Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-1-2021
© 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/se-12-1-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Jan 2021
Research article |
| 11 Jan 2021
| 11 Jan 2021
Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam scanning electron microscopy imaging
Arne Jacob
CORRESPONDING AUTHOR
Geosciences Institute, Johannes Gutenberg-University, J.-J. Becherweg
21, 55099 Mainz, Germany
Markus Peltz
Institute of Geography and Geology, University Greifswald,
Friedrich-Ludwig-Jahn-Str. 17a, 17487 Greifswald, Germany
Sina Hale
Institute of Applied Geosciences (AGW), Karlsruhe Institute of
Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, Germany
Frieder Enzmann
Geosciences Institute, Johannes Gutenberg-University, J.-J. Becherweg
21, 55099 Mainz, Germany
Olga Moravcova
Geosciences Institute, Johannes Gutenberg-University, J.-J. Becherweg
21, 55099 Mainz, Germany
Laurence N. Warr
Institute of Geography and Geology, University Greifswald,
Friedrich-Ludwig-Jahn-Str. 17a, 17487 Greifswald, Germany
Georg Grathoff
Institute of Geography and Geology, University Greifswald,
Friedrich-Ludwig-Jahn-Str. 17a, 17487 Greifswald, Germany
Philipp Blum
Institute of Applied Geosciences (AGW), Karlsruhe Institute of
Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, Germany
Michael Kersten
Geosciences Institute, Johannes Gutenberg-University, J.-J. Becherweg
21, 55099 Mainz, Germany
Related authors
No articles found.
Fabien Koch, Philipp Blum, Heide Stein, Andreas Fuchs, Hans Jürgen Hahn, and Kathrin Menberg
Hydrol. Earth Syst. Sci., 28, 4927–4946, https://doi.org/10.5194/hess-28-4927-2024, https://doi.org/10.5194/hess-28-4927-2024, 2024
Short summary
Short summary
In this study, we identify shifts in groundwater fauna due to natural or human impacts over 2 decades. We find no overall temporal or large-scale trends in fauna or abiotic parameters. However, at a local level, six monitoring wells show shifting or fluctuating faunal parameters. Our findings indicate that changes in surface conditions should be assessed in line with hydrochemical parameters to better understand changes in groundwater fauna and to obtain reliable biomonitoring results.
Haegyeong Lee, Manuel Gossler, Kai Zosseder, Philipp Blum, Peter Bayer, and Gabriel C. Rau
EGUsphere, https://doi.org/10.5194/egusphere-2024-1949, https://doi.org/10.5194/egusphere-2024-1949, 2024
Short summary
Short summary
A systematic laboratory experiment elucidates two-phase heat transport due to water flow in saturated porous media to understand thermal propagation in aquifers. Results reveal delayed thermal arrival in the solid phase, depending on grain size and flow velocity. Analytical modeling using standard local thermal equilibrium (LTE) and advanced local thermal non-equilibrium (LTNE) theory fails to describe temperature breakthrough curves, highlighting the need for more advanced numerical approaches.
Marco Fuchs, Anna Suzuki, Togo Hasumi, and Philipp Blum
Solid Earth, 15, 353–365, https://doi.org/10.5194/se-15-353-2024, https://doi.org/10.5194/se-15-353-2024, 2024
Short summary
Short summary
In this study, the permeability of a natural fracture in sandstone is estimated based only on its geometry. For this purpose, the topological method of persistent homology is applied to three geometric data sets with different resolutions for the first time. The results of all data sets compare well with conventional experimental and numerical methods. Since the analysis takes less time to the same amount of time, it seems to be a good alternative to conventional methods.
Christopher J. L. Wilson, Mark Peternell, Filomena Salvemini, Vladimir Luzin, Frieder Enzmann, Olga Moravcova, and Nicholas J. R. Hunter
The Cryosphere, 18, 819–836, https://doi.org/10.5194/tc-18-819-2024, https://doi.org/10.5194/tc-18-819-2024, 2024
Short summary
Short summary
As the temperature increases within a deforming ice aggregate, composed of deuterium (D2O) ice and water (H2O) ice, a set of meltwater segregations are produced. These are composed of H2O and HDO and are located in conjugate shear bands and in compaction bands which accommodate the deformation and weaken the ice aggregate. This has major implications for the passage of meltwater in ice sheets and the formation of the layering recognized in glaciers.
Jose M. Bastias Espejo, Chris Turnadge, Russell S. Crosbie, Philipp Blum, and Gabriel C. Rau
Hydrol. Earth Syst. Sci., 27, 3447–3462, https://doi.org/10.5194/hess-27-3447-2023, https://doi.org/10.5194/hess-27-3447-2023, 2023
Short summary
Short summary
Analytical models estimate subsurface properties from subsurface–tidal load interactions. However, they have limited accuracy in representing subsurface physics and parameter estimation. We derived a new analytical solution which models flow to wells due to atmospheric tides. We applied it to field data and compared our findings with subsurface knowledge. Our results enhance understanding of subsurface systems, providing valuable information on their behavior.
Ruben Stemmle, Haegyeong Lee, Philipp Blum, and Kathrin Menberg
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2023-62, https://doi.org/10.5194/hess-2023-62, 2023
Revised manuscript not accepted
Short summary
Short summary
Using 3D numerical heat transpot models, this study quantifies the potential of low-temperature Aquifer Thermal Energy Storage (ATES) in an urban setting in Southwest Germany. Comparing the determined potential with existing heating and cooling demands shows substantial heating and cooling supply rates that could be achieved by a widespread application of ATES systems. The study also highlights possible greenhouse gas emission savings compared to conventional heating and cooling technologies.
José M. Bastías Espejo, Andy Wilkins, Gabriel C. Rau, and Philipp Blum
Geosci. Model Dev., 14, 6257–6272, https://doi.org/10.5194/gmd-14-6257-2021, https://doi.org/10.5194/gmd-14-6257-2021, 2021
Short summary
Short summary
The hydraulic and mechanical properties of the subsurface are inherently heterogeneous. RHEA is a simulator that can perform couple hydro-geomechanical processes in heterogeneous porous media with steep gradients. RHEA is able to fully integrate spatial heterogeneity, allowing allocation of distributed hydraulic and geomechanical properties at mesh element level. RHEA is a valuable tool that can simulate problems considering realistic heterogeneity inherent to geologic formations.
