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1·Distribution of quartz are opposite to clay minerals.

石英分布与粘土矿物相反。

2·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。

3·Heat analysis is an effective method of studying clay minerals.

热分析是研究粘土矿物的一种特效方法。

4·One of the simplest examples of phyllosilicates is clay minerals.

验证层状硅酸盐存在的一个最简单证据就是粘土矿物。

5·There is also interaction between clay minerals and pesticide residues.

农药残留与粘土矿物也存在相互作用。

6·Arsenic of silicate mainly comes into crystal lattice of clay minerals.

硅酸盐态砷主要进入粘土矿物晶格。

7·The main types of clay minerals are illite, smectite, kaolinite and chlorite.

粘土矿物主要由伊利石、蒙皂石、高岭石和绿泥石组成。

8·Under the different geological conditions, the various clay minerals with high.

在不同的地质条件下形成不同的富铀粘土矿物。

9·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。

10·The composition of clay minerals is the main cause generating low-resistivity gas zone.

粘土矿物成份是造成气层电阻率低的主要原因。