On the relationship between indicators of geostatistical, flow and transport connectivity

被引:246
作者
Knudby, C [1 ]
Carrera, J [1 ]
机构
[1] Tech Univ Catalonia, Dept Geotech Engn & Geosci, Barcelona 08034, Spain
关键词
connectivity; heterogeneous media; preferential flow; channeling; effective permeability; geostatistics; entropy; contaminant transport;
D O I
10.1016/j.advwatres.2004.09.001
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Connectivity of high conductivity (K) paths is important because it can lead to channeling, i.e. flow along preferential paths, which can reduce travel times very significantly. Nevertheless, limited effort has been devoted to defining the concept quantitatively. We propose and evaluate nine indicators of connectivity. Three account for the presence of flow connectivity, that is, the flow rate increase caused by preferential flow paths. Two account for the presence of transport connectivity, that is, the existence of fast paths allowing early solute arrival. The remaining four are statistical indicators based on two- and multiple-point statistics. We test these indicators on heterogeneous conductivity fields with different visual connectivity. The indicators of flow connectivity and one of the transport connectivity indicators succeed in identifying the increased presence of connected high-K features. The two-point statistical indicators fail to do so. The directional multi-point statistical indicator performs better. None of the statistical indicators correlate with the flow and transport indicators. We find only weak dependence between the flow and transport indicators. Our results suggest that transport connectivity is much less sensitive to barriers, which control flow connectivity. Instead, transport connectivity appears to be controlled by the existence of narrow, possibly discontinuous high-K paths. Therefore, we conclude that connectivity is a process-dependent concept. (c) 2004 Published by Elsevier Ltd.
引用
收藏
页码:405 / 421
页数:17
相关论文
共 82 条
[61]   Use of sedimentological information for geometric simulation of natural porous media structure [J].
Scheibe, TD ;
Freyberg, DL .
WATER RESOURCES RESEARCH, 1995, 31 (12) :3259-3270
[62]  
SCHEIBE TD, 1993, THESIS STANFORD U PA
[63]   The importance of the third dimension on transport through saturated porous media: Case study based on transport of particles [J].
Silliman, SE .
JOURNAL OF HYDROLOGY, 1996, 179 (1-4) :181-195
[64]   STOCHASTIC-ANALYSIS OF PATHS OF HIGH HYDRAULIC CONDUCTIVITY IN POROUS-MEDIA [J].
SILLIMAN, SE ;
WRIGHT, AL .
WATER RESOURCES RESEARCH, 1988, 24 (11) :1901-1910
[65]  
SRIVASTAVA RM, AAPG COMPUT APPL GEO, V3, P3
[66]  
Stauffer D., 1991, INTRO PERCOLATION TH
[67]   Conditional simulation of complex geological structures using multiple-point statistics [J].
Strebelle, S .
MATHEMATICAL GEOLOGY, 2002, 34 (01) :1-21
[68]  
STREBELLE SB, 1999, SEQUENTIAL SIMULATIO
[69]   Flow channeling in heterogeneous fractured rocks [J].
Tsang, CF ;
Neretnieks, I .
REVIEWS OF GEOPHYSICS, 1998, 36 (02) :275-298
[70]   FLOW IN HETEROGENEOUS POROUS MEDIA [J].
WARREN, JE ;
PRICE, HS .
SOCIETY OF PETROLEUM ENGINEERS JOURNAL, 1961, 1 (03) :153-169