Validation of gas flow experiments for porous media by means of computer simulations

被引:7
作者
Laddha, Sunny [1 ]
Macher, Wolfgang [1 ]
Kargl, Guenter [1 ]
Zivithal, Stephan [1 ]
Blum, Juergen [2 ]
Gundlach, Bastian [2 ]
Guettler, Carsten [3 ]
Sierks, Holger [3 ]
Rose, Martin [4 ]
机构
[1] Austrian Acad Sci, Space Res Inst, Schmiedlstr 6, A-8042 Graz, Austria
[2] TU Braunschweig, Inst Geophys & Extraterr Phys IGeP, Mendelssohnstr 3, D-38106 Braunschweig, Germany
[3] Max Planck Inst Sonnensyst Forsch, Justus von Liebig Weg 3, D-37077 Gottingen, Germany
[4] Ingenieurbuero Dr Ing Martin Rose, Sommerhofenstr 148, D-71067 Sindelfingen, Germany
基金
奥地利科学基金会;
关键词
gas flow; porous media; measurement validation; TRANSPORT CHARACTERISTICS; SURFACE-LAYER; COMET; PERMEABILITY; NUCLEUS; BODIES; ICE;
D O I
10.1088/1361-6501/acb373
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A profound understanding of gas flow in porous media is of great interest for various technological and scientific fields. Its investigation by laboratory measurements, however, poses several challenges. In particular, the determination of macroscopic flow parameters from pressure and gas flow measurements is prone to various error influences, some of which are very difficult to analyze experimentally. Computer simulations are a solution in this context as they facilitate modifications of the underlying geometry and boundary conditions in a flexible way. Here we present a simulation framework for the analysis of a recent experiment for determining the Knudsen diffusion coefficient and viscous permeability of various porous granular materials. By combining the finite element method with analytical models and other numerical methods, we were able to identify previously neglected physical effects that increase the uncertainty of the measurements. In particular, the porosity increase due to finite sample dimensions, in a layer of about a grain diameter thickness near the container wall, creates a deviation of the measured pressure gradient. This deviation amounts to ca. 5% for a sample width of about 100 grains and a porosity of 0.5, and is indirectly proportional to the porosity. The second most prominent error source, the sample support sieve, causes a slight constriction of the flow volume. Simulations of this effect show an error around 4%-7%, dependent on the grain size. Based on these findings we recommend an overall sample dimension of 100 grains or larger. As an example of failures of the sample homogeneity, we elaborate how channels through the sample influence the flow properties. Respective suggestions for keeping all discussed effects negligible are discussed in detail. Our methodology demonstrates how the combination of finite element computations with analytical representations of the involved macroscopic parameters can assess the validity and accuracy of laboratory experiments.
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页数:18
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