Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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Djemil, Mahamat Moussa Tahir

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2022Microstructure Development in Artificially Cemented, Fine-Grained Soils7citations

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Chart of shared publication
Tschuchnigg, Franz
1 / 3 shared
Baldermann, Andre
1 / 11 shared
Marte, Roman
1 / 5 shared
Nachtnebel, Manfred
1 / 5 shared
Oberhollenzer, Simon
1 / 2 shared
Dietzel, Martin
1 / 20 shared
Chart of publication period
2022

Co-Authors (by relevance)

  • Tschuchnigg, Franz
  • Baldermann, Andre
  • Marte, Roman
  • Nachtnebel, Manfred
  • Oberhollenzer, Simon
  • Dietzel, Martin
OrganizationsLocationPeople

article

Microstructure Development in Artificially Cemented, Fine-Grained Soils

  • Djemil, Mahamat Moussa Tahir
  • Tschuchnigg, Franz
  • Baldermann, Andre
  • Marte, Roman
  • Nachtnebel, Manfred
  • Oberhollenzer, Simon
  • Dietzel, Martin
Abstract

<p>Fine-grained sedimentary deposits can bear an increased risk for building settlements due to their moderate stiffness and strength properties, as well as high groundwater tables. However, some buildings, e.g., situated on shallow foundations in Alpine basins, show only relatively small settlements because the formation of carbonate cement can create bridging bonds between the detrital soil particles, leading to increased stiffness. These weak bonds can be damaged through dynamic loads and high static loads, causing a weakening of the soil’s microstructure and resulting in large settlements in several cases. However, the environmental controls and mechanistic processes underlying the formation versus damaging of microstructure in fine-grained, postglacial sediments are, to date, poorly understood. In the present study, fine-grained sediments are artificially cemented by calcium carbonates (CaCO<sub>3</sub>) to investigate (i) the influence of a mild and sustainable cementation process on the stress–strain behavior of silicate- and carbonate-rich soils and (ii) the possibilities and limitations of artificial microstructure development for soil stabilization. Incremental load oedometer testing (IL), bender element testing (BE), X-ray diffraction (XRD), scanning electron microscopy (SEM) and Brunauer–Emmett–Teller (BET) specific surface area (SSA) measurements are used to characterize the development of cementation and to elucidate the improvements in the soil mechanical properties. It is shown that cementation induced by CaCO<sub>3</sub> mineralization (by 5–15% replacement) leads to an increased stiffness (factor ≈ 5–7) and shear wave velocity (factor ≈ 1.1), caused by the formation of nanocrystalline, particle-binding CaCO<sub>3</sub> cements. The improvement of soil stiffness is dependent on the CaCO<sub>3</sub> replacement level, reaction time and primary soil mineralogical composition.</p>

Topics
  • impedance spectroscopy
  • microstructure
  • surface
  • scanning electron microscopy
  • x-ray diffraction
  • strength
  • cement
  • Calcium