Description of Free Energy for Immiscible Two-Fluid Flow in Porous Media by Integral Geometry and Thermodynamics

被引:20
|
作者
Khanamiri, Hamid Hosseinzade [1 ]
Berg, Carl Fredrik [1 ]
Slotte, Per Arne [1 ]
Schlueter, Steffen [2 ]
Torsaeter, Ole [1 ]
机构
[1] Norwegian Univ Sci & Technol NTNU, PoreLab, Dept Geosci & Petr, Trondheim, Norway
[2] UFZ Helmholtz Ctr Environm Res, Dept Soil Syst Sci, Leipzig, Germany
关键词
porous media; two-phase flow; geometric state variables; integral geometry; energy description; energy dissipation; 2-PHASE FLOW; CAPILLARY-PRESSURE; RELATIVE PERMEABILITY; RELAXATION DYNAMICS; FLUID TOPOLOGY; HYSTERESIS; SATURATION; REGIMES; PHYSICS;
D O I
10.1029/2018WR023619
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In integral geometry, intrinsic volumes are a set of geometrical variables to characterize spatial structures, for example, distribution of fluids in two-fluid flow in porous media. McClure et al. (2018, ) utilized this principle and proposed a geometric state function based on the intrinsic volumes. In a similar approach, we find a geometrical description for free energy of a porous system with two fluids. This is also an extension of the work by Mecke (2000, ) for energy of a single fluid. Several geometrical sets of spatial objects were defined, including bulk of the two fluids, interfaces, and three-phase contact lines. We have simplified the description of free energy by showing how the intrinsic volumes of these sets are geometrically related. We obtain a description for energy as a function of seven microscopic geometrically independent variables. In addition, using a thermodynamic approach, we find an approximation for the free energy as a function of macroscopic parameters of saturation and pressure under quasi-static conditions. The combination of the two energy descriptions, by integral geometry and thermodynamics, completes the relation between the associated variables and enables us to find the unknown coefficients of the intrinsic volumes and to calculate the amount of dissipated energy in drainage and imbibition processes. We show that the theory is consistent with a set of experiments performed by Schluter et al. (2016a, , 2017a, ). However, in order to be more conclusive, it needs to be tested with larger data sets.
引用
收藏
页码:9045 / 9059
页数:15
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