S. Howarth
Thallium concentration and thallium stable isotope composition of lateritic terrains
Howarth, S.; Prytulak, J.; Little, S.H.; Hammond, S.J.; Widdowson, M.
Authors
Professor Julie Prytulak julie.prytulak@durham.ac.uk
Professor
S.H. Little
S.J. Hammond
M. Widdowson
Abstract
Continental weathering plays a key role in modifying the geochemical budget of terrestrial reservoirs. Laterites are the products of extreme sub-aerial continental weathering. This study presents the first investigation of thallium (Tl) abundances and stable isotopic compositions of lateritic terrains. Two laterite profiles from India of differing protolith and age are studied. Thallium concentrations range between 7 – 244 ng/g for a basalt-based lateritic profile and 37 – 652 ng/g within a greywacke lateritic profile. The average Tl stable isotope composition of the two profiles is similar to many typical igneous materials, however, the intense tropical weathering causes a small but resolvable fractionation of Tl stable isotopes towards heavy values in the residual soils. The profiles are dominated by significant positive isotope excursions (reported as ε205Tl relative to standard NBS997) of + 3.5 ± 0.5 2sd and + 6.2 ± 0.5 2sd at the inferred palaeowater tables within both laterite profiles. These signatures likely reflect combined changes in redox state and mineralogy. Extensive mineral dissolution under through-flowing fluids alongside the formation of new phases such as phyllosilicates and Mn- and Fe- oxides and hydroxides likely account for some of the Tl mobilisation, sorption and coprecipitation. In the case of laterites, the formation of the new phases and role of surface sorption likely contribute to stable Tl isotope fractionation. The identification of strong isotope excursions at inferred palaeowater tables encourages future research to determine specific mineral phases that may drive significant fractionation of Tl stable isotopes. This study showcases the magnitude of natural variation possible in terrestrial soils. Such information is key to the nascent applications of Tl isotope compositions as tracers of anthropogenic pollution.
Citation
Howarth, S., Prytulak, J., Little, S., Hammond, S., & Widdowson, M. (2018). Thallium concentration and thallium stable isotope composition of lateritic terrains. Geochimica et Cosmochimica Acta, 239, 446-462. https://doi.org/10.1016/j.gca.2018.04.017
Journal Article Type | Article |
---|---|
Acceptance Date | Apr 16, 2018 |
Online Publication Date | Apr 25, 2018 |
Publication Date | Oct 15, 2018 |
Deposit Date | Apr 24, 2018 |
Publicly Available Date | Apr 25, 2019 |
Journal | Geochimica et Cosmochimica Acta |
Print ISSN | 0016-7037 |
Electronic ISSN | 1872-9533 |
Publisher | Meteoritical Society |
Peer Reviewed | Peer Reviewed |
Volume | 239 |
Pages | 446-462 |
DOI | https://doi.org/10.1016/j.gca.2018.04.017 |
Public URL | https://durham-repository.worktribe.com/output/1328667 |
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Publisher Licence URL
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
© 2018 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
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