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Radiochim. Acta 2014; 102(11): 957–972 Isabelle LLorens, Pier Lorenzo Solari*, Bruno Sitaud, René Bes, Sebastiano Cammelli, Hervé Hermange, Guillaume Othmane, Sami Safi, Philippe Moisy, Sandrine Wahu, Carole Bresson, Michel L. Schlegel, Denis Menut, Jean-Luc Bechade, Philippe Martin, Jean-Louis Hazemann, Olivier Proux, and Christophe Den Auwer X-ray absorption spectroscopy investigations on radioactive matter using MARS beamline at SOLEIL synchrotron Abstract: The MARS beamline at the SOLEIL synchrotron is dedicated to the characterization of radioactive mate

REFERENCES 1. Kisiel, A. (2006). Synchrotron jako narzędzie: zastosowania promieniowania synchrotronowego w spektroskopii ciała stałego. Synchrotron Radiation in Natural Science , Vol. 5, No 3. 2. http://www.esrf.eu/ 3. Lipinski, P., Berveiller, M., (1989). Elastoplasticity of micro-inhomogeneous metals at large strains. Int. J. Plastic . 5, pp. 149–172. 4. A. Baczmański, L. Le Joncour, B. Panicaud, M. Francois, C. Braham, A. M. Paradowska, S. Wrooski, S. Amara and R. Chirone (2011). Neutron time-of-flight diffraction used to study aged duplex stainless steel

Rietveld refinement of energy-dispersive synchrotron measurements Daniel Apel*, I, Manuela KlausI, Christoph GenzelI and Davor BalzarII I Helmholtz-Zentrum Berlin für Materialien und Energie, Albert-Einstein-Straße 15, 12489 Berlin, Germany II University of Denver, Dep. Physics and Astronomy, 2112 E Wesley Ave, 80208 Denver, Colorado, USA Received July 13, 2011; accepted October 4, 2011 Energy-dispersive diffraction / Synchrotron radiation / Rietveld method / Line-profile analysis / Crystal microstructure Abstract. In the past two decades the energy

American Mineralogist, Volume 95, pages 19–23, 2010 0003-004X/10/0001–019$05.00/DOI: 10.2138/am.2010.3280 19 Anisotropic elasticity of jarosite: A high-P synchrotron XRD study Hongwu Xu,1,* YusHeng ZHao,2 JianZHong ZHang,2 YueJian wang,2 DonalD D. Hickmott,1 luke l. Daemen,2 monika a. Hartl,2 anD liping wang3 1Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, U.S.A. 2Los Alamos Neutron Science Center, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, U.S.A. 3Department of Geosciences

American Mineralogist, Volume 100, pages 926–934, 2015 0003-004X/15/0004–926$05.00/DOI: http://dx.doi.org/10.2138/am-2015-5093 926 * E-mail: Andrea.Gerson@unisa.edu.au Synchrotron micro-spectroscopic examination of Indonesian nickel laterites Rong Fan1 and andRea R. geRson1,* 1Minerals and Materials Science & Technology, Mawson Institute, University of South Australia, Mawson Lakes, South Australia 5095, Australia abstRact Nickel is typically distributed across several fine-grained minerals in nickel laterites, formed by intense tropical weathering of

American Mineralogist, Volume 94, pages 64–73, 2009 0003-004X/09/0001–064$05.00/DOI: 10.2138/am.2009.2914 64 Dehydration dynamics of barrerite: An in situ synchrotron XRPD study Silvia Ori, EdOardO MazzucatO, and GiOvanna vEzzalini* Dipartimento di Scienze della Terra, Largo S. Eufemia, 19, I-41100 Modena, Italy abStract The thermally induced structural modifications of the natural zeolite barrerite [Na16Al16Si56O144·52H2O, a = 13.6239(4) Å, b = 18.2033(5) Å, c = 17.8317(7) Å, V = 4422.3(3) Å3, space group Amma, frame- work type STI] were studied in a

Z. Phys. Chem. 227 (2013) 1605–1645 / DOI 10.1524/zpch.2013.0418 © by Oldenbourg Wissenschaftsverlag, München A Forty-Segment Molecular Synchrotron By Peter C. Zieger1, Chris J. Eyles1, Sebastiaan Y. T. van de Meerakker2, André J. A. van Roij2, Hendrick L. Bethlem3, and Gerard Meijer1,2,∗ 1 Fritz-Haber-Institut der Max-Planck-Gesellschaft, Faradayweg 4–6, 14195 Berlin, Germany 2 Radboud University Nijmegen, Institute for Molecules and Materials, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands 3 LaserLaB, Department of Physics and Astronomy, VU University

Notizen 607 \Iultistereo Synchrotron X-ray Topography T. Tuomi, V . K e l h ä *, K . Naukkarinen, ind M. Blomberg laboratory of Physics, Helsinki University Technology L Naturforsch. 37a, 6 0 7 - 6 1 0 (1982); eceived March 25, 1982 dedicated to Prof. G. Hildebrandt on the occasion of his >0th birthday Any two of several reflection or transmission x-ray opographs taken simultaneously with polychromatic vnchrotron radiation form a stereo pair. Multistereoscopic ransmission and reflection patterns of topographs taken rom a silicon and iron

crystalline sample (Mg159) shows many defects (Capitani * E-mail: g.capitani@geomin.uniba.it The crystal structure of a second antigorite polysome (m = 16), by single-crystal synchrotron diffraction GIAN CARLO CAPITANI1,* AND MARCELLO MELLINI2 1Dipartimento Geomineralogico, Via Orabona 4, 70125, Bari, Italy 2Dipartimento di Scienze della Terra, Via Laterina 8, 53100 Siena, Italy ABSTRACT A model for the modulated crystal structure of an antigorite polysome with m = 16 (where m is related to the number of tetrahedra spanning a wavelength along a) was reÞ ned by single

are still not well known. In this study, we used synchrotron powder X-ray dif- fraction data and Rietveld reÞ nements to better characterize the structure and behavior of sepiolite. We reÞ ned room-temperature structures for both a fully hydrated sepiolite and one for which the zeolitic H2O molecules were removed under vacuum. In the second part of our study, we used temperature-resolved real-time synchrotron X-ray powder diffraction and Rietveld reÞ nements to investigate in unprecedented detail changes in the sepiolite structure as it dehydrated from room