地下水矿化度，即单位体积地下水中可溶性盐类的质量，常用单位为g/L或mg/L。它是水质评价中常用的一个重要指标。
阿拉尔地区地下水矿化度含量高、水咸，地表水也随季节变化时咸时淡。
Subterranean water in Alar area is salty, with high total salinity, and surface water becomes less salty or saltier with seasonal rhythm.
该区地下水矿化度的“倒转”分布规律是因地下水的热对流运动而形成的。
The "reversed" distributive rule of TDS for the groundwater in this area is contributed to the hydrothermal convection of groundwater.
储层压力的影响因素有构造应力、地下水头高度及埋深、地下水矿化度等。
The major influencing factors are tectonic stress, height and burial depth of groundwater, the mineralization ability in groundwater and so on.
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