Mineralogy-based global anthropogenic combustion-iron emission inventory

Total and soluble iron modulate ocean biogeochemistry and global nitrogen and carbon cycle in over 40% of global ocean. The understanding of the current and future changes in oceanic productivity can be improved by understanding and constraining the atmospheric inputs of iron. Models generally agree...

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Bibliographic Details
Main Author: Rathod, Sagar Dilipbhai
Other Authors: Bond, Tami C
Format: Thesis
Language:English
Published: 2021
Subjects:
Online Access:http://hdl.handle.net/2142/105958
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spelling ftunivillidea:oai:www.ideals.illinois.edu:2142/105958 2023-05-15T18:24:55+02:00 Mineralogy-based global anthropogenic combustion-iron emission inventory Rathod, Sagar Dilipbhai Bond, Tami C 2021-11-26T20:59:54Z application/pdf http://hdl.handle.net/2142/105958 en eng http://hdl.handle.net/2142/105958 Copyright 2019 Sagar Rathod iron emissions ocean biogeochemistry dust industrial Thesis text 2021 ftunivillidea 2019-11-30T23:27:49Z Total and soluble iron modulate ocean biogeochemistry and global nitrogen and carbon cycle in over 40% of global ocean. The understanding of the current and future changes in oceanic productivity can be improved by understanding and constraining the atmospheric inputs of iron. Models generally agree with observations for total and soluble atmospheric iron concentrations over oceans except in the iron limited Southern Ocean where they underestimate by two to five orders of magnitudes. Anthropogenic combustion-iron emissions are thought to be the missing link in some of the ocean regions and are currently underestimated in inventories along with a poor fuel-based solubility representation approach in contrast to dust-iron emissions which are better constrained and have mineralogy-based solubility approach. Here we show that anthropogenic combustion-iron emissions can be about 1 Tg Fe/yr in the fine fraction, 10 times higher than all previous inventories. A large part of the difference is attributed to metal smelting which was not accounted for in previous inventories. Anthropogenic combustion-iron contributes 30-50% of the total and soluble iron to the iron limited North and Equatorial Pacific Ocean and less than 10% to the Southern Ocean. Modeled estimates agree with observations everywhere except in the Southern Ocean where the underestimation persists even with the realistic maximum anthropogenic emissions. For the first time, we represent anthropogenic combustion-iron as a function of its mineral components and transition from a fuel-specific solubility to a mineralogy-based solubility approach. We find that increasing complexity in representing anthropogenic combustion-iron solubility does not necessarily improve model-observation comparison. Limited Author requested closed access (OA after 2yrs) in Vireo ETD system Thesis Southern Ocean University of Illinois at Urbana-Champaign: IDEALS (Illinois Digital Environment for Access to Learning and Scholarship) Pacific Southern Ocean
institution Open Polar
collection University of Illinois at Urbana-Champaign: IDEALS (Illinois Digital Environment for Access to Learning and Scholarship)
op_collection_id ftunivillidea
language English
topic iron
emissions
ocean
biogeochemistry
dust
industrial
spellingShingle iron
emissions
ocean
biogeochemistry
dust
industrial
Rathod, Sagar Dilipbhai
Mineralogy-based global anthropogenic combustion-iron emission inventory
topic_facet iron
emissions
ocean
biogeochemistry
dust
industrial
description Total and soluble iron modulate ocean biogeochemistry and global nitrogen and carbon cycle in over 40% of global ocean. The understanding of the current and future changes in oceanic productivity can be improved by understanding and constraining the atmospheric inputs of iron. Models generally agree with observations for total and soluble atmospheric iron concentrations over oceans except in the iron limited Southern Ocean where they underestimate by two to five orders of magnitudes. Anthropogenic combustion-iron emissions are thought to be the missing link in some of the ocean regions and are currently underestimated in inventories along with a poor fuel-based solubility representation approach in contrast to dust-iron emissions which are better constrained and have mineralogy-based solubility approach. Here we show that anthropogenic combustion-iron emissions can be about 1 Tg Fe/yr in the fine fraction, 10 times higher than all previous inventories. A large part of the difference is attributed to metal smelting which was not accounted for in previous inventories. Anthropogenic combustion-iron contributes 30-50% of the total and soluble iron to the iron limited North and Equatorial Pacific Ocean and less than 10% to the Southern Ocean. Modeled estimates agree with observations everywhere except in the Southern Ocean where the underestimation persists even with the realistic maximum anthropogenic emissions. For the first time, we represent anthropogenic combustion-iron as a function of its mineral components and transition from a fuel-specific solubility to a mineralogy-based solubility approach. We find that increasing complexity in representing anthropogenic combustion-iron solubility does not necessarily improve model-observation comparison. Limited Author requested closed access (OA after 2yrs) in Vireo ETD system
author2 Bond, Tami C
format Thesis
author Rathod, Sagar Dilipbhai
author_facet Rathod, Sagar Dilipbhai
author_sort Rathod, Sagar Dilipbhai
title Mineralogy-based global anthropogenic combustion-iron emission inventory
title_short Mineralogy-based global anthropogenic combustion-iron emission inventory
title_full Mineralogy-based global anthropogenic combustion-iron emission inventory
title_fullStr Mineralogy-based global anthropogenic combustion-iron emission inventory
title_full_unstemmed Mineralogy-based global anthropogenic combustion-iron emission inventory
title_sort mineralogy-based global anthropogenic combustion-iron emission inventory
publishDate 2021
url http://hdl.handle.net/2142/105958
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation http://hdl.handle.net/2142/105958
op_rights Copyright 2019 Sagar Rathod
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