Mercury cyclic porosimetry: Measuring pore-size distributions corrected for both pore-space accessivity and contact-angle hysteresis

被引:7
|
作者
Gu, Zongyu [1 ]
Goulet, Remi [2 ]
Levitz, Pierre [3 ]
Ihiawakrim, Dris [4 ]
Ersen, Ovidiu [4 ]
Bazant, Martin Z. [1 ,5 ]
机构
[1] MIT, Dept Chem Engn, Cambridge, MA 02139 USA
[2] St Gobain Res North Amer, 9 Goddard Rd, Northborough, MA USA
[3] Sorbonne Univ, CNRS, UMR 8234, PHENIX Lab, 4 Pl Jussieu, F-75252 Paris, France
[4] Univ Strasbourg, Inst Phys & Chim Mat Strasbourg IPCMS, UMR 7504, CNRS, 23 Rue Loess, F-67034 Strasbourg 2, France
[5] MIT, Dept Math, Cambridge, MA 02139 USA
关键词
Porous media; Mercury porosimetry; Hysteresis; Accessivity connectivity; Pore-size distribution; CAPILLARY HYSTERESIS; SORPTION ISOTHERMS; NETWORK; CONNECTIVITY; INTRUSION; SOLIDS; ROCKS;
D O I
10.1016/j.jcis.2021.04.038
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We propose a set of simple formulae for interpreting "mercury cyclic porosimetry" measurements where multiple intrusion-extrusion cycles are carried out. By employing two parameters alpha is an element of [0, 1] and kappa is an element of [0, 1], our theory quantitatively breaks down any hysteresis observed in cyclic porosimetry data into contributions due to connectivity effects and contact-angle hysteresis, respectively. In particular, the parameter alpha, called "pore-space accessivity", characterizes any serial connectivity between different-size pores. It has long been recognized that the standard method for determining the pore-size distribution (PSD) from mercury intrusion data based on the capillary bundle assumption overestimates the fraction of smaller pores; that corresponds to the alpha -> 1 limit of our model. In contrast, for materials with alpha < 1, our theory predicts a broadened PSD shifted toward larger radii, thus representing a simple way of rectifying PSDs for connectivity effects. The proposed model also establishes mercury cyclic porosimetry as a standard experimental procedure for measuring alpha, which can then be used in continuum models of porous media where connectivity effects play a significant role, such as in multiphase flow. (C) 2021 Elsevier Inc. All rights reserved.
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页码:255 / 261
页数:7
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