Experimental study of the water depth and rainfall intensity effects on the bed roughness coefficient used in distributed urban drainage models

被引:30
作者
Fraga, Ignacio [1 ]
Cea, Luis [1 ]
Puertas, Jeronimo [1 ]
机构
[1] Univ A Coruna, ETS Caminos, GEAMA Environm & Water Engn Grp, La Coruna 15071, Spain
关键词
Flow resistance; Model calibration; Urban hydrology; Rainfall-runoff; Shallow water model; Overland flow; OVERLAND-FLOW; SURFACE-ROUGHNESS; PRECIPITATION DATA; WASH-OFF; EQUATIONS; POROSITY; AREAS; CATCHMENTS;
D O I
10.1016/j.jhydrol.2013.10.005
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The work presented in this paper analyses the effect of water depth and rainfall intensity on the surface roughness coefficients used in overland flow models based on the shallow water equations. The relation between the Manning coefficient and the water depth and rainfall intensity has been quantified using different methodologies based on the analysis of two sets of experimental data. In the first set uniform overland flow conditions were generated, and the bed roughness coefficient was computed from direct measurements of the water depth and discharge. In the second set of experiments, unsteady rainfall-runoff transformations with different rainfall intensities were generated in a flume and computed with a shallow water model in which different bed friction formulations were implemented and calibrated. Results show that for very low water depth values there is a significant increase in the surface resistance, which is not captured by any standard bed friction formulation. Rainfall intensity also increases surface resistance especially as the water depth diminishes below a critical threshold. Using a Reynolds dependent formulation for the Manning coefficient improves model predictions. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:266 / 275
页数:10
相关论文
共 39 条
[1]  
[Anonymous], 1972, NAT ENG HDB
[2]  
[Anonymous], 1959, OPEN CHANNEL FLOW
[3]  
Beven K.J., 2001, Rainfall-runoff Modelling, The Primer, P360
[4]   Influence of surface roughness in hydrological response of semiarid catchments [J].
Candela, A ;
Noto, LV ;
Aronica, G .
JOURNAL OF HYDROLOGY, 2005, 313 (3-4) :119-131
[5]   Overland flow computations in urban and industrial catchments from direct precipitation data using a two-dimensional shallow water model [J].
Cea, L. ;
Garrido, M. ;
Puertas, J. ;
Jacome, A. ;
Del Rio, H. ;
Suarez, J. .
WATER SCIENCE AND TECHNOLOGY, 2010, 62 (09) :1998-2008
[6]   Unstructured finite volume discretization of two-dimensional depth-averaged shallow water equations with porosity [J].
Cea, L. ;
Vazquez-Cendon, M. E. .
INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS, 2010, 63 (08) :903-930
[7]   Experimental validation of two-dimensional depth-averaged models for forecasting rainfall-runoff from precipitation data in urban areas [J].
Cea, L. ;
Garrido, M. ;
Puertas, J. .
JOURNAL OF HYDROLOGY, 2010, 382 (1-4) :88-102
[8]   Depth averaged modelling of turbulent shallow water flow with wet-dry fronts [J].
Cea, Luis ;
Puertas, Jeronimo ;
Vazquez-Cendon, Maria-Elena .
ARCHIVES OF COMPUTATIONAL METHODS IN ENGINEERING, 2007, 14 (03) :303-341
[9]  
Chen A.S., 2007, NOVATECH 2007 LYON, V11, P465
[10]   Modelling of water and sediment transport over grassed areas [J].
Deletic, A .
JOURNAL OF HYDROLOGY, 2001, 248 (1-4) :168-182