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kaolinite相关的网络例句

查询词典 kaolinite

与 kaolinite 相关的网络例句 [注:此内容来源于网络,仅供参考]

There are three evolution paths for the kaolinitic rocks in the diagenesis:one is that kaolinite is transformed to the mixed minerial of kaolinite/dickite and dickite in the acid environment; the second is to be trnasformed to the ammonium illite,chlorite and pyrophyllite in alkaline environment;The third is to be transformed to well ordered kaolinite in the superfacial environment. The highly orderization of kaolinite may be related to the hot solution underground.

提出煤系高岭岩三种成岩演化轨迹;一种是在酸性环境下朝高岭石/地开石间层矿物和地开石方面演化;另一种是在碱性环境中朝氨伊利石、绿泥石和叶腊石方向演化;第三种是在表生环境种朝高度有序高岭石方向演化,高岭石的高度有序化可能与热水溶液作用有关。

Paragenetic association I are composed of dissolved feldspar, quartz overgrowth and authigenetic kaolinite, This paragenetic association came into being acidic environment; Paragenetic association II include illite、albite、dissolved authigenetic quarze and kaolinite、dolomite、ankerite and ferrocalcite, the paragenetic association formed alkali environment; secondly, outcrop sandstones include paragenetic association III making up of dissolved feldspar、kaolinite、dickite and ironstone too, this paragenetic association came into being ground surface acidic environment.

成岩共生组合I由长石颗粒溶解、次生加大石英和自生高岭石组成,该组合形成于酸性成岩环境;成岩共生组合II由自生伊利石、自生钠长石、自生石英与高岭石溶解、白云石、铁白云石、铁方解石组成,该组合形成于碱性成岩环境;其次,露头砂岩还包括由长石颗粒溶解、高岭石、地开石、褐铁矿组成的第III种成岩共生组合,该组合形成于地表酸性成岩环境。

At the heavy metal concentration of 3-4ppm, our study on adsorption capacity, adsorption selectivity of montmorillonite, illite and kaolinite to Cu〓、 Pb〓、 Zn〓、 Cd〓、 Cr〓 shows that the adsorption capacity is mainly determined by the capacity of exchangeable cations and the adsorption capacity of the three clay minerals decreases in this sequence: montmorillonite >> illite>kaolinite. It is found that clay minerals have obvious adsorption selectivity to various heavy metals. Montmorillonite exhibits a stronger affinity to Cr〓 and Cu〓 while kaolinite and illite sorb Cr〓 and Pb〓 more effectively. At the same heavy metal concentration, adsorption amount of clay minerals to heavy metals increase with increasing pH value of the solution.

在痕量浓度下,研究了蒙脱石、伊利石、高岭石三种粘土矿物对Cu〓、Pb〓、Zn〓、Cd〓、Cr〓五种重金属离子的吸附容量、吸附选择性及其介质条件对吸附量的影响,结果表明,粘土矿物的阳离子交换容量越大,对重金属离子的吸附容量也越大,其大小顺序为蒙脱石>>伊利石>高岭石;同时,不同粘土矿物对重金属离子具有明显的吸附选择性,蒙脱石对Cr〓和Cu〓有较好的选择性,伊利石和高岭石则对Cr〓和Pb〓有较好的选择性;随着吸附溶液pH值的增大,其吸附量有增加的趋势。

The content of kaolinite varies in the range of 80%to 95%.Two occurrences of kaolinite are rev ealed:one is in the form of aggregate of vermiform crystals;another is in the form of cryptocrystalline or colloidal materials.Its crystallization index is calculated to be 0.54~0.74a nd 0.47~0.53,indicating its higher degree o f order.Chemical analyses show that the compositions of kaolinite are close to its theoretical values.

光学及扫描电子显微镜、 X射线衍射分析和红外分析等系统性研究的结果表明,高岭石主要有两种存在形式,一种呈蠕虫状集晶,另一种是隐晶质或胶状高岭石,测得其结晶指数分别为 0.54~ 0.74和 0.47~ 0.53,说明其有序度偏高;化学分析结果表明,其化学成分接近于高岭石的理论值, Al2O3含量达 35%~ 37%, SiO2含量为 47%~ 48%,碱金属、碱土金属及其他氧化物含量很低。

Alunite is a harmful impurity which is difficult to remove from kaolinite, and so is kaolinite in alunite ore.

明矾石是高岭土中难以除去的有害杂质,高岭石也是明矾石矿石中的有害杂质。

In general, in citric acid and oxalic acid solution, kaolinite nearly dissolved congruently in reactive metaphase or anaphase; In malic acid solution, stoichiometry of kaolinite dissolution is complex.

对于柠檬酸和草酸而言,一般情况下,高岭石是在反应中期或后期才趋于同步溶解;而对于苹果酸而言,高岭石溶解同步性较为复杂。4 有机酸能促进高岭石中 K+、Na+、Ca2+、Mg2+等盐基离子的释放,甚至在较低的浓度(100μM)。

Kaolin is mainly composed by small sheet form, tubular shaped Kaolinite minerals (the kaolinite, pearl stone, halloysite...etc.) that less than 2 microns. It is mainly used in porcelain and ceramics industry, deckle industry and the chemical engineering industry.

高岭土主要由小于2个微米的微小片状、管状、叠片状等高岭石簇矿物(高岭石、地开石、珍珠石、埃洛石等)组成,主要应用于陶瓷工业,造纸工业及化工工业填料,耐火材料,石油化工及尖端技术领域等。

The influences of several metal ions on the flotation of diaspore and kaolinite were investigated by flotation experiments and measurement of zeta potential. The results show that there are little influences of Na+ and K+ on the flotability and zeta potentials of diaspore and kaolinite.

摘 要:通过一水硬铝石和高岭石纯矿物的浮选试验和动电位测定,研究不同种类的金属离子对一水硬铝石和高岭石浮选行为的影响。

Due to its linear chain structure, polyacrylamide, combined with DDA, tends to form the high molecular collector with more surface activities. In addition, with the high molecular weight, polyacrylamides (with the exception of hydroxamic acid polyacrylamide) can strongly flocculate kaolinite, which can increase the adsorptive density of collector and activate the kaolinite flotation.

由于分子的直链结构,聚丙烯酰胺药剂易与捕收剂十二胺形成表面活性更高的高分子捕收剂,同时由于聚丙烯酰胺具有较高的分子量,对高岭石显示很好的絮凝作用,增加了捕收剂的吸附密度,活化了高岭石的浮选。

In addition, the ratio of illite /kaolinite percent content shows a negative interrelation with kaolinite percent content.

伊利石/高岭石含量的比值变化与高岭石含量变化呈明显的负相关关系。

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