In such vertical convection system, potassium ions were continuously enriched due to the concentration by evaporation. The current K-rich brines during the glauberite intergranular were formed eventually.

  • 在这种垂向对流系统中,蒸发浓缩作用导致钾离子不断富集,最后形成目前的钙芒硝晶间富钾卤水。

  • 互联网摘选 2025-01-20 11:39:45

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