Articles | Volume 4, issue 2
https://doi.org/10.5194/gc-4-303-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gc-4-303-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Fracking bad language – hydraulic fracturing and earthquake risks
Jennifer J. Roberts
CORRESPONDING AUTHOR
Department of Civil and Environmental Engineering, James Weir Building, University of Strathclyde, 75 Montrose Street, Glasgow G1 1XJ, Scotland, UK
Clare E. Bond
Department of Geology and Petroleum Geology, School of Geosciences,
Meston Building, University of Aberdeen, Aberdeen AB24 3UE, Scotland, UK
Zoe K. Shipton
Department of Civil and Environmental Engineering, James Weir Building, University of Strathclyde, 75 Montrose Street, Glasgow G1 1XJ, Scotland, UK
Related authors
Billy J. Andrews, Jennifer J. Roberts, Zoe K. Shipton, Sabina Bigi, M. Chiara Tartarello, and Gareth Johnson
Solid Earth, 10, 487–516, https://doi.org/10.5194/se-10-487-2019, https://doi.org/10.5194/se-10-487-2019, 2019
Short summary
Short summary
Rocks often contain fracture networks, which can strongly affect subsurface fluid flow and the strength of a rock mass. Through fieldwork and workshops we show that people report a different number of fractures from the same sample area of a fracture network. This variability results in significant differences in derived fracture statistics, which are often used as inputs for geological models. We suggest protocols to recognise, understand, and limit this effect on fracture data collection.
Jackie E. Kendrick, Anthony Lamur, Julien Mouli-Castillo, Andrew P. Fraser-Harris, Alexander Lightbody, Katriona Edlmann, Christopher McDermott, and Zoe Shipton
Adv. Geosci., 62, 11–19, https://doi.org/10.5194/adgeo-62-11-2023, https://doi.org/10.5194/adgeo-62-11-2023, 2023
Short summary
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By testing the strength of granite in compression and tension at a range of deformation rates, we found that the strength increases with faster deformation. This observation highlights that at these rates, relevant for example to geothermal exploration, we have to consider how the rate of deformation impacts the energy released when rocks crack. The results are promising for developing safe procedures for extracting resources from the subsurface.
Adam J. Cawood, Hannah Watkins, Clare E. Bond, Marian J. Warren, and Mark A. Cooper
Solid Earth, 14, 1005–1030, https://doi.org/10.5194/se-14-1005-2023, https://doi.org/10.5194/se-14-1005-2023, 2023
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Here we test conceptual models of fracture development by investigating fractures across multiple scales. We find that most fractures increase in abundance towards the fold hinge, and we interpret these as being fold related. Other fractures at the site show inconsistent orientations and are unrelated to fold formation. Our results show that predicting fracture patterns requires the consideration of multiple geologic variables.
Clare E. Bond, Jessica H. Pugsley, Lauren Kedar, Sarah R. Ledingham, Marianna Z. Skupinska, Tomasz K. Gluzinski, and Megan L. Boath
Geosci. Commun., 5, 307–323, https://doi.org/10.5194/gc-5-307-2022, https://doi.org/10.5194/gc-5-307-2022, 2022
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Virtual field trips are used to engage students who are unable to go into the field with geological field work. Here, we investigate the perceptions of staff and students before and after a virtual field trip, including the investigation of the success of mitigation measures designed to decrease barriers to engagement and inclusion. We conclude that negative and positive perceptions exist and that effective mitigation measures can be used to improve the student experience.
Lauren Kedar, Clare E. Bond, and David K. Muirhead
Solid Earth, 13, 1495–1511, https://doi.org/10.5194/se-13-1495-2022, https://doi.org/10.5194/se-13-1495-2022, 2022
Short summary
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Raman spectroscopy of carbon-bearing rocks is often used to calculate peak temperatures and therefore burial history. However, strain is known to affect Raman spectral parameters. We investigate a series of deformed rocks that have been subjected to varying degrees of strain and find that there is a consistent change in some parameters in the most strained rocks, while other parameters are not affected by strain. We apply temperature calculations and find that strain affects them differently.
Alexander Schaaf, Miguel de la Varga, Florian Wellmann, and Clare E. Bond
Geosci. Model Dev., 14, 3899–3913, https://doi.org/10.5194/gmd-14-3899-2021, https://doi.org/10.5194/gmd-14-3899-2021, 2021
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Uncertainty is an inherent property of any model of the subsurface. We show how geological topology information – how different regions of rocks in the subsurface are connected – can be used to train uncertain geological models to reduce uncertainty. More widely, the method demonstrates the use of probabilistic machine learning (Bayesian inference) to train structural geological models on auxiliary geological knowledge that can be encoded in graph structures.
Clare E. Bond and Adam J. Cawood
Geosci. Commun., 4, 233–244, https://doi.org/10.5194/gc-4-233-2021, https://doi.org/10.5194/gc-4-233-2021, 2021
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Virtual outcrop models are increasingly used in geoscience teaching, but their efficacy as a training tool for 3D thinking has been little tested. We find that using a virtual outcrop increases the participants' ability to choose the correct geological block model. That virtual outcrops are viewed positively, but only in a blended learning environment and not as a replacement for fieldwork, and virtual outcrop use could improve equality, diversity and inclusivity in geoscience.
