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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Razakamanantsoa, Andry Rico

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (9/9 displayed)

  • 2023Physicochemical and Microstructural Evaluation in Lime-Treated Silty Soil Exposed to Successive Wetting-Drying Cycles Submitted to Different Testing Conditions9citations
  • 2022Modeling of Hysteretic Behavior of Soil–Water Retention Curves Using an Original Pore Network Model6citations
  • 2020Experimental study of particle lift initiation on roller-compacted sand-clay mixtures4citations
  • 2018Shear strength performance of marine sediments stabilized using cement, lime and fly ash58citations
  • 2018Effects of Cement Treatment on Microstructural, Hydraulic, and Mechanical Properties of Compacted Soils: Characterization and Modeling30citations
  • 2018Toward a better understanding of the effects of cement treatment on microstructure and hydraulic properties of compacted soils2citations
  • 2016Long term chemo-hydro-mechanical behavior of compacted soil bentonite polymer complex submitted to synthetic leachate33citations
  • 2016Permeability prediction of soils including degree of compaction and microstructure42citations
  • 2015Feasibility study of chemical stabilization of dredged marine sediment1citations

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Chart of shared publication
Deneele, Dimitri
2 / 16 shared
Herrier, Gontran
1 / 2 shared
Das, Geetanjali
2 / 2 shared
Ranaivomanana, Harifidy
5 / 12 shared
Sediki, Ouardia
1 / 1 shared
Vern, Mickael Le
1 / 1 shared
Larrarte, Frédérique
1 / 1 shared
Murzyn, Frédéric
1 / 1 shared
Furlan, Ana Paula
1 / 1 shared
Levacher, Daniel
1 / 13 shared
Katsumi, Takeshi
1 / 1 shared
Amiri, Ouali
2 / 10 shared
Djeran-Maigre, Irini
1 / 4 shared
Liang, Yingjie
1 / 1 shared
Furlan, Ana Paola
1 / 1 shared
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Co-Authors (by relevance)

  • Deneele, Dimitri
  • Herrier, Gontran
  • Das, Geetanjali
  • Ranaivomanana, Harifidy
  • Sediki, Ouardia
  • Vern, Mickael Le
  • Larrarte, Frédérique
  • Murzyn, Frédéric
  • Furlan, Ana Paula
  • Levacher, Daniel
  • Katsumi, Takeshi
  • Amiri, Ouali
  • Djeran-Maigre, Irini
  • Liang, Yingjie
  • Furlan, Ana Paola
OrganizationsLocationPeople

article

Experimental study of particle lift initiation on roller-compacted sand-clay mixtures

  • Sediki, Ouardia
  • Vern, Mickael Le
  • Larrarte, Frédérique
  • Murzyn, Frédéric
  • Razakamanantsoa, Andry Rico
Abstract

Civil engineering works are sources of dust emissions, which can cause severe security, health and environmental damages to workers and neighbourhoods. This isarticularly significant for implementation of earthwork sites. The present paper reports a study conducted to characterise the soil-atmosphere interaction above compacted soils where particle lift is initiated. Mixtures of kaolin clay and sand have been compacted using a laboratory roller compactor that reproduces near-field compaction conditions. Shear testing conducted at the interface confirms that the sand content affects the friction angle between the soil and the compaction roller. The experimental velocity profiles above the compacted samples have been obtained in a wind tunnel using a non-intrusive measurement technique (laser Doppler velocimetry). Results show that the sand fraction affects velocity profiles. Compaction, therefore, may not fully reduce the roughness of the soil surface. The airflow friction velocities at the sample surfaces have been determined from the boundary layer profiles. The results achieved demonstrate that all tested soils reach the threshold friction velocity required to initiate particle lift, and the higher the sand content, the more likely it is that particle lift occurs.

Topics
  • impedance spectroscopy
  • surface