EPSRC grant EP/L012227/1: Development of Unified Experimental and Theoretical Approach to Predict Reactive Transport in Subsurface Porous Media. The effect of pore-scale heterogeneity on non-Darcy flow behaviour is investigated by means of direct flow simulations on 3-D images of Estaillades carbonate. The critical Reynolds number indicating the cessation of the creeping Darcy flow regime in Estaillades carbonate is two orders of magnitude smaller than in Bentheimer sandstone, and is three orders of magnitude smaller than in the beadpack. It is inferred from the examination of flow field features that the emergence of steady eddies in pore space of Estaillades at elevated fluid velocities accounts for the early transition away from the Darcy flow regime. Also available at https://www.digitalrocksportal.org/projects/10, DOI:10.17612/P73W2C. Further details can be found in Muljadi et al., Advances in Water Resources (2015), URL:http://dx.doi.org/10.1016/j.advwatres.2015.05.019.

This data repository contains the raw waveforms of seven hydraulic fracturing-induced seismic events, together with their rupture directivity analysis. The entire data is consolidated in one .mat file per seismic event (which can be read with Matlab and Octave). A detailed description of the .mat files, and a Matlab script to import and visualise the seismic data and rupture directivity analysis of each event, is also included in this repository. The passive seismic dataset was collected in a shale gas field near Fox Creek, Alberta, Canada, during a multi-stage hydraulic fracturing stimulation that induced shallow earthquakes (less than 5 km deep) of magnitudes up to 3.2. This area has experienced in recent years multiple cases on induced seismicity associated with oil and gas operations, including hydraulic fracturing and wastewater disposal, of magnitudes above 4.0 in some cases. The full passive seismic dataset was collected between October and November 2016 and made open source through a GitHub repository (https://github.com/ToC2ME). To determine the rupture directivity of each induced seismic event, we use the Empirical Green's Functions (EGF) method to first obtain apparent source time functions (ASTF), and then measure the rupture time at each seismic station. We then invert the rupture directivity of each seismic event based on the azimuthal variation of the measured rupture times at each seismic station. Observations of rupture directivity (the direction of propagation of the earthquake rupture) can provide important information as to the nature of the interactions between injection-induced pressure increases and earthquake nucleation. Measurement of rupture directivity could therefore have important implications for induced seismicity hazard management. The rupture directivity analysis of these hydraulic fracturing-induced seismic events was led and coordinated by Dr. James Verdon and Dr. Germán Rodríguez at the School of Earth Sciences, University of Bristol.

This dataset contains earthquake catalogs from induced seismicity cases in western Texas and northern Oklahoma/Kansas, and the results of earthquake magnitude forecasting methods (using Extreme Value Theory) applied to these datasets (Verdon and Eisner, 2024). The catalogs archived here were curated from regional earthquake datasets: for Oklahoma/Kansas the original data source was Park et al. (2022, DOI 10.1785/0320220020) and for Texas the original source was TexNet (https://catalog.texnet.beg.utexas.edu). Verdon and Eisner (2024) curated subsets of this data (drawn from within 20 x 20 km2 "blocks") in order to apply and test their forecasting methods on localised event catalogs. In this dataset we provide the localised catalogs, and the results of the forecasting models (tracking forecasted earthquake magnitudes over time in comparison with the observed evolution of events). The input data and forecasting results are provided in Matlab format structures (.mat). Matlab scripts and functions (.m files) are also provided to read the data and perform the analyses that are presented in Verdon and Eisner (2024). A README text file is provided that details the content of the Matlab structures. Reference: Verdon, J.P., and L. Eisner, 2024. An empirically constrained forecasting strategy for induced earthquake magnitudes using extreme value theory: Seismological Research Letters 95, 3278-3294. DOI: 10.1785/0220240061

This dataset includes raw point cloud and gridded data from repeat terrestrial laser scans (TLS) for measuring barchans and protodunes in the Huab Dune Field, Huab River Valley, Skeleton Coast, Namibia. As well as the TLS data, additional measurements include wind speed, wind direction and sediment transport for some of the measurement period.

