Journal of Jilin University(Earth Science Edition) ›› 2025, Vol. 55 ›› Issue (3): 893-905.doi: 10.13278/j.cnki.jjuese.20230299

Previous Articles     Next Articles

 A Mathematical Model of Low-Velocity Non-Darcy Flow in Clayey Soil Considering Change of Viscosity in Boundary Layer Fluid

Wang Fugang1,2, Guan Xiaotong1,2, He Qingcheng3, Cheng Hui1,2, Yang Guohua1,2, Cheng Zhongle1,2, Wang Yaohui1,2#br#

#br#
  

  1. 1. Key Laboratory of Groundwater Resources and Environment (Jilin University), Ministry of Education, Changchun 130021, China
    2. Jilin Provincial Key Laboratory of Water Resources and Water Environment, Changchun 130021, China
    3. Chinese Academy of Geological Sciences, Beijing 100037, China
  • Online:2025-05-26 Published:2025-06-06
  • Supported by:
    Supported by the National Natural Science Foundation of China (42072280,U2244215,41172250) and the National Key Research and Development Program of China (2019YFC0409103)

Abstract:  The boundary layer fluid and its viscosity changeshave a significant impact on the flow of fluids in low permeability media. Existing low-velocity non-Darcy flow models usually ignore the change of fluid viscosity, or simply treat the fluid viscosity as a function of pore radius. The viscosity of boundary layer fluids is usually related to contact angle. In this paper, based on capillary model and fractal theory, a new low-velocity non-Darcy flow model is proposed considering the influence of contact angle on the viscosity of boundary layer fluid. The reliability of the model was verified through experiments and the sensitivity analysis of key parameters was conducted. The results show that the contact angle has a significant impact on the viscosity of the boundary layer fluid, which in turn affects the flow behavior of the fluid. After considering the change of fluid viscosity in the boundary layer, the flow velocity decreases. In this experiment, compared with ignoring the change of fluid viscosity, the decrease in flow velocity can reach 57.1%. The flow velocity decreases with the increase of fractal dimension of pore distribution (Df) and increases with the increase of contact angle. In this paper, under the same pressure gradient, when Df increases from 1.2 to 1.8, for every 0.2 increase, the flow velocity decreases by 18.4%, 23.3%, and 29.1%, respectively; When the contact angle increases from 0° to 80°, for every 20° increase, the flow velocity increases by 10.9%, 12.3%, 14.0%, and 16.3%, respectively. As the pressure gradient increases, the boundary layer fluid participates in the flow, and the effective seepage section and fluid effective viscosity increase. The increase of fluid viscosity has retarding effect on the flow, but the effect is smaller than the gain effect of the increase in flow section on the flow velocity. Therefore, in general, the flow velocity increases with the increase of the pressure gradient.


Key words:  , groundwater, clayey soil, low-velocity non-Darcy flow, boundary layer, fluid viscosity, fractal theory

CLC Number: 

  • TU43
[1] Zhu Jie, Cao Jun, Tang Wencheng, Xiao Jianxun. Mechanical Properties of Metakaolin-Based Geopolymer-Modified Soil Under Free-zing Conditions [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 951-962.
[2] Wang Beidong, Yang Shenglai, Zhao Shuai, Deng Hui, Zhang Yuxiang, Bai Haoyan, Li Qinyi, Jiang Yi. Characteristics of Reservoir Space and Pore-Throat Structure in Intra-Platform Reservoir of the Member 4 of  Dengying Formation in Gaomo Area [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 804-817.
[3] Ren Xianjun, Shi Yunqian.  Genesis and Significance of Calc-Alkaline Volcanic Rocks of Cretaceous Huoshiling Formation in Southern Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 818-834.
[4] Zhang Haihong, Qiao Jinran, Chen Guoqiang, Xue Xiaogang, Deng Xinhui, Miao Changsheng, Li Xue, Gao Chunsheng.  Genesis of Early Jurassic I-Type Granites in Southern Zhangguangcai Range: Constraints from Chronology, Geochemistry, and Zircon Hf Isotopes [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 896-914.
[5] Hu Jintao, Zhang Hu, Li Zheng, Zheng Bo, Lu Ming, Dong Yuxuan. Variation Law and Model of Pore Pressure in Warm Saturated Frozen Soil [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 963-974.
[6] Yu Ying , Chen Junjie , Lin Gengwei , Li Qingsong .  Preparation of Porous Structure CuFe2O4-P Material and Its Catalytic Peroxymonosulfate Degradation of Caffeine [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 1002-1012.
[7] Ding Mengyan, Feng Xuan, Liu Cai. Influence of Fractures on the Nonlinear Elastic Characteristics of Rocks [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 1051-1061.
[8] Wang Jian , Zhang Yuanyuan, Wu Nan, Xu Qinghai, Cui Ziyue, Liu Xianfeng, Fu Qingmeng. Reservoir Characteristics and Classification Evaluation of Interlayered Type Shale Oil in Chang 7 Member of Zhijing-Ansai Area, Ordos Basin [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 453-468.
[9] ​He Tianxin , , Liu Rong, , Liu Qianghao, , Ning Ting, . Formation Mechanism of Fibrous Calcite Veins in Lower Cretaceous Bayingebi Formation of Yin’e Basin: Evidence from Hot Water Deposition and Isotopes [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 497-510.
[10] Xu Jun , Gao Yang, Liu Jun, Wang Xiaotong, . Genesis of  Sankuanggou Fe-Cu Deposit in  Northern Great Hinggan Range: Constraints from Garnet U-Pb Geochronology and Element Geochemistry [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 540-556.
[11] Du Xinqiang, Yin Chengshan, Fang Yongjun, Li Zihan, Guo Hui.

