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...
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
2003-06-01
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Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3395 |
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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 |
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1725807769990201344 |