三斜晶系
粘土矿物
锌
粉末衍射
堆积
八面体
乙二醇
伊利石
晶体结构
镁
结晶学
结构式
皂石
矿物学
无机化学
化学
材料科学
有机化学
烷基
作者
Qi Tao,Chaogang Xing,Seungyeol Lee,Long Yang,Qingjin Zeng,Shangying Li,Tian‐Qi Zhang,Guanglie Lv,Hongping He,Sridhar Komarneni
出处
期刊:American Mineralogist
[Mineralogical Society of America]
日期:2022-08-24
卷期号:108 (7): 1357-1367
被引量:3
摘要
Abstract An aluminum-free zinc-bearing smectite (Zn-smectite) was synthesized under hydrothermal conditions, together with its magnesium substituted products. Its layer charge calculated by cation exchange capacity (CEC) is 117.4 mmol/100 g. Powder X-ray diffraction (XRD) revealed turbostratic stacking and showed that the d06l value of the Zn-smectite was >1.525 Å, indicating that it is trioctahedral. Its d001 value increased from ca.12.8 Å to ca. 16.0 Å after ethylene glycol (EG) saturation. The Zn-smectite did not irreversibly collapse after heating the Li+-saturated sample to 300 °C, suggesting that its layer charge was generated from octahedral-site vacancies (defects). The Zn-smectite resembles zincsilite-like minerals with interlayer Na+ and Zn2+. The intralayer structure of zincsilite was confirmed by pair distribution function (PDF) analysis, and the whole crystal structure was built and optimized by DFT calculation in the CASTEP module of the Materials Studio software. Synthetic zincsilite is triclinic, space group P1, and its optimized unit-cell parameters are: a = 5.294 Å, b = 9.162 Å, c = 12.800 Å, α = 90.788°, β = 98.345°, and γ = 90.399°.
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