Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool

The Opalinus Clay is notable in Switzerland as being the selected host rock for deep geological disposal of radioactive waste. Since the early 1990’s, this argillaceous mudstone formation of Jurassic age has been intensively studied within the framework of national and international projects to char...

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Main Authors: Bruno Lauper, Géraldine N. Zimmerli, David Jaeggi, Gaudenz Deplazes, Stephan Wohlwend, Johannes Rempfer, Anneleen Foubert
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.645596/full
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author Bruno Lauper
Géraldine N. Zimmerli
David Jaeggi
Gaudenz Deplazes
Stephan Wohlwend
Johannes Rempfer
Anneleen Foubert
author_facet Bruno Lauper
Géraldine N. Zimmerli
David Jaeggi
Gaudenz Deplazes
Stephan Wohlwend
Johannes Rempfer
Anneleen Foubert
author_sort Bruno Lauper
collection DOAJ
description The Opalinus Clay is notable in Switzerland as being the selected host rock for deep geological disposal of radioactive waste. Since the early 1990’s, this argillaceous mudstone formation of Jurassic age has been intensively studied within the framework of national and international projects to characterize its geological, hydrological, mechanical, thermal, chemical, and biological properties. While there is no formal stratigraphic subdivision, the Opalinus Clay lithology is classically divided into several, dam- to m-scale sub-units (or facies), depending on location. Recent multi-proxy studies (combining petrographic, petrophysical, geochemical, and mineralogical analyses) have however demonstrated that high, intra-facies, lithological heterogeneity occurs at the dm- to cm-scale. To constrain this small-scale heterogeneity into distinct lithological units (subfacies), the present study aims at defining and presenting a convenient subfacies classification scheme covering the overall Opalinus Clay lithology across northern Switzerland. Petrographic (macro- and microfacies), mineralogical (X-ray diffraction) and textural (image analysis, machine learning and 3D X-ray computed tomography) analyses are performed on diverse drill cores from the Mont Terri rock laboratory (northwestern Switzerland), and results are extended further to the east (Riniken, Weiach, and Benken). Most of the investigated Opalinus Clay can be described by the use of five distinctive subfacies types (SF1 to SF5), which are visually and quantitatively distinguishable by texture (grain size, bedding, fabric, and color) and composition (nature and mineralogy of components). The five subfacies types can be further refined by additional attributes and sedimentary characteristics (biogenic, diagenetic, and structural). Eventually, the widespread and consistent use of standardized Opalinus Clay subfacies types provides the means to harmonize petrographic descriptions within multidisciplinary research projects, enhance reproducibility of in situ experiments, and further evidence the tight relations between lithology and various rock properties.
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spelling doaj.art-966d2dbdc0a64c409223470380053f8e2022-12-21T21:31:46ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-05-01910.3389/feart.2021.645596645596Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition ToolBruno Lauper0Géraldine N. Zimmerli1David Jaeggi2Gaudenz Deplazes3Stephan Wohlwend4Johannes Rempfer5Anneleen Foubert6Department of Geosciences, University of Fribourg, Fribourg, SwitzerlandDepartment of Geosciences, University of Fribourg, Fribourg, SwitzerlandFederal Office of Topography Swisstopo, Wabern, SwitzerlandNational Cooperative for the Disposal of Radioactive Waste (Nagra), Wettingen, SwitzerlandGeological Institute, ETH Zurich, Zurich, Switzerlandgeo7 AG, Bern, SwitzerlandDepartment of Geosciences, University of Fribourg, Fribourg, SwitzerlandThe Opalinus Clay is notable in Switzerland as being the selected host rock for deep geological disposal of radioactive waste. Since the early 1990’s, this argillaceous mudstone formation of Jurassic age has been intensively studied within the framework of national and international projects to characterize its geological, hydrological, mechanical, thermal, chemical, and biological properties. While there is no formal stratigraphic subdivision, the Opalinus Clay lithology is classically divided into several, dam- to m-scale sub-units (or facies), depending on location. Recent multi-proxy studies (combining petrographic, petrophysical, geochemical, and mineralogical analyses) have however demonstrated that high, intra-facies, lithological heterogeneity occurs at the dm- to cm-scale. To constrain this small-scale heterogeneity into distinct lithological units (subfacies), the present study aims at defining and presenting a convenient subfacies classification scheme covering the overall Opalinus Clay lithology across northern Switzerland. Petrographic (macro- and microfacies), mineralogical (X-ray diffraction) and textural (image analysis, machine learning and 3D X-ray computed tomography) analyses are performed on diverse drill cores from the Mont Terri rock laboratory (northwestern Switzerland), and results are extended further to the east (Riniken, Weiach, and Benken). Most of the investigated Opalinus Clay can be described by the use of five distinctive subfacies types (SF1 to SF5), which are visually and quantitatively distinguishable by texture (grain size, bedding, fabric, and color) and composition (nature and mineralogy of components). The five subfacies types can be further refined by additional attributes and sedimentary characteristics (biogenic, diagenetic, and structural). Eventually, the widespread and consistent use of standardized Opalinus Clay subfacies types provides the means to harmonize petrographic descriptions within multidisciplinary research projects, enhance reproducibility of in situ experiments, and further evidence the tight relations between lithology and various rock properties.https://www.frontiersin.org/articles/10.3389/feart.2021.645596/fullAalenianToarcianclaystone and shalemudstonerock classificationnuclear waste storage
spellingShingle Bruno Lauper
Géraldine N. Zimmerli
David Jaeggi
Gaudenz Deplazes
Stephan Wohlwend
Johannes Rempfer
Anneleen Foubert
Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
Frontiers in Earth Science
Aalenian
Toarcian
claystone and shale
mudstone
rock classification
nuclear waste storage
title Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
title_full Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
title_fullStr Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
title_full_unstemmed Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
title_short Quantification of Lithological Heterogeneity Within Opalinus Clay: Toward a Uniform Subfacies Classification Scheme Using a Novel Automated Core Image Recognition Tool
title_sort quantification of lithological heterogeneity within opalinus clay toward a uniform subfacies classification scheme using a novel automated core image recognition tool
topic Aalenian
Toarcian
claystone and shale
mudstone
rock classification
nuclear waste storage
url https://www.frontiersin.org/articles/10.3389/feart.2021.645596/full
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