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首页> 外文期刊>Advanced Science Letters >Comparison of Original and Sintered LUSI Mud from East Java, Indonesia as Raw Material for Making a Geopolymer
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Comparison of Original and Sintered LUSI Mud from East Java, Indonesia as Raw Material for Making a Geopolymer

机译:来自印度尼西亚东爪哇省的原始LUSI泥和烧结LUSI泥作为生产地质聚合物的原料的比较

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This paper presents the characterization of LUSI mud from East Java, Indonesia, as a potential raw material for making a geopolymer. Two types of LUSI mud were analyzed, i.e., original LUSI mud and LUSI mud that had been sintered at 800℃ for 2 h. Tests were conducted using X-ray fluorescence (XRF), particle size analyzer (PSA), X-ray diffraction (XRD), scanning electron microscope (SEM), and Fourier transform infrared (FTIR) equipment to evaluate these raw materials. The particle size of the original mud and the sintered mud was in the range of 209-240μm and 316-363μm, respectively. The major constituent of both materials was SiO_2, but the SiO_2 content was higher in the sintered mud than in the original mud. The SiO_2 peak for sintered mud was higher than the peak for original mud at 2 thetha, where 2 thetha = 26.8°, due to the higher intensity of quartz. SEM analysis showed that both the original mud and the sintered mud had a plate-like structure similar to kaolin. The FTIR adsorption band showed slight different between the original mud and the sintered mud.
机译:本文介绍了印度尼西亚东爪哇省LUSI泥浆的表征,该泥浆是制备地质聚合物的潜在原料。分析了两种LUSI泥,即原始LUSI泥和在800℃下烧结2 h的LUSI泥。使用X射线荧光(XRF),粒度分析仪(PSA),X射线衍射(XRD),扫描电子显微镜(SEM)和傅立叶变换红外(FTIR)设备进行了测试,以评估这些原料。原始泥浆和烧结泥浆的粒度分别在209-240μm和316-363μm的范围内。两种材料的主要成分均为SiO_2,但烧结后的泥浆中的SiO_2含量高于原始泥浆。由于石英强度较高,烧结泥的SiO_2峰高于原始泥在2 thetha的峰,其中2 thetha = 26.8°。 SEM分析表明,原始泥和烧结泥都具有类似于高岭土的板状结构。 FTIR吸附带显示出原始泥浆和烧结泥浆之间的细微差异。

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