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Keywords clay minerals;Hegang Coalfield;type;depositional environment; 粘土矿物;鹤岗煤田;类型;沉积环境;
Keywords Clay minerals;Solvable organic matter;Combination pattern;SFE; 粘土矿物;可溶有机质;结合关系;超临界抽提;
Keywords Clay minerals;Modification;Decolorizing Ceramsite;Mechanism;Printing and dyeing wastewater; 粘土矿物;改性;脱色陶粒;机理;印染废水;
Keywords clay mineral;crystallinity of illite;eolian loess;Xiashu loess; 下蜀黄土;黏土矿物;伊利石结晶度;风尘沉积;镇江;
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。
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。
SEM proves that the form of clay minerals is floccule and sheety. SEM结果显示东太平洋粘土矿物为絮状和片状；
Clay minerals are the mixture of chlorite and smectite and illite. 粘土矿物主要为绿泥石／蒙脱石混层和伊利石；
Keywords clay mineral;diagenetic change;physical properties of clastic rock;Shanshan Oil Field; 关键词粘土矿物;成岩变化;碎屑岩物性;鄯善油田;
In this paper,the adsorption effect of Zn~(2+) by three clay minerals,i. e. 探讨了在不同矿物投加量、不同振荡时间、不同Zn2+浓度、不同矿物颗粒细度和不同pH条件下,钠基膨润土、膨胀蛭石和沸石三种粘土矿物对Zn2+的吸附效果,并比较了三种粘土矿物对Zn2+的吸附差异性。
SiO-2, Al-2O-3 and Fe-2O-3 are three main parts in the clay minerals. 红土中粘粒部分的主要化学成分为SiO2 ,Al2 O3和Fe2 O3;
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。
The ability of clay minerals to catalyse decarboxylation has long been recognised. 粘土矿物能催化脱羧基是早已认识到的问题。
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。
Specific evidence for coordination complexes between pesticides and clay minerals is quite limited. 关于农药和粘土矿物之间的配位络合的明确证据是十分有限的。
The smectites are the most effective of the clay minerals as catalysts of these organic reactions. 对这些有机反应，蒙脱石是粘土矿物中最有效的催化剂。
Bentonite is an expandable three-layer clay mineral. 皂土是一种可膨胀的土层粘土矿物。
Clay minerals are widely applied in reconstructing paleoclimate, and many analysis methods are involved. 利用黏土矿物重建古气候近年来得到了广泛的应用,其分析测试方法较多。
Ore is in the phase of clay minerals in which gibbsite is less and kaolinite commonly coexists with illite. 矿石处在富粘土矿物阶段,少见三水铝石,一般为伊利石和高岭石共存。
On the condition of thermal contact metamorphism, clay minerals in coal are changed into andalusite. 无烟煤中红柱石是煤中粘土质矿物经热接触变质作用形成的。