V. Magni
Deep water recycling through time
Magni, V.; Bouilhol, P.; van Hunen, J.
Abstract
We investigate the dehydration processes in subduction zones and their implications for the water cycle throughout Earth's history. We use a numerical tool that combines thermo-mechanical models with a thermodynamic database to examine slab dehydration for present-day and early Earth settings and its consequences for the deep water recycling. We investigate the reactions responsible for releasing water from the crust and the hydrated lithospheric mantle and how they change with subduction velocity (vs), slab age (a) and mantle temperature (Tm). Our results show that faster slabs dehydrate over a wide area: they start dehydrating shallower and they carry water deeper into the mantle. We parameterize the amount of water that can be carried deep into the mantle, W (×105 kg/m2), as a function of vs (cm/yr), a (Myrs), and Tm (°C): inline image. We generally observe that a 1) 100°C increase in the mantle temperature, or 2) ∼15 Myr decrease of plate age, or 3) decrease in subduction velocity of ∼2 cm/yr all have the same effect on the amount of water retained in the slab at depth, corresponding to a decrease of ∼2.2×105 kg/m2 of H2O. We estimate that for present-day conditions ∼26% of the global influx water, or 7×108 Tg/Myr of H2O, is recycled into the mantle. Using a realistic distribution of subduction parameters, we illustrate that deep water recycling might still be possible in early Earth conditions, although its efficiency would generally decrease. Indeed, 0.5–3.7 × 108 Tg/Myr of H2O could still be recycled in the mantle at 2.8 Ga.
Citation
Magni, V., Bouilhol, P., & van Hunen, J. (2014). Deep water recycling through time. Geochemistry, Geophysics, Geosystems, 15(11), 4203-4216. https://doi.org/10.1002/2014gc005525
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 8, 2014 |
Publication Date | Nov 10, 2014 |
Deposit Date | Dec 18, 2014 |
Publicly Available Date | Apr 13, 2015 |
Journal | Geochemistry, Geophysics, Geosystems |
Electronic ISSN | 1525-2027 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 15 |
Issue | 11 |
Pages | 4203-4216 |
DOI | https://doi.org/10.1002/2014gc005525 |
Keywords | Deep water recycling, Subduction zone processes, Dehydration reactions, Water cycle, Modeling, Early Earth. |
Public URL | https://durham-repository.worktribe.com/output/1447939 |
Files
Published Journal Article
(1.6 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
© 2014. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.
You might also like
Delamination vs. break-off: the fate of continental collision
(2013)
Journal Article
Numerical models of slab migration in continental collision zones
(2012)
Journal Article
A numerical approach to melting in warm subduction zones
(2014)
Journal Article
Isotopic evidence for iron mobility during subduction
(2016)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2025
Advanced Search