Published May 28, 2013 | Version v1
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Mineralogical and Micro-fabric investigation of the Sandy Facies of Opalinus Clay (Mont Terri)

  • 1. Department of Structural Geology and Geodynamic, Georg-August University-Goettingen, Gold-schmidtstr. 3, 37077 Goettingen (Germany)
  • 2. Federal Institute for Geosciences and Natural Recources, Stilleweg 2, 30655 Hannover (Germany)

Description

In the field of geological disposal of radioactive waste in many countries argillaceous formations are considered as potential host rock. For the understanding of the long-term behaviour of clay host rock, it is important to understand the interaction between mechanical behaviour, micro-fabric, and mineral composition. Previous publications showed that particularly the carbonate content and the arrangement of the carbonate grains (as cement in the matrix or as shells) determines the mechanical strength of Opalinus Clay and Callovo-Oxfordian Clay specimens, respectively. Klinkenberg et al. (2009) studied the shaly facies of Opalinus Clay, however, the actual deposit is planned to be built in the sandy facies of Opalinus Clay. The aim of the present study is to investigate the relation between micro-fabric, mineral composition, and mechanical properties of different samples derived from the sandy facies (BLT-A2). Image analysis showed that the carbonates in the sandy facies mainly occur as 1) matrix which in turn acts as cement. Carbonates also occur 2) in the fine sand fraction and 3) biogenic carbonates as traces. The carbonates of the sandy facies, therefore, appear to be similar to the carbonates of the Callovo-Oxfordian Clay with respect to their possible influence on failure strength. The mechanical testing showed that the shear strength increases with increasing carbonate content. This phenomenon was also observed for the samples of the Callovo-Oxfordian Clay, while the opposite relation was found for the shaly facies of the Opalinus Clay. Preliminary results presented here, indicate that the sandy facies (drilling BLT-A2) and Callovo-Oxfordian Clay show similar mechanical properties - in detail: 1) Micro-fabric: carbonates predominate in the matrix, 2) Mineralogy: high carbonate content and 3) Mechanical testing: shear strength increases with increasing carbonate content, where the type of carbonates which controls the increase of strength has to be identified more extensively

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Part of:
Proceedings of the NEA Clay Club Workshop on Clay characterisation from nanoscopic to microscopic resolution

Additional details

Publishing Information

Imprint Title
Proceedings of the NEA Clay Club Workshop on Clay characterisation from nanoscopic to microscopic resolution
Imprint Pagination
168 p.
Journal Page Range
p. 53-57
Report number
NEA-RWM-CLAYCLUB--2013-1

Conference

Title
NEA Clay Club Workshop on clay characterisation from nanoscopic to microscopic resolution
Dates
6-8 Sep 2011
Place
Karlsruhe (Germany)

INIS

Country of Publication
Nuclear Energy Agency of the OECD (NEA)
Country of Input or Organization
Nuclear Energy Agency of the OECD (NEA)
INIS RN
46109576
Subject category
S36: MATERIALS SCIENCE; S58: GEOSCIENCES;
Resource subtype / Literary indicator
Conference
Descriptors DEI
CARBONATES; MICROSTRUCTURE; MINERALOGY; OPALINUS CLAY; QUANTITATIVE CHEMICAL ANALYSIS; QUARTZ; ROCK MECHANICS; SAND; SCANNING ELECTRON MICROSCOPY; SHEAR PROPERTIES; X-RAY DIFFRACTION
Descriptors DEC
CARBON COMPOUNDS; CHEMICAL ANALYSIS; CLAYS; COHERENT SCATTERING; DIFFRACTION; ELECTRON MICROSCOPY; MECHANICAL PROPERTIES; MECHANICS; MICROSCOPY; MINERALS; OXIDE MINERALS; OXYGEN COMPOUNDS; SCATTERING; SILICATE MINERALS

Optional Information

Notes
6 refs.