伊利石

基本解释 (translations)

illite

与伊利石相关的网络例句 [注：此内容来源于网络，仅供参考]

The clay minerals in the eluvial soils consist of illite/ montmorillonite, illite and kaolinite with low and intermediate dilatability, so their permeability is low or very low.

土中粘土矿物由伊利石，蒙脱石、伊利石和高岭石组成，具低-中等膨胀性，因而其渗透性低-极低。

The results of experiments and analysis shown that the clay mineral is mainly gerundive, montmorillonoid is little, but a great quantity of sodium-ion in gerundive soil and larger pH make the soil as well as montmorillonoid which is intense dispensability, These are two keys for the soil to disperse.

试验和分析结果表明，土样中的粘土矿物主要以伊利石为主，蒙脱石含量较少；伊利土中含有大量的钠离子，使得伊利土象钠蒙脱土一样具有强分散性；pH值较高，使得土壤颗粒之间的净势能表现为斥力，这也促使土样土样产生分散性。

The presence of ferric oxide in the ores is key factor resulting in low whiteness of illite.

河南舒山伊利石矿中氧化铁的存在是造成伊利石白度低的主要原因。

With a quantitative research on the chemical and clay compositions of marly stones, their weathering rocks and residuals, as well as SEM observations, the process of dissolution of CaCO 3 and concentration of clay minerals with complex...

通过泥灰质岩石及其不同风化岩和残坡积土的化学成分、粘土矿物成分定量研究和扫描电镜观察，揭示了 Ca CO3溶蚀和粘土矿物富集过程及粘土矿物的复杂成分，发现了风化过程中伊利石向伊利石/蒙脱石混层粘土矿物的转化，解释了岩土工程性质恶化的原因，从而提高了地质研究和地质灾害研究的水平。

With a quantitative research on the chemical and clay compositions of marly stones, their weathering rocks and residuals, as well as SEM observations, the process of dissolution of CaCO 3 and concentration of clay minerals with complex components has been disclosed, and the conversion of illite to mixed-layer illite/montmorillonite discovered, which explain the reason for deterioration of geotechnical properties of the rocks and soils, thereby enhancing the level of geological and geohazards researches.

通过泥灰质岩石及其不同风化岩和残坡积土的化学成分、粘土矿物成分定量研究和扫描电镜观察，揭示了CaCO3溶蚀和粘土矿物富集过程及粘土矿物的复杂成分，发现了风化过程中伊利石向伊利石/蒙脱石混层粘土矿物的转化，解释了岩土工程性质恶化的原因，从而提高了地质研究和地质灾害研究的水平。

With the Jinshan gold deposit in Jiangxi Province as an example, the authors determined the crystallinity, mean crystal size and lattice strain of illite and chlorite and, on such a basis, discussed the difference of crystallinity, mean crystal size and lattice strain between illite and chlorite caused by deformation of mylonite and untramylonite.

本文以江西金山金矿为例，通过对热液蚀变粘土矿物伊利石和绿泥石结晶度、平均结晶大小和晶格应变的测定，讨论了岩石变形对伊利石和绿泥石结晶生长差异的影响。

Illite fundamental particles showed platy to lath shapes. Platy particles exhibited various spiral growth patterns, i.e. circular, malformed circular, polygonal single unit-cell layer spirals, polygonal parallel step spiral, interlaced spiral patterns, etc.

伊利石单元粒子生长过程中，伊利石单元粒子呈现从板状体到条状体的生长，而板状颗粒又呈现各种螺旋生长图案，有圆形、残缺的圆形、多边螺旋、平行阶梯状螺旋、交错螺旋等。

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 recent achievements for illite fundamental particle including the formation mechanisms, the shape variations in the formation process, and the diagenetic stages division were also summarized in the paper.

还对伊利石单元粒子的生长机理及形成过程中的形态变化、利用伊利石单元拉子的厚度划分成岩作用阶段等方面的研究成果进行了综述。

There are three stages in the formation process of illite fundamental particle:① the nucleation stage of 2-nm thick illite particle at the incipient process of montmorillonite illitization;② the simultaneous nucleation and growth stage and ③ the surface-controlled growth stage.

伊利石单元粒子的形成过程有三个阶段：蒙脱石伊利石化过程中2nm厚的伊利石粒子的成核作用阶段、成核作用与生长作用阶段和表面控制生长阶段。

与伊利石相关的网络解释 [注：此内容来源于网络，仅供参考]

Illinoisan stage：伊利诺斯阶

Illinites 伊利粉属 | Illinoisan stage 伊利诺斯阶 | illite 伊利石

Illinoian glacial stage; Illinoisan glacial stage：伊利诺冰期

肠骨 ilium | 伊利诺冰期 Illinoian glacial stage; Illinoisan glacial stage | 伊利石 illite

hydromica：伊利石

hydromica slate 水云母石板瓦 | hydromica 伊利石 | hydromorphoe 氢吗啡酮

illite hydromica：伊利水云母

Illinois Central Gulf Railroad Company (美)伊利诺斯中央海湾铁路公司 | illite hydromica 伊利水云母 | illite structure 伊利石结构

illite：伊利石

) 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.

Illite mine：伊利石

强制通风:ventilation | 伊利石:Illite mine | 智能雷:Smart mine

stripped illite：剥露伊利石

条状地 striped ground | 剥露伊利石 stripped illite | 剥露构造面 stripped structural surface

degraded illite：劣质伊利石

减坡 degrade | 劣质伊利石 degraded illite | 下蚀河流 degrading stream

degraded illite：脱钾伊利石

减坡 degrade | 脱钾伊利石 degraded illite | 退变新生作用 degrading neomorphism

u Illite：(伊利石)

u Gypsum(石膏) | u Kaolinite(高岭石) | u Illite(伊利石)