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Abstract
Soil samples analyzed via Mössbauer spectroscopy at three temperatures (295K, 77K and 4.2K). In each case the sample is loaded into the machine without prior modification (no grinding) to an ideal thickness based on the amount of iron in the sample. Transmission 57Fe Mössbauer spectroscopy was performed with a variable temperature He-cooled system with a 1024 channel detector. A 57Co source (~50 mCi) embedded in a Rh matrix was used at room temperature. Samples were mounted between two pieces of 0.127 mm thickness Kapton tape. In some cases, this was done inside an anoxic glovebox, and transferred immediately to the spectrometer cryostat to avoid sample oxidation prior to analysis. In other cases dried samples were used. The velocity (i.e., gamma-ray energy) was calibrated using α-Fe foil at 298 K. The transducer was operated in constant acceleration mode and folding was performed against the calibrated Fe foil to achieve a flat background. The raw sample files here are folded spectra using the most recent collected calibration standard. Data collection times are typically 24 h per sample per temperature, however can be longer/shorter in samples with less/more iron concentration.
Subject Keywords
Coverage
Spatial
Temporal
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Content
ReadMe.md
CCZO -- Soil Geochemistry -- Mössbauer spectroscopy -- Calhoun CZO -- (2015)
OVERVIEW
Description/Abstract
Soil samples analyzed via Mössbauer spectroscopy at three temperatures (295K, 77K and 4.2K). In each case the sample is loaded into the machine without prior modification (no grinding) to an ideal thickness based on the amount of iron in the sample. Transmission 57Fe Mössbauer spectroscopy was performed with a variable temperature He-cooled system with a 1024 channel detector. A 57Co source (~50 mCi) embedded in a Rh matrix was used at room temperature. Samples were mounted between two pieces of 0.127 mm thickness Kapton tape. In some cases, this was done inside an anoxic glovebox, and transferred immediately to the spectrometer cryostat to avoid sample oxidation prior to analysis. In other cases dried samples were used. The velocity (i.e., gamma-ray energy) was calibrated using α-Fe foil at 298 K. The transducer was operated in constant acceleration mode and folding was performed against the calibrated Fe foil to achieve a flat background. The raw sample files here are folded spectra using the most recent collected calibration standard. Data collection times are typically 24 h per sample per temperature, however can be longer/shorter in samples with less/more iron concentration.
Creator/Author
Thompson, Aaron|Richter, Daniel deB.|Wilmoth, Jared|Barcellos, Diego
CZOs
Calhoun
Contact
Aaron Thompson, University of Georgia, AaronT@uga.edu; 706-410-1293
Subtitle
Soil depth: Enriched Fe horizon
SUBJECTS
Disciplines
Biogeochemistry|Soil Science / Pedology
Topics
Soil Geochemistry
Subtopic
Mössbauer spectroscopy
Keywords
Iron|soil|Calhoun
Variables
Velocity (mm/s)|intensity (counts)
Variables ODM2
Iron Fractionation|Velocity
TEMPORAL
Date Start
2015-05-01
Date End
2015-12-31
SPATIAL
Field Areas
Calhoun Long-Term Soil-Ecosystem Plots and Reference Areas
Location
Calhoun CZO
North latitude
34.60803
South latitude
34.60803
West longitude
-81.722091
East longitude
-81.722091
REFERENCE
Publications of this data
Thompson A, Barcellos D, Wilmoth J, & Richter D (2015). Depth Variation of Soil Iron Crystallinity at the Calhoun Critical Zone Observatory. Goldschmidt Conference, Prague, CZ
Thompson, A., Barcellos, D., Wilmoth, J., and Richter, D. (2015). Depth Variation of Soil Iron Crystallinity at the Calhoun Critical Zone Observatory. Calhoun CZO 2015 Summer Science Meeting
CZO ID
4678
COMMENTS
Comments
Soil samples of enriched and depleted iron horizons were collected previously by Dan Richter and passed to Aaron Thompson in 2015. Each sample was previously air-dried. Dried samples were loaded into the Mössbauer spec. at the University of Georgia, located in Barrow Hall on the main Athens campus and each sample was analyzed for ~24h at three temperatures (295K, 77K and 4.2K). Samples from the upper two horizons did not have sufficient iron to collect quality spectrum.
Additional Metadata
Name | Value |
---|---|
czos | Calhoun |
czo_id | 4678 |
comments | Soil samples of enriched and depleted iron horizons were collected previously by Dan Richter and passed to Aaron Thompson in 2015. Each sample was previously air-dried. Dried samples were loaded into the Mössbauer spec. at the University of Georgia, located in Barrow Hall on the main Athens campus and each sample was analyzed for ~24h at three temperatures (295K, 77K and 4.2K). Samples from the upper two horizons did not have sufficient iron to collect quality spectrum. |
keywords | Iron, soil, Calhoun |
subtitle | Soil depth: Enriched Fe horizon |
variables | Velocity (mm/s), intensity (counts) |
disciplines | Biogeochemistry, Soil Science / Pedology |
Related Resources
This resource is referenced by | Thompson A, Barcellos D, Wilmoth J, & Richter D (2015). Depth Variation of Soil Iron Crystallinity at the Calhoun Critical Zone Observatory. Goldschmidt Conference, Prague, CZ |
This resource is referenced by | Thompson, A., Barcellos, D., Wilmoth, J., and Richter, D. (2015). Depth Variation of Soil Iron Crystallinity at the Calhoun Critical Zone Observatory. Calhoun CZO 2015 Summer Science Meeting |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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