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Table 1 Summary statistics from borehole images and input parameters for 2-D DFNs

From: Modelling of flow through naturally fractured geothermal reservoirs, Taupō Volcanic Zone, New Zealand

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

  1. Measurements on borehole images from Massiot et al. (2017a).