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在浅水面以上的内生矿床矿石,其地球化学环境与原生矿石带有显著的不同。在地表附近,有机物,大气中的氧,温度的剧烈变化的作用以及水的物理及化学作用特别强烈。查明有元素的新的产出形式,即呈类质同像混入物并吸附于粘土矿物中以及呈离子状态吸着于土壤膠体中。一部分元素被微生物,植物所吸附,或者与土壤有机物化合。在疏松层中元素除继续进行垂直方向的移运外,尚广泛进行水平方向的位
In the shallow water above the endogenous ore deposits, the geochemical environment and the primary ore with a significant difference. Near the surface, the role of organic matter, atmospheric oxygen, dramatic temperature changes, and the physical and chemical actions of water are particularly strong. Identify new forms of production of the element, ie, a homogenous blend and adsorbed in clay minerals and being ionically adsorbed in soil colloids. Some of the elements are adsorbed by microorganisms, plants, or combined with soil organic matter. Elements in the loose layer in addition to continuing the vertical direction of the transport, but also a wide range of horizontal position