Sina Hale, Xavier Ries, David Jaeggi, and Philipp Blum
Solid Earth, 12, 1581–1600, https://doi.org/10.5194/se-12-1581-2021, https://doi.org/10.5194/se-12-1581-2021, 2021
Short summary
Short summary
The construction of tunnels leads to substantial alterations of the surrounding rock, which can be critical concerning safety aspects. We use different mobile methods to assess the hydromechanical properties of an excavation damaged zone (EDZ) in a claystone. We show that long-term exposure and dehydration preserve a notable fracture permeability and significantly increase strength and stiffness. The methods are suitable for on-site monitoring without any further disturbance of the rock.
Fabien Koch, Kathrin Menberg, Svenja Schweikert, Cornelia Spengler, Hans Jürgen Hahn, and Philipp Blum
Hydrol. Earth Syst. Sci., 25, 3053–3070, https://doi.org/10.5194/hess-25-3053-2021, https://doi.org/10.5194/hess-25-3053-2021, 2021
Short summary
Short summary
In this study, we address the question of whether groundwater fauna in an urban area is natural or affected in comparison to forested land. We find noticeable differences in the spatial distribution of groundwater species and abiotic parameters. An ecological assessment reveals that conditions in the urban area are mainly not good. Yet, there is no clear spatial pattern in terms of land use and anthropogenic impacts. These are significant findings for conservation and usage of urban groundwater.
Gabriel C. Rau, Mark O. Cuthbert, R. Ian Acworth, and Philipp Blum
Hydrol. Earth Syst. Sci., 24, 6033–6046, https://doi.org/10.5194/hess-24-6033-2020, https://doi.org/10.5194/hess-24-6033-2020, 2020
Short summary
Short summary
This work provides an important generalisation of a previously developed method that quantifies subsurface barometric efficiency using the groundwater level response to Earth and atmospheric tides. The new approach additionally allows the quantification of hydraulic conductivity and specific storage. This enables improved and rapid assessment of subsurface processes and properties using standard pressure measurements.
Chaojie Cheng, Sina Hale, Harald Milsch, and Philipp Blum
Solid Earth, 11, 2411–2423, https://doi.org/10.5194/se-11-2411-2020, https://doi.org/10.5194/se-11-2411-2020, 2020
Short summary
Short summary
Fluids (like water or gases) within the Earth's crust often flow and interact with rock through fractures. The efficiency with which these fluids may flow through this void space is controlled by the width of the fracture(s). In this study, three different physical methods to measure fracture width were applied and compared and their predictive accuracy was evaluated. As a result, the mobile methods tested may well be applied in the field if a number of limitations and requirements are observed.
Swarup Chauhan, Kathleen Sell, Wolfram Rühaak, Thorsten Wille, and Ingo Sass
Geosci. Model Dev., 13, 315–334, https://doi.org/10.5194/gmd-13-315-2020, https://doi.org/10.5194/gmd-13-315-2020, 2020
Short summary
Short summary
We present CobWeb 1.0, a graphical user interface for analysing tomographic images of geomaterials. CobWeb offers different machine learning techniques for accurate multiphase image segmentation and visualizing material specific parameters such as pore size distribution, relative porosity and volume fraction. We demonstrate a novel approach of dual filtration and dual segmentation to eliminate edge enhancement artefact in synchrotron-tomographic datasets and provide the computational code.
Gabriel C. Rau, Vincent E. A. Post, Margaret Shanafield, Torsten Krekeler, Eddie W. Banks, and Philipp Blum
Hydrol. Earth Syst. Sci., 23, 3603–3629, https://doi.org/10.5194/hess-23-3603-2019, https://doi.org/10.5194/hess-23-3603-2019, 2019
Short summary
Short summary
The flow of water is often inferred from water levels and gradients whose measurements are considered trivial despite the many steps and complexity of the instruments involved. We systematically review the four measurement steps required and summarise the systematic errors. To determine the accuracy with which flow can be resolved, we quantify and propagate the random errors. Our results illustrate the limitations of current practice and provide concise recommendations to improve data quality.
Susanne A. Benz, Peter Bayer, Gerfried Winkler, and Philipp Blum
Hydrol. Earth Syst. Sci., 22, 3143–3154, https://doi.org/10.5194/hess-22-3143-2018, https://doi.org/10.5194/hess-22-3143-2018, 2018
Short summary
Short summary
Climate change is one of the most pressing challenges modern society faces. Increasing temperatures are observed both above ground and, as discussed here, in the groundwater – the source of most drinking water. Within Austria average temperature increased by 0.7 °C over the past 20 years, with an increase of more than 3 °C in some wells and temperature decrease in others. However, these extreme changes can be linked to local events such as the construction of a new drinking water supply.
Kathleen Sell, Beatriz Quintal, Michael Kersten, and Erik H. Saenger
Solid Earth, 9, 699–711, https://doi.org/10.5194/se-9-699-2018, https://doi.org/10.5194/se-9-699-2018, 2018
Short summary
Short summary
Sediments containing hydrates dispersed in the pore space show a characteristic seismic anomaly: a high attenuation along with increasing seismic velocities. Recent major findings from synchrotron experiments revealed the systematic presence of thin water films between quartz and gas hydrate. Our numerical studies support earlier speculation that squirt flow causes high attenuation at seismic frequencies but are based on a conceptual model different to those previously considered.
Daniel Schweizer, Philipp Blum, and Christoph Butscher
Solid Earth, 8, 515–530, https://doi.org/10.5194/se-8-515-2017, https://doi.org/10.5194/se-8-515-2017, 2017
Short summary
Short summary
Any 3-D geological model is subject to uncertainty. We applied the concept of information entropy in order to visualize and quantify changes in uncertainty between geological models based on different types of geological input data. Furthermore, we propose two measures, the city-block and the Jaccard distance, to directly compare dissimilarities between models. The presented approach helps to locate areas of uncertainty within the model domain and quantify model improvements due to added data.
