Materials Map

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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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Topics

Publications (1/1 displayed)

  • 2024The intrinsic twinning and enigmatic twisting of aragonite crystals1citations

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Rečnik, Aleksander
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Daneu, Nina
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Aksenov, Sergey
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Korsakov, Andrey
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Rashchenko, Sergey
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Volkov, Sergey
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Banaev, Maksim V.
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Donskikh, Katerina G.
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2024

Co-Authors (by relevance)

  • Rečnik, Aleksander
  • Daneu, Nina
  • Aksenov, Sergey
  • Korsakov, Andrey
  • Rashchenko, Sergey
  • Volkov, Sergey
  • Banaev, Maksim V.
  • Donskikh, Katerina G.
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article

The intrinsic twinning and enigmatic twisting of aragonite crystals

  • Rečnik, Aleksander
  • Daneu, Nina
  • Aksenov, Sergey
  • Korsakov, Andrey
  • Mikhailenko, Denis
  • Rashchenko, Sergey
  • Volkov, Sergey
  • Banaev, Maksim V.
  • Donskikh, Katerina G.
Abstract

<jats:p>It is generally accepted that aragonite crystals of biogenic origin are characterized by significantly higher twin densities compared to samples formed during geological processes. Based on our single crystal X-ray diffraction (SCXRD) and transmission electron microscopy (TEM) study of aragonite crystals from various localities, we show that in geological aragonites, the twin densities are comparable to those of the samples from crossed lamellar zones of molluscs shells. The high twin density is consistent with performed calculations, according to which the Gibbs free energy of twin-free aragonite is close to that of periodically twinned aragonite structure. In some cases, high twin densities result in the appearance of diffuse scattering in SCXRD patterns. The obtained TEM and optical micrographs show that besides the twin boundaries (TBs) of growth origin, there are also TBs and especially stacking faults that were likely formed as the result of local strain compensation. SCXRD patterns of the samples from Tazouta, in addition to diffuse scattering lines, show Debye arcs in the<jats:inline-formula><mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline" overflow="scroll"><mml:mrow><mml:msup><mml:mi>a</mml:mi><mml:mo>∗</mml:mo></mml:msup><mml:msup><mml:mi>b</mml:mi><mml:mo>∗</mml:mo></mml:msup></mml:mrow></mml:math></jats:inline-formula>plane. These Debye arcs are present only on one side of the Bragg reflections and have an azimuthal extent of nearly 30°, making the whole symmetry of the diffraction pattern distinctly chiral, which has not yet been reported for aragonite. By analogy with biogenic calcite crystals, we associate these arcs with the presence of misoriented subgrains formed as a result of crystal twisting during growth.</jats:p>

Topics
  • density
  • impedance spectroscopy
  • single crystal X-ray diffraction
  • single crystal
  • transmission electron microscopy
  • stacking fault
  • twinned