PRINCIPAUX ENJEUX LIÉS AUX AQUIFÈRES DE SOCLE
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1 PRINCIPAUX ENJEUX LIÉS AUX AQUIFÈRES DE SOCLE John M. Sharp, Jr. Department of Geological Sciences Jackson School of Geosciences The University of Texas Austin, Texas, USA Uwe Troeger* Lehrstuhl fuer Hydrogeologie Technical University of Berlin Berlin, Deutschland * Chairman., IAH Network on Fractured Rock Hydrogeology
2 What is a hard-rock aquifer? Hard- rock aquifers occur primarily in fractured crystalline (igneous and metamorphic) rock systems and, in some cases, the overlying regolith. In hard-rock aquifers, fractures provide the major (or sole) permeability and, in many cases, the porosity and storativity.
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5 FRACTURES CONTROL BOTH FLOW AND TRANSPORT IN LOW PERMEABILITY MEDIA 1. Production of: Water (hard-rock aquifers) Oil and gas Geothermal energy (hot, dry rock) 2. Geotechnical/mining applications 3. Waste disposal (e.g., Sweden, Switzerland) 4. Many geological processes
6 In crystalline rocks, flow and transport is restricted to fractures.
7 WHAT AQUIFERS ARE FRACTURED MEDIA? All metamorphic rocks Almost all igneous rocks Possible exceptions: some unwelded tuffs; vesicular basalts and their flow tops Most sedimentary rocks Possible exceptions: coquinas; poorly cemented coarse sandstones Many unconsolidated deposits and soils Examples include: glacial tills, loess, and many soils Fracture-dominated flow and transport are more the rule than the exception!
8 1. Hard-rock systems cover much of the Earth s land surface. 2. Hard-rock aquifers are the only reliable water resource in many of these areas. 3. They underlie and interconnect shallower aquifers and sedimentary basins.
9 (U.S. Geological Survey, I-2781)
10 (U.S. Geological Survey, I-2781)
11 (U.S. Geological Survey, I-2781)
12
13 Krasny et al. (2014)
14 BLACK S LAW When dealing with fractured systems, we find that contaminants appear at places we don t expect and they appear faster than we had predicted. John Black, IAH - Oslo, 1993
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16 FRACTURE CHARACTERIZATION Sets Orientation (strike and dip, if planar) Spacing [L] or density [L -1 ] Aperture Roughness (asperities) Channeling Connectivity Skin properties
17 HYDROGEOLOGIC PARAMETERS Permeability (tensor) Porosity (scalar) Effective porosity (scalar or tensor) Skin properties Permeability Porosity Sorptivity Diffusion coefficient Note: These parameters may vary in space, over time, and with groundwater flow.
18 What is a fracture skin? Fracture skins are: zones of altered rock abutting a fracture surface and the coatings of the fracture surface by infiltered debris, precipitated minerals, and organic matter. Robinson and Sharp, 1997
19 Increased weathering occurs along fractures in granite because of a damage zone of microfractures and weathering processes.
20 The alteration zones are evident in this granite.
21 Skin Development in Elberton Granites Clay Infilling Core Softening (High Porosity) Chlorite Precipitation Garner, U.T. Ph.D., 2007
22 Importance? Flow and transport in many systems is fracture controlled. Skins may have a significant effect on: Rates of solute (including pollutant) transport. The length of time a fractured rock system will retain the solute. Black s Law
23 What does a fracture look like? Santana Tuff
24 Cue movie
25 Cardenas et al, 2008
26 What does a fracture look like? Particle Tracks for CC02-2
27 PERMEABILITY - Which aperture? Santana Tuff
28 CC02-2 Comparison of Means Flow data Aperture Geometric mean Harmonic mean Arithmetic mean (Sharp et al., 2014)
29 TRANSMISSIVITY Krasny et al. (2014)
30 VERTICAL ZONATION Upper / local (weathered) zone If present, the most productive zone Middle zone (regional) 10s -100s m k decreases with depth 100 m rule Lower (retarded flow) zone Flow in isolated fracture zones Sometimes surprisingly high
31 General vertical zonation (modified from Krasny et al., 2014, and Deere & Patton,1971) Note: See table in abstract.
32 Metamorphic rocks Plutonic rocks Deere & Patton (1971)
33 CHALLENGES How to characterize and parameterize these very inhomogeneous systems. Upscaling from lab-to-well field or from well field-to-regional scales. Finding appropriate data to validate or test numerical models of fracture system hydrogeology and transport of solutes, colloids, and heat.
34 QUESTION Is fractured rock hydrology so complex that there is little hope of making significant advances? Cliff Voss, 2003, Hydrogeology Journal, v. 11, p
35 Comment on Voss question More field, laboratory, and modeling studies are needed. New techniques are being developed. We need more data and case studies. Conferences like this one should point to promising new research directions and applications. There is definitely the potential to make significant advances.
36 Study Butte, Texas
37 Lands End, UK la fin!
38
39 sheeting joints, Missouri
40 GYPSUM-FILLED FRACTURES OPEN FRACTURES
41 Loess bluff Glasgow, Missouri
EVALUATION OF CRITICAL FRACTURE SKIN POROSITY FOR CONTAMINANT MIGRATION IN FRACTURED FORMATIONS
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