Evaluation of Exploitable Groundwater Resources Based on Groundwater Ecological Water Depth Threshold:An Example of Puyang Irrigation District of Sanjiang Plain [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 635-646.

[12] Shu Longcang, Wei Shujing, Che Limuge, Wen Zhongqi, Liu Bo.

Quantification of Groundwater Response and Uncertainty Related to Ecological Water Conveyance in Xiliaohe Plain [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 647-660.

[13] Zhang Yangyang, Du Wei.

Adaptive Finite Element Method for Audio-Frequency Magnetotelluric Forward Modeling Based on Super Convergent Patch Recovery [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 673-683.

[14] Yang Ting, Li Yaxin, Liu Na, Lin Xiaojun, Zeng Jingwen , Wang Xiujuan , Cai Qianyi, Luo Zifeng, Zhang Yuanling, Rong Jingnan, Yu Weida, Qiu Jinrong, Zhou Jianli. Zeolite as PRB Filling Medium for  Remediation of NH4+ Polluted Groundwater and Its In-Situ Regeneration Performance [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(2): 661-672.
[15] Qin Chuanyu, You Kaihong, Li Xiaoqi, Zhang Chengwu, Yu Lijuan. Effects of Common Groundwater Anions on Nitrobenzene Degradation by Dual-Modified Nano Zero-Valent Iron and Underlying Mechanisms [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(1): 342-351.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] You Minxin,Liu Jianmin. Application Status and Progress of Isotopic Geochemistry in Research of Emeishan Large Igneous Province (ELIP)[J]. Journal of Jilin University(Earth Science Edition), 2014, 44(4): 1231 -1243 .
[2] YANG Chun-mei, LI Hong-qi,LU Da-wei,ZHANG Fang-li,GAO Yuan,SHAO Ying-chao. The Relationship Between Rock Resistivity and Water Saturation in WaterDriveOil and OilDriveWater Process[J]. J4, 2005, 35(05): 667 -671 .
[3] ZHU Hong-chen,ZHANG Jiong-fei,QUAN Heng. Two Stages of Mesozoic Lithogenesis and Mineralization in Daxing’anling Mountains[J]. J4, 2005, 35(04): 436 -0442 .
[4] ZHU Jian-wei, ZHAO Gang, LIU Bo, GUO Wei, CHENG Jun. Identification Technology and It’s Application of Well-Logging About Oil Shale[J]. J4, 2012, 42(2): 289 -295 .
[5] CHEN Li, LIANG Hai-an,ZHANG Wen-juan,RONG Fan. Application of Fuzzy Mathematics in Division of Engineering Geo-Environment of Cities-An Example of Fushun City[J]. J4, 2008, 38(5): 837 -0840 .
[6] GAO Gui-mei,SU Ke,WANG Wen-ying,GAN Shu-cai,LIU Zhao-jun. Study on Rare Earth and Trace Elements in Oil Shale Samples, Huadian, Jilin Province[J]. J4, 2006, 36(6): 974 -0979 .
[7] WU Kong-yun,JIANG Zhong-cheng,YE Ye. Influence of Different Plant Communities On Erosion Rates of Limestone Rock Blocks[J]. J4, 2007, 37(5): 967 -0971 .
[8] ZHOU Yan-zhang, CHI Bao-ming, LIU Zhong-pei. Mode of Structural Control about Groundwater Pour-in Mechanism in Xiadian Gold Deposits in Shandong Province[J]. J4, 2008, 38(2): 255 -0260 .
[9] ZHANG Yuan, LIU Lian-deng,SUN Jing-gui,CHEN Guo-hua,ZHANG Hong-xi,YAN Fu-chuan, YANG Kai-chun. Two Phase Overprinting Mineralization in Huangbuling Gold Deposit in Northwestern Jiaodong Peninsula[J]. J4, 2008, 38(1): 21 -0026 .
[10] LU Cheng-peng, SHU Long-cang, YUAN Li-bo, ZHANG Rong-rong, HUANG Bi-juan, WANG Bin-bin. Determination of Hydrogeologic Parameters of Karst Aquifer Based on Tracer Test[J]. J4, 2009, 39(4): 717 -721 .