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水力驱动作用下的地貌演变数值模拟--Ⅰ.模型建立 被引量:3

Numerical Simulation of Hydrologically-driven Landscape Evolution(Ⅰ):Model Developing
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摘要 介绍了一个复杂的严格基于物理概念的水文/侵蚀数值模型InHM (Integrated Hydrology Model)的模型结构和控制方程.InHM通过求解水流在地表和空隙介质中的偏微分流动方程,而不是应用经验/半经验公式或回归关系,来模拟水文响应.模拟的水文响应结果被用来驱动一个泥沙搬运算法.InHM考虑的水文响应过程包括蒸发蒸腾、入渗、地表产流、地下水运动(饱和/非饱和)、地表水运动等.InHM考虑的地表侵蚀过程包括由于雨滴溅击和地表水流引起的泥沙颗粒侵蚀、搬运和沉积. The model structure and governing equations of a rigorous complex physics-based hydrologic-response/erosion model, Integrated Hydrology Model (InHM), are introduced. Instead of deploying empirical/semi-empirical equations and regression relationships, InHM simulates hydrologic-response based upon solution to the partial-differential equations governing water flow within porous media and on the surface. The simulated hydrologic-response was then employed to drive a sediment transport algorithm. Hydrologic-response processes considered by InHM include evaporatranspiration, infiltration, surface runoff generation, groundwater flow ( saturated/unsaturated), and surface water flow. Erosion processes considered by InHM include detachment ,transport, and deposition caused by both rainsplash and hydraulic erosion.
出处 《应用基础与工程科学学报》 EI CSCD 2008年第3期305-317,共13页 Journal of Basic Science and Engineering
基金 水沙科学与水利水电工程国家重点实验室开放基金资助(编号:2006-B-01) 国家重点基础研究计划(973)资助项目(编号:2007CB714100)
关键词 水文 侵蚀 地貌演变 数值模拟 InHM hydrology erosion landscape evolution numerical simulation InHM
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  • 1Jamieson R A, Beaumont C. Orogeny and metamorphism: A model for deformation and pressure-temperature-time paths with application to the central and southern Appalachians[ J]. Tectonics, 1988,7:417-445 被引量:1
  • 2Beaumont C, Fullsack P, Hamilton J. Erosional control of active compressional orogens [ A ]//McClay K R. Thrust Tectonics [ C ]. Chapman and Hall, London, 1992,1-18 被引量:1
  • 3Chase C G. Fluvial landsculpfing and the fractal dimension of topography[ J]. Geomorphology, 1992,5:39-57 被引量:1
  • 4Willett S, Beaumont C, Fullsack P. Mechanical models for the tectonics of doubly vergent compressional orogens [ J ]. Geology, 1993,21 : 371-374 被引量:1
  • 5Rosenbloom N A, Anderson R S. Hillslope and channel evolution in a marine terraced landscape, Santa Cruz, California [ J ]. J. Geophys. Res. , 1994,99 : 14013-14029 被引量:1
  • 6Tucker G E, Slingerland R L. Erosional dynamics, flexural isostasy, and long-lived escarpments: A numerical modeling study [ J ]. J. Geophys. Res. , 1994,99 : 12229-12243 被引量:1
  • 7Kooi H, Beaumont C. Escarpment evolution on high-elevation rifled margins: Insights derived from a surface processes model that combines diffusion, advection and reaction[ J]. J. Geophys. Res. , 1994,99 : 12191-12209 被引量:1
  • 8Kooi H, Beaumont C. Large-scale geomorphology:classical concepts reconciled and integrated with contemporary ideas via a surface processes model[ J]. J. Geophy. Res. , 1996,101:3361-3386 被引量:1
  • 9Braun J, Sambridge M. Modelling landscape evolution on geological time scales.a new method based on irregular spatial discretization [ J ]. Basin Res. , 1997,9:27-52 被引量:1
  • 10Roering J J, Kirchner J W, Dietrich W E. Evidence for nonlinear, diffusive sediment transport on hillslopes and implications for landscape morphology[ J]. Water Resour. Res. , 1999,35:853-870 被引量:1

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