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。
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。
The potassium compounds are enriched at the lowest water level in the brine lake by the processes of selective solution.
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