渗入水的溶滤作用主要发生在腐岩的演化阶段。
The leaching of seepage water takes place in the evolution stages of the saprolite.
经过漫长地质年代的溶滤作用是控制深层地下水中氟含量的主要地球化学作用。
Lixiviation is chief geochemistry action to control fluorine content undergo very long geological age.
溶滤和蒸发作用是内陆干旱盆地平原区松散沉积层地下水咸化的主要原因。
Lixiviation and evaporation are main salinization processes of groundwater stored in loose sediments in inland arid basins.
溶滤和蒸发作用是内陆干旱盆地平原区松散沉积层地下水咸化的主要原因。
Lixiviation and evaporation are main salinization processes of groundwater stored in loose sediments in inland arid basins.
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