The high-pressure structure of (1-x)Na 0.5 Bi 0.5 TiO 3 -xBaTiO 3 at the morphotropic phase boundary.

Autor: Rösche C; Department of Earth System Sciences, Universität Hamburg, Grindelallee 48, 20146, Hamburg, Germany. constanze.roesche@uni-hamburg.de., Boffa Ballaran T; Bayerisches Geoinstitut, Universität Bayreuth, Universitätsstraße 30, 95447, Bayreuth, Germany., Malcherek T; Department of Earth System Sciences, Universität Hamburg, Grindelallee 48, 20146, Hamburg, Germany., Paulmann C; Department of Earth System Sciences, Universität Hamburg, Grindelallee 48, 20146, Hamburg, Germany., Angel RJ; Istituto di Geoscienze e Georisorse, CNR, Corso Stati Uniti 4, 35127, Padova, Italy., Gorfman S; Department of Materials Science and Engineering, Tel Aviv University, Wolfson Building for Mechanical Engineering, Tel Aviv, 6997801, Israel., Mihailova B; Department of Earth System Sciences, Universität Hamburg, Grindelallee 48, 20146, Hamburg, Germany.

Publikováno v: Scientific reports [Sci Rep] 2024 Aug 13; Vol. 14 (1), pp. 18799. Date of Electronic Publication: 2024 Aug 13.

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Kinetics of hydrogen diffusion in riebeckite, Na2Fe3+2Fe2+3Si8O22(OH)2: an HT-FTIR study

Autor: Della Ventura G., Radica F., Galdenzi F., Susta U, Cinque G., Mihailova B., Marcelli A.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::5492f0a3318ace5c5d3cfed2ed4a9a99
https://hdl.handle.net/11590/424688

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Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates

Autor: Mihailova B.[1], Della Ventura G.[2, Waeselmann N.[1], Xu W.[4], Schlüter J.[5], Galdenzi F.[2, Marcelli A.[3, Redhammer G.J.[7], Boiocchi M.[8], Oberti R.[9]

Publikováno v: Communications materials 2 (2021): 1–10. doi:10.1038/s43246-021-00161-y
info:cnr-pdr/source/autori:Mihailova B.[1], Della Ventura G.[2,3], Waeselmann N.[1], Xu W.[4], Schlüter J.[5], Galdenzi F.[2,3], Marcelli A.[3,6], Redhammer G.J.[7], Boiocchi M.[8], Oberti R.[9]/titolo:Atomistic insight into lithospheric conductivity revealed by phonon-electron excitations in hydrous iron-bearing silicates/doi:10.1038%2Fs43246-021-00161-y/rivista:Communications materials/anno:2021/pagina_da:1/pagina_a:10/intervallo_pagine:1–10/volume:2
Communications Materials, Vol 2, Iss 1, Pp 1-10 (2021)

Amphiboles are essential components of the continental crust and subduction zones showing anomalous anisotropic conductivity. Rock properties depend on the physical properties of their constituent minerals, which in turn depend on the crystal phonon

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89f52faed313de873f1c4341da3f2eda
https://hdl.handle.net/11590/424697