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Stormwater drainage systems are designed to operate in a free surface flow regime, however, transition into a pressurized flow regime may occur during intense rain events as the inflow exceeds the transport capacity of the system in free surface flow mode. The air phase within the sewers may then become pressurized, significantly altering the dynamics of the flow. Mixed flows, also referred to as flow regime transitions, have been linked to the occurrence of serious operational problems in stormwater systems, such as geysering and structural damage of sewers. While such flow conditions have…mehr

Produktbeschreibung
Stormwater drainage systems are designed to operate in a free surface flow regime, however, transition into a pressurized flow regime may occur during intense rain events as the inflow exceeds the transport capacity of the system in free surface flow mode. The air phase within the sewers may then become pressurized, significantly altering the dynamics of the flow. Mixed flows, also referred to as flow regime transitions, have been linked to the occurrence of serious operational problems in stormwater systems, such as geysering and structural damage of sewers. While such flow conditions have been investigated previously, the current knowledge on this problem is still limited and fragmented, particularly regarding the role of the air phase in the filling process. The investigation presented in this work includes experiments performed in reduced scale models representing stormwater storage tunnels, sewers and ventilation towers of stormwater systems. Numerical investigation was alsoperformed to create models to simulate flow regime transition caused by rapid filling of stormwater system, including some relevant effects of air pressurization.
Autorenporträt
Dr. Vasconcelos is an Assistant Professor with the Department of Civil Engineering at Auburn University. He obtained his Ph.D. in Environmental Engineering from the University of Michigan. His research focuses in Urban Water Systems, and his numerical models were used to simulate extreme flows in cities such as Washington, DC, and London, UK.