Scientific Program
Research Techniques
X-Ray Microprobe and Spectroscopy
X-ray fluorescence (XRF) microprobe allows non-destructive determination of elemental composition of samples, especially for heavy elements (Z>16). By scanning a sample in a micron-scale X-ray beam, images of elemental distribution can be made. X-ray absorption fine structure (XAFS) probes the local atomic and chemical environment of a selected atomic species by scanning the X-ray energy across the binding energy of a core electron of a selected element. X-ray absorption near-edge spectra (XANES) is sensitive to the valence state of the selected element. The extended XAFS (EXAFS) modulations in the absorption well above the X-ray absorption edge threshold give quantitative information about coordination species, number and distance of the selected element.
Interface, Surface Studies & Powder Diffraction
Surface and interface diffraction techniques are used to obtain fundamental knowledge on the structures of surfaces, how these surfaces are modified during hydroxylation and dehydroxylation processes, sorption reactions that occur on these surfaces and the role of biota in controlling the stabilization of toxins and contaminants on these surfaces.
High Pressure / High Temperature Diamond Anvil Cell
The main goal of the diamond anvil cell program is to address geochemical and geophysical problems across the entire pressure- temperature range of the Earth and other terrestrial planets.
High pressure research using diamond anvil cells (DACs) provide access to the sample volume for x-rays as low as 15 keV, allowing powder and single crystal diffraction measurements to be made. These measurements will help to unravel the chemical and physical secrets of the deep Earth including phase transitions of mantle minerals and core alloys and dynamics of core formation.
High Pressure / High Temperature Large Volume Press
The Large Volume Press (LVP) facilities hosts the following devices:
- 1000 ton multi-function press at 13-ID-D
- 250 ton multi-function press at 13-BM-D
- 230 ton Paris-Edinburgh press at 16-BM-B of HPCAT
Tomography
Tomographic imaging techniques are used to study the internal microstructures of complex materials. At GSECARS, computed microtomography is used to study a variety of geological samples. These range from the internal structures of precious samples like fossils, the distribution and location of inclusions in diamonds, the porosity and density of weathered rocks, studies of granular flow, and the transport of fluids such as water and oils in porous media.
Scientific Contacts
Matt Newville
Microprobe
(630) 252-0431
newville@cars.uchicago.edu
Tony Lanzirotti
Microprobe
(630) 252-0433
lanzirotti@uchicago.edu
Steve Sutton
Microprobe
(630) 252-0426
sutton@cars.uchicago.edu
Peter Eng
Interface / Surface Studies and Powder Diffraction
(630) 252-0424
eng@cars.uchicago.edu
Joanne Stubbs
Interface / Surface Studies and Powder Diffraction
(630) 252-0427
stubbs@cars.uchicago.edu
Vitali Prakapenka
High Pressure / High Temperature Diamond Anvil Cell (DAC)
(630) 252-0439
prakapenka@cars.uchicago.edu
Yanbin Wang
Large Volume Press (LVP)
(630) 252-0425
wang@cars.uchicago.edu
Tony Yu
Large Volume Press (LVP)
(630) 252-6148
tyu@cars.uchicago.edu
Mark Rivers
Tomography
(630) 252-0422
rivers@cars.uchicago.edu