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Researches on Fractal Features of Graphite Porous Materials

机译:石墨多孔材料分形特征研究

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The mercury porosimetry experiment has tested three different kinds of porosity graphite and the microscopic structure of impregnation antimony materials, and has calculated the corresponding fractal dimension by using the Manger model. The results show that: the main pore diameter of the graphite materials is in the interval of 1 ~ 3μm, most of which can be filled by impregnation antimony, and graphite and impregnation antimony materials both have the fractal characteristics. Graphite materials also have the dual fractal characteristics. Its fractal inflection point aperture is about 1μm, and the fractal dimension (3.05 ~ 3.25) of the small pores (Φ≤1μm) is less than the one (3.71 ~ 3.95) of the large pores (Φ>1μm). The reason why existing the dual fractal characteristics is that the size of the pore formation mechanism is different. Impregnation occurs mainly in the range of large pores, characteristics of which is an important factor to influence the quality of impregnation materials. The material formula is the main factor to influence the large pores and an important guarantee to improve the quality of impregnation products.
机译:汞孔隙测定法实验已经测试了三种不同种类的孔隙率石墨和浸渍锑材料的微观结构,并通过使用造纸模型计算了相应的分形维数。结果表明:石墨材料的主孔径在1〜3μm的间隔,大部分可以通过浸渍锑填充,并且石墨和浸渍锑材料都具有分形特征。石墨材料也具有双重分形特性。其分形拐点孔径约为1μm,小孔(φ≤1μm)的分形尺寸(3.05〜3.25)小于大孔(φ>1μm)的一(3.71〜3.95)。现有双分形特性的原因是孔隙形成机制的尺寸不同。浸渍主要发生在大孔的范围内,其特征是影响浸渍材料质量的重要因素。材料配方是影响大孔隙的主要因素,以及提高浸渍产品质量的重要保证。

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