Distribution of quartz are opposite to clay minerals.
石英分布与粘土矿物相反。
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。
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。
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。
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。
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。
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。
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。
Clay minerals are widely distributed in the salt-bearing series in the Arming basin.
粘土矿物在安宁盆地含盐系中分布很广。
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。
Formation of late authigenic clay minerals and recrystallization of early clay minerals.
晚期自生粘土矿物的形成和早期粘土矿物的重结晶作用。
The REE in coals is concentrated in clay minerals, and the main occurrence is in kaolinite.
稀土元素在粘土矿物中含量高，主要以高岭石的形式赋存。
The work to develop nature clay minerals as novel catalyzer carrier has been paid great attention.
开发天然粘土矿物新型催化剂载体的工作一直为人们所重视。
The result shows that the main types of clay minerals are illite , smectite, kaolinite and chlorite.
这些粘土矿物主要由伊利石、蒙皂石、高岭石和绿泥石组成。
The surface area of crystalline clay minerals is highly dependent on the extent of lattice expansion.
结晶粘土矿物的表面积主要依赖于晶格膨胀的程度。
The next step is to try to staunch the flow proper with drilling mud, a mixture of water and clay minerals.
下一步是设法很巧妙地用由水与黏土矿物质组成钻探泥浆堵住原油的涌出。
This charge, which accumulates mainly at interfaces between clay minerals, is responsible for the IP effect.
这些聚集在粘土矿物界面上的电荷就产生了激发极化效应。
The main structure unit of clay minerals contains silicon-oxygen tetrahedron and aluminium-oxygen octahedron.
其主要结构单元是硅一氧四面体和铝一氧八面体。
These clay minerals mainly come from parent material, a few from pedogenic processes, and dust input is minute.
它们主要来源于母质，其次来自成土过程，降尘输入量极有限。
The content of mineral-fixed ammonium in soil was related not only to soil clay minerals but also to fertilization.
固定态铵的含量不仅与土壤中的粘土矿物有关，施肥对其也有影响。
Shown by analysis, the main factors causing the reservoir sensibility in this area are clay minerals and carbonate.
分析表明，储层填隙物中的粘土矿物、碳酸盐矿物是导致该区储层敏感性的主要因素。
Electric current flows through clayey soils by the conduction of void water, electric double layer and clay minerals.
粘性土是通过孔隙水、粘粒周围的双电层以及粘土矿物来导电的。
The results showed that the releasing characteristics and availability ofnonexchangeable K related remarkably to clay minerals.
结果表明，供试土壤非交换性钾释放特性和有效性与粘土矿物密切相关。
In this paper, characteristics of neogenic clay minerals and micro-surface texture of quartz fragment in fault gouge are discussed.
本文主要研究断层泥中新生的粘土矿物特征，并研究断层泥中石英碎砾表面溶蚀的显微形貌结构特征。
Selective catalysis of different clay minerals within source rock is the most important factor of affecting hydrocarbon composition.
烃源岩不同粘土矿物的选择性催化特征是影响油气组成的最重要因素。
A group of clay minerals formed during the alteration of silicate minerals such as mica and feldspar and commonly found in Marine shales.
硅酸盐矿物(如云母和长石)的蚀变作用期间形成的一族粘土矿物，通常见于海相页岩内。
It is composed of a variety of mineral water aluminum silicate, a basic element of minerals kaolinite, water, such as kaolinite clay minerals.
它是由多种矿物组成的含水铝硅酸盐，基本矿物成份有高岭石、多水高岭石等粘土矿物。
Many sedimentary rocks contain clay minerals and 76% of forming-rock minerals of slope rocks can produce clay minerals during the weathering processes.
除沉积岩斜坡含粘土矿物外，76%以上的斜坡岩石造岩矿物还可形成次生粘土矿物。
The anomalous high pressure originated from integrated effect of generation of hydrocarbons, differential compaction and transformation of clay minerals.
异常高压是由烃的生成、差异压实以及粘土矿物的转化等因素共同作用而导致。
The effect and mechanism of phosphorus removed was summarized, in order to set good foundation for exploring clay minerals better in waste water treatment.
因此， 系统总结粘土矿物对磷的去除效果与机理，为更好的开发粘土矿物在废水处理的应用奠定基础。
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