FOR 581: Coupling of Flow and Deformation Processes for Modelling the Movement of Natural Slopes

大型斜坡的运动发展到破坏是水文、地下-水力和土壤-力学过程在大的空间和时间尺度上复杂相互作用的结果。由于目前还没有可靠的模拟方法，因此提出了新的解决方案，将改进的过程模型与耦合、平均和升级方法结合起来，同时结合确定性和随机性方法，考虑到过程的复杂性以及不同尺度上的可用数据。

The development of the movement of large hillslopes until failure is the result of complex interactions of hydrological, subsurface-hydraulic and soil-mechanical processes ranging over large space and time scales. As no reliable simulation methods exist today for such purposes, new solutions are suggested which bring together improved process models with coupling, averaging and upscaling methods while combining deterministical and stochastical approaches to take the complexity of the processes as well as the available data on the different scales into account.