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 | 149-214 |
| Number of pages | 66 |
| 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
The relatively large isotopic fractionations found for all stable isotope systems at low temperatures has attracted extensive interest in low-temperature environments, and stable Fe isotopes are no exception. The organization of this chapter starts with the continents, addressing weathering and soil-formation processes. We then move to terrestrial rivers and groundwater systems, followed by discussion of redox-stratified water bodies and their sediments, including lakes and the Black Sea. Next, we focus on modern marine sediments, which record extensive Fe biogeochemical cycling and authigenic mineral formation that is key to understanding the modern marine Fe budget.
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
- Chemistry(all)
- Spectroscopy
Sustainable Development Goals
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Iron Geochemistry: An Isotopic Perspective. Cham: Springer Nature, 2020. p. 149-214 (Advances in Isotope Geochemistry).
Research output: Chapter in book/report/conference proceeding › Contribution to book/anthology › Research › peer review
}
TY - CHAP
T1 - The modern surficial world
AU - Johnson, Clark
AU - Beard, Brian
AU - Weyer, Stefan
PY - 2020/1/10
Y1 - 2020/1/10
N2 - The relatively large isotopic fractionations found for all stable isotope systems at low temperatures has attracted extensive interest in low-temperature environments, and stable Fe isotopes are no exception. The organization of this chapter starts with the continents, addressing weathering and soil-formation processes. We then move to terrestrial rivers and groundwater systems, followed by discussion of redox-stratified water bodies and their sediments, including lakes and the Black Sea. Next, we focus on modern marine sediments, which record extensive Fe biogeochemical cycling and authigenic mineral formation that is key to understanding the modern marine Fe budget.
AB - The relatively large isotopic fractionations found for all stable isotope systems at low temperatures has attracted extensive interest in low-temperature environments, and stable Fe isotopes are no exception. The organization of this chapter starts with the continents, addressing weathering and soil-formation processes. We then move to terrestrial rivers and groundwater systems, followed by discussion of redox-stratified water bodies and their sediments, including lakes and the Black Sea. Next, we focus on modern marine sediments, which record extensive Fe biogeochemical cycling and authigenic mineral formation that is key to understanding the modern marine Fe budget.
UR - http://www.scopus.com/inward/record.url?scp=85078109824&partnerID=8YFLogxK
U2 - 10.1007/978-3-030-33828-2_5
DO - 10.1007/978-3-030-33828-2_5
M3 - Contribution to book/anthology
AN - SCOPUS:85078109824
SN - 9783030338275
T3 - Advances in Isotope Geochemistry
SP - 149
EP - 214
BT - Iron Geochemistry
PB - Springer Nature
CY - Cham
ER -