kaolinite ['keiəlinait]

kaolinite的基本解释

n.

高岭石

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。

与kaolinite相关的网络解释 [注：此内容来源于网络，仅供参考]

kaolinite：高岭石

) 粘土矿物( 粘土矿物(Clay mineral) 可以指示水介质:高岭石( Kaolinite)多形成于 ) 酸性水介质中; 伊利石( Illite)则发育在碱性水介质中. 鲕绿泥石( ):在现代沉积物中,鲕绿泥石多出现在热带浅海中, 鲕绿泥石(Chamosite): ): 水深不超过60米.

kaolinite：高岭土

正长石(Orthoclase)(铝硅酸盐长石(aluminosilicate feldspar)) + 碳酸 + 水 -> 高岭土(Kaolinite)(为一种黏土矿物) + 硅酸溶液 + 溶液中的钾(potassium)及重碳酸盐离子种种金属在风化环境中会产生氧化作用(Oxidation).

kaolinite：土的分类高岭石

3. 土的分类粉质粘土silty clay | 3. 土的分类高岭石kaolinite | 3. 土的分类过压密土(台)overconsolidated soil

kaolinite：高岭石;纯高岭土

kaolin 白陶土;高岭土[陶土的高级品种] | kaolinite 高岭石;纯高岭土 | kapok oil 木棉(籽)油

kaolinite clay：高岭土

flame chipping 热修整(铸造的) 烧剥 火焰表面清理 | kaolinite clay 高岭土 | bronze medal winner 铜质奖章获得者, 第三名