TY  - THES
A1  - Schreiber, J.
A1  - Stahn, R.
A1  - Schenk, Jörg A.
A1  - Karsten, U.
A1  - Pecher, Gabriele
T1  - Binding of tumor antigen mucin (MUC1) derived peptides to the heat shock protein DnaK
Y1  - 2000
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  - 
TY  - JOUR
A1  - Kowarik, Stefan
A1  - Gerlach, Andreas
A1  - Leitenberger, Wolfram
A1  - Hu J, Witte
A1  - Wöll, Christoph
A1  - Schreiber, Frank
T1  - Energy-dispersive X-ray reflectivity and GID for real-time growth studies of pentacene thin films
N2  - We use energy-dispersive X-ray reflectivity and grazing incidence diffraction (GID) to follow the growth of the crystalline organic semiconductor pentacene on silicon oxide in-situ and in real-time. The technique allows for monitoring Bragg reflections and measuring X-ray growth oscillations with a time resolution of 1 min in a wide q-range in reciprocal space extending over 0.25-0.80 angstrom(-1), i.e. sampling a large number of Fourier components simultaneously. A quantitative analysis of growth oscillations at several q-points yields the evolution of the surface roughness, showing a marked transition from layer-by-layer growth to strong roughening after four monolayers of pentacene have been deposited. (c) 2006 Elsevier B.V. All rights reserved.
Y1  - 2007
UR  - http://www.sciencedirect.com/science/journal/00406090
U6  - https://doi.org/10.1016/j.tsf.2006.12.020
SN  - 0040-6090
ER  -