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Effect of salts on earthen materials deterioration after humidity cycling 被引量:4
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作者 SHEN Yun-xia CHEN Wen-wu +1 位作者 KUANG Jing DU Wei-fe 《Journal of Central South University》 SCIE EI CAS CSCD 2017年第4期796-806,共11页
Salt weathering leads to destruction of many valuable cultural heritage monuments and porous building material. The present study aims at providing more laboratory evidence for evaluating the effects of salt precipita... Salt weathering leads to destruction of many valuable cultural heritage monuments and porous building material. The present study aims at providing more laboratory evidence for evaluating the effects of salt precipitation on the deterioration process. In view of this, the remoulded soil specimens were mixed with three kinds of salts(i.e., NaCl, Na_2SO_4 and their mixture) with different salt concentrations, and the specimens were kept in environment cabinet for undergoing different wet-dry cycles. After each cycle, the ultrasound velocity measurements were employed to monitor the deterioration process. For the specimens that have suffered three wet-dry cycles, the mechanical properties(i.e. shear strength and compression strength) were determined to evaluate the degree of deterioration. Furthermore, considering the realistic conservation environment of earthen sites, mechanical stability of these specimens against sediment-carrying wind erosion was conducted in a wind tunnel. These experiments results indicate that the overall average velocities of the specimens after the third cycle are significantly lower than those subjected to only one cycle. Ultrasound velocity, mechanical strength and wind erosion rate decrease when salt content increases. However, the internal friction angle increases firstly, and then decreases with the increase in salt content added to the specimens. Na_2SO_4 contributes most of the surface deterioration, while NaCl plays little role in the deterioration. The damage potential of the salt mixture is less obvious and largely dependent on the crystallisation location. 展开更多
关键词 earthen archaeological SITES wet-dry cycles DETERIORATION SALT content SALT crystallization
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多次干湿循环后原状和重塑黄土的持水性试验研究 被引量:1
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作者 张小辉 王勇华 +3 位作者 张登飞 杨丽娜 卜崇鹏 王明皎 《Journal of Central South University》 SCIE EI CAS CSCD 2023年第9期3145-3161,共17页
干湿循环的风化作用是引发中国黄土地区基础设施破坏的重要影响因素。黄土的持水性能是此类黄土工程问题物理成因的关键物性。为了探究在干湿循环的环境驱动作用下不同地区原状和重塑黄土的持水性能及其变化规律,利用压力板仪和电镜扫描... 干湿循环的风化作用是引发中国黄土地区基础设施破坏的重要影响因素。黄土的持水性能是此类黄土工程问题物理成因的关键物性。为了探究在干湿循环的环境驱动作用下不同地区原状和重塑黄土的持水性能及其变化规律,利用压力板仪和电镜扫描仪(SEM)开展了持水曲线(SWRC)和微观结构的系列室内试验。研究结果表明,干湿循环的风化作用对原状和重塑黄土的持水性能有显著影响,且第一次循环的影响程度最为明显;原状黄土的SWRC呈双峰型,重塑黄土的SWRC呈单峰型;利用概念模型很好地解释了持水性的特征、变化规律及其与微观结构之间的联系。提出了一个考虑干湿循环次数、土的结构、区域差异影响的新持水模型,可以统一描述具有双峰特性的原状黄土和具有单峰特性的重塑黄土的持水特性,模型参数能够很好表达SWRC的变化特征,所提出模型在预测黄土和其他土的持水性能方面,具有较高的实用性和有效性。 展开更多
关键词 黄土 持水性 风化作用 干湿循环 土结构
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