MEASUREMENT OF INTERFACIAL-TENSION AND SPREADING COEFFICIENT UNDER RESERVOIR CONDITIONS - EXPERIMENTAL INVESTIGATION

Authors
Citation
R. Amin et Tn. Smith, MEASUREMENT OF INTERFACIAL-TENSION AND SPREADING COEFFICIENT UNDER RESERVOIR CONDITIONS - EXPERIMENTAL INVESTIGATION, Colloids and surfaces. A, Physicochemical and engineering aspects, 137(1-3), 1998, pp. 35-43
Citations number
14
Categorie Soggetti
Chemistry Physical
ISSN journal
09277757
Volume
137
Issue
1-3
Year of publication
1998
Pages
35 - 43
Database
ISI
SICI code
0927-7757(1998)137:1-3<35:MOIASC>2.0.ZU;2-C
Abstract
The variation of interfacial tension with temperature and pressure inf luences the transport of the fluid in a reservoir strongly. This makes the interfacial tension probably the most important of the factors th at make one-third of the total oil in place (in reservoir rock) unreco verable by gas drive or water flooding. Several models and correlation s were used to predict the measured data presented here. We have studi ed the applicability of four of the most commonly used IFT-correlation s, those of Katz et al. [AIME Technical Publications No. 1624, pp. 285 -294], Hough and Stegemeier [Soc. Pet. Eng. J. (1961) 259-263], Lee an d Chien [SPE/DOE 12643, Fourth Symp. on EOR, Tulsa, OK], and Pedersen et al. [Properties of oils and natural gases, Gulf Publishing Co., 198 9, pp. 196-207]. The experimental results from the three binary system s as well as the recombined crude oil system have shown that the inter facial tension in the high pressure region (below saturation pressure) remains quite low despite large pressure decrements. This study was t hen extended to include measurements of the equilibrium interfacial te nsion for oil-brine, oil-gas and gas-brine at reservoir temperature an d pressure over the range 250 to 3728 psia. The interfacial tensions w ere used to evaluate the spreading coefficient as a function of pressu re at reservoir temperature. The viscosity and density of the oil and gas and brine phases were also measured over the same range of reservo ir conditions. (C) 1998 Elsevier Science B.V.