Structure and thermal stability of organo-vermiculite
Structure and thermal stability of organo-vermiculite
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有机蛭石的结构和热稳定性
DOI:
10.1016/j.clay.2016.06.011
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发表时间:
2016-11
影响因子:
5.6
通讯作者:
Runliang Zhu
中科院分区:
文献类型:
--
作者:
Xiaoli Su;Lingya Ma;Jingming Wei;Runliang Zhu
In this study, organo-vermiculites (HEVrm) were prepared by modifying expanded vermiculite (EVrm) with different amounts of surfactant (hexadecyltrimethyl ammonium bromide, HDTMAB). The obtained HEVrm were characterized by using X-ray diffraction (XRD), Fourier transform infrared spectroscopy (FTIR), and thermogravimetric analysis (TG). Instead of a gradual increase of the basal spacing for organo-montmorillonite (OMt) as reported in literatures, a one-stepped increase of the basal spacing was observed for HEVrm. As such, the intercalation of surfactant into the interlayer space of EVrm is not homogeneous. In particular, only part of the interlayer spaces of EVrm were intercalated by surfactants at low HDTMAB concentration; with the increase of surfactant concentration, more and more interlayer spaces were intercalated, reaching a “saturation” state at last. The intercalated surfactant adopted a paraffin-monolayer arrangement withall-transconformation within the interlayer space. The decomposition temperature of the intercalated surfactant in HEVrm is very similar to that of neat surfactant. The protection of the clay mineral layers for the thermal stability of the intercalated surfactant is not obvious, which is very different from that for OMt. This may be due to the one-stepped increase of the basal spacing in HEVrm with relatively large interlayer height. These findings are of high importance for preparation and application of HEVrm.
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影响因子:
5.6
作者:
He, Hongping;Ma, Yuehong;Qing, Yanhong
通讯作者:
Qing, Yanhong
影响因子:
1.5
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影响因子:
5.6
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通讯作者:
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影响因子:
3.3
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通讯作者:
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9.9
作者:
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通讯作者:
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