TY - GEN A1 - Spiekermann, Georg A1 - Harder, M. A1 - Gilmore, Keith A1 - Zalden, Peter A1 - Sahle, Christoph J. A1 - Petitgirard, Sylvain A1 - Wilke, Max A1 - Biedermann, Nicole A1 - Weis, Thomas A1 - Morgenroth, Wolfgang A1 - Tse, John S. A1 - Kulik, E. A1 - Nishiyama, Norimasa A1 - Yavaş, Hasan A1 - Sternemann, Christian T1 - Persistent Octahedral Coordination in Amorphous GeO₂ Up to 100 GPa by Kβ'' X-Ray Emission Spectroscopy T2 - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe N2 - We measure valence-to-core x-ray emission spectra of compressed crystalline GeO₂ up to 56 GPa and of amorphous GeO₂ up to 100 GPa. In a novel approach, we extract the Ge coordination number and mean Ge-O distances from the emission energy and the intensity of the Kβ'' emission line. The spectra of high-pressure polymorphs are calculated using the Bethe-Salpeter equation. Trends observed in the experimental and calculated spectra are found to match only when utilizing an octahedral model. The results reveal persistent octahedral Ge coordination with increasing distortion, similar to the compaction mechanism in the sequence of octahedrally coordinated crystalline GeO₂ high-pressure polymorphs. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 699 KW - rutile-type KW - glass KW - crystalline KW - pressures KW - complexes KW - silicon KW - oxygen KW - SIO₂ KW - MO KW - CU Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-427755 SN - 1866-8372 IS - 699 ER - TY - JOUR A1 - Spiekermann, Georg A1 - Harder, M. A1 - Gilmore, Keith A1 - Zalden, Peter A1 - Sahle, Christoph J. A1 - Petitgirard, Sylvain A1 - Wilke, Max A1 - Biedermann, Nicole A1 - Weis, Thomas A1 - Morgenroth, Wolfgang A1 - Tse, John S. A1 - Kulik, E. A1 - Nishiyama, Norimasa A1 - Yavaş, Hasan A1 - Sternemann, Christian T1 - Persistent Octahedral Coordination in Amorphous GeO₂ Up to 100 GPa by Kβ'' X-Ray Emission Spectroscopy JF - Physical Review X N2 - We measure valence-to-core x-ray emission spectra of compressed crystalline GeO₂ up to 56 GPa and of amorphous GeO₂ up to 100 GPa. In a novel approach, we extract the Ge coordination number and mean Ge-O distances from the emission energy and the intensity of the Kβ'' emission line. The spectra of high-pressure polymorphs are calculated using the Bethe-Salpeter equation. Trends observed in the experimental and calculated spectra are found to match only when utilizing an octahedral model. The results reveal persistent octahedral Ge coordination with increasing distortion, similar to the compaction mechanism in the sequence of octahedrally coordinated crystalline GeO₂ high-pressure polymorphs. KW - rutile-type KW - glass KW - crystalline KW - pressures KW - complexes KW - silicon KW - oxygen KW - SIO₂ KW - MO KW - CU Y1 - 2019 U6 - https://doi.org/10.1103/PhysRevX.9.011025 SN - 2469-9926 SN - 0556-2791 SN - 1050-2947 SN - 1094-1622 VL - 9 IS - 1 PB - American Physical Society by the American Institute of Physics CY - Melville, NY ER - TY - JOUR A1 - Niskanen, Johannes A1 - Fondell, Mattis A1 - Sahle, Christoph J. A1 - Eckert, Sebastian A1 - Jay, Raphael Martin A1 - Gilmore, Keith A1 - Pietzsch, Annette A1 - Dantz, Marcus A1 - Lu, Xingye A1 - McNally, Daniel E. A1 - Schmitt, Thorsten A1 - Vaz da Cruz, Vinicius A1 - Kimberg, Victor A1 - Föhlisch, Alexander A1 - Gel’mukhanov, Faris T1 - Compatibility of quantitative X-ray spectroscopy with continuous distribution models of water at ambient conditions JF - Proceedings of the National Academy of Sciences of the United States of America N2 - The phase diagram of water harbors controversial views on underlying structural properties of its constituting molecular moieties, its fluctuating hydrogen-bonding network, as well as pair-correlation functions. In this work, long energy-range detection of the X-ray absorption allows us to unambiguously calibrate the spectra for water gas, liquid, and ice by the experimental atomic ionization cross-section. In liquid