Billy James Andrews, Zoe Kai Shipton, Richard Lord, and Lucy McKay
Solid Earth, 11, 2119–2140, https://doi.org/10.5194/se-11-2119-2020, https://doi.org/10.5194/se-11-2119-2020, 2020
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Through geological mapping we find that fault zone internal structure depends on whether or not the fault cuts multiple lithologies, the presence of shale layers, and the orientation of joints and coal cleats at the time of faulting. During faulting, cementation of fractures (i.e. vein formation) is highest where the fractures are most connected. This leads to the counter-intuitive result that the highest-fracture-density part of the network often has the lowest open-fracture connectivity.
Lucía Pérez-Díaz, Juan Alcalde, and Clare E. Bond
Solid Earth, 11, 889–897, https://doi.org/10.5194/se-11-889-2020, https://doi.org/10.5194/se-11-889-2020, 2020
Juan Alcalde, Clare E. Bond, Gareth Johnson, Armelle Kloppenburg, Oriol Ferrer, Rebecca Bell, and Puy Ayarza
Solid Earth, 10, 1651–1662, https://doi.org/10.5194/se-10-1651-2019, https://doi.org/10.5194/se-10-1651-2019, 2019
Cristina G. Wilson, Clare E. Bond, and Thomas F. Shipley
Solid Earth, 10, 1469–1488, https://doi.org/10.5194/se-10-1469-2019, https://doi.org/10.5194/se-10-1469-2019, 2019
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In this paper, we outline the key insights from decision-making research about how, when faced with uncertainty, humans constrain decisions through the use of heuristics (rules of thumb), making them vulnerable to systematic and suboptimal decision biases. We also review existing strategies to debias decision-making that have applicability in the geosciences, giving special attention to strategies that make use of information technology and artificial intelligence.
Alexander Schaaf and Clare E. Bond
Solid Earth, 10, 1049–1061, https://doi.org/10.5194/se-10-1049-2019, https://doi.org/10.5194/se-10-1049-2019, 2019
Short summary
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Seismic reflection data allow us to infer subsurface structures such as horizon and fault surfaces. The interpretation of this indirect data source is inherently uncertainty, and our work takes a first look at the scope of uncertainties involved in the interpretation of 3-D seismic data. We show how uncertainties of fault interpretations can be related to data quality and discuss the implications for the 3-D modeling of subsurface structures derived from 3-D seismic data.
Johannes M. Miocic, Gareth Johnson, and Clare E. Bond
Solid Earth, 10, 951–967, https://doi.org/10.5194/se-10-951-2019, https://doi.org/10.5194/se-10-951-2019, 2019
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When carbon dioxide is introduced into the subsurface it will migrate upwards and can encounter faults, which, depending on their hydrogeological properties and composition, can form barriers or pathways for the migrating fluid. We analyse uncertainties associated with these properties in order to better understand the implications for the retention of CO2 in the subsurface. We show that faults that form seals for other fluids may not be seals for CO2, which has implications for storage sites.
Billy J. Andrews, Jennifer J. Roberts, Zoe K. Shipton, Sabina Bigi, M. Chiara Tartarello, and Gareth Johnson
Solid Earth, 10, 487–516, https://doi.org/10.5194/se-10-487-2019, https://doi.org/10.5194/se-10-487-2019, 2019
Short summary
Short summary
Rocks often contain fracture networks, which can strongly affect subsurface fluid flow and the strength of a rock mass. Through fieldwork and workshops we show that people report a different number of fractures from the same sample area of a fracture network. This variability results in significant differences in derived fracture statistics, which are often used as inputs for geological models. We suggest protocols to recognise, understand, and limit this effect on fracture data collection.
Related subject area
Subject: Geoscience policy | Keyword: Risk communication
Telling the boiling frog what he needs to know: why climate change risks should be plotted as probability over time
Simon Sharpe
Geosci. Commun., 2, 95–100, https://doi.org/10.5194/gc-2-95-2019, https://doi.org/10.5194/gc-2-95-2019, 2019
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Humanity's situation with respect to climate change is sometimes likened to that of a frog in a slow-boiling pot of water. But are we telling the frog what he needs to know? Most climate science is communicated to governments in the form of predictions of what is most likely to happen. I argue it should instead answer the following questions: what is the worst that could happen, and how likely will that become as time goes by? The risks and need to act will then become much clearer to see.
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Short summary
The potential for hydraulic fracturing (fracking) to induce seismicity is a topic of widespread interest. We find that terms used to describe induced seismicity are poorly defined and ambiguous and do not translate into everyday language. Such bad language has led to challenges in understanding, perceiving, and communicating risks around seismicity and fracking. Our findings and recommendations are relevant to other geoenergy topics that are potentially associated with induced seismicity.
The potential for hydraulic fracturing (fracking) to induce seismicity is a topic of widespread...
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