长江科学院院报 ›› 2019, Vol. 36 ›› Issue (2): 91-96.DOI: 10.11988/ckyyb.20170693

• 岩土工程 • 上一篇    下一篇

南阳膨胀土冻融循环后的土水特征试验研究

王也1,王建磊2,鲁洋1,梁妍3   

  1. 1. 河海大学 水利水电学院,南京 210098;
    2. 中国电建集团 中南勘测设计研究院有限公司,长沙 410014;
    3. 江苏省镇江市京口区农业委员会,江苏 镇江 212000
  • 收稿日期:2017-06-15 修回日期:2017-08-13 出版日期:2019-02-01 发布日期:2019-03-11
  • 通讯作者: 鲁 洋(1991-),男,江苏南京人,博士研究生,主要从事水工岩土工程方面的研究。E-mail:luy@hhu.edu.cn
  • 作者简介:王 也(1994-),女,江苏宿迁人,硕士研究生,主要从事土石坝工程和特殊土方面的研究。E-mail:wangye_hhu@163.com
  • 基金资助:
    江苏省普通高校研究生科研创新计划项目(KYLX_0472)

Experimental Research on Soil-Water Characteristics of Nanyang Expansive Soil Subjected to Freeze-Thaw Cycles

WANG Ye1, WANG Jian-lei2, LU Yang1,LIANG Yan3   

  1. 1. College of Water Conservancy and Hydropower, Hohai University, Nanjing 210098, China;
    2.Power China Zhongnan Engineering Corporation Limited, Changsha 410014, China;
    3.Jingkou Agricultural Committee of Zhenjiang City, Zhenjiang 212000, China
  • Received:2017-06-15 Revised:2017-08-13 Published:2019-02-01 Online:2019-03-11

摘要: 南水北调中线工程的膨胀土渠道容易遭受季节性冻融的影响。为探究冻融作用对膨胀土土水特征的影响规律,以南阳膨胀土为试验对象,采用滤纸法测定经历不同冻融次数的膨胀土土样的总吸力和基质吸力,绘制其试验散点图,并分别采用VG模型和幂函数模型对基质吸力及总吸力与土体含水率的关系进行拟合。结果表明:随着冻融循环次数的增加,基质吸力和总吸力土水曲线整体向左下方偏移,进气值逐渐减小,持水性能降低;渗透吸力在含水率增大时逐渐减小,但不同冻融次数的渗透吸力数值并无显著差别;采用VG模型和幂函数模型分别拟合本试验中的基质吸力土水曲线和总吸力土水曲线,相关系数高,形式简单,模型参数在冻融循环中逐渐趋于稳定值。研究成果可供处在季节性冻土区的膨胀土工程建设及维护提供参考。

关键词: 膨胀土, 冻融循环, 土水特征, 滤纸法, 总吸力, 基质吸力, 曲线拟合

Abstract: The expansive soil canal in the Middle Route of South-to-North Water Transfer Project is easily subjected to the effect of freeze-thaw cycles. In order to investigate the influence of freeze-thaw cycles on soil-water characteristics of expansive soil, we measured the total suction and matric suction of Nanyang expansive soil subjected to different freeze-thaw cycles using the filter paper method, and fitted the relationship between matric suction, total suction and water content with Van Genuchten model and power function model, respectively. Results show that as the freeze-thaw cycle proceeds, the soil and water characteristic curves (SWCCs) of the matric suction and total suction shifted to the lower left side, with the air entry value and water holding capacity both declining. The osmotic suction decreased gradually with the increase of water content, but the osmotic suction at different freeze-thaw cycles did not vary significantly. Finally, the fitting models used in the paper are of high correlation coefficients and simple forms, and the parameters of the models tend to be stable as the number of freeze-thaw cycles increases.

Key words: expansive soil, freeze-thaw cycles, soil-water characteristics, filter paper method, total suction, matric suction, curve fitting

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