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- mica clay mineral 云母粘土矿物
- Bentonite is an expandable three-layer clay mineral. 皂土是一种可膨胀的土层粘土矿物。
- The clay cation exchange capacity is affected by 2:1 type Clay mineral content. 粘粒阳离子交换量的高低与2:1型粘土矿物含量的多少相吻合。
- It occurs as an exchangeable base in the clay mineral and organic fractions of soils. 钙是以交换性盐基在粘土矿物及土壤的有机部分出现的。
- 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。
- XRD is used to measure the crystalizaiton index of the illite in the clay mineral. 摘要利用X射线衍射仪可以测量粘土矿物中伊利石结晶程度。
- While with SOM content below 1%,clay mineral played an important role in pyrene sorption and desorption process. 有机质含量低于1%25时,黏粒和有机质含量都对土壤的吸附/解吸能力有重要影响。
- The identification of the clay mineral types by using natural gamma-ray spectrosc-opy log method was discussed. 自然伽马能谱测井不仅可以测得地层的总自然伽马值,同时还能得到地层的铀、钍、钾含量。
- 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。
- The petrographic thin section indicates that themain types of clay mineral is chlorite, kaolinite and illite. 据岩石薄片鉴定，粘土矿物类型主要有伊利石、绿泥石和高岭石。
- 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。
- Clay mineral contain rich illite and chlorite but lean kaolinite and illite/smectite mixed layer. 粘土矿物组成富含伊利石和绿泥石，贫高岭石和伊利石／蒙皂石。
- In the tectonic activity stage, the evolution of clay mineral was influenced by hydrocarbon emplacement and deep fluid. 有机质成熟期主要受成岩作用影响，在酸性成岩环境下高岭石大量产生；
- The dissolution of detrital grain, clay mineral and calcite is the main factor for forming secondary pores. 碎屑颗粒、粘土矿物及碳酸盐的溶解是形成次生孔隙的主要因素；
- 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；
- Although the main clay mineral is Kaolinite, the structural change during heating is different from pure kaolinite. 其主要粘土矿物是高岭石，但加热相变有别于纯净的高岭石。
- 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；
- Illite is used in various fields as a new clay mineral, but many problems exist to be researched in its application. 伊利石作为一种新的粘土矿物,已经在多个领域中获得了不同程度的应用,但是在其应用中仍然存在很多问题有待于研究。
- Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the Meso-Cainozoic detrital rocks in Tarim basin. 根据自生矿物与粘土矿物组合，在塔里木中新生界碎屑岩中可以识别出两种成岩环境。
