在水热条件下形成具有高岭土结构的10a相,初始化学成分不同

IF 0.8 Q4 NANOSCIENCE & NANOTECHNOLOGY
N. Leonov, D. Kozlov, D. Kirilenko, N. Bert, A. Pelageikina, A. Nechitailov, M. Alikin, A. Krasilin
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引用次数: 0

摘要

摘要本文研究了通过改变初始组成参数来获得纳米结构高岭土的过程。在c6h14 - nh3·h2o体系中,通过(c3h7o) 3al和(c2h5o) 4si的共水解合成了初始组分。在水热条件下(220◦C, 2 MPa, 96 h)合成了成分为al2si2o5 (OH) 4的氢硅酸铝,得到了平均长度为100 ~ 200 nm,厚度为60 nm的片状颗粒。PXRD图谱显示了两相的存在。发现板状高岭石。我们还观察到形成了一个类似埃洛石的相。对合成样品的红外光谱和热分析表明,有机改性的氢硅酸盐在412℃左右发生相变,所得到的相有希望用于研究吸附和进一步剥离过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Formation of a 10 A phase with halloysite structure under hydrothermal conditions with varying initial chemical composition
A BSTRACT We studied the process of obtaining nanostructured halloysite by varying the parameters for creating the initial composition. The initial composition was synthesized by co-hydrolysis of (C 3 H 7 O) 3 Al and (C 2 H 5 O) 4 Si in the C 6 H 14 –NH 3 · H 2 O system. Aluminum hydrosilicate with the composition Al 2 Si 2 O 5 (OH) 4 was synthesized under hydrothermal conditions (220 ◦ C, 2 MPa, 96 h). Particles of plate-like morphology with average length 100 – 200 nm and 60 nm thickness were obtained. The PXRD patterns revealed the presence of two phases. Plate-like kaolinites are found. Also we observed the formation of a halloysite-like phase. Studies of synthesized samples by IR spectroscopy and thermal analysis revealed the presence of organic-modified hydrosilicate with phase transition around 412 ◦ C. The resulting phase is promising for studying the processes of adsorption and further exfoliation.
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来源期刊
Nanosystems: Physics, Chemistry, Mathematics
Nanosystems: Physics, Chemistry, Mathematics NANOSCIENCE & NANOTECHNOLOGY-
CiteScore
1.80
自引率
11.10%
发文量
64
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