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李建东, 王旭, 张延杰, 蒋代军, 刘德仁, 胡渊. 球形蒸汽源增湿非饱和黄土水热运移规律试验研究[J]. 岩土工程学报, 2022, 44(4): 687-695. DOI: 10.11779/CJGE202204011
引用本文: 李建东, 王旭, 张延杰, 蒋代军, 刘德仁, 胡渊. 球形蒸汽源增湿非饱和黄土水热运移规律试验研究[J]. 岩土工程学报, 2022, 44(4): 687-695. DOI: 10.11779/CJGE202204011
LI Jian-dong, WANG Xu, ZHANG Yan-jie, JIANG Dai-jun, LIU De-ren, HU Yuan. Experimental study on thermal moisture migration of unsaturated loess humidified by spherical steam source[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(4): 687-695. DOI: 10.11779/CJGE202204011
Citation: LI Jian-dong, WANG Xu, ZHANG Yan-jie, JIANG Dai-jun, LIU De-ren, HU Yuan. Experimental study on thermal moisture migration of unsaturated loess humidified by spherical steam source[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(4): 687-695. DOI: 10.11779/CJGE202204011

球形蒸汽源增湿非饱和黄土水热运移规律试验研究

Experimental study on thermal moisture migration of unsaturated loess humidified by spherical steam source

  • 摘要: 非饱和土中的水-汽-热耦合运移是一个受多因素影响的复杂过程。利用重塑非饱和黄土填筑模型,通入一定压力的高温水蒸气,研究蒸汽压梯度、温度梯度和含水率梯度共同作用下重塑非饱和黄土中的热湿迁移规律,并利用模型试验边界条件,解得球形蒸汽源增湿非饱和黄土时水热运移主控方程的一组特解。结果表明:球形蒸汽源在非饱和黄土中运移时,水分和温度的迁移范围近似于椭球体。水蒸气沿径向运移时,随着蒸汽压逐渐消散,运移速率降低,温度传导速率减小。蒸汽压较大时,增湿速率、增湿范围和增湿程度都将增大;在有效增湿范围内,土体含水率在11%~17%间变化,接近土体的最优含水率,增湿效果较好;高温水蒸气在土体中的传热包括高温蒸汽传热和温度梯度引起的热传导,有效增湿范围内主要以高温蒸汽传热为主,温度迁移速率属于快速迁移阶段。有效增湿范围外以温度梯度引起的热传导为主,属于缓慢迁移阶段;实测值和计算值对比发现,代数显式解析特解能较好地反映试验中土体温度和含水率的变化规律。研究结果可为非饱和黄土中水热迁移和蒸汽增湿技术提供理论参考。

     

    Abstract: The water-vapor-thermal coupling transport in unsaturated soils is a complex process affected by multiple factors. The experiment is designed to use the remolding unsaturated loess filling model, and the high-temperature steam with a certain pressure is ventilated in order to study the law of thermal mass migration in remolded unsaturated loess under the action of vapor pressure gradient, temperature gradient and water content gradient. Based on the boundary conditions of the model tests, a set of special solutions to the governing equation for heat-wet transport in unsaturated loess under humidification of spherical steam source are obtained. The results show that when the spherical steam sources diffuse in unsaturated loess, the migration range of water and temperature is similar to an ellipsoid. When the water vapor moves along the radial direction, the vapor pressure gradually dissipates, the migration rate decreases, and the temperature conduction rate decreases. When the vapor pressure is large, the humidification rate, range and degree will increase. In the effective humidification range, the moisture content of soils varies between 11% and 17%, which is close to the optimal moisture content of the soils, and the humidification effect is better. The heat transfer of high-temperature steam in the soils includes the heat transfer caused by the high-temperature steam and temperature gradient. The effective humidification range is mainly decided by the high-temperature steam heat transfer, and the temperature migration rate belongs to the rapid migration stage. The temperature migration outside the effective humidification range is mainly decided by the heat transfer caused by the temperature gradient, which belongs to the slow migration stage. The comparison between the measured and calculated values shows that the algebraic explicit analytical special solution can better reflect the variation law of soil temperature and moisture content in the experiment. The research results can provide a theoretical reference for the new technology of water-heat coupled migration and vapor humidification in unsaturated loess.

     

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