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Numerical analysis of hydrological response in loess excavation and filling area under multi-year precipitation infiltration

机译:多年降水入渗下黄土开挖充填区水文响应数值分析

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In order to study the evolution of the hydrological environment in loess excavation and filling project under multi-yearprecipitation infiltration, the hydrological responses of the excavation and filling area in Yan’an New District are simulated,based on the actual precipitation data of several years and field monitoring results. In addition, the drainage rate of the blindditch is defined to characterize the drainage state of the blind ditch. Considering the variation of the drainage state andmulti-year precipitation infiltration, different simulated cases are established. The results show that the proposed model isverified by the field monitoring results, which could reliably reflect the evolution of the pore water pressure (PWP) and thegroundwater table (GWT). The transient saturated zone is formed near the excavation and filling interface due to the multiyearprecipitation infiltration. And the formation and development of the transient saturated zone are closely related to thehydrological response of the loess excavation and filling area. The spatial and temporal variations of PWP and GWT aremainly affected by the changes in precipitation infiltration and drainage capacity of the blind ditch. Moreover, the hydrologicalresponse has a certain hysteresis to precipitation and is controlled by the topography and stratum difference of theundisturbed foundation. The research results should be helpful for the stability evaluation of loess excavation and fillingproject and the design of drainage facilities.
机译:为研究多年降水渗透下黄土开填工程水文环境的演变,基于几年的实际降水数据和野外监测结果,模拟了延安新区开挖填土区水文响应。此外,还定义了盲沟的排水速率,以表征盲沟的排水状态。考虑排水状态和多年降水入渗的变化,建立了不同的模拟案例。结果表明,所提模型经过现场监测结果验证,能够可靠地反映孔隙水压力(PWP)和地下水位(GWT)的演变。由于多年降水的渗透,在开挖和充填界面附近形成了瞬态饱和带。瞬态饱和带的形成发育与黄土开挖充填区的水文响应密切相关。PWP和GWT的时空变化主要受盲沟降水入渗和排水能力变化的影响。此外,水文响应对降水有一定的滞后性,并受未受干扰地基的地形和地层差异的控制。研究结果有助于黄土开填工程稳定性评价和排水设施设计。

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