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SIPSON——管网中管流与地表漫流相互作用的模拟。

SIPSON--simulation of interaction between pipe flow and surface overland flow in networks.

作者信息

Djordjević S, Prodanović D, Maksimović C, Ivetić M, Savić D

机构信息

School of Engineering, Computer Science and Mathematics, University of Exeter, North Park Road, Exeter EX4 4QF, United Kingdom.

出版信息

Water Sci Technol. 2005;52(5):275-83.

Abstract

The new simulation model, named SIPSON, based on the Preissmann finite difference method and the conjugate gradient method, is presented in the paper. This model simulates conditions when the hydraulic capacity of a sewer system is exceeded, pipe flow is pressurized, the water flows out from the piped system to the streets, and the inlets cannot capture all the runoff. In the mathematical model, buried structures and pipelines, together with surface channels, make a horizontally and vertically looped network involving a complex interaction of flows. In this paper, special internal boundary conditions related to equivalent inlets are discussed. Procedures are described for the simulation of manhole cover loss, basement flooding, the representation of street geometry, and the distribution of runoff hydrographs between surface and underground networks. All these procedures are built into the simulation model. Relevant issues are illustrated on a set of examples, focusing on specific parameters and comparison with field measurements of flooding of the Motilal ki Chal catchment (Indore, India). Satisfactory agreement of observed and simulated hydrographs and maximum surface flooding levels is obtained. It is concluded that the presented approach is an improvement compared to the standard "virtual reservoir" approach commonly applied in most of the models.

摘要

本文介绍了一种名为SIPSON的新模拟模型,该模型基于普雷斯曼有限差分法和共轭梯度法。该模型模拟了下水道系统水力容量超限时的情况,即管道水流处于压力状态,水从管道系统流出到街道,且进水口无法捕捉所有径流。在数学模型中,地下结构和管道与地表渠道一起构成了一个水平和垂直的环状网络,涉及水流的复杂相互作用。本文讨论了与等效进水口相关的特殊内部边界条件。描述了模拟井盖损失、地下室洪水、街道几何形状表示以及地表和地下网络之间径流水位图分布的程序。所有这些程序都已纳入模拟模型。通过一组示例说明了相关问题,重点关注特定参数以及与莫蒂拉尔基查尔集水区(印度印多尔)洪水现场测量结果的比较。观测和模拟的水位图以及最大地表洪水水位取得了令人满意的一致性。得出的结论是,与大多数模型中常用的标准“虚拟水库”方法相比,本文提出的方法有所改进。

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