Diffusion with space memory modelled with distributed order space fractional differential equations

Distributed order fractional differential equations (Caputo, 1995, 2001; Bagley and Torvik, 2000a,b) were fi rst used in the time domain; they are here considered in the space domain and introduced in the constitutive equation of diffusion. The solution of the classic problems are obtained, with clo...

Full description

Bibliographic Details
Main Author: M. Caputo
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2003-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3395
id doaj-31b89358e4174016aa92424913756569
record_format Article
spelling doaj-31b89358e4174016aa924249137565692020-11-24T22:10:31ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2003-06-0146210.4401/ag-3395Diffusion with space memory modelled with distributed order space fractional differential equationsM. CaputoDistributed order fractional differential equations (Caputo, 1995, 2001; Bagley and Torvik, 2000a,b) were fi rst used in the time domain; they are here considered in the space domain and introduced in the constitutive equation of diffusion. The solution of the classic problems are obtained, with closed form formulae. In general, the Green functions act as low pass fi lters in the frequency domain. The major difference with the case when a single space fractional derivative is present in the constitutive equations of diffusion (Caputo and Plastino, 2002) is that the solutions found here are potentially more fl exible to represent more complex media (Caputo, 2001a). The difference between the space memory medium and that with the time memory is that the former is more fl exible to represent
 local phenomena while the latter is more fl exible to represent variations in space. Concerning the boundary value
 problem, the difference with the solution of the classic diffusion medium, in the case when a constant boundary pressure is assigned and in the medium the pressure is initially nil, is that one also needs to assign the fi rst order space derivative at the boundary.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3395distributed orderfractional orderdifferential equationsconstitutive equationsdiffusionspace fractional derivative
collection DOAJ
language English
format Article
sources DOAJ
author M. Caputo
spellingShingle M. Caputo
Diffusion with space memory modelled with distributed order space fractional differential equations
Annals of Geophysics
distributed order
fractional order
differential equations
constitutive equations
diffusion
space fractional derivative
author_facet M. Caputo
author_sort M. Caputo
title Diffusion with space memory modelled with distributed order space fractional differential equations
title_short Diffusion with space memory modelled with distributed order space fractional differential equations
title_full Diffusion with space memory modelled with distributed order space fractional differential equations
title_fullStr Diffusion with space memory modelled with distributed order space fractional differential equations
title_full_unstemmed Diffusion with space memory modelled with distributed order space fractional differential equations
title_sort diffusion with space memory modelled with distributed order space fractional differential equations
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2003-06-01
description Distributed order fractional differential equations (Caputo, 1995, 2001; Bagley and Torvik, 2000a,b) were fi rst used in the time domain; they are here considered in the space domain and introduced in the constitutive equation of diffusion. The solution of the classic problems are obtained, with closed form formulae. In general, the Green functions act as low pass fi lters in the frequency domain. The major difference with the case when a single space fractional derivative is present in the constitutive equations of diffusion (Caputo and Plastino, 2002) is that the solutions found here are potentially more fl exible to represent more complex media (Caputo, 2001a). The difference between the space memory medium and that with the time memory is that the former is more fl exible to represent
 local phenomena while the latter is more fl exible to represent variations in space. Concerning the boundary value
 problem, the difference with the solution of the classic diffusion medium, in the case when a constant boundary pressure is assigned and in the medium the pressure is initially nil, is that one also needs to assign the fi rst order space derivative at the boundary.
topic distributed order
fractional order
differential equations
constitutive equations
diffusion
space fractional derivative
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3395
work_keys_str_mv AT mcaputo diffusionwithspacememorymodelledwithdistributedorderspacefractionaldifferentialequations
_version_ 1725807769990201344