Temperature and structure measurements of heavy-ion-heated diamond using in situ X-ray diagnostics

Author:

Lütgert J.1ORCID,Hesselbach P.23ORCID,Schörner M.1ORCID,Bagnoud V.2ORCID,Belikov R.4ORCID,Drechsel P.2,Heuser B.15ORCID,Humphries O. S.56ORCID,Katrik P.2ORCID,Lindqvist B.1ORCID,Qu C.1ORCID,Redmer R.1ORCID,Riley D.7ORCID,Schaumann G.8ORCID,Schumacher S.1ORCID,Tauschwitz A.2ORCID,Varentsov D.2ORCID,Weyrich K.2ORCID,Yu X.29,Zielbauer B.2ORCID,Major Zs.1210ORCID,Neumayer P.2ORCID,Kraus D.15ORCID

Affiliation:

1. Institut für Physik, Universität Rostock 1 , Albert-Einstein-Str. 23, 18059 Rostock, Germany

2. GSI Helmholtzzentrum für Schwerionenforschung 2 , Planckstr. 1, 64291 Darmstadt, Germany

3. Institut für Angewandte Physik, Goethe-Universität Frankfurt am Main 3 , Max-von-Laue-Str. 1, 60438 Frankfurt am Main, Germany

4. Institut für Geowissenschaften, Goethe-Universität Frankfurt am Main 4 , Altenhöferallee 1, 60438 Frankfurt am Main, Germany

5. Helmholtz-Zentrum Dresden-Rossendorf 5 , Bautzner Landstr. 400, 01328 Dresden, Germany

6. European XFEL GmbH 6 , Holzkoppel 4, 22869 Schenefeld, Germany

7. Centre for Plasma Physics, School of Mathematics and Physics, Queen’s University Belfast 7 , University Road, Belfast BT7 1NN, United Kingdom

8. Institut für Kernphysik, Technische Universität Darmstadt 8 , Schlossgartenstr. 9, 64289 Darmstadt, Germany

9. State Key Laboratory of Nuclear Physics and Technology, Institute of Heavy Ion Physics, Peking University 9 , Beijing 100871, China

10. Helmholtz Institut Jena 10 , Fröbelstieg 3, 07743 Jena, Germany

Abstract

We present in situ measurements of spectrally resolved X-ray scattering and X-ray diffraction from monocrystalline diamond samples heated with an intense pulse of heavy ions. In this way, we determine the samples’ heating dynamics and their microscopic and macroscopic structural integrity over a timespan of several microseconds. Connecting the ratio of elastic to inelastic scattering with state-of-the-art density functional theory molecular dynamics simulations allows the inference of average temperatures around 1300 K, in agreement with predictions from stopping power calculations. The simultaneous diffraction measurements show no hints of any volumetric graphitization of the material, but do indicate the onset of fracture in the diamond sample. Our experiments pave the way for future studies at the Facility for Antiproton and Ion Research, where a substantially increased intensity of the heavy ion beam will be available.

Funder

GSI Helmholtzzentrum für Schwerionenforschung

Deutsche Forschungsgemeinschaft

Bundesministerium für Bildung und Forschung

Helmholtz Association

Publisher

AIP Publishing

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