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| Theoretical model of water movement and wetting-induced deformation for remolded loess under one-dimensional loading-wetting condition and its experimental verification |
| HU Haijun1,WANG Chen1,LV Tongyang1,LI Bopeng1,2 |
(1. College of Water Resources and Architectural Engineering,Northwest A&F University,Yangling,Shaanxi 712100,China;
2. China Construction Third Bureau Green Industry Investment Co.,Ltd.,Wuhan,Hubei 430100,China) |
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Abstract The water movement and the collapse deformation development in loess under one-dimensional loading-wetting condition influence each other. A model for predicting water movement and wetting-induced deformation considering their interactions was proposed and the corresponding method of determining the model parameters was given. In order to verify the reliability of the model,one-dimensional load-wetting tests on remolded Lanzhou loess soil were carried out by using a self-made one-dimensional soil column infiltration instrument,and the model parameters were obtained through the indoor element tests. The model was applied to predict the water movement process and the collapse deformation development in the loading-wetting tests. The predicted and measured values were compared,and the model parameters were analyzed and inversed. The results show that the established model can reasonably predict the decrease of the rate of wetting front advancing with the applied vertical pressure and the relation between the collapse deformation and the depth of wetting front. Considering fully saturated zone at the end of soil column,flow in macropores and the assumption in the model,the saturated permeability coefficient of the equivalent saturated body and the effective suction head at wetting front were inversed. The laws of the two inversed parameters changing with the vertical pressure are the same as those determined by indoor element tests with close values respectively,which indicates that the model is reasonable. The inversed parameters provide reference for the application of the model.
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[1] LI P,QIAN H,WU J H. Environment:accelerate research on land creation[J]. Nature,2014,510(7503):29–31.
[2] 张爱军,邢义川,汪海涛,等. 基于增湿变形的渠道工程黄土渠基湿陷性评价方法[J]. 水利学报,2017,48(1):41–51,60.(ZHANG Aijun,XING Yichuan,WANG Haiyang,et al. Evaluation method for collapsibility of channel engineering with Loess foundation based on moistening deformation[J]. Journal of Hydraulic Engineering,2017,48(1):41–51,60.(in Chinese))
[3] 中华人民共和国国家标准编写组. GB 50025—2018湿陷性黄土地区建筑标准[S]. 北京:中国建筑工业出版社,2018.(The National Standards Compilation Groups of the People's Republic of China. GB 50025—2018 Standard for building construction in collapsible loess regions[S]. Beijing:China Building Industry Press,2018.(in Chinese))
[4] 谢定义. 黄土力学特性与应用研究的过去、现在与未来[J]. 地下空间,1999,19(4):273–284.(XIE Dingyi. The past,present and future of the research on mechanical characteristics and application of loess[J]. Underground Space,1999,19(4):273–284.(in Chinese))
[5] 崔月娥. 关于黄土湿陷敏感性问题探讨[J]. 煤炭工程,2010,(8):76–78.(CUI Yuee. Discussion on the issue of sensitivity of loess collapse[J]. Coal Engineering,2010,(8):76–78.(in Chinese))
[6] 张苏民,郑建国. 湿陷性黄土(Q3)的增湿变形特征[J]. 岩土工程学报,1990,12(4):21–31.(ZHANG Sumin,ZHENG Jianguo. The deformation characteristics of collapsible loess during moistening process[J]. Chinese Journal of Geotechnical Engineering,1990,12(4):21–31.(in Chinese))
[7] JIANG M J,HU H J,LIU F. A summary of collapsible behaviour of artificially structured loess in oedometer and triaxial wetting tests[J]. Canadian Geotechnical Journal,2012,49(10):1 147–1 157.
[8] 李喜安,洪 勃,李林翠,等. 黄土湿陷对渗透系数影响的试验研究[J]. 中国公路学报,2017,30(6):198–208.(LI Xian,HONG Bo,LI Lincui,et al. Experimental research on permeability coefficient under influence of loess collapsibility[j]. Chinese Journal of Highway,2017,30(6):198–208.(in Chinese))
[9] 沈珠江. 二元介质模型在黄土增湿变形分析中的应用[J]. 水利学报,2005,36(2):129–134.(SHEN Zhujiang. Application of binary medium model in deformation analysis of loess during wetting[J]. Journal of Hydraulic Engineering,2005,36(2):129–134.(in Chinese))
[10] COSTA L M,PONTES I D S,GUIMARÃES L J N,et al. Numerical modelling of hydro-mechanical behaviour of collapsible soils[J]. Communications in Numerical Methods in Engineering,2008,24(12):1 839–1 852.
[11] WU L Z,LIU G G,WANG L C,et al. Numerical analysis of 1D coupled infiltration and deformation in layered unsaturated porous medium[J]. Environmental Earth Sciences,2016,75(9):761.
