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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Bibliographic Details
Main Authors: Sánchez,M., Medina,A., Rojano,A.
Format: Digital revista
Language:English
Published: Sociedad Mexicana de Física 2005
Online Access:http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0035-001X2005000400002
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