Science – Society – Technology
Parameter | Lithologies | Borehole measurements | Input for 2-D models (this study) |
---|---|---|---|
Fracture centre location | All | No discerned clustering | Uniform distribution in each of X and Y directions |
Orientation | All | Dominant population: Dip magnitude: subvertical (82° ± 6°), dip direction to NW and SE Strike: NE-SW Minor population 1: dip magnitude 67° ± 12° and strike N-S Minor population 2: dip magnitude between 30 and 70° and varied strike | Dominant population: Dip magnitude: Normal distribution, mean = 90° (vertical) and standard deviation = 15° Strike: models are orientated NW–SE, i.e., perpendicular to the measured dominant fracture strike Minor populations: not modelled (see text for explanation) |
Linear density (P10, m−1) | Sheet-like andesite | 0.6 (n = 1405; Length of image = 2334 m) | 0.6 |
Pyroclastic rocks/ignimbrite | 0.8 (n = 648, Length of image = 807 m) | 0.8 | |
Rhyolite lava and breccia | 1.7 (n = 826; Length of image = 496 m) | 1.7 | |
Length (L, m) | All | Unknown | Doubly-truncated power law PDF: P(L) = A/Lλ A = (1/a – 1/b) with: a = 1, b = 100, λ = 2; a ≤ L ≤ b |
Geometric aperture (ag, m) | All | Power law PDF: P(ag) = A/agα, α = 2.6 | ag = L/1000 |
Volume of fractures and veins per volume of rock (P33, dimensionless) | All | 0.01–0.1 at thin section, core and acoustic image scales | 0.05 naturally results from choice of ag |
Hydraulic aperture (ah, m) | All | Unknown | ah = β L/1000 with: β = 0.002 |