Spontaneous imbibition in a porous medium under longitudinal temperature gradients
In this work, the influence of a longitudinal temperature gradient on the spontaneous imbibition into a homogeneous porous medium has been analyzed. Theory and experiments done on a permeable rock (Berea sandstone) allow us to show how this gradient modifies the temporal evolution of the averaged imbibition front h(t). Despite the existence of a thermal boundary layer outside the rock, experimental data are in good agreement with the theoretical profiles of h(t).
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Autores principales: | , , |
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Formato: | Digital revista |
Idioma: | English |
Publicado: |
Sociedad Mexicana de Física
2005
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Acceso en línea: | http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0035-001X2005000400002 |
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