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Optimization of the Dehydration Temperature of Goethite to Control Pore Morphology

机译:针铁矿脱水温度的优化控制孔隙形态

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This study optimizes the dehydration temperature of goethite to control pore morphology. The pore morphology was characterized by using transmission electron microscopy and the nitrogen adsorption method. When the goethite was dehydrated at 200–250°C, slit-like pores with a width lesser than 2 nm were formed along the [010] direction. These slit-like pores changed to spherical micropores (300–500°C), and eventually disappeared (600–800°C). Compared to the synthetic goethite, natural goethite has a lower crystallinity and smaller primary particle size of under 100 nm. The natural goethite before dehydration contained 4 nm pores as cracks that remained even after heating to 800°C. In the case of natural goethite, the optimum dehydration temperature for higher surface area and pore volume was 350°C, which was higher than that of 250°C for the synthetic goethite.
机译:这项研究优化了针铁矿的脱水温度,以控制孔的形态。用透射电子显微镜和氮吸附法表征了孔的形貌。当针铁矿在200–250°C脱水时,沿[010]方向形成宽度小于2 nm的狭缝状孔。这些狭缝状的孔变成球形微孔(300–500°C),并最终消失(600–800°C)。与合成针铁矿相比,天然针铁矿具有较低的结晶度和较小的100 nm以下的初级粒径。脱水前的天然针铁矿含有4 nm的细孔,即使加热到800°C也仍然保留。对于天然针铁矿,较高表面积和孔体积的最佳脱水温度为350°C,高于合成针铁矿的250°C。

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