Details
| Original language | English |
|---|---|
| Title of host publication | Iron Geochemistry |
| Subtitle of host publication | An Isotopic Perspective |
| Place of Publication | Cham |
| Publisher | Springer Nature |
| Pages | 17-38 |
| Number of pages | 22 |
| ISBN (electronic) | 9783030338282 |
| ISBN (print) | 9783030338275 |
| Publication status | Published - 10 Jan 2020 |
Publication series
| Name | Advances in Isotope Geochemistry |
|---|---|
| ISSN (Print) | 2364-5105 |
| ISSN (electronic) | 2364-5113 |
Abstract
Iron has four naturally occurring stable isotopes: 54Fe (5.85%), 56Fe (91.75%), 57Fe (2.12%) and 58Fe (0.28%) and its isotopic composition has been of interest since the invention of isotope ratio mass spectrometry. For example, Fe isotopes have been used to evaluate if extra-terrestrial Fe has the same isotope composition of terrestrial Fe (Valley and Anderson 1947), how Fe is cycled in the human body (Tang and Trassy 1986; Walczyk 1997), and the extent to which Fe is fractionated by geological processes (Beard and Johnson 1999; Bullen et al. 2001; Dixon et al. 1992). In this chapter, we discuss how Fe isotope analyses are conducted, with an emphasis on the methods used to ensure accurate Fe isotope analysis.
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
- Chemistry(all)
- Spectroscopy
Cite this
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Iron Geochemistry: An Isotopic Perspective. Cham: Springer Nature, 2020. p. 17-38 (Advances in Isotope Geochemistry).
Research output: Chapter in book/report/conference proceeding › Contribution to book/anthology › Research › peer review
}
TY - CHAP
T1 - Analytical methods
AU - Johnson, Clark
AU - Beard, Brian
AU - Weyer, Stefan
PY - 2020/1/10
Y1 - 2020/1/10
N2 - Iron has four naturally occurring stable isotopes: 54Fe (5.85%), 56Fe (91.75%), 57Fe (2.12%) and 58Fe (0.28%) and its isotopic composition has been of interest since the invention of isotope ratio mass spectrometry. For example, Fe isotopes have been used to evaluate if extra-terrestrial Fe has the same isotope composition of terrestrial Fe (Valley and Anderson 1947), how Fe is cycled in the human body (Tang and Trassy 1986; Walczyk 1997), and the extent to which Fe is fractionated by geological processes (Beard and Johnson 1999; Bullen et al. 2001; Dixon et al. 1992). In this chapter, we discuss how Fe isotope analyses are conducted, with an emphasis on the methods used to ensure accurate Fe isotope analysis.
AB - Iron has four naturally occurring stable isotopes: 54Fe (5.85%), 56Fe (91.75%), 57Fe (2.12%) and 58Fe (0.28%) and its isotopic composition has been of interest since the invention of isotope ratio mass spectrometry. For example, Fe isotopes have been used to evaluate if extra-terrestrial Fe has the same isotope composition of terrestrial Fe (Valley and Anderson 1947), how Fe is cycled in the human body (Tang and Trassy 1986; Walczyk 1997), and the extent to which Fe is fractionated by geological processes (Beard and Johnson 1999; Bullen et al. 2001; Dixon et al. 1992). In this chapter, we discuss how Fe isotope analyses are conducted, with an emphasis on the methods used to ensure accurate Fe isotope analysis.
UR - http://www.scopus.com/inward/record.url?scp=85078079268&partnerID=8YFLogxK
U2 - 10.1007/978-3-030-33828-2_2
DO - 10.1007/978-3-030-33828-2_2
M3 - Contribution to book/anthology
AN - SCOPUS:85078079268
SN - 9783030338275
T3 - Advances in Isotope Geochemistry
SP - 17
EP - 38
BT - Iron Geochemistry
PB - Springer Nature
CY - Cham
ER -