Kathleen Sell, Erik H. Saenger, Andrzej Falenty, Marwen Chaouachi, David Haberthür, Frieder Enzmann, Werner F. Kuhs, and Michael Kersten
Solid Earth, 7, 1243–1258, https://doi.org/10.5194/se-7-1243-2016, https://doi.org/10.5194/se-7-1243-2016, 2016
Georg H. Grathoff, Markus Peltz, Frieder Enzmann, and Stephan Kaufhold
Solid Earth, 7, 1145–1156, https://doi.org/10.5194/se-7-1145-2016, https://doi.org/10.5194/se-7-1145-2016, 2016
Short summary
Short summary
This study improves our understanding of the evolution of pores in shales for modelling transport properties. 3-D microscopy on early and postmature Posidonia Shales showed similar porosities and pore size distributions. Large isolated pore clusters are within carbonates and clay minerals. Pores form during maturation in the postmature-matrix-filling organic matter. Modelled permeabilities are lowest perpendicular to bedding. They decrease with increasing maturity and are comparable to experimental data.
Tobias Kling, Da Huo, Jens-Oliver Schwarz, Frieder Enzmann, Sally Benson, and Philipp Blum
Solid Earth, 7, 1109–1124, https://doi.org/10.5194/se-7-1109-2016, https://doi.org/10.5194/se-7-1109-2016, 2016
Short summary
Short summary
A method is introduced to implement medical CT data of a fractured sandstone under varying confining pressures into fluid flow simulations to reproduce experimental permeabilities. The simulation results reproduce plausible fracture flow features (e.g. flow channeling, fracture closing/opening) and approximate the actual permeabilities, which are affected by the CT resolution and compositional matrix heterogeneities. Additionally, some recommendations are presented concerning future studies.
Steven Henkel, Dieter Pudlo, Frieder Enzmann, Viktor Reitenbach, Daniel Albrecht, Leonhard Ganzer, and Reinhard Gaupp
Solid Earth, 7, 917–927, https://doi.org/10.5194/se-7-917-2016, https://doi.org/10.5194/se-7-917-2016, 2016
Short summary
Short summary
This study investigates the experimentally induced effects of CO2 storage on underground reservoir sandstones by applying high-resolution computer tomography and standard petrophysical methods. The results of digital rock physic calculations derived from the µ-CT scans are compared with measurements achieved by the standard methods. Both approaches lead to similar results for coarse- and medium-grained sandstones but differ for fine-grained sediments.
Faisal Khan, Frieder Enzmann, and Michael Kersten
Solid Earth, 7, 481–492, https://doi.org/10.5194/se-7-481-2016, https://doi.org/10.5194/se-7-481-2016, 2016
Short summary
Short summary
X-ray microtomography image processing involves artefact reduction and image segmentation. The beam-hardening artefact is removed, applying a new algorithm, which minimizes the offsets of the attenuation data points. For the segmentation, we propose using a non-linear classifier algorithm. Statistical analysis was performed to quantify the improvement in multi-phase classification of rock cores using and without using our advanced beam-hardening correction algorithm.
M. Huebsch, F. Grimmeisen, M. Zemann, O. Fenton, K. G. Richards, P. Jordan, A. Sawarieh, P. Blum, and N. Goldscheider
Hydrol. Earth Syst. Sci., 19, 1589–1598, https://doi.org/10.5194/hess-19-1589-2015, https://doi.org/10.5194/hess-19-1589-2015, 2015
Short summary
Short summary
Two different in situ spectrophotometers, which were used in the field to determine highly time resolved nitrate-nitrogen (NO3-N) concentrations at two distinct spring discharge sites, are compared: a double and a multiple wavelength spectrophotometer. The objective of the study was to review the hardware options, determine ease of calibration, accuracy, influence of additional substances and to assess positive and negative aspects of the two sensors as well as troubleshooting and trade-offs.
K. Menberg, P. Blum, B. L. Kurylyk, and P. Bayer
Hydrol. Earth Syst. Sci., 18, 4453–4466, https://doi.org/10.5194/hess-18-4453-2014, https://doi.org/10.5194/hess-18-4453-2014, 2014
M. Huebsch, O. Fenton, B. Horan, D. Hennessy, K. G. Richards, P. Jordan, N. Goldscheider, C. Butscher, and P. Blum
Hydrol. Earth Syst. Sci., 18, 4423–4435, https://doi.org/10.5194/hess-18-4423-2014, https://doi.org/10.5194/hess-18-4423-2014, 2014
Related subject area
Subject area: The evolving Earth surface | Editorial team: Stratigraphy, sedimentology, geomorphology, morphotectonics, and palaeontology | Discipline: Sedimentology
What does it take to restore geological models with “natural” boundary conditions?
Impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, the Dolomites, northern Italy)
The influence of extraction of various solvents on chemical properties on Chang 7 shale, Ordos Basin, China
Deep vs. shallow – two contrasting theories? A tectonically activated Late Cretaceous deltaic system in the axial part of the Mid-Polish Trough: a case study from southeast Poland
Miocene high elevation in the Central Alps
What makes seep carbonates ignore self-sealing and grow vertically: the role of burrowing decapod crustaceans
Dawn and dusk of Late Cretaceous basin inversion in central Europe
Birth and closure of the Kallipetra Basin: Late Cretaceous reworking of the Jurassic Pelagonian–Axios/Vardar contact (northern Greece)
Sediment history mirrors Pleistocene aridification in the Gobi Desert (Ejina Basin, NW China)
Tectonic processes, variations in sediment flux, and eustatic sea level recorded by the 20 Myr old Burdigalian transgression in the Swiss Molasse basin
Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits
Can anaerobic oxidation of methane prevent seafloor gas escape in a warming climate?
Precipitation of dolomite from seawater on a Carnian coastal plain (Dolomites, northern Italy): evidence from carbonate petrography and Sr isotopes
The Ogooue Fan (offshore Gabon): a modern example of deep-sea fan on a complex slope profile
Formation of linear planform chimneys controlled by preferential hydrocarbon leakage and anisotropic stresses in faulted fine-grained sediments, offshore Angola
From oil field to geothermal reservoir: assessment for geothermal utilization of two regionally extensive Devonian carbonate aquifers in Alberta, Canada
Sedimentary mechanisms of a modern banded iron formation on Milos Island, Greece
Melchior Schuh-Senlis, Guillaume Caumon, and Paul Cupillard
Solid Earth, 15, 945–964, https://doi.org/10.5194/se-15-945-2024, https://doi.org/10.5194/se-15-945-2024, 2024
Short summary
Short summary
This paper presents the application of a numerical method for restoring models of the subsurface to a previous state in their deformation history, acting as a numerical time machine for geological structures. The method is applied to a model based on a laboratory experiment. The results show that using force conditions in the computation of the deformation allows us to assess the value of some previously unknown physical parameters of the different materials inside the model.
