2017
DOI: 10.1088/1361-6420/aa58d1
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Weak unique continuation property and a related inverse source problem for time-fractional diffusion-advection equations

Abstract: In this paper, we first establish a weak unique continuation property for timefractional diffusion-advection equations. The proof is mainly based on the Laplace transform and the unique continuation properties for elliptic and parabolic equations. The result is weaker than its parabolic counterpart in the sense that we additionally impose the homogeneous boundary condition. As a direct application, we prove the uniqueness for an inverse problem on determining the spatial component in the source term in by inte… Show more

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Cited by 125 publications
(149 citation statements)
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“…Note that m ≤ 0 implies M k ≥ 0. Thus, due to (18), the properties of g and the monotonicity of E (−z), we obtain…”
Section: Solutions Of the Sequence Of Linear Equationsmentioning
confidence: 95%
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“…Note that m ≤ 0 implies M k ≥ 0. Thus, due to (18), the properties of g and the monotonicity of E (−z), we obtain…”
Section: Solutions Of the Sequence Of Linear Equationsmentioning
confidence: 95%
“…For instance, it is an extension to the fractional case of the parabolic integro‐differential equation u t =ϰ(Δ u + m ∗Δ u )+ F that describes heat processes with memory . Moreover, it is a generalization of an equation with multiple Caputo derivatives βu+j=1lbjμju=ϰnormalΔu+z, 0< μ j < β <1, that was studied in previous works . Rewriting the latter equation as βu+kβu=ϰnormalΔu+z,1emwhere1emkfalse(tfalse)=truej=1lbjtβμj1normalΓfalse(βμjfalse), defining m as a solution of the Volterra equation of the second kind m + k ∗ m =− k and applying the operator scriptI+m, where scriptI is the unity operator, to the Equation , we reach with F = z + m ∗ z .…”
Section: Formulation Of Direct and Inverse Problemsmentioning
confidence: 99%
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