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基于电磁驱动的滑坡模型水分迁移理论及试验研究
引用本文:周昌,胡新丽,徐楚,王强,徐迎. 基于电磁驱动的滑坡模型水分迁移理论及试验研究[J]. 岩土力学, 2018, 39(9): 3347-3354. DOI: 10.16285/j.rsm.2017.1349
作者姓名:周昌  胡新丽  徐楚  王强  徐迎
作者单位:中国地质大学(武汉) 工程学院,湖北 武汉 430074
基金项目:国家自然科学基金项目(No.41630643,No.41272305);国家重点基础研究发展计划(973)项目(No.2011CB710604);中央高校基本科研业务费专项资金资助项目(No.CUGCJ1701,No.18010491A26)。
摘    要:加快模型试验中水的渗流速率对库岸滑坡研究意义重大。考虑滑坡渗流特性,基于电磁驱动原理,在滑坡模型中施加相互垂直的电场、磁场,推导出孔隙水受力公式,根据电渗固结理论,推导水分迁移速率v与电压Ve、磁场强度B的关系式,进而获得时间相似比,实现了通过电磁场强度来控制滑坡模型水分迁移速率,改进模型试验,为研究库水位升降对滑坡的影响提供条件。通过试验进行验证:电磁场对水分迁移速度的影响具有显著效果,且电压大小对模型的稳定渗流场影响较小。说明在不改变模型材料参数的条件下,改变磁场强度和电压可获得任意孔隙水的渗流速度,为研究库水位波动条件下的滑坡演化机制奠定基础。

关 键 词:库水位涨落  电渗  电磁驱动  模型试验  
收稿时间:2017-06-22

Theory and experimental study of electromagnetic-driven moisture migration of landslide model
ZHOU Chang,HU Xin-li,XU Chu,WANG Qiang,XU Ying. Theory and experimental study of electromagnetic-driven moisture migration of landslide model[J]. Rock and Soil Mechanics, 2018, 39(9): 3347-3354. DOI: 10.16285/j.rsm.2017.1349
Authors:ZHOU Chang  HU Xin-li  XU Chu  WANG Qiang  XU Ying
Affiliation:Engineering Faculty, China University of Geosciences, Wuhan, Hubei 430074, China
Abstract:How to accelerate the seepage rate of water in model test is significant to the study of bank landslide. Based on the principle of electromagnetism, the force of pore water was calculated by applying mutually perpendicular electric and magnetic fields in the landslide model. According to the theory of electroosmotic consolidation, the resultant force of groundwater is calculated, and the relationship between the migration rate and the voltage and magnetic field intensity is deduced, then the time similarity ratio is obtained. The water migration rate of landslide model is improved by controlling the voltage and magnetic field strength applied to the model, and the effect of the electromagnetic field on the soil moisture is verified by experiments. The influence of electromagnetic field significantly affects the water migration velocity, and the voltage has little effect on the stable seepage field of the model. Without changing the parameters of model material, the changes of the magnetic field strength and voltage can determine the seepage velocity of any pore water lays which can be the foundation for studying the evolution mechanism of the landslide under fluctuating reservoir water conditions.
Keywords:water level fluctuation  electro-osmosis  electromagnetic drive  model test  
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