Deprecated: $wgMWOAuthSharedUserIDs=false is deprecated, set $wgMWOAuthSharedUserIDs=true, $wgMWOAuthSharedUserSource='local' instead [Called from MediaWiki\HookContainer\HookContainer::run in /var/www/html/w/includes/HookContainer/HookContainer.php at line 135] in /var/www/html/w/includes/Debug/MWDebug.php on line 372
A cusp-like free-surface flow due to a submerged source or sink - MaRDI portal

A cusp-like free-surface flow due to a submerged source or sink

From MaRDI portal
Publication:3313450

DOI10.1017/S0334270000004197zbMath0531.76018MaRDI QIDQ3313450

E. O. Tuck, Jean-Marc Vanden-Broeck

Publication date: 1984

Published in: The Journal of the Australian Mathematical Society. Series B. Applied Mathematics (Search for Journal in Brave)




Related Items (40)

Selective withdrawal from an intake channel connected to a reservoirFlow induced by a line sink near a vertical wall in a fluid with a free surface. I: Infinite depthSteady free surface flows induced by a submerged ring source or sinkWithdrawal of fluid through a line sink beneath a free surface above a sloping boundaryFlow induced by a line sink near a vertical wall in a fluid with a free surface. II: Finite depthFlow due to a sink near a vertical wall, in infinitely deep fluidUnsteady draining flows from a rectangular tankThe effect of surface tension on free surface flow induced by a point sink in a fluid of finite depthProgress toward a mining strategy based on mineral leaching with secondary recoveryOn 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 bottomDraining of a fluid of finite depth into a vertical slotUnsteady draining of a fluid from a circular tankA line sink in a flowing stream with surface tension effectsA simple model of magnetic fields associated with outflow from a source; new orthogonal polynomialsUnsteady flows induced by a point source or sink in a fluid of finite depthUnsteady free surface flow induced by a line sink in a fluid of finite depthA hybrid perturbation–Galerkin solution to a problem in selective withdrawalTHE EFFECT OF SURFACE TENSION ON FREE-SURFACE FLOW INDUCED BY A POINT SINKThe lens of freshwater in a tropical island-- 2D withdrawal.On starting conditions for a submerged sink in a fluidCritical withdrawal from a two-layer fluid through a line sinkWithdrawal of a fluid of finite depth through a line sink with a cusp in the free surfaceBow flows in water of finite depthSubcritical free-surface flow caused by a line source in a fluid of finite depthPotential-flow studies of steady two-dimensional jets, waterfalls, weirs and spraysFlow from a vertical slot into a layer of finite depthA NOTE ON STEADY FLOW INTO A SUBMERGED POINT SINKTwo-dimensional steady free surface flow into a semi-infinite mat sinkImpact of a falling jetA NOTE ON WITHDRAWAL FROM A TWO-LAYER FLUID THROUGH A LINE SINK IN A POROUS MEDIUMSteady free surface potential flow of an ideal fluid due to a singular sink on the flat bottomA boundary integral method applied to the 3D water coning problemWaves generated by a source below a free surface in water of finite depthPrefaceAxisymmetric outflows from binary point-source systems in the presence of an interfacePotential flow of fluid from an elevated, two-dimensional sourceSupercritical free-surface flow with a stagnation point due to a submerged sourceCommunications and forumThe flow induced in a three-layer stratified fluid by a submerged sink or source with stagnation points on the free surfacesOn the computation of steady axisymmetric withdrawal from a two-layer fluid




This page was built for publication: A cusp-like free-surface flow due to a submerged source or sink