具有耗散抛物性和正格的矢量阶非齐次微分方程

V. Litovchenko, M. Gorbatenko
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引用次数: 0

摘要

彼得罗夫斯基和希洛夫意义上的抛物性都具有标量特征。它不能考虑到环境异质性的特殊性。在这方面,在70年代早期,S.D. Eidelman提出了所谓的$\vec{2b}$-抛物线性,这是对各向异性介质情况下Petrovsky抛物线性的自然推广。在S.D. Eidelman、S.D. Ivasishena、M.I. Matiichuk及其学生的著作中,详细地研究了此类抛物性方程的柯西问题。各向异性介质的抛物性根据希洛夫的推广是$\{\vec{p},\vec h\}$-抛物性。具有抛物性的方程类是相当广泛的,它包括Eidelman, Petrovskii和Shilov类,并允许统一抛物方程的柯西问题的经典理论。本文研究了具有向量正属的非齐次$\{\vec{p},\vec h\}$-抛物型方程中具有Gelfand分布和Shilov分布的广义初始函数类的Cauchy问题正确可解的条件。同时,方程的非齐次性对于变量集是有限光滑的连续函数,对于空间变量是递减的,对于时间变量是无界的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
INHOMOGENEOUS DIFFERENTIAL EQUATIONS OF VECTOR ORDER WITH DISSIPATIVE PARABOLICITY AND POSITIVE GENUS
Parabolicity in the sense of both Petrosky and Shilov has a scalar character. It is not able to take into account the specificity of the heterogeneity of the environment. In this regard, in the early 70-s, S.D. Eidelman proposed the so-called $\vec{2b}$-parabolicity, which is a natural generalization of the Petrovsky parabolicity for the case of an anisotropic medium. A detailed study of the Cauchy problem for equations with such parabolicity was carried out in the works of S.D. Eidelman, S.D. Ivasishena, M.I. Matiichuk and their students. An extension of parabolicity according to Shilov for the case of anisotropic media is $\{\vec{p},\vec h\}$-parabolicity. The class of equations with such parabolicity is quite broad, it includes the classes of Eidelman, Petrovskii, and Shilov and allows unifying the classical theory of the Cauchy problem for parabolic equations. In this work, for inhomogeneous $\{\vec{p},\vec h\}$-parabolic equations with vector positive genus, the conditions under which the Cauchy problem in the class of generalized initial functions of the type of Gelfand and Shilov distributions will be correctly solvable are investigated. At the same time, the inhomogeneities of the equations are continuous functions of finite smoothness with respect to the set of variables, which decrease with respect to the spatial variable, and are unbounded with the integrable feature with respect to the time variable.
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