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
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Murzyn, Frédéric
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Furlan, Ana Paula
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Levacher, Daniel
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Katsumi, Takeshi
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Amiri, Ouali
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Djeran-Maigre, Irini
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Liang, Yingjie
1 / 1 shared
Furlan, Ana Paola
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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

Physicochemical and Microstructural Evaluation in Lime-Treated Silty Soil Exposed to Successive Wetting-Drying Cycles Submitted to Different Testing Conditions

  • Deneele, Dimitri
  • Razakamanantsoa, Andry Rico
  • Herrier, Gontran
  • Das, Geetanjali
Abstract

Physicochemical and microstructural evolution in lime-treated soil subjected to successive wetting and drying (W-D) cycles was investigated, and the relevance of the laboratory-implemented testing condition with in situ conditions was discussed. Lime-treated soils were exposed to 17 W-D cycles using different testing conditions. Two laboratory testing conditions were operated at laboratory temperature, consisting of W-D duration representing the saturation level close to the one experienced in the in situ soil during rainy and drought periods. The results obtained were interpreted in terms of those obtained using a reference procedure from current standards, which involved oven-drying specimens at 71 degrees C. Drying of lime-treated soil at 71 degrees C reduced the water content from about 20% to 0.85%. This has led to greater contact between soil particles, thus increasing the suction from about 143.5 to 270 MPa. Such a phenomenon increased the unconfined compressive strength (UCS) of the oven-dried soil up to about three times compared with the air-dried specimen, although the available cementitious bonding, reflected by the presence of pores smaller than 3,000 angstrom, was comparatively low in the former compared with the latter. Percentage leaching of calcium components with respect to the initial calcium content of the soil was significantly low during W-D cycles due to greater exposure of only the outer part of the compacted soil structure during wetting. However, the leaching was comparatively higher in the oven-dried soil. The implemented wetting duration and drying temperature influenced the wetting front velocity of water, which significantly affects the duration taken by infiltered water to invade the core of an earthen structure, and hence its durability.

Topics
  • pore
  • strength
  • leaching
  • Calcium
  • durability
  • drying
  • lime