Onyedika Anthony Igbokwe, Jithender J. Timothy, Ashwani Kumar, Xiao Yan, Mathias Mueller, Alessandro Verdecchia, Günther Meschke, and Adrian Immenhauser
Solid Earth, 15, 763–787, https://doi.org/10.5194/se-15-763-2024, https://doi.org/10.5194/se-15-763-2024, 2024
Short summary
Short summary
We present a workflow that models the impact of stress regime change on the permeability of fractured Latemar carbonate buildup using a displacement-based linear elastic finite-element method (FEM) and outcrop data. Stress-dependent heterogeneous apertures and effective permeability were calculated and constrained by the study area's stress directions. Simulated far-field stresses at NW–SE subsidence deformation and N–S Alpine deformation increased the overall fracture aperture and permeability.
Yan Cao, Zhijun Jin, Rukai Zhu, and Kouqi Liu
Solid Earth, 14, 1169–1179, https://doi.org/10.5194/se-14-1169-2023, https://doi.org/10.5194/se-14-1169-2023, 2023
Short summary
Short summary
Fourier transform infrared (FTIR) was performed on shale before and after solvent extraction. The extraction yield from shale with THF is higher than other solvents. The organic-C-normalized yield of a mature sample is higher than other samples. The aromaticity of organic matter increases, and the length of organic matter aliphatic chains does not vary monotonically with increasing maturity. The results will help in the selection of organic solvents for oil-washing experiments of shale.
Zbyszek Remin, Michał Cyglicki, and Mariusz Niechwedowicz
Solid Earth, 13, 681–703, https://doi.org/10.5194/se-13-681-2022, https://doi.org/10.5194/se-13-681-2022, 2022
Short summary
Short summary
Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted as the deepest and most subsiding part of the basin during the Cretaceous times. We interpret this area conversely, as representing a landmass – the Łysogóry–Dobrogea Land. Inversion-related tectonics, uplift on the one hand and enhanced subsidence on the other, drove the development of the Szozdy Delta within the axial part of the basin. New heavy mineral data suggest different burial histories.
Emilija Krsnik, Katharina Methner, Marion Campani, Svetlana Botsyun, Sebastian G. Mutz, Todd A. Ehlers, Oliver Kempf, Jens Fiebig, Fritz Schlunegger, and Andreas Mulch
Solid Earth, 12, 2615–2631, https://doi.org/10.5194/se-12-2615-2021, https://doi.org/10.5194/se-12-2615-2021, 2021
Short summary
Short summary
Here we present new surface elevation constraints for the middle Miocene Central Alps based on stable and clumped isotope geochemical analyses. Our reconstructed paleoelevation estimate is supported by isotope-enabled paleoclimate simulations and indicates that the Miocene Central Alps were characterized by a heterogeneous and spatially transient topography with high elevations locally exceeding 4000 m.
Jean-Philippe Blouet, Patrice Imbert, Sutieng Ho, Andreas Wetzel, and Anneleen Foubert
Solid Earth, 12, 2439–2466, https://doi.org/10.5194/se-12-2439-2021, https://doi.org/10.5194/se-12-2439-2021, 2021
Short summary
Short summary
Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine sediments. Seep carbonates may act as seals and force lateral deviations of rising hydrocarbons. However, crustacean burrows may act as efficient vertical fluid channels allowing hydrocarbons to pass through upward, thereby allowing the vertical growth of carbonate stacks over time. This mechanism may explain the origin of carbonate columns in marine sediments throughout hydrocarbon provinces worldwide.
Thomas Voigt, Jonas Kley, and Silke Voigt
Solid Earth, 12, 1443–1471, https://doi.org/10.5194/se-12-1443-2021, https://doi.org/10.5194/se-12-1443-2021, 2021
Short summary
Short summary
Basin inversion in central Europe is believed to have started during Late Cretaceous (middle Turonian) and probably proceeded until the Paleogene. Data from different marginal troughs in central Europe point to an earlier start of basin inversion (in the Cenomanian). The end of inversion is overprinted by general uplift but had probably already occurred in the late Campanian to Maastrichtian. Both the start and end of inversion occurred with low rates of uplift and subsidence.
Lydia R. Bailey, Filippo L. Schenker, Maria Giuditta Fellin, Miriam Cobianchi, Thierry Adatte, and Vincenzo Picotti
Solid Earth, 11, 2463–2485, https://doi.org/10.5194/se-11-2463-2020, https://doi.org/10.5194/se-11-2463-2020, 2020
Short summary
Short summary
The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
Georg Schwamborn, Kai Hartmann, Bernd Wünnemann, Wolfgang Rösler, Annette Wefer-Roehl, Jörg Pross, Marlen Schlöffel, Franziska Kobe, Pavel E. Tarasov, Melissa A. Berke, and Bernhard Diekmann
Solid Earth, 11, 1375–1398, https://doi.org/10.5194/se-11-1375-2020, https://doi.org/10.5194/se-11-1375-2020, 2020
Short summary
Short summary
We use a sediment core from the Gobi Desert (Ejina Basin, NW China) to illustrate the landscape history of the area. During 2.5 million years a sediment package of 223 m thickness has been accumulated. Various sediment types document that the area turned from a playa environment (shallow water environment with multiple flooding events) to an alluvial–fluvial environment after the arrival of the Heihe in the area. The river has been diverted due to tectonics.
Philippos Garefalakis and Fritz Schlunegger
Solid Earth, 10, 2045–2072, https://doi.org/10.5194/se-10-2045-2019, https://doi.org/10.5194/se-10-2045-2019, 2019
Short summary
Short summary
The controls on the 20 Myr old Burdigalian transgression in the Swiss Molasse basin have been related to a reduction in sediment flux, a rise in global sea level, or tectonic processes in the adjacent Alps. Here, we readdress this problem and extract stratigraphic signals from the Upper Marine Molasse deposits in Switzerland. In conclusion, we consider rollback tectonics to be the main driving force controlling the transgression, which is related to a deepening and widening of the basin.