water, we extract the mean value of 1.74 +/- 2.1% donated and accepted hydrogen bonds per molecule, pointing to a continuous-distribution model. In addition, resonant inelastic X-ray scattering with unprecedented energy resolution also supports continuous distribution of molecular neighborhoods within liquid water, as do X-ray emission spectra once the femtosecond scattering duration and proton dynamics in resonant X-ray-matter interaction are taken into account. Thus, X-ray spectra of liquid water in ambient conditions can be understood without a two-structure model, whereas the occurrence of nanoscale-length correlations within the continuous distribution remains open. KW - structure of water KW - X-ray spectroscopy KW - continuous distribution model Y1 - 2019 U6 - https://doi.org/10.1073/pnas.1815701116 SN - 0027-8424 VL - 116 IS - 10 SP - 4058 EP - 4063 PB - National Acad. of Sciences CY - Washington ER - TY - GEN A1 - Niskanen, Johannes A1 - Fondell, Mattis A1 - Sahle, Christoph J. A1 - Eckert, Sebastian A1 - Jay, Raphael Martin A1 - Gilmore, Keith A1 - Pietzsch, Annette A1 - Dantz, Marcus A1 - Lu, Xingye A1 - McNally, Daniel E. A1 - Schmitt, Thorsten A1 - Vaz da Cruz, Vinicius A1 - Kimberg, Victor A1 - Föhlisch, Alexander T1 - Reply to Pettersson et al.: Why X-ray spectral features are compatible to continuous distribution models in ambient water T2 - Proceedings of the National Academy of Sciences of the United States of America Y1 - 2019 U6 - https://doi.org/10.1073/pnas.1909551116 SN - 0027-8424 VL - 116 IS - 35 SP - 17158 EP - 17159 PB - National Acad. of Sciences CY - Washington ER - TY - JOUR A1 - Kaa, Johannes M. A1 - Sternemann, Christian A1 - Appel, Karen A1 - Cerantola, Valerio A1 - Preston, Thomas R. A1 - Albers, Christian A1 - Elbers, Mirko A1 - Libon, Lelia A1 - Makita, Mikako A1 - Pelka, Alexander A1 - Petitgirard, Sylvain A1 - Plückthun, Christian A1 - Roddatis, Vladimir A1 - Sahle, Christoph J. A1 - Spiekermann, Georg A1 - Schmidt, Christian A1 - Schreiber, Anja A1 - Sakrowski, Robin A1 - Tolan, Metin A1 - Wilke, Max A1 - Zastrau, Ulf A1 - Konopkova, Zuzana T1 - Structural and electron spin state changes in an x-ray heated iron carbonate system at the Earth's lower mantle pressures JF - Physical review research N2 - The determination of the spin state of iron-bearing compounds at high pressure and temperature is crucial for our understanding of chemical and physical properties of the deep Earth. Studies on the relationship between the coordination of iron and its electronic spin structure in iron-bearing oxides, silicates, carbonates, iron alloys, and other minerals found in the Earth's mantle and core are scarce because of the technical challenges to simultaneously probe the sample at high pressures and temperatures. We used the unique properties of a pulsed and highly brilliant x-ray free electron laser (XFEL) beam at the High Energy Density (HED) instrument of the European XFEL to x-ray heat and probe samples contained in a diamond anvil cell. We heated and probed with the same x-ray pulse train and simultaneously measured x-ray emission and x-ray diffraction of an FeCO3 sample at a pressure of 51 GPa with up to melting temperatures. We collected spin state sensitive Fe K beta(1,3) fluorescence spectra and detected the sample's structural changes via diffraction, observing the inverse volume collapse across the spin transition. During x-ray heating, the carbonate transforms into orthorhombic Fe4C3O12 and iron oxides. Incipient melting was also observed. This approach to collect information about the electronic state and structural changes from samples contained in a diamond anvil cell at melting temperatures and above will considerably improve our understanding of the structure and dynamics of planetary and exoplanetary interiors. Y1 - 2022 U6 - https://doi.org/10.1103/PhysRevResearch.4.033042 SN - 2643-1564 VL - 4 IS - 3 PB - American Physical Society CY - College Park ER -