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Characterization of multi-scale porous structure of fly ash/phosphate geopolymer hollow sphere structures: From submillimeter to nano-scale

机译:粉煤灰/磷酸盐地质聚合物空心球结构的多尺度多孔结构的表征:从亚毫米到纳米尺度

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In the present work, the porous structure of fly ash/phosphate geopolymer hollow sphere structures (FPGHSS), prepared by pre-bonding and curing technology, has been characterized by multi-resolution methods from sub-millimeter to nano-scale. Micro-CT and confocal microscopy could provide the macroscopic distribution of porous structure on sub-millimeter scale, and hollow fly ashes with sphere shape and several sub-millimeter open cells with irregular shape were identified. SEM is more suitable to illustrate the distribution of micro-sized open and closed cells, and it was found that the open cells of FPGHSS were mainly formed in the interstitial porosity between fly ashes. Mercury porosimeter measurement showed that the micro-sized open cell of FPGHSS demonstrated a normal/bimodal distribution, and the peaks of pore size distribution were mainly around 100 and 10 mu m. TEM observation revealed that the phosphate geopolymer was mainly composed of the porous area with nano-pores and dense areas, which were amorphous Al-O-P phase and alpha-Al2O3 respectively. The pore size of nano-pores demonstrated a quasi-normal distribution from about 10 to 100 nm. Therefore, detailed information of the porous structure of FPGHSS could be revealed using multiple methods. (C) 2014 Elsevier Ltd. All rights reserved.
机译:在目前的工作中,通过预结合和固化技术制备的粉煤灰/磷酸盐地质聚合物空心球结构(FPGHSS)的多孔结构已通过从亚毫米到纳米尺度的多分辨率方法进行了表征。显微CT和共聚焦显微镜可以提供亚毫米级的多孔结构的宏观分布,并鉴定出球形的空心飞灰和几个不规则形状的亚毫米开孔。扫描电镜更适合于说明微小的开孔和闭孔的分布,并且发现FPGHSS的开孔主要形成在粉煤灰之间的间隙中。汞孔隙率仪测量结果表明,FPGHSS的微细开孔呈正态/双峰分布,孔径分布的峰值主要在100和10μm附近。 TEM观察表明,磷酸盐地质聚合物主要由具有纳米孔的多孔区域和致密区域组成,分别为非晶态的Al-O-P相和α-Al2O3。纳米孔的孔径显示出约10至100nm的准正态分布。因此,可以使用多种方法揭示FPGHSS多孔结构的详细信息。 (C)2014 Elsevier Ltd.保留所有权利。

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