粘土矿物

The ability of clay minerals to catalyse decarboxylation has long been recognised.

粘土矿物能催化脱羧基作用是早已认识到的问题。

Two basic types of clay minerals are present in most soils.

大多数土壤中出现了两类主要的粘土矿物。

They are stabilized through absorption by clay minerals.

它们通过粘土矿物的吸收作用而得到稳定。

Bentonite is an expandable three - layer clay mineral.

皂土是一种可膨胀的土层粘土矿物。

These changes reflect the effects of burial diagenesis on the originally deposited clay mineral assemblage.

这种变化反映了埋藏成岩作用对原来沉积的粘土矿物组合的影响。