Laura Stutenbecker, Peter M. E. Tollan, Andrea Madella, and Pierre Lanari
Solid Earth, 10, 1581–1595, https://doi.org/10.5194/se-10-1581-2019, https://doi.org/10.5194/se-10-1581-2019, 2019
Short summary
Short summary
The Aar and Mont Blanc regions in the Alps are large granitoid massifs characterized by high topography. We analyse when these granitoids were first exhumed to the surface. We test this by tracking specific garnet grains, which are exclusively found in the granitoid massifs, in the sediments contained in the alpine foreland basin. This research ties in with ongoing debates on the timing and mechanisms of mountain building.
Christian Stranne, Matt O'Regan, Martin Jakobsson, Volker Brüchert, and Marcelo Ketzer
Solid Earth, 10, 1541–1554, https://doi.org/10.5194/se-10-1541-2019, https://doi.org/10.5194/se-10-1541-2019, 2019
Maximilian Rieder, Wencke Wegner, Monika Horschinegg, Stefanie Klackl, Nereo Preto, Anna Breda, Susanne Gier, Urs Klötzli, Stefano M. Bernasconi, Gernot Arp, and Patrick Meister
Solid Earth, 10, 1243–1267, https://doi.org/10.5194/se-10-1243-2019, https://doi.org/10.5194/se-10-1243-2019, 2019
Short summary
Short summary
The formation of dolomite (CaMg(CO3)2), an abundant mineral in Earth's geological record, is still incompletely understood. We studied dolomites embedded in a 100 m thick succession of coastal alluvial clays of Triassic age in the southern Alps. Observation by light microscopy and Sr isotopes suggests that dolomites may spontaneously from concentrated evaporating seawater, in coastal ephemeral lakes or tidal flats along the western margin of the Triassic Tethys sea.
Salomé Mignard, Thierry Mulder, Philippe Martinez, and Thierry Garlan
Solid Earth, 10, 851–869, https://doi.org/10.5194/se-10-851-2019, https://doi.org/10.5194/se-10-851-2019, 2019
Short summary
Short summary
A large quantity a continental material is transported to the oceans by the world rivers. Once in the ocean, these particles can be transported down the continental shelf thanks to underwater avalanches. The repetition of such massive events can form very important sedimentary deposits at the continent–ocean transition. Data obtained during an oceanic cruise in 2010 allowed us to study such a system located offshore of Gabon and to evaluate the importance sediment transport in this area.
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
Short summary
Short summary
A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Leandra M. Weydt, Claus-Dieter J. Heldmann, Hans G. Machel, and Ingo Sass
Solid Earth, 9, 953–983, https://doi.org/10.5194/se-9-953-2018, https://doi.org/10.5194/se-9-953-2018, 2018
Short summary
Short summary
This study focuses on the assessment of the geothermal potential of two extensive upper Devonian aquifer systems within the Alberta Basin (Canada). Our work provides a first database on geothermal rock properties combined with detailed facies analysis (outcrop and core samples), enabling the identification of preferred zones in the reservoir and thus allowing for a more reliable reservoir prediction. This approach forms the basis for upcoming reservoir studies with a focus on 3-D modelling.
Ernest Chi Fru, Stephanos Kilias, Magnus Ivarsson, Jayne E. Rattray, Katerina Gkika, Iain McDonald, Qian He, and Curt Broman
Solid Earth, 9, 573–598, https://doi.org/10.5194/se-9-573-2018, https://doi.org/10.5194/se-9-573-2018, 2018
Short summary
Short summary
Banded iron formations (BIFs) are chemical sediments last seen in the marine sedimentary record ca. 600 million years ago. Here, we report on the formation mechanisms of a modern BIF analog in the Cape Vani sedimentary basin (CVSB) on Milos Island, Greece, demonstrating that rare environmental redox conditions, coupled to submarine hydrothermal activity and microbial processes, are required for these types of rocks to form in the modern marine biosphere.
Cited articles
Abell, A. B., Willis, K. L., and Lange, D. A.: Mercury Intrusion Porosimetry
and Image Analysis of Cement-Based Materials, J. Colloid Interf. Sci., 211, 39–44, https://doi.org/10.1006/jcis.1998.5986, 1999.
Ahmad, K. M., Kristaly, F., and Docs, R.: Effects of clay mineral and
physico-chemical variables on sandstone rock permeability, J. Oil Gas Petrochem. Sci., 1, 18–26, https://doi.org/10.30881/jogps.00006, 2018.
Alyafei, N., Raeini, A. Q., Paluszny, A., and Blunt, M. J.: A Sensitivity
Study of the Effect of Image Resolution on Predicted Petrophysical
Properties, Transp. Porous. Med., 110, 157–169,
https://doi.org/10.1007/s11242-015-0563-0, 2015.
Andrä, H., Combaret, N., Dvorkin, J., Glatt, E., Han, J., Kabel, M.,
Keehm, Y., Krzikalla, F., Lee, M., Madonna, C., Marsh, M., Mukerji, T.,
Saenger, E. H., Sain, R., Saxena, N., Ricker, S., Wiegmann, A., and Zhan, X.:
Digital rock physics benchmarks—Part I: Imaging and segmentation,
Comput. Geosci., 50, 25–32, https://doi.org/10.1016/j.cageo.2012.09.005, 2013a.
Andrä, H., Combaret, N., Dvorkin, J., Glatt, E., Han, J., Kabel, M., Keehm, Y., Krzikalla, F., Lee, M., Madonna, C., Marsh, M., Mukerji, T., Saenger, E. H., Sain, R., Saxena, N., Ricker, S., Wiegmann, A., and Zhan, X.: Digital rock physics benchmarks–part II: Computing effective properties, Comput. Geosci., 50, 33–43, https://doi.org/10.1016/j.cageo.2012.09.008, 2013b.
Aplin, A. C., Matenaar, I. F., McCarty, D. K., and van der Pluijm, B. A.:
Influence of mechanical compaction and clay mineral diagenesis on the
microfabric and pore-scale properties of deep-water Gulf of Mexico
mudstones, Clay. Clay. Miner., 54, 500–514,
https://doi.org/10.1346/CCMN.2006.0540411, 2006.
