Cusp-like free-surface flows due to a submerged source or sink in the presence of a flat or sloping bottom
From MaRDI portal
Publication:3712000
DOI10.1017/S0334270000004665zbMath0586.76019OpenAlexW1981547607MaRDI QIDQ3712000
Publication date: 1985
Published in: The Journal of the Australian Mathematical Society. Series B. Applied Mathematics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0334270000004665
exact solutionsline sourcenumerical solutionsconformal mapping techniquesimpermeable basessink beneath a cusped free surface
Related Items (max. 100)
The problem of the flow of an ideal fluid with a singular sink at a depression on the bottom ⋮ Steady free surface flows induced by a submerged ring source or sink ⋮ Withdrawal of fluid through a line sink beneath a free surface above a sloping boundary ⋮ Flow induced by a line sink near a vertical wall in a fluid with a free surface. II: Finite depth ⋮ Progress toward a mining strategy based on mineral leaching with secondary recovery ⋮ On the shape of the free-surface problem of an ideal incompressible fluid flow with a singular sink at the top of a triangular ledge at the bottom ⋮ Draining of a fluid of finite depth into a vertical slot ⋮ Unsteady free surface flow due to a line sink at an arbitrary location with surface tension ⋮ Unsteady flows induced by a point source or sink in a fluid of finite depth ⋮ Unsteady free surface flow induced by a line sink in a fluid of finite depth ⋮ THE EFFECT OF SURFACE TENSION ON FREE-SURFACE FLOW INDUCED BY A POINT SINK ⋮ A NOTE ON APPROXIMATE BENCHMARK SOLUTIONS FOR VISCOUS TWO-LAYER FLOWS ⋮ Critical withdrawal from a two-layer fluid through a line sink ⋮ Withdrawal of a fluid of finite depth through a line sink with a cusp in the free surface ⋮ Bow flows in water of finite depth ⋮ Subcritical free-surface flow caused by a line source in a fluid of finite depth ⋮ Flow from a vertical slot into a layer of finite depth ⋮ Impact of a falling jet ⋮ Steady free surface potential flow of an ideal fluid due to a singular sink on the flat bottom ⋮ Waves generated by a source below a free surface in water of finite depth ⋮ Supercritical free-surface flow with a stagnation point due to a submerged source ⋮ Communications and forum
This page was built for publication: Cusp-like free-surface flows due to a submerged source or sink in the presence of a flat or sloping bottom