First experimental results from IBM/TENN/TULANE/LLNL/LBL undulator beamline at the advanced light source
- Department of Physics, University of Tennessee, Knoxville, Tennessee 37996 (United States)
- IBM T. J. Watson Research Center, Yorktown Heights, New York 10598 (United States)
- IBM Almaden Research Center, San Jose, California 95120 (United States)
- Department of Physics, Tulane University, New Orleans, Louisiana 70118 (United States)
- Lawrence Livermore National Laboratory, Livermore, California 94550 (United States)
- Lawrence Berkeley Laboratory, Berkeley, California 94720 (United States)
The IBM/TENN/TULANE/LLNL/LBL Beamline 8.0 at the advanced light source combining a 5.0 cm, 89 period undulator with a high-throughput, high-resolution spherical grating monochromator, provides a powerful excitation source over a spectral range of 70--1200 eV for surface physics and material science research. The beamline progress and the first experimental results obtained with a fluorescence end station on graphite and titanium oxides are presented here. The dispersive features in K emission spectra of graphite excited near threshold, and found a clear relationship between them and graphite band structure are observed. The monochromator is operated at a resolving power of roughly 2000, while the spectrometer has a resolving power of 400 for these fluorescence experiments.
- DOE Contract Number:
- AC03-76SF00098; W-7405-ENG-48
- OSTI ID:
- 6851213
- Journal Information:
- Review of Scientific Instruments; (United States), Vol. 66:2; ISSN 0034-6748
- Country of Publication:
- United States
- Language:
- English
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SUPERCONDUCTIVITY AND SUPERFLUIDITY
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ADVANCED LIGHT SOURCE
USES
GRAPHITE
X-RAY SPECTRA
TITANIUM OXIDES
ELECTRONIC STRUCTURE
FLUORESCENCE
LAWRENCE BERKELEY LABORATORY
LAWRENCE LIVERMORE LABORATORY
ONDULATOR RADIATION
PROGRESS REPORT
BREMSSTRAHLUNG
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ELEMENTAL MINERALS
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NATIONAL ORGANIZATIONS
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OXIDES
OXYGEN COMPOUNDS
RADIATION SOURCES
RADIATIONS
SPECTRA
SYNCHROTRON RADIATION SOURCES
TITANIUM COMPOUNDS
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US AEC
US DOE
US ERDA
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