Bear, J.: Dynamics of fluids in porous media, American Elsevier Pub. Co, New
York, 1972.
Berg, S., Saxena, N., Shaik, M., and Pradhan, C.: Generation of ground truth
images to validate micro-CT image-processing pipelines, Leading Edge,
37, 412–420, https://doi.org/10.1190/tle37060412.1, 2018.
Berg, S., Kutra, D., Kroeger, T., Straehle, C. N., Kausler, B. X., Haubold,
C., Schiegg, M., Ales, J., Beier, T., Rudy, M., Eren, K., Cervantes, J. I.,
Xu, B., Beuttenmueller, F., Wolny, A., Zhang, C., Koethe, U., Hamprecht, F.
A., and Kreshuk, A.: ilastik: interactive machine learning for (bio)image
analysis, Nat. Methods, https://doi.org/10.1038/s41592-019-0582-9, 2019.
Brinkman, H. C.: Calculations on the flow of heterogeneous mixtures through
porous media, Appl. Sci. Res., 1, 333, https://doi.org/10.1007/BF02120339, 1949.
Brunke, O., Brockdorf, K., Drews, S., Müller, B., Donath, T., Herzen, J.,
and Beckmann, F.: Comparison between x-ray tube-based and synchrotron
radiation-based µCT, edited by: Stock, S. R., San Diego,
California, USA., 2008.
Buades, A., Coll, B., and Morel, J.-M.: Non-Local Means Denoising, Image
Processing On Line, 1, 208–212, https://doi.org/10.5201/ipol.2011.bcm_nlm, 2011.
Darcy, H.: Les Fontaines Publiques de la Ville de Dijon, Les Fontaines Publiques de la Ville de Dijon: Exposition et Application des Principes a Suivre et des Formulesa Employer dans les Questions de Distribution d’Eau, Dalmont, 1856.
De Boever, W., Derluyn, H., Van Loo, D., Van Hoorebeke, L., and Cnudde, V.:
Data-fusion of high resolution X-ray CT, SEM and EDS for 3D and pseudo-3D
chemical and structural characterization of sandstone, Micron, 74, 15–21,
https://doi.org/10.1016/j.micron.2015.04.003, 2015.
Desbois, G., Urai, J. L., Hemes, S., Schröppel, B., Schwarz, J.-O., Mac,
M., and Weiel, D.: Multi-scale analysis of porosity in diagenetically altered
reservoir sandstone from the Permian Rotliegend (Germany), J.
Petrol. Sci. Eng., 140, 128–148, https://doi.org/10.1016/j.petrol.2016.01.019, 2016.
Doebelin, N. and Kleeberg, R.: Profex?: a graphical user interface for the Rietveld refinement program BGMN, J. Appl. Crystallogr., 48, 1573–1580, https://doi.org/10.1107/S1600576715014685, 2015.
Filomena, C. M., Hornung, J., and Stollhofen, H.: Assessing accuracy of gas-driven permeability measurements: a comparative study of diverse Hassler-cell and probe permeameter devices, Solid Earth, 5, 1–11, https://doi.org/10.5194/se-5-1-2014, 2014.
Fischer, C., Dunkl, I., Von Eynatten, H., Wijbrans, J. R., and Gaupp, R.:
Products and timing of diagenetic processes in Upper Rotliegend sandstones
from Bebertal (North German Basin, Parchim Formation, Flechtingen High,
Germany), Geol. Mag., 149, 827–840, https://doi.org/10.1017/S0016756811001087, 2012.
Gane, P. A. C., Ridgway, C. J., Lehtinen, E., Valiullin, R., Furó, I.,
Schoelkopf, J., Paulapuro, H., and Daicic, J.: Comparison of NMR
Cryoporometry, Mercury Intrusion Porosimetry, and DSC Thermoporosimetry in
Characterizing Pore Size Distributions of Compressed Finely Ground Calcium
Carbonate Structures, Ind. Eng. Chem. Res., 43, 7920–7927,
https://doi.org/10.1021/ie049448p, 2004.
Gao, H. and Li, H. A.: Pore structure characterization, permeability
evaluation and enhanced gas recovery techniques of tight gas sandstones,
J. Nat. Gas Sci. Eng., 28, 536–547,
https://doi.org/10.1016/j.jngse.2015.12.018, 2016.
Gluyas, J. G. and Swarbrick, R. E.: Petroleum geoscience, Blackwell Pub,
Malden, MA, USA, 2004.
Grathoff, G. H., Peltz, M., Enzmann, F., and Kaufhold, S.: Porosity and permeability determination of organic-rich Posidonia shales based on 3-D analyses by FIB-SEM microscopy, Solid Earth, 7, 1145–1156, https://doi.org/10.5194/se-7-1145-2016, 2016.
Guan, K. M., Nazarova, M., Guo, B., Tchelepi, H., Kovscek, A. R., and Creux,
P.: Effects of Image Resolution on Sandstone Porosity and Permeability as
Obtained from X-Ray Microscopy, Transp. Porous. Med., 127, 233–245,
https://doi.org/10.1007/s11242-018-1189-9, 2019.
Heidsiek, M., Butscher, C., Blum, P., and Fischer, C.: Small-scale diagenetic
facies heterogeneity controls porosity and permeability pattern in reservoir
sandstones, Environ. Earth Sci., 79, 425, https://doi.org/10.1007/s12665-020-09168-z, 2020.
Hemes, S., Desbois, G., Urai, J. L., Schröppel, B., and Schwarz, J.-O.:
Multi-scale characterization of porosity in Boom Clay (HADES-level, Mol,
Belgium) using a combination of X-ray µ-CT, 2D BIB-SEM and FIB-SEM
tomography, Micropor. Mesopor. Mat., 208, 1–20,
https://doi.org/10.1016/j.micromeso.2015.01.022, 2015.
Iliev, O. and Laptev, V.: On numerical simulation of flow through oil
filters, Comput. Visual. Sci., 6, 139–146, https://doi.org/10.1007/s00791-003-0118-8, 2004.
Jacob, A., Enzmann, F., Hinz, C., and Kersten, M.: Analysis of Variance of Porosity and
Heterogeneity of Permeability at the Pore Scale, Transp. Porous. Med., 130,
867–887, https://doi.org/10.1007/s11242-019-01342-7, 2019.
