卤水比蒸发系数的数学模型——氯化镁饱和阶段  

The Mathematical Mode of the Ratio of Relative Evaporation Rate of Brine.—in the Bischofite Crystallizing Stage

作　　者：张军[1] 张宝全[1] 刘铸唐[1] 王建中[1] 王萍 

机构地区：[1]中国科学院青海盐湖研究所,西宁810008

出　　处：《盐湖研究》1993年第4期45-51,共7页Journal of Salt Lake Research

摘　　要：本文在察尔汗盐湖氯化镁饱和不同浓缩阶段卤水比蒸发实验的基础上,处理了在氯化镁析出阶段卤水的比蒸发实验数据,完成了比蒸发系数二元参数的拟合,给出了该卤水的蒸发模型。并与石盐析出阶段和光卤石析出阶段比蒸发系数的数学模型相衔接,对氧化镁饱和前后不同蒸发机理进行了探讨。Based on the test of relative evaporation rate of brines of Chaerhan salt-lake in different concertrating stages, the paper deals with the data of the test systematically, establishes the mathematical mode of the ratio of the relative evaporation rate of the brines in the bischofite crystllizing stage, and provides the empirical equition that depends on two parameters: the density of the brine and the relative moisture of the air.

关 键 词：比蒸发系数 氯化镁结晶 卤水 

分 类 号：P641.464[天文地球—地质矿产勘探]