Abstract
Understanding of flow and transport in fractured media requires a good knowledge of fractures and fracture networks, which are privileged pathways for water and solutes. The Roselend underground laboratory (French Alps) gives the opportunity to fully investigate flow and solute transport through such a medium. Fracture traces and water fluxes have been determined along the Roselend tunnel.
The major objectives of this work are to derive a three dimensional fracture network consistent with the observations to calculate its percolation properties, and the macroscopic permeability of the medium.
In the tunnel, fractures can be classified into two families of large and small fractures. While large fractures intersect entirely the tunnel, small fractures partially intersect it. Variograms of both trace length and fracture orientation do not show any significant correlation with distance along the tunnel axis or with distance between fractures.
A stereological analysis of the trace length probability densities of the small fractures provides the fracture diameter probability density distribution which is best described by a power law. The large fractures are assumed monodisperse, with a radius equal to 5 m. Numerical simulations show that the networks obtained by combining large and small fractures do percolate while networks constituted of small fractures only do not percolate.
For three different sections along the gallery reflecting the major contrasts in dripping water fluxes, fracture networks are repeatedly generated according to the observed fracture densities. The permeability of these networks is systematically calculated. Results compare well to conductivity properties of similar media and show good consistency with observed water fluxes.
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References
Adler PM (1992) Porous media: Geometry and Transports. Butterworth-Heinemann, Boston
Balberg I, Anderson CH, Alexander S, Wagner N (1984) Excluded volume and its relation to the onset of percolation. Phys Rev B 30(7):3933–3943
Berkowitz B (1994) Modelling flow and contaminant transport in fractured media. Adv Porous Media 2:397–451
Berkowitz B, Adler PM (1998) Stereological analysis of fracture network structure in geological formations. J Geophys Res-Solid Earth 103(B7):15339–15360
Bogdanov II, Mourzenko VV, Thovert JF Adler PM (2003) Effective permeability of fractured porous media in steady state flow. Water Resour Res 39(1):1023 DOI: 10.1029/2001WR000756
Dezayes C, Villemin T (2002) Etat de la fracturation dans la galerie CEA de Roselend et analyse de la dèformation cassante dans le massif du Méraillet, Technical report CEA contract n 46 000 32745: Université de Savoie LGCA
Domenico PA, Schwartz FW (1998) Physical and chemical hydrology. John Wiley and sons, New York
Gonzalez-Garcia R, Huseby O, Thovert JF, Ledesert B, Adler PM (2000) Three-dimensional characterization of a fractured granite and transport properties. J Geophys Res 105(B9):21387–21401
Gudmundsson A, Berg SS, Lyslo KB Skurtveit E (2001) Fracture networks and fluid transport in active fault zones. J Struct Geol 23(2–3):343–353
Gupta AK, Adler PM (2006) Stereological analysis of fracture networks along cylindrical galleries. Math Geol 38(3) DOI: 10.1007/s11004-005-9018-4
Huseby O, Thovert JF Adler PM (1997) Geometry and topology of fracture systems. J Phys A-Math Gen 30(5):1415–1444
Johnston JD, McCaffrey KJW (1996) Fractal geometries of vein systems and the variation of scaling relationships with mechanism. J Struct Geol 18(2-3):349–358
Koudina N, Garcia RG, Thovert JF, Adler PM (1998) Permeability of three-dimensional fracture networks. Phys Rev E 57(4):4466–4479
Mauldon M, Mauldon JG (1997) Fracture sampling on a cylinder: From scanlines to boreholes and tunnels. Rock Mech Rock Eng 30(3): 129–144
Mourzenko VV, Thovert JF, Adler PM (2005) Percolation of three-dimensional fracture networks with power-law size distribution. Phys Rev E 72:036103 DOI: 10.1103/PhysRevE.72.036103
Peacock DCP, Harris SD, Mauldon M (2003) Use of curved scanlines and boreholes to predict fracture frequencies. J Struct Geol 25(1): 109–119
Piggott AR (1997) Fractal relations for the diameter and trace length of disc-shaped fractures. J Geophys Res-Solid Earth 102(B8): 18121–18125
Pili E, Perrier F, Richon P (2004) Dual porosity mechanism for transient groundwater and gas anomalies induced by external forcing. Earth Planet Sci Lett 227(3-4):473-480 DOI: 10.1016/j.epsl.2004.07.043
Provost A-S, Richon P, Pili E, Perrier F, Bureau S (2004) Fractured porous media under influence: the Roselend experiment. Eos Trans AGU 85:113
Sisavath S, Mourzenko V, Genthon P, Thovert JF, Adler PM (2004) Geometry, percolation and transport properties of fracture networks derived from line data. Geophys J Int 157(2):917–934 DOI: 10.1111/j.1365-246X.2004.02185.x
Thovert JF, Adler PM (2004) Trace analysis for fracture networks of any convex shape. Geophys Res Lett 31(22):L22502 DOI: 10.1029/2004GL021317
Thovert JF, Salles J, Adler PM (1993) Computerized characterization of the geometry of real porous-media - Their discretization, analysis and interpretation. J Microsc-Oxf 170: 65–79
Vermilye JM, Scholz CH (1995) Relation between vein length and aperture. J Struct Geol 17(3): 423–434
Walmann T, Malthe-Sorenssen A, Feder J, Jossang T, Meakin P, Hardy HH (1996) Scaling relations for the lengths and widths of fractures. Phys Rev Lett 77(27): 5393–5396
Warburton PM (1980a) A stereological interpretation of joint trace data. Int J Rock Mech Min Sci 17(4): 181–190
Warburton PM (1980b) Stereological interpretation of joint trace data - Influence of joint shape and implications for geological surveys. Int J Rock Mech Min Sci 17(6): 305–316
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Patriarche, D., Pili, E., Adler, P., Thovert, JF. (2008). Fracture Analysis and Flow Simulations in the Roselend Fractured Granite. In: Soares, A., Pereira, M.J., Dimitrakopoulos, R. (eds) geoENV VI – Geostatistics for Environmental Applications. Quantitative Geology and Geostatistics, vol 15. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-6448-7_15
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