Jiang, S.: Clay Minerals from the Perspective of Oil and Gas Exploration, in:
Clay Minerals in Nature – Their Characterization, Modification and
Application, edited by: Valaskova, M., IntechOpen, 2012.
Kessler, R. M., Ellis, J. R., and Eden, M.: Analysis of Emission Tomographic
Scan Data: Limitations Imposed by Resolution and Background, J.
Comput. Assist. Tomo., 8, 514–522, https://doi.org/10.1097/00004728-198406000-00028, 1984.
Ketcham, R. A. and Carlson, W. D.: Acquisition, optimization and
interpretation of X-ray computed tomographic imagery: applications to the
geosciences, Comput. Geosci., 27, 381–400,
https://doi.org/10.1016/S0098-3004(00)00116-3, 2001.
Khan, F., Enzmann, F., and Kersten, M.: Multi-phase classification by a least-squares support vector machine approach in tomography images of geological samples, Solid Earth, 7, 481–492, https://doi.org/10.5194/se-7-481-2016, 2016.
Kling, T., Vogler, D., Pastewka, L., Amann, F., and Blum, P.: Numerical
Simulations and Validation of Contact Mechanics in a Granodiorite Fracture,
Rock. Mech. Rock. Eng., 51, 2805–2824, https://doi.org/10.1007/s00603-018-1498-x, 2018.
Klinkenberg, L. J.: The permeability of porous Media to liquids and gases, Drilling and Production Practice, API-41-200,
1941.
Leu, L., Berg, S., Enzmann, F., Armstrong, R. T., and Kersten, M.: Fast X-ray
Micro-Tomography of Multiphase Flow in Berea Sandstone: A Sensitivity Study
on Image Processing, Transp. Porous. Med., 105, 451–469,
https://doi.org/10.1007/s11242-014-0378-4, 2014.
Linden, S., Wiegmann, A., and Hagen, H.: The LIR space partitioning system
applied to the Stokes equations, Graphical Models, 82, 58–66,
https://doi.org/10.1016/j.gmod.2015.06.003, 2015.
Lindquist, W. B., Venkatarangan, A., Dunsmuir, J. and Wong, T.: Pore and throat size distributions measured from synchrotron X-ray tomographic images of Fontainebleau sandstones, J. Geophys. Res., 105, 21509–21527, https://doi.org/10.1029/2000JB900208, 2000.
Lis-Śledziona, A.: Petrophysical rock typing and permeability prediction in tight sandstone reservoir, Acta Geophys., 67, 1895–1911,
https://doi.org/10.1007/s11600-019-00348-5, 2019.
Liu, G., Bai, Y., Fan, Z., and Gu, D.: Determination of Klinkenberg
Permeability Conditioned to Pore-Throat Structures in Tight Formations,
Energies, 10, 1575, https://doi.org/10.3390/en10101575, 2017.
Liu, M. and Mostaghimi, P.: Reactive transport modelling in dual porosity
media, Chem. Eng. Sci., 190, 436–442, https://doi.org/10.1016/j.ces.2018.06.005,
2018.
Liu, M., Starchenko, V., Anovitz, L. M., and Stack, A. G.: Grain detachment and transport clogging during mineral dissolution in carbonate rocks with
permeable grain boundaries, Geochem. Cosmochim. Ac., 280, 202–220, https://doi.org/10.1016/j.gca.2020.04.022, 2020.
Markussen, Ø., Dypvik, H., Hammer, E., Long, H., and Hammer, Ø.: 3D
characterization of porosity and authigenic cementation in Triassic
conglomerates/arenites in the Edvard Grieg field using 3D micro-CT imaging,
Mar. Petrol. Geol., 99, 265–281, https://doi.org/10.1016/j.marpetgeo.2018.10.015, 2019.
Maurer, C. R., Rensheng, Q., and Raghavan, V.: A linear time algorithm for
computing exact Euclidean distance transforms of binary images in arbitrary
dimensions, IEEE T. Pattern Anal., 25, 265–270,
https://doi.org/10.1109/TPAMI.2003.1177156, 2003.
Mayo, S., Josh, M., Nesterets, Y., Esteban, L., Pervukhina, M., Clennell, M.
B., Maksimenko, A., and Hall, C.: Quantitative micro-porosity
characterization using synchrotron micro-CT and xenon K-edge subtraction in
sandstones, carbonates, shales and coal, Fuel, 154, 167–173,
https://doi.org/10.1016/j.fuel.2015.03.046, 2015.
Menke, H., Gao, Y., Linden, S., and Andrew, M.: Using nano-XRM and
high-contrast imaging to inform micro-porosity permeability during
Stokes-Brinkman single and two-phase flow simulations on micro-CT images,
preprint, EarthArXiv, https://doi.org/10.31223/osf.io/ubg6p, 2019.
Moosmann, J., Ershov, A., Weinhardt, V., Baumbach, T., Prasad, M. S.,
LaBonne, C., Xiao, X., Kashef, J., and Hofmann, R.: Time-lapse X-ray
phase-contrast microtomography for in vivo imaging and analysis of
morphogenesis, Nat. Protoc., 9, 294–304, https://doi.org/10.1038/nprot.2014.033, 2014.
Moulinec, H. and Suquet, P.: A FFT-Based Numerical Method for Computing the
Mechanical Properties of Composites from Images of their Microstructures, in:
IUTAM Symposium on Microstructure-Property Interactions in Composite
Materials, edited by: Pyrz, R., Springer Netherlands, Dordrecht, 235–246, 1995.
Münch, B. and Holzer, L.: Contradicting Geometrical Concepts in Pore
Size Analysis Attained with Electron Microscopy and Mercury Intrusion,
J. Am. Ceram. Soc., 91, 4059–4067, https://doi.org/10.1111/j.1551-2916.2008.02736.x, 2008.
Neale, G. and Nader, W.: Practical significance of brinkman's extension of
darcy's law: Coupled parallel flows within a channel and a bounding porous
medium, Can. J. Chem. Eng., 52, 475–478, https://doi.org/10.1002/cjce.5450520407,
1974.
Okabe, H. and Blunt, M. J.: Prediction of permeability for porous media
reconstructed using multiple-point statistics, Phys. Rev. E, 70, 066135,
https://doi.org/10.1103/PhysRevE.70.066135, 2004.
