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degree of mineralization meaning in Chinese

矿化程度
矿化度

Examples

  1. Results the study had revealed that not only the bone tubular and the degree of mineralization , but also the activity expression of alkaline phosphatase of osteoblasts in fluoride group were better than the control group
    结果研究发现氟组成骨细胞不仅其矿化结节和矿化程度,而且其碱性磷酸酶活性表达都要早于对照组。
  2. The result show that degree of mineralization and total hardness have both increased to different extent in majority survey station , hydrochemistry type has transformed in individual station and reflecting the deteriorated water quality
    对比结果表明:大多数测站的矿化度和总硬度均有一定程度的增大,水化学类型个别站点有所改变,显示水质变差。
  3. According to hydrochemistry monitoring material of northwest rivers in recent five years , and compared with the first northwest rivers water resources investigation appraisal result in 80 ’ s of last century , we analyzed the main rivers hydrochemistry condition , runoff degree of mineralization , total hardness and the hydrochemistry type distribution
    根据近5a来对西北诸河的水化学监测资料,统计出了主要河流水化学状况;分析了河川径流矿化度、总硬度和水化学类型的地区分布,并与20世纪80年代第一次西北诸河水资源调查评价的结果进行了比较。
  4. 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。
  5. Beginning with the analyse of present situation and cause of formation of saline - alkali land , the irrigated area overall water salt trends are analysed , and the irrigated area saline - alkali land and the groundwater level and distribution law of groundwater degree of mineralization are expounded , the trendence of irrigated area saline - alkali land is put forward . then water salt balance model is estanbished according to the relationship of irrigating and drainage . regarding the irrigated area as a balance area , by analysis of mineralization degree of water pumping from the yellow river and drained off water from irrigated area , the change of the draining off water ion is forcasted in water reducing condition
    课题研究主要从盐碱地现状与成因及灌区总体水盐动态分析两方面入手,阐述了灌区盐碱地、地下水位、地下水矿化度的分布规律,分析了灌区盐碱地的成因及变化趋势;根据灌区灌溉、排水条件与以上各种因素的关系,建立了灌区水盐均衡模型;把灌区作为一个均衡区,通过对黄河来水矿化度、灌区排水矿化度的分析,预测了在灌溉引水、排水减少时排水离子量的变化;运用灌区水盐动态模型原理,对灌区现状( 1998 、 2000年)与规划水平年总体水盐平衡进行了计算;总结分析了灌区水盐动态变化趋势,计算并提出了排水控制标准。
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