Aluminum ion occupancy in the structure of synthetic saponites: Effect on crystallinity

Aluminum ion occupancy in the structure of synthetic saponites: Effect on crystallinity
复制标题

合成皂石结构中铝离子的占据:对结晶度的影响

DOI:
10.2138/am.2014.4543
复制
发表时间:
2014
影响因子:
3.1
通讯作者:
Zhu Runliang
Zhu Runliang
中科院分区:
地球科学3区
文献类型:
--
作者:
He Hongping;Li Tian;Tao Qi;Chen Tianhu;Zhang Dan;Zhu Jianxi;Yuan Peng;Zhu Runliang

文献摘要

参考文献

被引文献

相似文献

摘要采用水热法合成了固定(Si+Al)/Mg和Si/Mg比的两个系列皂石。采用XRD、XRF、27 Al和29 Si MAS NMR、SEM和TEM对产物进行了表征。XRD图谱表明,在初始Si/Al比为5.43-7.89的范围内得到了有序的皂石。超过该Si/Al比范围,获得具有小结晶颗粒的不良结晶皂石,这可以从TEM图像中看出。当用表面活性剂插层皂石时,插层产物显示出强烈且有序的(00 l)反射,表明本研究成功地合成了层状皂石。27 Al MAS NMR谱表明,结晶良好的合成皂石比结晶不良的合成皂石具有更高的Al(IV)/Al(VI)比值,这是影响合成皂石结晶度的重要因素。一对一替换(即,1 Al ~(3+)→ 1 Mg ~(2+)的取代对合成皂石的结晶度有负面影响。在用硅烷接枝合成皂石之后,在-86ppm处的29 Si NMR信号的强度降低以及Q3 Si(0Al)和Q3 Si(1Al)信号的强度增加强烈地表明在约86 ppm处的信号降低。~ 86 ppm对应于皂石层边缘处的Q2 Si。
Abstract Two series of saponites with fixed (Si+Al)/Mg and Si/Mg ratios, respectively, were synthesized by using hydrothermal methods. The obtained products were characterized by XRD, XRF, 27Al, and 29Si MAS NMR, SEM, and TEM. XRD patterns showed that well-ordered saponites were obtained in the initial Si/Al ratio range of 5.43-7.89. Beyond this Si/Al ratio range, poorly crystallized saponites were obtained with small crystallized particles, which can be seen from TEM images. When intercalating saponite with surfactant, the intercalated products displayed strong and well-ordered (00l) reflections, indicating that layered saponite has been successfully synthesized in the present study. 27Al MAS NMR spectra demonstrated that well-crystallized synthetic saponites had a higher Al(IV)/Al(VI) ratio than the poorly crystallized samples, which is an important factor affecting the crystallinity of synthetic saponite. A one-to-one substitution (i.e., 1 Al3+ → 1 Mg2+) actually occurred in the octahedral sheet and this substitution had a negative effect on the crystallinity of the synthetic saponites. After grafting the synthetic saponites with silane, the decreased intensity of the 29Si NMR signal at -86 ppm and the increased intensity of Q3 Si(0Al) and Q3 Si(1Al) signals strongly suggested that the signal at ca. -86 ppm corresponded to Q2 Si at the layer edges of saponite.
DOI: 10.1016/j.clay.2009.11.024
发表时间: 2010-03-01
影响因子: 5.6
作者:
He, Hongping;Ma, Yuehong;Qing, Yanhong
通讯作者: Qing, Yanhong
DOI: --
发表时间: 1989-02
影响因子: 3.1
作者:
D. Woessner
通讯作者: D. Woessner
DOI: 10.1016/j.catcom.2005.05.005
发表时间: 2005-08
影响因子: 3.7
作者:
M. Casagrande;L. Storaro;M. Lenarda;S. Rossini
通讯作者: M. Casagrande;L. Storaro;M. Lenarda;S. Rossini
DOI: 10.1007/3-540-69711-x_3
发表时间: 1999
影响因子: --
作者:
E. Giannelis;R. Krishnamoorti;E. Manias
通讯作者: E. Giannelis;R. Krishnamoorti;E. Manias
DOI: 10.1016/j.jcis.2008.01.032
发表时间: 2008-05-15
影响因子: 9.9
作者:
Daniel, Lisa M.;Frost, Ray L.;Zhu, Huai Yong
通讯作者: Zhu, Huai Yong