1) salt body
盐体
1.
Under the influence of regional tectogenesis,the salt body underwent three times of plastic fluxion in geological history.
受区域性构造运动的影响，盐体在地史时期曾经历了三次较为明显的塑性流动：第一次发生在早二叠世末期，表现为盐体向南流动了２～２－８ ｋｍ ；第二次发生在晚三叠世—早侏罗世早期，盐体向南流动距离为１ ～２ 。
2.
According to the research of seismic data and drilling section of Carboniferous salt body in Akekule uplift,the geometry,inner stucture and spacial distribution characteristics were affirmed.
通过对塔里木盆地艾协克地区石炭系盐体的地质和钻井剖面研究，确定盐体的几何形态、内部结构和空间分布特征。
2) salt-water system
水盐体系
1.
Through the summary for the thermodynamic properties of binary,ternary and multi-dimensional salt-water systems containing sodium chloride at various temperatures.
总结了近几十年来含氯化钠电解质水溶液体系热力学性质的研究成果及其在盐湖、地下卤水、油田水和海盐制备等领域的应用,并对含钠水盐体系在不同温度下的热力学性质进行了总结,对于推动含钠水盐体系电解质溶液理论的发展和促进富盐湖卤水、地下卤水及海水的开发利用具有重要的意义。
2.
Studies on the phase diagrams of the lithium-containing salt-water systems are of great importance for the development of salt lake resources.
盐湖资源是我国西部的优势矿产资源之一,其成功开发需以相应的相平衡与相图为指导,因此含锂水盐体系的相平衡研究对于盐湖卤水资源的开发利用具有重要的意义。
3) rock salt mass
盐岩体
1.
According to the reality of bedded rock salt and clay interlayer in China,the constitutive model of seepage in rock salt mass is constituted and some numerical simulations are carried out in this paper.
结合中国地下油气储库建造过程中所出现层状盐岩体问题,建立盐岩体裂缝流体渗流数学模型,并进行了相应的数值模拟。
4) salt system
有盐体系
1.
Nano-silica white was prepared from salt system containing silica,Al3+ and Mg2+,in this preparation process some dispersant and surface modifying agent were applied and ammonia was used to adjust the pH of the solution.
利用含镁、铝盐的有盐硅酸体系,以氨水调节其pH,加入分散剂及表面改性剂,制备出平均粒径为60nm左右的白炭黑样品,通过此体系的pH值与所制样品比表面积的关系,探讨了有盐体系中硅酸的聚合机理,发现:当pH<3。
2.
Nano-silica white was prepared from salt system containing silica, Al3+ and Mg2+, in this preparation process some dispersant and surface modifying agent were applied and ammonia was used to adjust the pH of the solution.
利用含镁、铝盐的有盐硅酸体系,以氨水调节其pH,加入分散剂及表面改性剂,制备出平均粒径为60nm左右的白炭黑样品,通过此体系的pH值与所制样品比表面积的关系,探讨了有盐体系中硅酸的聚合机理,发现:当pH<3。
5) fluid salinity
流体盐度
1.
It is found that the ore-forming temperature decreases from early ore-forming period through ore-forming period to late ore-forming period, but the fluid salinity has no obvious change and the uranium deposits in Xiazhuang orefield was formed in mid-temperature (187～275℃) and low salinity (1.
研究结果表明,下庄铀矿田从成矿早期→成矿期→成矿晚期均一温度明显降低,但流体盐度变化不大,均为低盐度的流体。
6) sonar measuring technique
盐穴腔体
1.