Synchrotron X‐ray fluorescence spectroscopy of salts in natural sea ice
We describe the use of synchrotron‐based X‐ray fluorescence spectroscopy to examine the microstructural location of specific elements, primarily salts, in sea ice. This work was part of an investigation of the location of bromine in the sea ice‐snowpack‐blowing snow system, where it plays a part in...
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Published in | Earth and space science (Hoboken, N.J.) Vol. 3; no. 11; pp. 463 - 479 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Hoboken
John Wiley & Sons, Inc
01.11.2016
American Geophysical Union (AGU) |
Subjects | |
Online Access | Get full text |
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Summary: | We describe the use of synchrotron‐based X‐ray fluorescence spectroscopy to examine the microstructural location of specific elements, primarily salts, in sea ice. This work was part of an investigation of the location of bromine in the sea ice‐snowpack‐blowing snow system, where it plays a part in the heterogeneous chemistry that contributes to tropospheric ozone depletion episodes. We analyzed samples at beamline 13‐ID‐E of the Advanced Photon Source at Argonne National Laboratory. Using an 18 keV incident energy beam, we produced elemental maps of salts for sea ice samples from the Ross Sea, Antarctica. The distribution of salts in sea ice depends on ice type. In our columnar ice samples, Br was located in parallel lines spaced roughly 0.5 mm apart, corresponding to the spacing of lamellae in the skeletal region during initial ice growth. The maps revealed concentrations of Br in linear features in samples from all but the topmost and bottommost depths. For those samples, the maps revealed rounded features. Calibration of the Br elemental maps showed bulk concentrations to be 5–10 g/m3, with concentrations ten times larger in the linear features. Through comparison with horizontal thin sections, we could verify that these linear features were brine sheets or layers.
Plain Language Summary
Synchrotron‐based X‐ray fluorescence spectroscopy at the Advanced Photon Source at the Argonne National Laboratory is used to examine the microstructural location of specific elements, particularly Br, in Antarctic sea ice. In columnar ice, Br concentrations were ten times larger in parallel lines spaced ~0.5 mm apart than in the sampled area as a whole. Through comparison with thin sections, we verified that these linear features were brine sheets or layers formed as the ice grew.
Key Points
Synchrotron X‐ray fluorescence spectroscopy maps salts in sea ice
Bromine concentration in brine inclusions is ten times the bulk concentration |
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Bibliography: | USDOE Office of Science (SC), Basic Energy Sciences (BES) National Science Foundation (NSF) FG02-94ER14466; OPP-1043145; EAR-1128799 |
ISSN: | 2333-5084 2333-5084 |
DOI: | 10.1002/2016EA000172 |