›› 2013, Vol. 34 ›› Issue (2): 347-352.

• 基础理论与实验研究 • 上一篇    下一篇

利用溢出量数据确定非饱和土-水力学参数

陈 辉1,韦昌富2,胡国辉3   

  1. 1.江西科技学院 土木工程学院,南昌 330098;2.中国科学院武汉岩土力学研究所 岩土力学与工程国家重点实验室,武汉 430071; 3.江西工商职业技术学院,南昌 330200
  • 收稿日期:2011-05-26 出版日期:2013-02-11 发布日期:2013-03-01
  • 通讯作者: 韦昌富,男,1966年生,博士,研究员,主要从事多相孔隙介质理论及其应用研究。E-mail:cfwei@whram.ac.cn E-mail:chenhuifang3589@163.com
  • 作者简介:陈辉,男,1980年生,博士,讲师,主要从事多孔介质理论及其应用研究
  • 基金资助:

    国家自然基金项目(No. 10872211);国家自然基金项目(No. 11072255);江西科技学院自然科学基金项目(No. XYKY11102);江西省科技计划项目(No. 20123BBG70180)

Determining hydraulic parameters of unsaturated soils by transient multi-step outflow experiment

CHEN Hui1, WEI Chang-fu2, HU Guo-hui3   

  1. 1. School of Civil Engineering, Jiangxi University of Technology, Nanchang 330098, China; 2. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 430071, China; 3. Jiangxi Technology Business Polytechnic College, Nanchang 330200, China
  • Received:2011-05-26 Online:2013-02-11 Published:2013-03-01

摘要: 在Wei & Muraleetharan基于非饱和土两相流交界面上的动态相容条件提出的多孔介质热动力学混合物理论模型基础上,推导出能描述溢出量与时间关系的溢出量演化方程。根据溢出量演化方程,结合一定变化规律的基质吸力序列,建立了给定基质吸力序列作用下利用多步流动试验瞬态溢出量数据确定非饱和土-水力学参数的方法。通过对低液限粉土、低液限黏土的多步流动试验研究发现,利用瞬态溢出量数据的拟合来确定非饱和土-水力学参数的方法而得到的各基质吸力作用下试样饱和度和渗透系数预估值,与联合测试系统测得的各基质吸力作用下试样的饱和度及渗透系数接近。

关键词: 多步流动试验, 溢出量数据, 水力学参数

Abstract: Based on the thermodynamic mixture theory model which can consider the mechanical interaction occurring on the interface between two components in unsaturated soils is proposed by Wei and Muraleetharan, an evolution equation of outflow in an unsaturated sample is developed. The equation describes well the variation of outflow with time in a multi-step outflow experiment. According to the evolution equation, the method that can predict hydraulic parameters of unsaturated soils, including the soil-water characteristic curve and the hydraulic function, by transient multi-step outflow experiment under a given series of matric suction, is built. Through the multi-step outflow experiment, it is seen that, for the low liquid limit silt and clay, the predicted values of saturation and hydraulic conductivity under the given matric sunction which are calculated from outflow data of the multi-step outflow experiment, are very close to the measured values of that measured by the combined laboratory system.

Key words: multi-step outflow experiment, outflow data, hydraulic parameters

中图分类号: 

  • TU 43
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[2] 魏进兵,邓建辉,谭国焕,李焯芬. 泄滩滑坡碎块石土饱和与非饱和水力学参数的现场试验研究[J]. , 2007, 28(2): 327-330.
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