Quantitative morphology and network representation of soil pore structure

被引:303
作者
Vogel, HJ [1 ]
Roth, K [1 ]
机构
[1] Univ Heidelberg, Inst Environm Phys, D-69120 Heidelberg, Germany
关键词
network model; topology; hydraulic properties; water retention; porous media;
D O I
10.1016/S0309-1708(00)00055-5
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Pore-network models are attractive to relate pore geometry and transport processes in soil. In this contribution a 'morphological path' is presented to generate a network model based on quantitative morphological investigations of the 3D pore geometry in order to predict soil hydraulic properties. The 3D-geometry of pores larger than 0.04 mm in diameter is obtained using serial sections through impregnated samples. Beside pore-size distribution an important topological aspect of pore geometry is the spatial connectivity of the pore space which is difficult to measure. A connectivity function is proposed defined by the 3D-Euler number. The goodness in the estimation of the Euler number using serial sections is investigated in subsamples of different sizes and shapes. Then, a simple network model is generated which can be adapted to a predefined pore-size distribution and connectivity function. Network simulations of hydraulic properties are compared to independent measurements at the same soil material and the effect of topology on water flow and solute transport is investigated. It is concluded that a rough estimation of pore-size distribution and topology defined by the connectivity function might be sufficient to predict hydraulic properties. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:233 / 242
页数:10
相关论文
共 19 条
[1]   RECENT ADVANCES IN PORE SCALE MODELS FOR MULTIPHASE FLOW IN POROUS-MEDIA [J].
CELIA, MA ;
REEVES, PC ;
FERRAND, LA .
REVIEWS OF GEOPHYSICS, 1995, 33 :1049-1057
[2]   Three-dimensional analysis of a loamy-clay soil using pore and solid chord distributions [J].
Cousin, I ;
Levitz, P ;
Bruand, A .
EUROPEAN JOURNAL OF SOIL SCIENCE, 1996, 47 (04) :439-452
[3]  
FATT I, 1956, T AM I MIN MET ENG, V207, P144
[4]   THE EFFECT OF HETEROGENEITY ON THE DRAINAGE CAPILLARY-PRESSURE SATURATION RELATION [J].
FERRAND, LA ;
CELIA, MA .
WATER RESOURCES RESEARCH, 1992, 28 (03) :859-870
[5]   Prediction of relative and absolute permeabilities for gas and water from soil water retention curves using a pore-scale network model [J].
Fischer, U ;
Celia, MA .
WATER RESOURCES RESEARCH, 1999, 35 (04) :1089-1100
[6]   On the transport properties of anisotropic networks of capillaries [J].
Friedman, SP ;
Seaton, NA .
WATER RESOURCES RESEARCH, 1996, 32 (02) :339-347
[7]   THE EFFECT OF PORE-STRUCTURE ON HYSTERESIS IN RELATIVE PERMEABILITY AND CAPILLARY-PRESSURE - PORE-LEVEL MODELING [J].
JERAULD, GR ;
SALTER, SJ .
TRANSPORT IN POROUS MEDIA, 1990, 5 (02) :103-151
[8]   Prediction of relative permeabilities for unconsolidated soils using pore-scale network models [J].
Rajaram, H ;
Ferrand, LA ;
Celia, MA .
WATER RESOURCES RESEARCH, 1997, 33 (01) :43-52
[9]   Structure and transport properties of a porous magnetic gel via x-ray microtomography [J].
Rintoul, MD ;
Torquato, S ;
Yeong, C ;
Keane, DT ;
Erramilli, S ;
Jun, YN ;
Dabbs, DM ;
Aksay, IA .
PHYSICAL REVIEW E, 1996, 54 (03) :2663-2669
[10]  
Serra J., 1982, Image Analysis and Mathematical Morphology