Abstract
The magnetite/maghemite content within iron oxide nanoparticles can be determined using the mean isomer shift (δ¯¯). However, accurate characterisation of the composition is limited by the uncertainty associated with δ¯¯.
We have identified four independent sources of uncertainty and
developed a quantitative expression for the uncertainty budget. Sources
of uncertainty are categorised as follows: that from the fitting of the
Mössbauer spectrum (σ
fit), that of the calibration of the α-Fe reference spectrum (σ
cal), thermal corrections to the spectrum due to second order Doppler shift (SODS) (σ
Δδ
) and other experimental errors (σ
err). Each contribution is discussed in detail using 57Fe
Mössbauer spectra obtained from an iron oxide nanoparticle system at
temperatures between 16 K and 295 K on different spectrometers in two
different laboratories.
Original language | English |
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Journal | Hyperfine Interactions |
Volume | 237 |
Issue number | 1 |
Pages (from-to) | 23 |
Number of pages | 11 |
ISSN | 0304-3843 |
DOIs | |
Publication status | Published - 2016 |
Event | The International Conference on the Applications of the Mössbauer Effect - Hamburg, Germany Duration: 13 Sept 2015 → 18 Sept 2015 |
Conference
Conference | The International Conference on the Applications of the Mössbauer Effect |
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Country/Territory | Germany |
City | Hamburg |
Period | 13/09/2015 → 18/09/2015 |
Bibliographical note
This article is part of the Topical Collection on Proceedings of the International Conference on the Applications of the Mössbauer Effect (ICAME 2015), Hamburg, Germany, 13–18 September 2015Keywords
- 57Fe Mössbauer
- Isomer shift
- Second order Doppler shift
- Uncertainty budget