地层水矿化度的英文
formation water salinity
reservoir water salinity
例句与用法
更多例句： 下一页- 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。
