首页> 外文期刊>Journal of the European Ceramic Society >Preparation of phosphoric acid-based geopolymer foams using limestone as pore forming agent - Thermal properties by in situ XRPD and Rietveld refinements
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Preparation of phosphoric acid-based geopolymer foams using limestone as pore forming agent - Thermal properties by in situ XRPD and Rietveld refinements

机译:使用石灰石作为成孔剂制备磷酸基地质聚合物泡沫-原位XRPD和Rietveld精制的热学性质

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In this work, geopolymer foams were obtained by reacting metakaolin with phosphoric acid and using natural calcite/dolomite as foaming agent. Total porosity and thermal conductivity were ca. 70% and 0.083 +/- 0.008 W/mK, respectively. Rietveld refinements, using both ex- and in situ XRPD data, were performed in order to elucidate the phase stability of the formed binder up to 1200 degrees C. The results showed that the amorphous matrix partially crystallized in tridymite and cristobalite type structures of AlPO4-SiO2 solid solutions at about 700 degrees C. At 1000 degrees C, 3:2 mullite started to crystallize, possibly from unreacted metakaolinite, resulting in co-crystallization of SiO2 cristobalite. At the same time, the amount of tridymite-type structure decreased, possibly due to selective phase transformation of AlPO4 tridymite to cristobalite, leaving behind the SiO2 isostructure. The geopolymer paste composition allows to tailor the mullite content in the refractory foam. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在这项工作中,通过使偏高岭土与磷酸反应并使用天然方解石/白云石作为发泡剂,获得了地聚合物泡沫。总孔隙率和热导率约为。分别为70%和0.083 +/- 0.008 W / mK。为了阐明在高达1200摄氏度时所形成的粘合剂的相稳定性,使用了异位和原位XRPD数据进行了Rietveld精炼。结果表明,非晶态基质在AlPO4-的鳞石英和方石英型结构中部分结晶SiO2固溶体在约700摄氏度下发生。在1000摄氏度下,3:2莫来石开始结晶,可能从未反应的偏高岭土开始结晶,导致SiO2方石英共结晶。同时,鳞茎型结构的数量减少了,这可能是由于AlPO4鳞茎型向方石英的选择性相变而留下的SiO2同构。地聚合物糊剂组合物允许定制耐火泡沫中的莫来石含量。 (C)2015 Elsevier Ltd.保留所有权利。

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