摘要
根据Na+,K+,Mg2+∥Cl-,SO42-五元水盐体系介稳相图的理论分析,对昆特依盐湖卤水进行自然蒸发,研究昆特依卤水在自然条件(蒸发温度为12℃~30℃之间,大气压为77.33 kPa,海拔2 260 m^2 500 m。)下的析盐规律,获取了该湖晶间卤水蒸发结晶路线及物料关系并相应建立数学模型。
According to theoretical analysis of the five-salt system and metastable the phase diagram of Na＋,K＋,Mg2＋∥Cl-,SO2-4,and study the law of precipition of mineral salts in Kunteyi Salt lake brine under natural conditions（Evaporation temperature is between 12 to 30 degrees,Atmospheric pressure is 580 mm measuring column,the Altitude of this place is 2 260-2 500 m） by natural evaporation,getting the line of evaporation and crystallization of intercrystalline brine of the salt lake,and establishing the corresponding mathematical model.
出处
《盐业与化工》
CAS
2011年第4期39-42,共4页
Jounral of Salt and Chemical Industry
关键词
卤水
数学模型
昆特依
光卤石
蒸发
bine
mathematical model
Kunteyi
carnallite
evaporation
