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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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2006Suction Induced Effects on the Fabric of a Structured Soil76citations

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Cuisinier, Olivier
1 / 15 shared
Vulliet, Laurent
1 / 1 shared
Laloui, Lyesse
1 / 3 shared
Chart of publication period
2006

Co-Authors (by relevance)

  • Cuisinier, Olivier
  • Vulliet, Laurent
  • Laloui, Lyesse
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article

Suction Induced Effects on the Fabric of a Structured Soil

  • Cuisinier, Olivier
  • Vulliet, Laurent
  • Laloui, Lyesse
  • Koliji, Azad
Abstract

This paper presents the mathematical modelling of the modification of the pore space geometry of a structured soil subjected to suction increase. Structured soil concepts are first introduced considering different fabric units, such as aggregates and fissures. The numerical modelling of the structural evolution is based on experimental test results in which the evolution of the structure of the samples subjected to different suctions is determined using the mercury intrusion porosimetry technique. From this information, the macro and micropore volume evolutions are determined. The results show that drying produces a reduction in the soil total porosity which mainly corresponds to a reduction of the macropore volume. Associated with this phenomenon, an increase in micropore volume is also observed. The proposed model divides pore size distribution into three pore classes (micropores, macropores and non-affected areas). Using the concept of a suction-influenced domain, the proposed model is able to reproduce the main observed fabric evolution between the saturated and dry states.

Topics
  • impedance spectroscopy
  • pore
  • porosity
  • drying
  • porosimetry
  • Mercury