Peng, S., Hu, Q., Dultz, S., and Zhang, M.: Using X-ray computed tomography
in pore structure characterization for a Berea sandstone: Resolution effect,
J. Hydrol., 472–473, 254–261, https://doi.org/10.1016/j.jhydrol.2012.09.034,
2012.
Peng, S., Marone, F., and Dultz, S.: Resolution effect in X-ray microcomputed
tomography imaging and small pore's contribution to permeability for a Berea
sandstone, J. Hydrol., 510, 403–411, https://doi.org/10.1016/j.jhydrol.2013.12.028, 2014.
Pittman, E. D. and Thomas, J. B.: Some Applications of Scanning Electron
Microscopy to the Study of Reservoir Rock, J. Petrol. Tech.,
31, 1375–1380, https://doi.org/10.2118/7550-PA, 1979.
Prill, T., Schladitz, K., Jeulin, D., Faessel, M., and Wieser, C.:
Morphological segmentation of FIB-SEM data of highly porous media, J. Microsc.-Oxford, 250, 77–87, https://doi.org/10.1111/jmi.12021, 2013.
Saxena, N., Hofmann, R., Alpak, F. O., Berg, S., Dietderich, J., Agarwal,
U., Tandon, K., Hunter, S., Freeman, J., and Wilson, O. B.: References and
benchmarks for pore-scale flow simulated using micro-CT images of porous
media and digital rocks, Adv. Water Resour., 109, 211–235,
https://doi.org/10.1016/j.advwatres.2017.09.007, 2017.
Saxena, N., Hows, A., Hofmann, R., O. Alpak, F., Freeman, J., Hunter, S., and
Appel, M.: Imaging and computational considerations for image computed
permeability: Operating envelope of Digital Rock Physics, Adv. Water
Resour., 116, 127–144, https://doi.org/10.1016/j.advwatres.2018.04.001, 2018.
Shah, S. M., Gray, F., Crawshaw, J. P., and Boek, E. S.: Micro-computed
tomography pore-scale study of flow in porous media: Effect of voxel
resolution, Adv. Water Resour., 95, 276–287,
https://doi.org/10.1016/j.advwatres.2015.07.012, 2016.
Soulaine, C., Gjetvaj, F., Garing, C., Roman, S., Russian, A., Gouze, P., and
Tchelepi, H. A.: The Impact of Sub-Resolution Porosity of X-ray
Microtomography Images on the Permeability, Transp. Porous. Med., 113,
227–243, https://doi.org/10.1007/s11242-016-0690-2, 2016.
Spanne, P., Thovert, J. F., Jacquin, C. J., Lindquist, W. B., Jones, K. W.,
and Adler, P. M.: Synchrotron Computed Microtomography of Porous Media:
Topology and Transports, Phys. Rev. Lett., 73, 2001–2004,
https://doi.org/10.1103/PhysRevLett.73.2001, 1994.
Tinet, A.-J., Corlay, Q., Collon, P., Golfier, F., and Kalo, K.: Comparison of various 3D pore space reconstruction methods and implications on transport
properties of nanoporous rocks, Adv. Water Resour., 141, 103615, https://doi.org/10.1016/j.advwatres.2020.103615, 2020.
Ufer, K., Kleeberg, R., Bergmann, J., and Dohrmann, R.: Rietveld Refinement
of Disordered Illite-Smectite Mixed-Layer Structures by a Recursive
Algorithm. II: Powder-Pattern Refinement and Quantitative Phase Analysis,
Clay. Clay. Miner., 60, 535–552, https://doi.org/10.1346/CCMN.2012.0600508, 2012.
Villiéras, F., Michot, L. J., Bardot, F., Cases, J. M., François, M. and Rudziński, W.: An Improved Derivative Isotherm Summation Method To Study Surface Heterogeneity of Clay Minerals †, Langmuir, 13, 1104–1117, https://doi.org/10.1021/la9510083, 1997.
Washburn, E. W.: The Dynamics of Capillary Flow, Phys. Rev., 17,
273–283, https://doi.org/10.1103/PhysRev.17.273, 1921.
Wilson, M. D. and Pittman, E. D.: Authigenic Clays in Sandstones:
Recognition and Influence on Reservoir Properties and Paleoenvironmental
Analysis, J. Sediment. Res., 47, 3–31,
https://doi.org/10.1306/212F70E5-2B24-11D7-8648000102C1865D, 1977.
Worden, R. H. and Morad, S.: Clay Minerals in Sandstones: Controls on
Formation, Distribution and Evolution, in Clay Mineral Cements in
Sandstones, edited by: Worden, R. H. and Morad, S., Blackwell
Publishing Ltd., Oxford, UK, 1–41, 1999.
Yoon, H. and Dewers, T. A.: Nanopore structures, statistically
representative elementary volumes, and transport properties of chalk:
NANOPORE STRUCTURES, SREV, AND FIB-SEM, Geophys. Res. Lett., 40,
4294–4298, https://doi.org/10.1002/grl.50803, 2013.
Zhang, D., Zhang, R., Chen, S., and Soll, W. E.: Pore scale study of flow in porous media: Scale dependency, REV, and statistical REV, Geophys. Res. Lett., 27, 1195–1198, https://doi.org/10.1029/1999GL011101, 2000.
Zhao, H., Ning, Z., Wang, Q., Zhang, R., Zhao, T., Niu, T., and Zeng, Y.:
Petrophysical characterization of tight oil reservoirs using
pressure-controlled porosimetry combined with rate-controlled porosimetry,
Fuel, 154, 233–242, https://doi.org/10.1016/j.fuel.2015.03.085, 2015.
Download
The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.
- Article
(10812 KB) - Full-text XML
- Corrigendum
-
Supplement
(1632 KB) - BibTeX
- EndNote
Short summary
In this work, we combined different imaging and experimental measuring methods for analysis of cross-scale effects which reduce permeability of tight reservoir rocks. Simulated permeability of digital images of rocks is often overestimated, which is caused by non-resolvable clay content within the pores of a rock. By combining FIB-SEM with micro-XCT imaging, we were able to simulate the true clay mineral abundance to match experimentally measured permeability with simulated permeability.
In this work, we combined different imaging and experimental measuring methods for analysis of...
