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)

  • 2007Effects of carbonation on the pore structure of non-hydraulic lime mortars134citations

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Dayala, D.
1 / 4 shared
Rigby, Sean
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Mays, Timothy
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Walker, Peter
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2007

Co-Authors (by relevance)

  • Dayala, D.
  • Rigby, Sean
  • Mays, Timothy
  • Walker, Peter
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article

Effects of carbonation on the pore structure of non-hydraulic lime mortars

  • Dayala, D.
  • Rigby, Sean
  • Lawrence, R. M. H.
  • Mays, Timothy
  • Walker, Peter
Abstract

The pore structures of carbonated non-hydraulic lime mortars made with a range of different aggregates and concentrations of lime have been determined using mercury intrusion porosimetry (MIP). MIP data have been correlated with scanning electron microscopy images and other porosity data. During carbonation there is an increase in pore volume in the ~0.1 μm pore diameter range across all mortar types which is attributed to the transformation of portlandite to calcite. Also there is a monotonic increase in the volumes of pores with diameters below 0.03 μm. A model is proposed for the changes in pore structure caused by carbonation. This attributes the increase in the volume of sub 0.03 μm pores to the attachment of calcite crystals to the surface of aggregate particles, and in some cases to the surface of portlandite crystals. This phenomenon may explain the continuing presence of portlandite in mortars that, apparently, have fully carbonated.

Topics
  • impedance spectroscopy
  • pore
  • surface
  • scanning electron microscopy
  • porosity
  • lime
  • porosimetry
  • Mercury