
     APPLICATION OF KCP MUD FLUID IN THE DRILLING OF GEOTHERMAL WELL
     KCP泥浆在地热井钻进中的应用
短句来源
     FLUID THERAPY
     液体疗法
     The geothermal potential.
     可是具有良好地热田远景的区域。
短句来源
     Fluid Controller
     流体控制装置
短句来源
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  geothermal fluid
Constant rate production of geothermal fluid from a two-phase vertical column II: Examples
      
Constant rate production of geothermal fluid from a two-phase vertical column I: Theory
      
Present gas and brine compositions from crater fumaroles and hot springs indicate boiling of an immature Cl-SO4 geothermal fluid of near-neutral pH at approximately 200?°C, rather than direct discharge from magma.
      
Mixing of the two fluids along the unconformity led to gold solubility in the geothermal fluid dropping more than four orders of magnitude causing gold mineralisation there.
      
Using a F minimum approach temperature between the geothermal fluid and process air, a well with 230o F fluid is required.
      
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There are four active hydrothermalareas in the Xian Shui-he fracture Zone of western Sichuan province; Kang-Ding、Zhong-Ku、Chan-ning and Dao-Fu、These include more than thirty hot spring groups. Based upon analytic data on hot water quality,The author has Calcu- lated the cold water portion,the original temperature and The main ionic contents of the mixetd hot watr of each hydrothermal region.The forming,concentrating and migrating characteristic of thechemtical consit- uents of hot water,and the differences of...

There are four active hydrothermalareas in the Xian Shui-he fracture Zone of western Sichuan province; Kang-Ding、Zhong-Ku、Chan-ning and Dao-Fu、These include more than thirty hot spring groups. Based upon analytic data on hot water quality,The author has Calcu- lated the cold water portion,the original temperature and The main ionic contents of the mixetd hot watr of each hydrothermal region.The forming,concentrating and migrating characteristic of thechemtical consit- uents of hot water,and the differences of the hydrogeochemical Zones are discussed in detail.Finally,the writer Suggests a model for the formation and circulation of hot water. Hydrothermal areas do not exist alone,They hare the same aquifer (or geothermal reserveir),and belong to e ormous interconnected hydro- thermal systems.Recent magma activity under the depth of Kang-Dang hydrothermal area heated the cool water which infiltrated from the grou- nd surface.The hot water contains high enthalpy chlorid-bicarbonte with rich concentrations of CO_2-H_2S gas,reserved in both upper and lower aquifers. affected by rising geothermal fluid and the earth stress field,hot water rises vertically along the main fracture Zone and moves to the nor- thwest.When it reaches Kang-Ding Zong-Ku.Chan-ning and Dao-Fu regions,it ascends Continuously along the Sub-fractures and forms Sub- hydrothemal systems.Thus four hydrogeochemical Zones have fomed: (1). a high hot water zone Containing CO_2-H_2S;(2).a high-told temperature water zone Containing CO+2; (3).a mid-lower temperature water zone Con- taining N_2-CO_2;(4).a Cool carbonate water zone.

四川西部的鲜水河断裂带有四个水热活动区,即康定,中谷、乾宁和道孚,总计30多处温热泉群。本文根据热水水质分析资料,计算了各热区混合热水中的冷水份额、原始热水温度和主要离子含量,着重讨论断裂带热水化学组分的形成和迁移富集特征以及热水水文地球化学分带,在此基础上提出了热水形成与循环模式。鲜水河断裂带各区热水不是孤立存在的,它们来自共同热储,属于相互联系的庞大水热系统。康定热区深部存在近期岩浆活动,加温地表入渗冷水,形成富含CO_2—H_2S 气体的氯化物、重碳酸盐高温热水,并储存在上,下两层热储中。在热对流和地应力场驱动下,热水沿断裂带垂直上升,并向西北方向运移,依次在康定、中谷、乾宁、道孚等地沿次级断裂上升,形成次级水热系统,并构成下列四个水文地球化学带:(1)含 CO_2—H_2S 高温水带:(2)CO_2含高中温水带;(3)含N_2—CO_2,中低温水带;(4)冷碳酸水带。

The results of investigation of stable isotope, minor element(gold ) of rocks and geological characteristics indicate that the source of mineralized material of gold deposit from Jinchangzi in Ningxia comes from the upper crust, and gold,silver, lead, copper etc.and surphur, selenium, arsenic, chlorine, fluorine etc. take its source at Carboniferous and Devonian sedimentary rocks. The ore -forming fluid is a mixed solution of the atmospheric water and sedimentary stratal water. Gold mineralization is related...

The results of investigation of stable isotope, minor element(gold ) of rocks and geological characteristics indicate that the source of mineralized material of gold deposit from Jinchangzi in Ningxia comes from the upper crust, and gold,silver, lead, copper etc.and surphur, selenium, arsenic, chlorine, fluorine etc. take its source at Carboniferous and Devonian sedimentary rocks. The ore -forming fluid is a mixed solution of the atmospheric water and sedimentary stratal water. Gold mineralization is related to metallogeneses of transmis-sive hot brine geothermal fluid and of supergene weathering.

稳定同位素、岩石微量元素(金)和地质特征研究的结果,表明金场子金矿床的成矿物质来源系上地壳源,并且金、银、铅、铜等金属和硫、硒、砷、氯、氟、碳等来源于石炭纪和泥盆纪沉积岩。成矿流体是大气水和沉积地层水的混合溶液。金矿化与地热流体渗流热卤水成矿作用和表生风化成矿作用有关。

The status quo of geothermal power generation in Yangbajing, Xizang (Tibet) is presented, together with a description of the geothermal wells and their flow characteristics, the adopted geothermal fluid transportation system and material used for the equipment. Some suggestions are also proposed.

介绍了西藏羊八井地热发电的概况。叙述了地热生产井及其流量特性、地热流体输送系统、地热发电设备的材料,并提出了若干建议。

 
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