A combined methodology for the hydraulic rehabilitation of urban drainage networks

During medium and high intensity storm events, urban drainage networks can rapidly reach their maximum capacity, and subsequently floods can occur. Owing to the non-linearity of the processes involved, it is evident that the return period of a rainfall is different from the return period of the generated overflows. Therefore, the assessment of the maximum overflow volume related to a given return period is a key element in the management of urban drainage networks, since it may cause problems to infrastructure and economic losses. In this paper, a combined methodology for the hydraulic rehabilitation of such networks is proposed, by expressing their hydraulic critical conditions in terms of overflow volumes rather than rainfall volumes and considering both observed rainfall data and synthetic hyetographs derived from statistical analysis. The first application of the proposed methodology to the sewer network of the Mesola Municipality is presented and commented on.

[1]  F. Rossi,et al.  Regional flood estimation methods , 1994 .

[2]  Mauro Fiorentino,et al.  Two‐Component Extreme Value Distribution for Flood Frequency Analysis , 1984 .

[3]  H. Abida,et al.  A triangular model for the generation of synthetic hyetographs , 2009 .

[4]  Salvatore Gabriele,et al.  A hierarchical approach to regional flood frequency analysis , 1991 .

[5]  Aart Overeem,et al.  Rainfall depth-duration-frequency curves and their uncertainties , 2008 .

[6]  農業土木学会応用水文研究部会,et al.  応用水文 = Applied hydrology , 1991 .

[7]  Slobodan P. Simonovic,et al.  Generation of Synthetic Design Storms for the Upper Thames River Basin , 2004 .

[8]  Adrian J. Saul,et al.  Influence of rainfall estimation error and spatial variability on sewer flow prediction at a small urban scale , 2012 .

[9]  Slobodan P. Simonovic,et al.  Development of Probability Based Intensity- Duration-Frequency Curves under Climate Change , 2011 .

[10]  Clint J. Keifer,et al.  Synthetic Storm Pattern for Drainage Design , 1957 .

[11]  A. Brath,et al.  Assessing the reliability of regional depth‐duration‐frequency equations for gaged and ungaged sites , 2002 .

[12]  Günter Blöschl,et al.  On the role of storm duration in the mapping of rainfall to flood return periods , 2008 .

[13]  Wayne C. Huber,et al.  Hydrology and Floodplain Analysis , 1989 .

[14]  A. Brath,et al.  Relationships between statistics of rainfall extremes and mean annual precipitation: an application for design-storm estimation in northern central Italy , 2005 .

[15]  V. T. Chow,et al.  DESIGN HYETOGRAPHS FOR SMALL DRAINAGE STRUCTURES , 1980 .

[16]  E. Gumbel The Return Period of Flood Flows , 1941 .

[17]  V. Ferro,et al.  Regional Analysis of Rainfall-Depth-Duration Equation for South Italy , 1999 .

[18]  C. Kidd,et al.  A logical approach to the design storm concept , 1980 .

[19]  D. Stephenson,et al.  Stormwater hydrology and drainage , 1981 .

[20]  Francesco Laio,et al.  A simulation experiment for optimal design hyetograph selection , 2008 .

[21]  Timothy Carter,et al.  Vegetated roofs for stormwater management at multiple spatial scales , 2007 .

[22]  Sandro Artina,et al.  Simulation of a storm sewer network in industrial area: Comparison between models calibrated through experimental data , 2007, Environ. Model. Softw..

[23]  D. Veneziano,et al.  Best linear unbiased design hyetograph , 1999 .

[24]  A. Allen Bradley,et al.  Flood frequency analysis of simulated flows , 1992 .

[25]  Günter Blöschl,et al.  On the role of the runoff coefficient in the mapping of rainfall to flood return periods , 2009 .