[12] 付艳斌,王铁行,赵树德,等. 黄土地基水分入渗分析及增湿变形计算[J]. 西安建筑科技大学学报:自然科学版,2005,37(2):210‐214.(FU Yanbin,WANG Tiehang,ZHAO Shude,et al. Calculation method for seepage flow and water–increased deformation in loess foundation with certain infiltration capacity[J]. Journal of Xi?an University of Architecture and Technology:Natural Science,2005,37(2):210‐214.(in Chinese))
[13] 李博鹏,胡海军,严武庆,等. 兰州压实黄土水分迁移规律试验与数值模拟[J]. 人民黄河,2020,42(12):139–144.(LI Bopeng,HU Haijun,YAN Wuqing,et al. Experiment and numerical simulation analysis of water migration of Lanzhou compacted loess[J]. Yellow River,2020,42(12):139–144.(in Chinese))
[14] 刘保健,谢定义,郭增玉. 黄土地基增湿变形的实用算法[J]. 岩土力学,2004,25(2):270–274.(LIU Baojian,XIE Dingyi,GUO Zengyu. A practical method for moistening deformation of loess foundation[J]. Rock and Soil Mechanics,2004,25(2):270–274.(in Chinese))
[15] 雷志栋,杨诗秀,谢森传. 土壤水动力学[M]. 北京:清华大学出版社,1988:77–130.(LEI Zhidong,YANG Shixiu,XIE Senchuan. Soil hydrodynamics[M]. Beijing:Tsinghua University Press,1998:77–130.(in Chinese))
[16] MEIN R G,LARSON C L. Modeling the infiltration component of the rainfall-runoff process[R]. Minneapolis,Minnesota:Water Resources Research Center,University of Minnesota,1971.
[17] CHU X F,MIGUEL A M. Determination of ponding condition and infiltration into layered soils under unsteady rainfall[J]. Journal of Hydrology,2005,313(3):195–207.
[18] CHEN L,YONG M H. Green-ampt infiltration model for sloping surfaces[J]. Water Resources Research,2006,42(7):1–9.
[19] 张 林,张登飞,陈存礼,等. 竖向压力作用下重塑黄土土柱压缩湿陷及渗水试验研究[J]. 水利学报,2019,50(10):1 214–1 221. (ZHANG Lin,ZHANG Dengfei,CHEN Cunli,et al. Experimental study on compression collapsibility and infiltration of remolded loess soil column under vertical pressure[J]. Journal of Hydraulic Engineering,2019,50(10):1 214–1 221.(in Chinese))
[20] 胡海军,李博鹏,田堪良,等. 积水和降雨下非饱和重塑黄土水分入渗模拟[J]. 同济大学学报:自然科学版,2019,47(11):1 565–1 573. (HU Haijun,LI Bopeng,TIAN Kanliang,et al. Simulation of water movement in unsaturated remolded loess under ponding infiltration and rainfall infiltration[J]. Journal of Tongji University:Nature Sience,2019,47(11):1 565–1 573.(in Chinese))
[21] 王文焰,汪志荣,王全九,等. 黄土中Green-Ampt入渗模型的改进与验证[J]. 水利学报,2003,35(1):30–35.(WANG Wenyan,WANG Zhirong,WANG Jiuquan,et al. Improvement and evaluation of the Green-Ampt model in loess soil[J]. Journal of Hydraulic Engineering,2003,35(1):30–35.(in Chinese))
[22] 安 鹏,张爱军,刘宏泰,等. 重塑饱和黄土长期渗流劣化机制及其渗透性分析[J]. 岩土力学,2013,34(7):1 965–1 971.(AN Peng,ZHANG Aijun,LIU Hongtai,et al. Degradation mechanism of long-term seepage and permeability analysis of remolded saturated loess[J]. Rock and Soil Mechanics,2013,34(7):1 965–1 971.(in Chinese))
[23] SAMARASINGHE A M,HUANG Y H. Permeability and consolidation of normally consolidated soils[J]. Journal of the Geotechnical Engineering,1982,108(6):835–850.
[24] 谢康和,齐 添,胡安峰,等. 基于GDS的黏土非线性渗透特性试验研究[J]. 岩土力学,2008,29(2):420–424.(XIE Kanghe,QI Tian,HU Anfeng,et al. Experimental study on nonlinear permeability characteristics of Xiaoshan clay[J]. Rock and Soil Mechanics,2008,29(2):420–424.(in Chinese))
[25] MEIN R G,FARRELL D A. Determination of wetting front suction in the Green-Ampt equation[J]. Soil Science Society of America Proceedings,1974,38(4):872–876.
[26] 胡 冉,陈益峰,周创兵. 基于孔隙分布的变形土土水特征线模型[J]. 岩土工程学报,2013,35(8):1 451–1 462.(HU Ran,CHEN Yifeng,ZHOU Chuangbing. A water retention curve model for deformable soils based on pore size distribution[J]. Chinese Journal of Geotechnical Engineering,2013,35(8):1 451–1 462.(in Chinese))
[27] 姚志华,黄雪峰,陈正汉,等. 兰州地区大厚度自重湿陷性黄土场地浸水试验综合观测研究[J]. 岩土工程学报,2012,34(1):65–74.(YAO Zhihua,HUANG Xuefeng,CHEN Zhenghan,et al. Comprehensive soaking tests on self-weight collapse loess with heavy section in Lanzhou region[J]. Chinese Journal of Geotechnical Engineering,2012,34(1):65–74.(in Chinese))
[28] SIMUNEK J,JARVIS N J,VAN GENUCHTEN M T,et al. Review and comparison of models for describing non-equilibrium and preferential flow and transport in the vadose zone[J]. Journal of Hydrology,2003,272(1/4):14–35.
[29] BODMAN G B,COLMAN E A. Moisture and energy conditions during downward entry of water into soils[J]. Soil Science Society of America Proceedings,1944,8(1):116–122. |
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