Iron K-edge X-ray absorption spectroscopy for West African Margin, Greenland, and North Pacific sediments
Iron K-edge X-ray absorption spectroscopy for West African Margin, Greenland, and North Pacific sediments
These are iron K-edge X-ray absorption spectroscopy data (averages for 2 scans) collected at the Stanford Synchrotron Radiation Lightsource beamline 4-1, including mu collected in fluorescence mode for the sample (indicated with filepaths containing Files) and mu collected in transmission mode for the foil (indicated with filepaths containing Foils). Energy is in units of electronvolts.
Shoenfelt, Elizabeth
4651c23a-205e-45f1-8c59-aa0aeb2a676b
Winckler, Gisela
cff5621d-33ef-4562-b9dd-f6c4d863247c
Annett, Amber
de404d72-7e90-4dbd-884a-1df813808276
Hendry, Katharine
886d0da8-ae2d-4fa7-8e83-e850a6623392
Bostick, Benjamin
5826dfb0-f9ae-47c5-87a5-052d4e025539
Shoenfelt, Elizabeth
4651c23a-205e-45f1-8c59-aa0aeb2a676b
Winckler, Gisela
cff5621d-33ef-4562-b9dd-f6c4d863247c
Annett, Amber
de404d72-7e90-4dbd-884a-1df813808276
Hendry, Katharine
886d0da8-ae2d-4fa7-8e83-e850a6623392
Bostick, Benjamin
5826dfb0-f9ae-47c5-87a5-052d4e025539
(2019)
Iron K-edge X-ray absorption spectroscopy for West African Margin, Greenland, and North Pacific sediments.
Harvard Dataverse
doi:10.7910/dvn/upti67
[Dataset]
Abstract
These are iron K-edge X-ray absorption spectroscopy data (averages for 2 scans) collected at the Stanford Synchrotron Radiation Lightsource beamline 4-1, including mu collected in fluorescence mode for the sample (indicated with filepaths containing Files) and mu collected in transmission mode for the foil (indicated with filepaths containing Foils). Energy is in units of electronvolts.
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Published date: 1 January 2019
Identifiers
Local EPrints ID: 449267
URI: http://eprints.soton.ac.uk/id/eprint/449267
PURE UUID: 44c69d5f-99bd-440c-8fea-0b48b403b034
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Date deposited: 20 May 2021 16:35
Last modified: 23 Aug 2023 01:50
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Contributors
Contributor:
Elizabeth Shoenfelt
Contributor:
Gisela Winckler
Contributor:
Katharine Hendry
Contributor:
Benjamin Bostick
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