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肖泽岸, 李康良, 段杰云, 王启航, 郭茂亮. 降温过程中氯化钠盐渍土相变的电化学特征[J]. 岩土工程学报. DOI: 10.11779/CJGE20231193
引用本文: 肖泽岸, 李康良, 段杰云, 王启航, 郭茂亮. 降温过程中氯化钠盐渍土相变的电化学特征[J]. 岩土工程学报. DOI: 10.11779/CJGE20231193
Electrochemical characteristics of phase transition process in sodium chloride saline soil during cooling[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20231193
Citation: Electrochemical characteristics of phase transition process in sodium chloride saline soil during cooling[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20231193

降温过程中氯化钠盐渍土相变的电化学特征

Electrochemical characteristics of phase transition process in sodium chloride saline soil during cooling

  • 摘要: 氯盐渍土是我国西北寒旱区一种典型的盐渍土类型,其电化学特征是深入理解盐渍土腐蚀病害机理的关键。为探究盐渍土孔隙溶液相变与其电化学特征之间的联系,本文以氯化钠盐渍粉质黏土为研究对象,测试了不同含盐量和温度条件下氯化钠盐渍土的电化学阻抗谱。研究表明:氯化钠盐渍土阻抗随着测试频率的增加而逐步降低,并在高频率时逐步达到稳定。氯化钠盐渍土的阻抗模的对数值在冻结前随温度的降低线性增加,而在冻结后,冰晶和盐结晶的生成导致土体阻抗模值发生显著增加。氯化钠盐渍土在冻结前表现为一段容抗弧,而在冻结后,由相变导致的土体水盐迁移使得土体在出现阻抗弧后又存在一段扩散阻抗。根据土体在冻结前后的导电路径,本文建立了土体在冻结前后的等效电路模型,并在此基础上分析了土体孔隙溶液相变与对应电路元件之间的联系。此研究对深入理解盐渍土电化学特征及孔隙溶液相变规律具有重要意义。

     

    Abstract: Chlorine saline soil is a typical type of saline soil in the cold and arid regions of northwest China, and its electrochemical characteristic is crucial for understanding of the corrosion mechanism of saline soil. To explore the relationship between the phase transition of pore solution in saline soil and its electrochemical characteristics, sodium chloride saline silty clay was taken as the research object, and its electrochemical impedance spectra were measured under different salt content and temperature conditions. The results revealed that the impedance of sodium chloride saline soil gradually decreases with the increase of frequency, and reaches stable state at high frequency condition. The logarithm of the impedance modulus of sodium chloride saline soil increases linearly with temperature decreasing before freezing, while the generation of ice crystals and salt crystals leads to a significant increase in the impedance modulus of the soil after freezing. Sodium chloride saline soil exhibits a capacitive impedance arc before freezing, while the migration of soil water and salt caused by phase transition results in a diffusion impedance of the soil after freezing. Based on the conductivity path of the soil before and after freezing, the equivalent circuit model of the soil before and after freezing were established, and the relationship between the phase transition of the soil pore solution and the corresponding circuit components were analyzed. It is of great significance for understanding the electrochemical characteristics of saline soil and the phase transition process of pore solution.

     

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