地层水矿化度的英文

• formation water salinity
• reservoir water salinity

• "地层"英文翻译    stratum; layer; serati; geos ...
• "水"英文翻译    water
• "高矿化度地层水" 英文翻译 :    highly mineralized formation brines
• "地下水矿化度" 英文翻译 :    groundwater mineralization
• "矿化度" 英文翻译 :    degree of mineralization; extent of mineralization; mineral content; mineral salt concentration , mineralization; mineral salt concentration ， mineralization; salinity
• "矿化，矿化度" 英文翻译 :    mineralization
• "地层水" 英文翻译 :    formation water; local water; stratum water
• "低矿化度水" 英文翻译 :    low salinity water
• "高矿化度" 英文翻译 :    high salinity; hypersalinity
• "高矿化度水" 英文翻译 :    concentrated water
• "矿化度在25" 英文翻译 :    g/l
• "泥浆矿化度" 英文翻译 :    mud salinity
• "总矿化度" 英文翻译 :    total mineralization
• "热水矿化溶液" 英文翻译 :    hydrothermal mineralizing solution
• "高矿化度泥浆" 英文翻译 :    high-salinity mud
• "高矿化度盐水" 英文翻译 :    high-salinity brine
• "矿化度测井图" 英文翻译 :    salinity log
• "矿化度指示比" 英文翻译 :    salinity indicator ratio; sir
• "硫酸盐矿化度" 英文翻译 :    sulphate salinity
• "饮用水矿化装置" 英文翻译 :    drinking water mineralizing plant
• "地层水 层状水" 英文翻译 :    stratumwater
• "地层水产量" 英文翻译 :    formation water rate
• "地层水桶数" 英文翻译 :    bfw
• "地层水图" 英文翻译 :    formation water map
• "含气地层水" 英文翻译 :    aerated formation water

• In recent years , some physical techniques such as ultrasonic , electric field and magnetic field are also applied
  由于地层水矿化度高、机械杂质含量高，使注水管网腐蚀结垢，导致注水系统能耗增大、生产效率降低，甚至影响正常生产。
• Measurement theory of coaxial line phase water cut meter and flowing feature of water oil two - phase flow have been studied in this paper . and it has been found that the response of coaxial line phase water cut meter is not only related to water cut , but also related to temperature , salinity of formation water and flowing characteristics . based on soft - measuring theory and operating theory of the meter , soft - measuring model of coaxial line phase water cut meter has been set up with directly obtainable facts such as flux , temperature of oil and water mixture and salinity of formation water
  本文在对同轴线相位法含水率计的测量机理和油井两相流动特性研究的基础上，揭示出同轴线相位法含水率计的仪器响应除了与油井含水率有关之外，而且还与油水混合介质的温度、地层水矿化度以及两项流动状态有关；结合软测量技术理论和同轴线相位法含水率计本身的测量机理以及与仪器响应有关的可以直接测量的流量、油水混合介质的温度、地层水矿化度等参数，建立基于同轴线相位法含水率计机理的软测量模型。
• The separation of gas and oil and water only limits to small system of gas pool and there are not separation of gas and water in the large bound . the border water is not active , the system of gas and water is small and driving power of water is poor . the degree of mineralization of strata water is lower , the type of water is sodium carbonate and respects the character of closing transition in the continent circumstance
  油气水分异仅限于一个小气藏系统，不存在大范围的气水分异现象；气藏边底水不活跃，气水系统连通范围较小，水体驱动能量有限；地层水矿化度较低，水型以碳酸钠型为主，代表大陆环境下的封闭过渡带特征。
• It is found that the degree of mineralization and metamorphic coefficient and conversion potential of formation water , the fault is zone of sluicing of atmospheric infiltration water flowing from basin west margin to east ( centripetal flow ) and sedimentary compaction water flowing from qija gulong depression to west ( centrifugal flow )
  通过地层水矿化度和变质系数等参数的分布规律及一系列折算水位剖面图的分析发现，该断裂对水是不封闭的，并且是盆地西缘大气渗入水向东流动（向心流）及齐家古龙坳陷沉积压实水向西流动（离心流）的共同泄水带。
• Using evidence weight method , the authors selected tectonic activities , hydrocarbon abundance and thickness of source rocks , level of reservoir , complexity of reservoir , degree of mineralization of formation water as the evidence layers to evaluate the favorable zones of lower palaeozoic pools at the north edge of the middle and lower yangtze area
  摘要利用地质异常研究中的证据权重法，选择构造活动、烃源岩有机质丰度、烃源岩厚度、储层级别、储层复杂程度、盖层发育程度、地层水矿化度作为证据层，对中下扬子北缘下古生界油气成藏有利区带进行了评价。
• Based on experimental research on electrical property of waterflooded rock we have found that variation of salinity has much effect on rock resistivity , and it makes that relation curves of complex resistivity and in - phase resistivity of rock under single frequency with water saturation are characteristic of u - style curve , just like relation curves of waterflooded rock resisitivity with water saturation , but salinity variation has little effect on rock dispersion property
  摘要通过水淹岩石岩电特性的实验研究发现，地层水矿化度的变化，对岩石电阻率幅值的影响较大，致使单一频率下的岩石复电阻率幅值和同相电阻率也会象常规电阻率一样，随着含水饱和度的变化，出现" u "形曲线，而相对而言，地层水矿化度对岩石频散特性的影响较小。