1994
DOI: 10.1090/s0002-9947-1994-1216335-0
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Weak solutions of hyperbolic-parabolic Volterra equations

Abstract: Abstract. The existence of a global weak solution, satisfying certain a priori L°°-bounds, of the equation ut(t, x) = /0' k(t -s)(o(ux))x{s, x)ds + f{t, x) is established. The kernel k is locally integrable and log-convex, and a1 has only one local minimum which is positive.

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Cited by 9 publications
(6 citation statements)
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“…Assuming that the stress depends nonlinearly on y x , that is, τ = σ ( y x ), where σ is the first Piola–Kirchhoff stress component in one space dimension (see (2.2) for the definition), we obtain the nonlinear wave equation ρR ytt=σfalse(yxfalse)x,2emfalse(x,tfalse)normalΩ×false(0,normal∞false), where σ = W ′ (see (2.2) for the general definition) stands for the non-monotone stress as in figure 2. By the results of MacCamy & Mizel [27], we know that global solutions for equation (3.2), even for smooth initial data, do not exist in general due to the fact that second derivatives of the solutions may become infinite in finite time (see also the discussion in [28] for a hyperbolic-parabolic formulation related to Volterra equations and [29] for a discussion in three-space dimension). In particular, as Pego [30] explains, when y x is in the ranges where σ is decreasing, the equation becomes elliptic and this makes the initial value problem ill-posed.…”
Section: Governing Equationsmentioning
confidence: 99%
“…Assuming that the stress depends nonlinearly on y x , that is, τ = σ ( y x ), where σ is the first Piola–Kirchhoff stress component in one space dimension (see (2.2) for the definition), we obtain the nonlinear wave equation ρR ytt=σfalse(yxfalse)x,2emfalse(x,tfalse)normalΩ×false(0,normal∞false), where σ = W ′ (see (2.2) for the general definition) stands for the non-monotone stress as in figure 2. By the results of MacCamy & Mizel [27], we know that global solutions for equation (3.2), even for smooth initial data, do not exist in general due to the fact that second derivatives of the solutions may become infinite in finite time (see also the discussion in [28] for a hyperbolic-parabolic formulation related to Volterra equations and [29] for a discussion in three-space dimension). In particular, as Pego [30] explains, when y x is in the ranges where σ is decreasing, the equation becomes elliptic and this makes the initial value problem ill-posed.…”
Section: Governing Equationsmentioning
confidence: 99%
“…The FPDE (1.3)-(1.4) interpolates two PDEs (see e.g. [9]), namely semilinear wave (α = 2) and heat (α = 1) equations, which have been widely investigated in the last years. These PDEs present many differences in the theory of existence and asymptotic behavior of solutions in scaling invariant spaces (critical spaces).…”
Section: Introduction and Resultsmentioning
confidence: 99%
“…For ao 4 3 this task is essentially solved (see [10]). By different methods, the existence, but not the uniqueness, of a solution u satisfying uAW 1;N loc ðR þ ; L 2 ð0; 1ÞÞ-L 2 loc ðR þ ; W 2;2 0 ð0; 1ÞÞ was proved in [12], for the range aA½ 4 3 ; 3 2 : For 3 2 oao2; only existence of global weak solutions has been proved [11]. We do however conjecture that unique smooth, global solutions do exist for the entire range aAð0; 2Þ:…”
Section: An Examplementioning
confidence: 99%