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Change of pore structure and uniaxial compressive strength of sandstone under electrochemical coupling

机译:电化学耦合作用下砂岩孔隙结构变化及单轴抗压强度

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摘要

The effect of electrochemical modification of the physical and mechanical properties of sandstone from Paleozoic coal measure strata was investigated by means of liquid nitrogen physical adsorption, X-ray diffraction and uniaxial compressive strength (UCS) tests using purified water, 1 mol/L NaCl, 1 mol/L CaCl2 and 1 mol/L AlCl3 aqueous solution as electrolytes. Electrochemical corrosion of electrodes and wire leads occurred mainly in the anodic zone. After electrochemical modification, pore morphology showed little change in distribution, decrease in total pore specific surface area and volume, and increased average pore diameter. The total pore specific surface area in the anodic zone was greater than in the cathodic zone, but total pore volume was less. Mineralogical composition was unchanged by the modification. Changes in UCS were caused by a number of factors, including corrosion, weakening by aqueous solutions, and electrochemical cementation, and electrochemical cementation stronger than corrosion and weakening by aqueous solutions.
机译:通过液氮物理吸附,X射线衍射和使用纯净水,1 mol / L NaCl的单轴抗压强度(UCS)测试,研究了电化学改性对古生代煤成因地层中砂岩物理力学性能的影响。 1 mol / L的CaCl2和1 mol / L的AlCl3水溶液作为电解质。电极和导线的电化学腐蚀主要发生在阳极区域。电化学修饰后,孔的形态几乎没有变化,总的孔比表面积和体积减少,平均孔径增加。阳极区的总孔比表面积大于阴极区,但总孔容较小。修改后矿物学组成没有变化。 UCS的变化是由许多因素引起的,包括腐蚀,水溶液的弱化和电化学粘结,以及电化学腐蚀比水溶液的腐蚀和弱化更强。

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