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首页> 外文期刊>Hydrology and Earth System Sciences Discussions >Demonstrating the “unit hydrograph” and flow routing processes involving active student participation – a university lecture experiment
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Demonstrating the “unit hydrograph” and flow routing processes involving active student participation – a university lecture experiment

机译:演示涉及学生积极参与的“单元水位图”和流程路由过程–大学讲座实验

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The unit hydrograph?(UH) has been one of the most widely employed hydrological modelling techniques to predict rainfall–runoff behaviour of hydrological catchments, and is still used to this day. Its concept is based on the idea that a unit of effective precipitation per time unit (e.g.?mm?h sup?1/sup ) will always lead to a specific catchment response in runoff. Given its relevance, the UH is an important topic that is addressed in most (engineering) hydrology courses at all academic levels. While the principles of the UH seem to be simple and easy to understand, teaching experiences in the past suggest strong difficulties in students' perception of the UH theory and application. In order to facilitate a deeper understanding of the theory and application of the UH for students, we developed a simple and cheap lecture theatre experiment which involved active student participation. The seating of the students in the lecture theatre represented the “hydrological catchment” in its size and form. A set of plastic balls, prepared with a piece of magnetic strip to be tacked to any white/black board, each represented a unit amount of effective precipitation. The balls are evenly distributed over the lecture theatre and routed by some given rules down the catchment to the “catchment outlet”, where the resulting hydrograph is monitored and illustrated at the black/white board. The experiment allowed an illustration of the underlying principles of the UH, including stationarity, linearity, and superposition of the generated runoff and subsequent routing. In addition, some variations of the experimental setup extended the UH concept to demonstrate the impact of elevation, different runoff regimes, and non-uniform precipitation events on the resulting hydrograph. In summary, our own experience in the classroom, a first set of student exams, as well as student feedback and formal evaluation suggest that the integration of such an experiment deepened the learning experience by active participation. The experiment also initialized a more experienced based discussion of the theory and assumptions behind the UH. Finally, the experiment was a welcome break within a 3?h lecture setting, and great fun to prepare and run.
机译:单位水位图(UH)是预测水文集水区降雨-径流行为的最广泛采用的水文建模技术之一,至今仍在使用。其概念基于这样的思想,即每时间单位有效降水量的单位(例如?mm?h ?1 )将始终导致径流中特定的集水区响应。鉴于其相关性,UH是所有学术水平的大多数(工程)水文学课程都涉及的重要主题。虽然UH的原理似乎很简单易懂,但过去的教学经验表明,学生对UH理论和应用的认识存在很大的困难。为了使学生对UH的理论和应用有更深入的了解,我们开发了一个简单且廉价的演讲厅实验,该实验涉及学生的积极参与。学生在演讲厅的座位就其规模和形式而言代表了“水文集水区”。一组用一块磁条粘贴到任何白板上的塑料球,每个塑料球代表有效量的单位沉淀量。这些球均匀地分布在演讲厅上,并按照一些给定的规则沿集水区向下流到“集水口”,在这里监控水文图并在黑白板上显示。实验允许对UH的基本原理进行说明,包括平稳性,线性以及所生成径流和后续路径的叠加。此外,实验设置的一些变化扩展了UH概念,以证明海拔,不同的径流形式和不均匀的降水事件对所得水文图的影响。总之,我们在课堂上的经验,第一组学生考试以及学生的反馈和正式评估表明,这种实验的整合通过积极参与而加深了学习经验。实验还启动了对UH背后的理论和假设的更加有经验的讨论。最后,该实验是在3小时的授课环境中令人欣喜的休息,准备和运行起来非常有趣。

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