Showing 1-10 of 82
  • Publication
    Comptes Rendus Physique
    Kociak, M,; Stéphan, O.; Gloter, A.; Zagonel, L. F.; Tizei, L. H. G.; Tencé, M.; March, K.; Blazit, J. D.; Mahfoud, Z.; Losquin, A.; Meuret, S.; Colliex, C.
  • Publication
    Chemical Engineering Journal
    Bharat, L. K.; Rao, B. V.; Yu, J. S.

    Spindle shaped tetragonal La2(MoO4)3: Eu3+ phosphors were synthesized by a polyol mediated solvothermal synthesis method. Growth mechanism for the formation of spindles was explained by increasing the reaction temperature.

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    Data courtesy of Dr. R. Williams, Ohio State University.

    a) Dark field STEM image of GaN/AlN heterostructure nanowire with nominally 3 nm thick GaN quantum wells and 4 nm thick AlN barrier layers; GaN is bright in DF image; (b) Cathodoluminescence (CL) spectrum-image acquired from region indicated by green rectangle in (a) with intensity at 491 ±10 nm

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    Cathodoluminescence analysis of a gold prism of side length 200 nm.

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    Cathodoluminescence (CL) and EELS analysis of gold prism of 250 nm side length.

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    Sample courtesy of J. Griffiths, University of Cambridge

    (a) Dark field STEM image revealing six 3 nm thick InGaN wells; (b) Cathodoluminescence (CL) image of same region (acquired simultaneously) showing up to 20x variation in the luminescence efficiency locally; (c) Overlay of DF and CL STEM images with the position of threading dislocations shown by

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    Data courtesy of Dr. G. Fern, ETC, University of Brunel

    Cathodoluminescence spectrum of Europium-doped yttrium oxide particle measured with Vulcan system.  Europium ion d-to-f interband transitions produce narrow emission lines; excellent energy resolution of Vulcan™ system resolves two spectral peaks with peak-to-peak separation of only 1.6 meV.  

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    Image courtesy of Dr. J. Schieber, Indiana University.

    Quartz grains from granite and metamorphic source with low temperature quartz cement (bluish). There is a later (hotter) overprint (reddish) along grain boundaries in the overgrowth.

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    Images (a), (b) and (d) –(f) courtesy of Dr. J. Schieber, Indiana University.

    Color cathodoluminescence reveals provenance of populations of quartz grains (a) Cleveland shale (Devonian); low grade metamorphic acadian orogeny; (b) Barnett shale (Miss.) Texas; low grade metamorphic ouchita orogeny; (c) Unspecified; (d) Santa Barbara basin shale (modern); plutonic (Sierra Nev

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    Data courtesy of Dr. M. Bosman, A*STAR IMRE, Singapore

    Cathodoluminescence investigation of gold prisms in the STEM: (a) and (b) are bright field TEM images and (c) and (d) are the cathodoluminescence intensity maps recorded in STEM mode from particles (a) and (b) respectively.