brine lake

基本解释

The potassium compounds are enriched at the lowest water level in the brine lake by the processes of selective solution.
由于选择性溶解作用使钾富集在水位最低的卤水湖内，并在干盐滩与卤水湖之间的平坦湖滨地带形成钾盐层。
A fresh supply of yellow froth (probably the same type of elemental sulfur found in the "cool acid-brine" crater lake at Kawa Ijen) is brought up by the plume and pushed out toward the crater wall.
一个新的黄色气泡（与在Kawa Ijen“冷酸海水”火山湖中的元素硫是同一类）是由热烟柱带出湖面，并推向岩壁。
Seismic velocity and wave impedance properties of brine lake formations are analyzed using 2D seismic data with high resolution factor, forward, inversion and forecasting method for model are studied.
利用高分辨率二维地震资料，分析了盐湖地层地震速度和波阻抗特点，并对模型进行了正、反演及预测方法研究。