卤水比蒸发系数的数学模型——石盐析出阶段和光卤石析出阶段  

The Mathematical Model of Specific Evaporation Rate of Brine——in the hylite and carnallite crystallization stages

作　　者：张军[1] 刘铸唐[1] 

机构地区：[1]中国科学院盐湖研究所,西宁810008

出　　处：《盐湖研究》1993年第2期23-27,共5页Journal of Salt Lake Research

摘　　要：本文在察尔汗盐湖卤水不同浓缩阶段比蒸发实验的基础上,比较系统地处理了该实验的数据,建立了在石盐析出阶段和光卤石析出阶段卤水比蒸发系数的数学模型,给出了与卤水密度和大气相对湿度相关的经验方程式。Based on the test of specific evaporation rate of brines of Chaerhan salt lake in different concertration stages, a systematical treatment of test data is given in this paper. And also the mathematical model of the specific evaporation rate of the brines in the hylite and carnallite crystllization stages is developed and an empirical formula with two parameters, the density of the brine and the relative moisture of the air, is provided.

关 键 词：卤水 比蒸发系数 石盐 光卤石 

分 类 号：P641.5[天文地球—地质矿产勘探]