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基于现场非饱和入渗的渗流模型参数识别

Identification of parameters for infiltration ontology model based on field unsaturated infiltration

  • 摘要: 针对非饱和渗流本构模型参数识别困难的问题,以海南省屯昌县迈湾水利枢纽土质高边坡为研究对象,借助无线传输器和数据采集仪等监测装置,现场开展了坡面入渗试验,获取监测数据结合差分进化法对Van Genuchten模型参数(\alpha n\theta _\texts\theta _\textrK_\texts)进行了全局反演。通过PLAXIS软件建立了有限元模型进行数值模拟,分析了模拟值并与实测值进行对比,验证了反演参数的可靠性。结果表明:反演参数驱动数值模拟结果与实测数据具有高度一致性,各深度处误差均在较小范围内。研究结果可为热带地区土质边坡非饱和渗流研究提供参数依据,也可为该类土体的非饱和水力学参数识别提供借鉴。

     

    Abstract: This study takes the high slope of Maiwan Water ConserVancy Hub in Tunchang County, Hainan Province as the research object, focusing on the challenges of identifying parameters for the unsaturated seepage intrinsic models. Utilizing wireless transmitter, data acquisition instruments, and other monitoring devices, on-site slope infiltration experiments were conducted. The collected monitoring data were combined with the differential evolution method to perform a global inversion of the Van Genuchten model's parameters (\alpha , n, \theta _\texts, \theta _\textr, K_\texts). A finite element model was established using PLAXIS software for numerical simulation, analyzing the variation patterns of simulated values and comparing them with measured values to validate the reliability of the inverted parameters. The results demonstrate that the numerical simulations driven by the inverted parameters exhibit high consistency with the measured data, with errors at each depth remaining within 5%. Experimental verification confirms the accuracy of the numerical simulations, providing a parameter basis for unsaturated seepage studies in tropical slopes and a reference for determing unsaturated hydraulic parameters in similar soils.

     

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