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对５１２铀矿床粘土矿物质量分数、分布特征进行了较全面的分析，指出该矿床中粘土矿物以成岩期为主，在后生成矿作用中又叠加了新的粘土蚀变产物，各亚带粘土矿物组成基本类似但又存在一定差异．粘土总量和蒙皂石能较好地反映各亚带的成矿物理化学条件的改变；粘土矿物对Ｕ有明显的吸附富集作用，但又有抑制作用，即粘土质量分数过高或氧化带粘土蚀变太强烈不利于铀在过渡带沉淀富集成矿．此外，对粘土矿物成分对地浸工艺开采过程中的不利影响进行了分析，提出地浸工艺中必须重视对粘土组分的研究．
The comprehensive analysis of the clay minerals in 512 uranium deposits shows that the clay minerals in this deposit are dominated by diagenesis and that new clay alteration products are superimposed in the post-forming mineralization. Mineral composition similar but there are some differences. The total amount of clay and smectite can well reflect the change of the physicochemical conditions of mineralization in each subzone; clay mineral has obvious adsorption and enrichment effect on U, but has inhibitory effect, ie, the clay mass fraction is too high or the oxidation zone Clay alteration too strong is not conducive to uranium deposition in the transition zone enrichment of mineralization. In addition, the adverse effects of the clay minerals on the in-situ leaching process were analyzed, and the research on the clay components must be emphasized in the ground-leaching process.