由风化作用形成的水溶胶,再经胶凝作用固结为成分复杂的隐晶质或非晶质固体物质称为胶体矿物.
这就是判断胶体矿物和胶体沉积时地质环境的理论根据。
This is the theoretical basis to judge the geological environment of the sedimentation of colloform and colloid minerals.
有机化学和矿物化学的结合，以及无定形材料化学和胶体材料化学的结合，是这一世纪混凝土成功的秘诀。
The combination of organic chemistry and mineral chemistry, as well as the combination of non - fixed form material and colloid material chemistry are the secret formula in this century.
DNA在红壤胶体或矿物表面的吸附是一个熵增过程。
DNA adsorption on soil colloids and minerals is driven by an increase in entropy.
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