The aim of this paper is the investigation of gravitycurrents moving on both smooth andrough beds by laboratory experiments. Gravity currents were produced in a Perspex tank of rectangular cross-section by lock exchange release experiments. The tank is divided into two parts by a sliding gate: one filled with tap water and the other one filled with salt water to the same height. Nine experiments were performed varying both the bed roughness and the initial density of the gravity current. All the expe-riments were recorded by a camera and an image analysis technique was applied to measure the space-time evolution of the gravity current's profile. For the experiments with a smooth bed three different phases were observed in the gravity current’s dynamics: a first slumping or constant speed phase; a second self-similar phase, in which the front speed decreased as t-1/3, where t is the time measured from release; a third viscous phase, in which the front velocity decreased as t-4/5. In the experiments performed with a rough bed the measured front’s velocities were observed to be lower than the front’s velocity of gravity currents moving on a smooth bed.
Adduce, C., LA ROCCA, M., Lombardi, V., Sciortino, G. (2010). Laboratory experiments on gravity currents moving on smooth and rough beds. In River Flow 2010 Conference Proceedings (pp.605-611). Bundesanstalt für Wasserbau (DEU).
Laboratory experiments on gravity currents moving on smooth and rough beds
LA ROCCA, MICHELE;LOMBARDI, VALENTINA;SCIORTINO, Giampiero
2010-01-01
Abstract
The aim of this paper is the investigation of gravitycurrents moving on both smooth andrough beds by laboratory experiments. Gravity currents were produced in a Perspex tank of rectangular cross-section by lock exchange release experiments. The tank is divided into two parts by a sliding gate: one filled with tap water and the other one filled with salt water to the same height. Nine experiments were performed varying both the bed roughness and the initial density of the gravity current. All the expe-riments were recorded by a camera and an image analysis technique was applied to measure the space-time evolution of the gravity current's profile. For the experiments with a smooth bed three different phases were observed in the gravity current’s dynamics: a first slumping or constant speed phase; a second self-similar phase, in which the front speed decreased as t-1/3, where t is the time measured from release; a third viscous phase, in which the front velocity decreased as t-4/5. In the experiments performed with a rough bed the measured front’s velocities were observed to be lower than the front’s velocity of gravity currents moving on a smooth bed.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.