Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia
Rivers are significant contributors of Fe to theocean. However, the characteristics of chemically reactive Fe remain poorly constrained, especially in large Arctic rivers, which drain landscapes highly susceptible to climate change and carbon cycle alteration. The aim of this study was a detailed ch...
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Naturhistoriska riksmuseet, Enheten för geovetenskap
2017
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ftnrm:oai:DiVA.org:nrm-2470 2024-09-15T17:54:10+00:00 Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia Hirst, Catherine Andersson, Per Shaw, Samuel Burke, Ian Kutscher, Liselott Murphy, Melissa Maximov, Trofim Pokrovsky, Oleg Mörth, Carl-Magnus Porcelli, Don 2017 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-2470 https://doi.org/10.1016/j.gca.2017.07.012 eng eng Naturhistoriska riksmuseet, Enheten för geovetenskap University of Manchester University of Leeds Oxford University Institute for Biological Problems of the Cryolithozone, Siberian Branch of the Russian Academy of Sciences, Yakutsk University of Toulouse Stockholm University Cambridge Geochimica et Cosmochimica Acta, 0016-7037, 2017, 213, s. 553-573 info:eu-repo/grantAgreement/EC/FP7/290336 orcid:0000-0002-1752-6469 http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-2470 doi:10.1016/j.gca.2017.07.012 info:eu-repo/semantics/openAccess Lena River Iron particles colloids TEM imaging STMX imaging Geochemistry Geokemi Article in journal info:eu-repo/semantics/article text 2017 ftnrm https://doi.org/10.1016/j.gca.2017.07.012 2024-07-05T03:00:55Z Rivers are significant contributors of Fe to theocean. However, the characteristics of chemically reactive Fe remain poorly constrained, especially in large Arctic rivers, which drain landscapes highly susceptible to climate change and carbon cycle alteration. The aim of this study was a detailed characterisation (size, mineralogy, and speciation) of riverine Fe-bearing particles (> 0.22 µm) and colloids (1 kDa – 0.22 µm) and their association with organic carbon (OC), in the Lena River and tributaries, which drain a catchment almost entirely underlain by permafrost. Samples fromthe main channel and tributaries representing watersheds that span a wide rangein topography and lithology were taken after the spring flood in June 2013 and summer baseflow in July 2012. Fe-bearing particles were identified, usingTransmission Electron Microscopy, as large (200 nm – 1 µm) aggregates of smaller (20 nm - 30 nm) spherical colloids of chemically-reactive ferrihydrite.In contrast, there were also large (500 nm – 1 µm) aggregates of clay (illite) particles and smaller (100 - 200 nm) iron oxide particles (dominantly hematite) that contain poorly reactive Fe. TEM imaging and Scanning Transmission X-raymicroscopy (STXM) indicated that the ferrihydrite is present as discrete particles within networks of amorphous particulate organic carbon (POC) and attached to the surface of primary produced organic matter and clay particles.Together, these larger particles act as the main carriers of nanoscale ferrihydrite in the Lena River basin. The chemically reactive ferrihydrite accounts for on average 70 ± 15 % of the total suspended Fe in the Lena River and tributaries. These observations place important constraints on Fe and OC cycling in the Lena River catchment area and Fe-bearing particle transport to the Arctic Ocean. The Lena River Study Article in Journal/Newspaper Arctic Ocean Climate change lena river permafrost Swedish Museum of Natural History: Publications (DiVA) Geochimica et Cosmochimica Acta 213 553 573 |
institution |
Open Polar |
collection |
Swedish Museum of Natural History: Publications (DiVA) |
op_collection_id |
ftnrm |
language |
English |
topic |
Lena River Iron particles colloids TEM imaging STMX imaging Geochemistry Geokemi |
spellingShingle |
Lena River Iron particles colloids TEM imaging STMX imaging Geochemistry Geokemi Hirst, Catherine Andersson, Per Shaw, Samuel Burke, Ian Kutscher, Liselott Murphy, Melissa Maximov, Trofim Pokrovsky, Oleg Mörth, Carl-Magnus Porcelli, Don Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
topic_facet |
Lena River Iron particles colloids TEM imaging STMX imaging Geochemistry Geokemi |
description |
Rivers are significant contributors of Fe to theocean. However, the characteristics of chemically reactive Fe remain poorly constrained, especially in large Arctic rivers, which drain landscapes highly susceptible to climate change and carbon cycle alteration. The aim of this study was a detailed characterisation (size, mineralogy, and speciation) of riverine Fe-bearing particles (> 0.22 µm) and colloids (1 kDa – 0.22 µm) and their association with organic carbon (OC), in the Lena River and tributaries, which drain a catchment almost entirely underlain by permafrost. Samples fromthe main channel and tributaries representing watersheds that span a wide rangein topography and lithology were taken after the spring flood in June 2013 and summer baseflow in July 2012. Fe-bearing particles were identified, usingTransmission Electron Microscopy, as large (200 nm – 1 µm) aggregates of smaller (20 nm - 30 nm) spherical colloids of chemically-reactive ferrihydrite.In contrast, there were also large (500 nm – 1 µm) aggregates of clay (illite) particles and smaller (100 - 200 nm) iron oxide particles (dominantly hematite) that contain poorly reactive Fe. TEM imaging and Scanning Transmission X-raymicroscopy (STXM) indicated that the ferrihydrite is present as discrete particles within networks of amorphous particulate organic carbon (POC) and attached to the surface of primary produced organic matter and clay particles.Together, these larger particles act as the main carriers of nanoscale ferrihydrite in the Lena River basin. The chemically reactive ferrihydrite accounts for on average 70 ± 15 % of the total suspended Fe in the Lena River and tributaries. These observations place important constraints on Fe and OC cycling in the Lena River catchment area and Fe-bearing particle transport to the Arctic Ocean. The Lena River Study |
format |
Article in Journal/Newspaper |
author |
Hirst, Catherine Andersson, Per Shaw, Samuel Burke, Ian Kutscher, Liselott Murphy, Melissa Maximov, Trofim Pokrovsky, Oleg Mörth, Carl-Magnus Porcelli, Don |
author_facet |
Hirst, Catherine Andersson, Per Shaw, Samuel Burke, Ian Kutscher, Liselott Murphy, Melissa Maximov, Trofim Pokrovsky, Oleg Mörth, Carl-Magnus Porcelli, Don |
author_sort |
Hirst, Catherine |
title |
Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
title_short |
Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
title_full |
Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
title_fullStr |
Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
title_full_unstemmed |
Characterisation of Fe-bearing particles and colloids in the Lena River basin, NE Russia |
title_sort |
characterisation of fe-bearing particles and colloids in the lena river basin, ne russia |
publisher |
Naturhistoriska riksmuseet, Enheten för geovetenskap |
publishDate |
2017 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-2470 https://doi.org/10.1016/j.gca.2017.07.012 |
genre |
Arctic Ocean Climate change lena river permafrost |
genre_facet |
Arctic Ocean Climate change lena river permafrost |
op_relation |
Geochimica et Cosmochimica Acta, 0016-7037, 2017, 213, s. 553-573 info:eu-repo/grantAgreement/EC/FP7/290336 orcid:0000-0002-1752-6469 http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-2470 doi:10.1016/j.gca.2017.07.012 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.gca.2017.07.012 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
213 |
container_start_page |
553 |
op_container_end_page |
573 |
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1810430377156673536 |