大部分微量元素，包括锰和砷，通过自然过程中的岩石风化作用进入水体。
Most trace elements, including manganese and arsenic, get into the water through the natural process of rock weathering.
岩石的风化作用基本上是一种静力作用。
风化作用改变了岩石的矿物成分，岩石在风化过程中表现出来的阶段性，反映了岩石的不同风化程度。
Weathering action changes the mineral composition of rocks, and the periods of weathering process reflect weathering intensity.
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