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首页> 外文期刊>Advances in civil engineering >Damage Characteristics of Sandstone Subjected to Coupled Effect of Freezing-Thawing Cycles and Acid Environment
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Damage Characteristics of Sandstone Subjected to Coupled Effect of Freezing-Thawing Cycles and Acid Environment

机译:冻融循环与酸性环境耦合作用下的砂岩破坏特征

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In order to figure out the damage characteristics and mechanisms of sandstone under coupled effect of acid erosion and recurrent freezing-thawing cycles, sulfuric acid is chosen as acid solution, and sandstone, representative stone in Sichuan province, is chosen as a sample to conduct the freezing-thawing cycling test. In the meantime, chemical component of the solution is also tested and recorded in the progress of freezing-thawing cycling. Then, the nuclear magnetic resonance (NMR) test and magnetic resonance images (MRI) test on samples are conducted with the help of the AniMR-150 NMR imaging system. After a series of tests, the sample’s appearance, dry mass, porosity, T2 spectrum, solution’s pH, solution’s metallic ion concentration, and magnetic resonance images are obtained and analyzed. The results show that dry mass loss and porosity grow with F-T cycles increase and pH value decrease. Montmorillonite, illite, and clay in sandstone react with sulfuric acid solution; as a consequence, K+, Mg2+, Fe3+, and Al3+ separate out, and the solution’s pH and concentration of K+, Mg2+, Fe3+, and Al3+ increase with F-T cycles. Acid erosion and F-T cycling lead to the generation of new micropores and expansion of micropores at the beginning; when the acid solution is exhausted, new micropores generate under the effect of freezing-thawing cycling, and micropores in samples keep developing and expanding with the increase of freezing-thawing cycles. Coupled effect of acid corrosion and recurrent freezing-thawing cycling causes much more serious deterioration to sandstone samples than acid corrosion.
机译:为了弄清砂岩在酸蚀和反复冻融循环作用下的破坏特征和机理,以硫酸为酸溶液,以四川省代表性的砂岩为样本进行酸蚀试验。冻融循环试验。同时,还在冻融循环过程中测试并记录了溶液的化学成分。然后,借助AniMR-150 NMR成像系统对样品进行核磁共振(NMR)测试和磁共振图像(MRI)测试。经过一系列测试,获得并分析了样品的外观,干重,孔隙率,T2光谱,溶液的pH值,溶液的金属离子浓度和磁共振图像。结果表明,干物质损失和孔隙率随F-T循环的增加和pH值的降低而增加。蒙脱石,伊利石和砂岩中的粘土与硫酸溶液反应。结果,K +,Mg2 +,Fe3 +和Al3 +分离出来,溶液的pH值和K +,Mg2 +,Fe3 +和Al3 +的浓度随F-T循环的增加而增加。酸蚀和F-T循环会在开始时导致新的微孔的产生和微孔的扩展。当酸溶液耗尽时,在冻融循环的作用下会产生新的微孔,并且随着冻融循环的增加,样品中的微孔会不断发展和扩展。酸腐蚀和反复冻融循环的共同作用比酸腐蚀对砂岩样品的破坏更为严重。

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