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A conservation Law with Point Source and Discontinuous Flux Function Modelling Continuous Sedimentation

Stefan Diehl

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Source: Crossref

Published: Apr 1, 1996

DOI: 10.1137/s0036139994242425

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Source abstract

Continuous sedimentation of solid particles in a liquid takes place in a clarifier-thickener unit, which has one feed inlet and two outlets. The aim of the paper is to formulate and analyse a dynamic model for this process under idealized physical conditions. The conservation of mass yields the scalar conservation law ∂u(x,t)∂t+∂∂x(F(u(x,t),x))=s(t)δ(x)\frac{\partial u( {x,t} )}{\partial t} + \frac{\partial }{\partial x}( {F( {u( {x,t} ),x} )} ) = s( t )\delta ( x ), where δ\delta is the Dirac measure, s is a source, and F is a flux function, which is discontinuous at three points in the one-dimensional space coordinate x. Under certain regularity assumptions a procedure for constructing a solution, locally in time, is presented. The nonlinear phenomena are complicated, and so is the general construction of a solution. The problem of nonuniqueness due to the discontinuities of F(u,⋅)F( {u, \cdot } ) is handled by a generalized entropy condition. An advantage of this approach is that the a priori boundary conditions (at the discontinuities of F(u,⋅) F( {u, \cdot } ) that have been used earlier can be omitted. The steady-state solutions are also presented.

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A conservation Law with Point Source and Discontinuous Flux Function Modelling Continuous Sedimentation — Mathematical Frontier Network