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黄河大堤非饱和土土-水特性试验研究 被引量:39

Test and study on soil water curve of unsaturated soil of Yellow River dyke
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摘要 模拟工程中非饱和土体的实际受力状态,利用改进的非饱和土三轴仪对黄河大堤非饱和土在不同围压条件下的土-水特性进行了试验研究。根据试验结果,分析了黄河大堤非饱和土体在外荷作用下土-水特征曲线及其变化规律。并对相应的土-水特征曲线模型进行了拟合,得出其拟合函数。根据土-水特征曲线可知,非饱和土的基质吸力随着土体所受周围压力的增大而减小,随着含水量的增大而减小;对于某一类土而言,在高含水量(含水量>20 %) 时,土的基质吸力随含水量的变化较小,而在低含水量 (含水量≤20 %)时,土的基质吸力随含水量的变化较大。随着含水量的增加,非饱和土的工程性质向弱性变化。 With the improved triaxial equipment for unsaturated soil, we tested and studied soil water characteristics of Yellow River dyke's unsaturated soil under different confining pressures simulating the real condition exposed on unsaturated soil in engineering. And according to fest results, the curves of soil-water characteristics of unsaturated soil are obtained and the water-soil characteristics and their rules under additional load are discussed. At the same time, the function of fitted curves is gained. Based on the water-soil curves, the results are known that the matric suctions reduce with increasing the surrounding pressure and water content. To the same type soil, the matric suction changes small with change of water content when the water content is higher than 20%, but it changes greatly when the water content is less than 20%. The engineering characteristics become weak with increasing water contents.
出处 《岩土力学》 EI CAS CSCD 北大核心 2005年第3期347-350,共4页 Rock and Soil Mechanics
基金 中国科学院武汉岩土力学研究所岩土力学重点实验室开放课题资助项目(No. 110205)。
关键词 黄河大堤 非饱和土 不同围压 土-水特征曲线 试验研究 拟合 Curve fitting Pressure Rivers Soils
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参考文献11

  • 1吴宏伟,陈守义,庞宇威.雨水入渗对非饱和土坡稳定性影响的参数研究[J].岩土力学,1999,20(1):1-14. 被引量:373
  • 2孟黔灵,姚海林,邱伦锋.吸力对非饱和土抗剪强度的贡献[J].岩土力学,2001,22(4):423-426. 被引量:27
  • 3黄义,张引科.非饱和土土-水特征曲线和结构强度理论[J].岩土力学,2002,23(3):268-271. 被引量:12
  • 4DG弗雷德隆德 H拉哈尔佐.非饱和土土力学[M].北京:中国建筑工业出版社,1993.78-98.
  • 5Aassouline S, Tessier D, Bruand A. Conceptual model of the soil water retention curve[J]. Water Resources Research, 1998, 34(2): 223-231.
  • 6Panjit Kumar Ghost. Estimation of soil moisture characteristics from mechanical properties of soils[J]. Soil Science, 1979, 130(2): 312-330.
  • 7Arya I M, Richter J C, Davidson S A. A comparison of soil moisture characteristics predicted by the Arya-Paris model with laboratory-measured data[J]. National Aeronautics and Space Administration, 1982, (3): 136-138.
  • 8徐永福,董平.非饱和土的水分特征曲线的分形模型[J].岩土力学,2002,23(4):400-405. 被引量:78
  • 9King L G. Description of soil characteristics from partially saturated flows[J]. Soil Science Society of America, 1965, 29(5): 332-338.
  • 10Hutson J L, Cass A. A retentivity function for use in soil water simulation models[J]. Journal of Soil Science, 1987, 38(5): 157-166.

二级参考文献45

  • 1雅·贝尔 许涓铭译.地下水水力学[M].北京:地质出版社,1985..
  • 2DG弗雷德隆德 H拉哈尔佐.非饱和土土力学[M].北京:中国建筑工业出版社,1997.392-405.
  • 3[1]Xu Y F, Sun D A. Determination on of expansive sofl trength using a fractal model[J ]. Fractals, 2001, 9(1): 51-60.
  • 4[2]Fredlund D G, Xing A, Fredlund M D. The relationship of the unsaturated soil shear strength function to the soil water characteristics[J ]. Can. Geotech. J., 1996,33(3): 440-448.
  • 5[3]Fredlund D G, Rahardjo H. Soil Mechanics for Unsaturated Soils[M]. New York: Wiley & his sors, 1993.
  • 6[4]Brooks R H, Corey A T. Properties of porous media affecting fluid flow[J]. ASCE, Irrig. Drain. Div., 1966, 92: 61-68.
  • 7[5]van Genuchten M Th. A close-form equation for predicting the hydraulic conductivity of unsaturated soils[J]. Soil Sci. Soc. Am. J., 1980, 44:892-898.
  • 8[6]Tyler S W, Wheatcraft S W. Fractal process in soil water retention[J]. Water Resources Res., 1990, 26(5):1 047- 1054.
  • 9[7]Kovacs G. Seepage Hydraulics[M]. Amsterdam: Elsevier Science Publishers, 1981.
  • 10[8]Barbour S L. Nineteenth Canadian Geotechnical Colloquium: The soil-water characteristic curve: a historical perspective[J ]. Can. Geotech. J., 1998, 35:873-894.

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