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首页> 外文期刊>Acta Crystallographica, Section B. Structural Science >In-situ X-ray diffraction activation study on an Fe/TiO_2 pre-catalyst
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In-situ X-ray diffraction activation study on an Fe/TiO_2 pre-catalyst

机译:Fe / TiO_2预催化剂的原位X射线衍射活化研究

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This study focuses on the use of in situ powder X-ray diffraction (PXRD) and quantitative phase analysis using the Rietveld method to monitor the structural properties of a titania-supported iron (10% Fe/TiO_2) pre-catalyst during calcination (oxidation) and activation (reduction) in the temperature range 25-900℃. The TiO_2 oxidation study revealed an increase in anatase particle size before the anatase to rutile phase transformation, lending credibility to the bridging mechanism proposed by Kim et al. [(2007), Mater. Sci. Forum, 534-536, 65-68]. Pre-catalyst oxidation experiments allowed for the determination of a suitable calcination temperature (450℃) of the pre-catalyst in terms of maximum hematite concentration and appropriate particle size. These experiments also confirmed that the anatase to rutile phase transformation occurred at higher temperatures after Fe addition and that anatase was the sole donor of Ti~(4+) ions, which are known to migrate into hematite (Gennari et al., 1998), during the formation of pseudobrookite (Fe_2TiO_5) at temperatures above 690℃. Using the results from the oxidation experiments, two pre-catalyst samples were calcined at different temperatures; one to represent the preferred case and one to represent a case where the pre-catalyst had been excessively heated. Samples of the excessively heated catalysts were exposed to different reducing gas atmospheres (5, 10 and 100% H_2/N_2) and heated in the in situ PXRD reactor, so that diffraction data could be collected during the activation process. The results show that reduction with gases containing low concentrations of H_2 (5 and 10%) led to the formation of ilmenite (FeTiO_3) and we were able to show that both anatase and rutile are consumed in the reaction. Higher concentrations of H_2 led to the formation of magnetite (Fe_3O_4) and metallic iron (Fe~0). We also noted a decrease in the anatase to rutile transformation temperature under reducing atmospheres when compared with the pre-catalyst heat-treatment experiment. A reduced calcination temperature prior to reduction allowed more facile Fe reduction.
机译:这项研究的重点是使用原位粉末X射线衍射(PXRD)和使用Rietveld方法进行定量相分析,以监测二氧化钛负载的铁(10%Fe / TiO_2)预催化剂在煅烧(氧化)过程中的结构性能。 )并在25-900℃的温度范围内激活(还原)。 TiO_2氧化研究揭示了锐钛矿向金红石相转变之前锐钛矿粒径的增加,这为Kim等人提出的架桥机制提供了可信度。 [(2007),Mater。科学论坛,534-536,65-68]。催化剂前氧化实验可以根据最大赤铁矿浓度和合适的粒径确定催化剂的合适煅烧温度(450℃)。这些实验还证实,添加铁后,在较高的温度下发生了锐钛矿相向金红石相的转变,并且锐钛矿是Ti〜(4+)离子的唯一供体,已知该离子会迁移到赤铁矿中(Gennari et al。,1998),在温度高于690℃时形成假板钛矿(Fe_2TiO_5)。利用氧化实验的结果,在不同的温度下煅烧了两种预催化剂样品。一种代表优选的情况,另一种代表预催化剂被过度加热的情况。将过度加热的催化剂样品暴露于不同的还原性气体气氛(5%,10%和100%H_2 / N_2)中,并在原位PXRD反应器中加热,以便可以在活化过程中收集衍射数据。结果表明,用低浓度H_2(5%和10%)的气体进行还原会导致钛铁矿(FeTiO_3)的形成,并且我们能够证明锐钛矿和金红石在反应中均被消耗。较高浓度的H_2导致形成磁铁矿(Fe_3O_4)和金属铁(Fe〜0)。我们还注意到,与还原前的热处理实验相比,在还原气氛下锐钛矿到金红石转化温度的降低。还原前降低煅烧温度可使铁还原更加容易。

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