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The swelling transition of lepidocrocite-type protonated layered titanates into anatase under hydrothermal treatment

机译:水热处理下纤铁矿型质子化层状钛酸盐的溶胀转变为锐钛矿

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摘要

The common facets of anatase crystals are the (001) and (101) planes. However, the phase transformation from lepidocrocite-type titanate into anatase by hydrothermal processing yields an anatase microstructure with high concentration of exposed (010) planes. The phase transformation of a lepidocrocite-type protonated layered titanate (HTO) into anatase was studied using XRD, TEM, FTIR, and measurement of pH and zeta potential. It was found that HTO is proton-deficient. The phase transformation process begins after uptake of a sufficient number of protons into the lepidocrocite-type structure. With the uptake of protons new hydroxyl groups form on the internal surfaces of the layered titanate and result in a bilayer state of HTO. The phase transformation reaction is a topotactic dehydration reaction in which anatase forms and water is expelled by syneresis.
机译:锐钛矿晶体的常见面是(001)和(101)平面。但是,通过水热处理从纤铁矿型钛酸酯到锐钛矿的相变产生具有高浓度的暴露(010)平面的锐钛矿微观结构。使用XRD,TEM,FTIR以及pH和Zeta电位的测量方法研究了纤铁矿型质子化层状钛酸酯(HTO)向锐钛矿的相变。发现HTO是质子缺陷的。相变过程在将足够数量的质子摄入到纤铁矿型结构中之后开始。随着质子的吸收,新的羟基在层状钛酸酯的内表面上形成并导致HTO的双层状态。相变反应是全电位脱水反应,其中锐钛矿形成,并且通过脱水作用排出水。

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