Author/Authors :
Kewen Li، نويسنده , , Rol، N. Horne، نويسنده ,
Abstract :
Although steam–water capillary pressure is of central importance in geothermal reservoir engineering, it
is nevertheless still poorly understood because of the difficulties involved in making direct measurements. To
this end, we have conducted some experimental and theoretical studies. Unique methods have been developed
to measure capillary pressures in order to overcome the complications in laboratory procedures associated
with mass transfer as temperature and pressure changes. Both steam–water and air–water capillary pressures
were measured and compared. Significant differences were found; in the cases studied, the steam–water
capillary pressures were smaller. The drainage capillary pressure was greater than the imbibition capillary
pressure, as was expected. Using experimental data, an empirical model was derived to calculate steamwater
capillary pressure directly. Also developed was a generalized capillary pressure model based on
fractal modeling of a porous medium; it encompasses the frequently used Brooks–Corey model (Brooks,
R.H., Corey, A.T., 1964. Hydraulic Properties of Porous Media. Colorado State University, Hydro paper No.
3, Fort Collins, CO, USA, 24 pp.) as well as others. Recent studies on the topic are summarized and reviewed.
© 2007 CNR. Published by Elsevier Ltd. All rights reserved.
Keywords :
Fractals , Experimental data , The Geysers , USA , Capillary pressure model , Steam–water flow