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察尔汗盐湖是干旱内陆闭流盆地型现代盐湖。随着湖水的不断蒸发浓缩,有以岩盐为主的各种盐类沉积。在岩盐中赋存有饱和的晶间卤水(钾镁盐液相矿床)。察尔汗区段除南、北边部之外,大部份晶间卤水水化学类型属于氯化物型的 K~+、Na~+、Mg~(2+)/Cl~- —H_2O对四元体系。本文着重论述该四元体系晶间卤水比重和运动粘滞系数二者之间的变化关系、空间分布规律、换算方法及其与卤水浓度的关系。如所周知,晶间卤水的粘度和比重对渗流速度、盐田蒸发速率、抽水设备选择和管
Chalhan Salt Lake is a modern saline lake in arid inland closure basin. As the lake continues to evaporate and concentrate, there are a variety of salt-based sediments. Saturated intergranular brine (potassium-magnesium salt liquid-phase deposit) is present in the rock salt. Most of intergranular brine water chemistry types belong to the chloride type K ~ +, Na ~ +, Mg ~ (2 +) / Cl ~ - -H_2O for quaternary system. This article focuses on the quaternary system intergranular brine specific gravity and kinematic viscosity of the relationship between changes in the relationship between the spatial distribution of the conversion method and its relationship with the concentration of brine. As we all know, the intergranular brine viscosity and gravity on the seepage velocity, salt field evaporation rate, pumping equipment selection and pipe