Data recorded during triaxial rock deformation experiments of Westerly granite in the presence of pressurised pore fluids (water). Data consists of mechanical data (load, displacement, confining pressure) and pore pressure data (up- and downstream pore pressure, upstream intensifier volume, four pore pressure transducers mounted on sample) for two experiments, recorded at low and high acquisition frequencies. Also contains .h5 files with all ultrasonic waveforms (active surveys and acoustic emissions). Dataset complementary to dataset ID165485 . Contains all data necessary to evaluate the results presented in the paper entitled: 'Rupture and afterslip controlled by spontaneous local fluid flow in crustal rock' by Aben and Brantut, submitted to Geophysical Research Letters, and available at arXiv (arXiv:).

Grant: NE/N016173/1.The data presented herein comprises raw and segmented X-Ray micro-CT data, CMG simulation files and Matlab processing files for the paper 'Representative elementary volumes, hysteresis and heterogeneity in multiphase flow from the pore to continuum scale'. The data is organised as Core 1 and Core 2 respectively. Full core scans are obtained at a resolution of 6 microns. Region of interest (ROI) scans are obtained at 3.45 micron and 2 micon (core 1) and 3.5 micron (core 2). Resolution information is contained within the file names. Voxel sizes in the image files can be changed to match these values. Experimental post-processing files contain the upscaled saturations and porosity values in 3D, which are used in the paper. It also contains the pore-filling analysis. The CMG simulation files contain the input deck, 3D digitial core information (porosity, capillary pressure) needed to simulate both the drainage and imbibition core floods, with corresponding Matlab analysis files. These are Bentheimer outcrop cores obtained from Shell, Amsterdam. It is a shallow marine rock, deposited during the Lower Cretaceous. It outcrops between Enschede and Schoonenbeek in the Netherlands.

The data are nanoindentation, high-angular resolution electron backscatter diffraction (HR-EBSD), and transmission electron microscopy data collected on samples of synthetic forsterite bicrystals at room temperature. The data were collected in two samples, with high- and low- angle grain boundaries (HAGB, 60°, [100]/(011) and SB, 13°, [100]/(016)). The EBSD data are the basis for the HR-EBSD calculation. The HR-EBSD results are presented as Matlab data files. The nanoindentation data are categorised as a function of sample (‘ol13’ – low-angle grain boundary; and ‘ol60’ – high-angle grain boundary), and indenter tip geometry (spherical (with a 10 or 5 micron radius) and pyramidal (Berkovich). The data are presented in .xls files. The TEM data are presented as .tif files. The TEM data were collected in specific indents with various distances from the interfaces. These data have been published in the manuscript: : The Role of Grain Boundaries in Low-Temperature Plasticity of Olivine Revealed by Nanoindentation, with the DOI: 10.1029/2023JB026763

Supporting data for the paper 'Small-scale capillary heterogeneity linked to rapid plume migration during CO2 storage'. We supply experimental, analytical and numerical simulation data used in the paper. The supplied zipped folders follow the same order as the main paper, with codes to reproduce each figure (and those in the supporting information PDF). There are also video files (in the 5_Field_scale_simulation zipped folder) showing the final CO2 plume evolution from the static images in the main paper Figure 4. Descriptions of each of the folders are given below: 0 - README. This contains detailed instructions on the data and using the supplied files. 1 - Scaling analysis. This contains the scaling analysis analytical methods, with figure generation for Figure 1 in the main paper. 2 - Petrophysics. This contains all the petrophysical experimental data, analysis files and core flood simulation files. This is used to produce Figure 2 in the main paper. 3 - Fine_resolution_simulations. This contains the simulation files, Matlab post processing files and figure generation for the fine resolution simulations, presented in Figure 3 in the main paper. 4 - MIP_upscaling. This contains simulations files, Matlab post processing files and figure generation for the macroscopic invasion percolation scheme. The results of this are presented in the supporting information document. 5 - Field_scale_simulation. This contains the simulations files, Matlab post processing files and figure generation for the final field scale simulations in the main manuscript Figure 4 and in the supporting information. In each folder are separate READMEs containing specific information relevant for the included files.