UCL Discovery Stage
UCL home » Library Services » Electronic resources » UCL Discovery Stage

Fluid‐driven tensile fracture and fracture toughness in Nash Point shale at elevated pressure

Gehne, S; Forbes Inskip, ND; Benson, PM; Meredith, PG; Koor, N; (2020) Fluid‐driven tensile fracture and fracture toughness in Nash Point shale at elevated pressure. Journal of Geophysical Research: Solid Earth , 125 (2) , Article e2019JB018971. 10.1029/2019jb018971. Green open access

[thumbnail of Gehne_et_al-2020-Journal_of_Geophysical_Research__Solid_Earth.pdf]
Preview
Text
Gehne_et_al-2020-Journal_of_Geophysical_Research__Solid_Earth.pdf - Published Version

Download (5MB) | Preview

Abstract

A number of key processes, both natural and anthropogenic, involve the fracture of rocks subjected to tensile stress, including vein growth and mineralization, and the extraction of hydrocarbons through hydraulic fracturing. In each case, the fundamental material property of mode‐I fracture toughness must be overcome in order for a tensile fracture to propagate. While measuring this parameter is relatively straightforward at ambient pressure, estimating fracture toughness of rocks at depth, where they experience confining pressure, is technically challenging. Here we report a new analysis that combines results from thick‐walled cylinder burst tests with quantitative acoustic emission to estimate the mode‐I fracture toughness (K_{Ic}) of Nash Point Shale at confining pressure simulating in situ conditions to approximately 1‐km depth. In the most favorable orientation, the pressure required to fracture the rock shell (injection pressure, P_{inj}) increases from 6.1 MPa at 2.2‐MPa confining pressure (P_{c}), to 34 MPa at 20‐MPa confining pressure. When fractures are forced to cross the shale bedding, the required injection pressures are 30.3 MPa (at P_{c} = 4.5MPa) and 58 MPa (P_{c} = 20 MPa), respectively. Applying the model of Abou‐Sayed et al. (1978, https://doi.org/10.1029/JB083iB06p02851) to estimate the initial flaw size, we calculate that this pressure increase equates to an increase in K_{Ic} from 0.36 to 4.05 MPa·m^{1/2} as differential fluid pressure (P_{inj} - P_{c}) increases from 3.2 to 22.0 MPa. We conclude that the increasing pressure due to depth in the Earth will have a significant influence on fracture toughness, which is also a function of the inherent anisotropy.

Type: Article
Title: Fluid‐driven tensile fracture and fracture toughness in Nash Point shale at elevated pressure
Open access status: An open access version is available from UCL Discovery
DOI: 10.1029/2019jb018971
Publisher version: https://doi.org/10.1029/2019JB018971
Language: English
Additional information: This version is the version of record. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Fracture Toughness, Shale, Tensile Fracture
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery-pp.ucl.ac.uk/id/eprint/10091525
Downloads since deposit
3,240Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item