Mathematical models in dynamics of non-Newtonian fluids and in glaciology

time. Abstract. This paper deals with the study of some qualitative properties of solutions of mathematical models in non-Newtonian isothermal fluid flows and in theoretical glaciology. In the first type of models, we consider the extinction in a finite time of the solutions by using a global energy...

Full description

Bibliographic Details
Main Authors: S. N. Antontsev, J. I. Díaz, H. B De Oliveira, Centro De Matemática
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.589.5451
http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.589.5451
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.589.5451 2023-05-15T16:40:31+02:00 Mathematical models in dynamics of non-Newtonian fluids and in glaciology S. N. Antontsev J. I. Díaz H. B De Oliveira Centro De Matemática The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.589.5451 http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.589.5451 http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf non-Newtonian fluids glaciology extinction in a finite time finite speed of propagation waiting text 2007 ftciteseerx 2016-01-08T13:24:57Z time. Abstract. This paper deals with the study of some qualitative properties of solutions of mathematical models in non-Newtonian isothermal fluid flows and in theoretical glaciology. In the first type of models, we consider the extinction in a finite time of the solutions by using a global energy method. We prove that this property holds for pseudo-plastic fluids or for the general class of Newtonian and dilatant fluids, assumed the presence of a dissipation term (which may have an anisotropic nature and can vanish in, at most, one spatial direction). In the case of the ice sheet model in Glaciology (with a formulation involving a quasi-linear degenerate equation similar to the ones arising in non-Newtonian flows), we analyze the behavior of the free boundary (given by the support of the height h of the ice sheet) for different cases and according to the values of the ablation function and the initial hight. We use here some other energy methods of a local nature and so completely different to the method used in the first part of the paper. 1 Text Ice Sheet Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic non-Newtonian fluids
glaciology
extinction in a finite time
finite speed of propagation
waiting
spellingShingle non-Newtonian fluids
glaciology
extinction in a finite time
finite speed of propagation
waiting
S. N. Antontsev
J. I. Díaz
H. B De Oliveira
Centro De Matemática
Mathematical models in dynamics of non-Newtonian fluids and in glaciology
topic_facet non-Newtonian fluids
glaciology
extinction in a finite time
finite speed of propagation
waiting
description time. Abstract. This paper deals with the study of some qualitative properties of solutions of mathematical models in non-Newtonian isothermal fluid flows and in theoretical glaciology. In the first type of models, we consider the extinction in a finite time of the solutions by using a global energy method. We prove that this property holds for pseudo-plastic fluids or for the general class of Newtonian and dilatant fluids, assumed the presence of a dissipation term (which may have an anisotropic nature and can vanish in, at most, one spatial direction). In the case of the ice sheet model in Glaciology (with a formulation involving a quasi-linear degenerate equation similar to the ones arising in non-Newtonian flows), we analyze the behavior of the free boundary (given by the support of the height h of the ice sheet) for different cases and according to the values of the ablation function and the initial hight. We use here some other energy methods of a local nature and so completely different to the method used in the first part of the paper. 1
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author S. N. Antontsev
J. I. Díaz
H. B De Oliveira
Centro De Matemática
author_facet S. N. Antontsev
J. I. Díaz
H. B De Oliveira
Centro De Matemática
author_sort S. N. Antontsev
title Mathematical models in dynamics of non-Newtonian fluids and in glaciology
title_short Mathematical models in dynamics of non-Newtonian fluids and in glaciology
title_full Mathematical models in dynamics of non-Newtonian fluids and in glaciology
title_fullStr Mathematical models in dynamics of non-Newtonian fluids and in glaciology
title_full_unstemmed Mathematical models in dynamics of non-Newtonian fluids and in glaciology
title_sort mathematical models in dynamics of non-newtonian fluids and in glaciology
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.589.5451
http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_source http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.589.5451
http://w3.ualg.pt/~holivei/ADO-Porto-2007.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766030916162945024