Predicted versus observed sediment arsenic fluxes in relation to temperature.
Predicted As fluxes from Lower Martin Lake sediment (calculated using Fick’s law) for each temperature treatment in comparison to measured As fluxes in duplicate cores.
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2022
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Online Access: | https://doi.org/10.1371/journal.pone.0279412.g006 |
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ftunivfreestate:oai:figshare.com:article/21765414 2023-05-15T16:23:06+02:00 Predicted versus observed sediment arsenic fluxes in relation to temperature. Brittany C. Astles (14290341) John Chételat (529889) Michael J. Palmer (3189375) Jesse C. Vermaire (5464793) 2022-12-21T18:30:54Z https://doi.org/10.1371/journal.pone.0279412.g006 unknown https://figshare.com/articles/figure/Predicted_versus_observed_sediment_arsenic_fluxes_in_relation_to_temperature_/21765414 doi:10.1371/journal.pone.0279412.g006 CC BY 4.0 CC-BY Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified low organic matter contained predominately clay 7 ° c 21 ° c strongly enhance sediment sediment redox conditions lower martin lake great slave lake experimental incubation approach either sediment type warmer temperatures associated reported temperature enhancement overlying oxic waters duplicate sediment batches div >< p lake sediments either yellowknife bay sediments warmer temperatures yellowknife bay surface waters overlying water experimental investigation contaminated sediment yellowknife area contaminated sediments warming effects thermal stratification term warming temperature treatments study assessed published studies northwest territories microbial metabolism legacy arsenic internal loading indirect effects higher solid fluxes ranging evaluating climate environmental concern duplicate cores direct effect controlled chamber continued remobilization climate change arsenic fluxes Image Figure 2022 ftunivfreestate https://doi.org/10.1371/journal.pone.0279412.g006 2022-12-23T00:20:49Z Predicted As fluxes from Lower Martin Lake sediment (calculated using Fick’s law) for each temperature treatment in comparison to measured As fluxes in duplicate cores. Still Image Great Slave Lake Northwest Territories Yellowknife KovsieScholar Repository (University of the Free State - UFS UV) Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) Northwest Territories Yellowknife Yellowknife Bay ENVELOPE(-114.336,-114.336,62.367,62.367) |
institution |
Open Polar |
collection |
KovsieScholar Repository (University of the Free State - UFS UV) |
op_collection_id |
ftunivfreestate |
language |
unknown |
topic |
Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified low organic matter contained predominately clay 7 ° c 21 ° c strongly enhance sediment sediment redox conditions lower martin lake great slave lake experimental incubation approach either sediment type warmer temperatures associated reported temperature enhancement overlying oxic waters duplicate sediment batches div >< p lake sediments either yellowknife bay sediments warmer temperatures yellowknife bay surface waters overlying water experimental investigation contaminated sediment yellowknife area contaminated sediments warming effects thermal stratification term warming temperature treatments study assessed published studies northwest territories microbial metabolism legacy arsenic internal loading indirect effects higher solid fluxes ranging evaluating climate environmental concern duplicate cores direct effect controlled chamber continued remobilization climate change arsenic fluxes |
spellingShingle |
Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified low organic matter contained predominately clay 7 ° c 21 ° c strongly enhance sediment sediment redox conditions lower martin lake great slave lake experimental incubation approach either sediment type warmer temperatures associated reported temperature enhancement overlying oxic waters duplicate sediment batches div >< p lake sediments either yellowknife bay sediments warmer temperatures yellowknife bay surface waters overlying water experimental investigation contaminated sediment yellowknife area contaminated sediments warming effects thermal stratification term warming temperature treatments study assessed published studies northwest territories microbial metabolism legacy arsenic internal loading indirect effects higher solid fluxes ranging evaluating climate environmental concern duplicate cores direct effect controlled chamber continued remobilization climate change arsenic fluxes Brittany C. Astles (14290341) John Chételat (529889) Michael J. Palmer (3189375) Jesse C. Vermaire (5464793) Predicted versus observed sediment arsenic fluxes in relation to temperature. |
topic_facet |
Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified low organic matter contained predominately clay 7 ° c 21 ° c strongly enhance sediment sediment redox conditions lower martin lake great slave lake experimental incubation approach either sediment type warmer temperatures associated reported temperature enhancement overlying oxic waters duplicate sediment batches div >< p lake sediments either yellowknife bay sediments warmer temperatures yellowknife bay surface waters overlying water experimental investigation contaminated sediment yellowknife area contaminated sediments warming effects thermal stratification term warming temperature treatments study assessed published studies northwest territories microbial metabolism legacy arsenic internal loading indirect effects higher solid fluxes ranging evaluating climate environmental concern duplicate cores direct effect controlled chamber continued remobilization climate change arsenic fluxes |
description |
Predicted As fluxes from Lower Martin Lake sediment (calculated using Fick’s law) for each temperature treatment in comparison to measured As fluxes in duplicate cores. |
format |
Still Image |
author |
Brittany C. Astles (14290341) John Chételat (529889) Michael J. Palmer (3189375) Jesse C. Vermaire (5464793) |
author_facet |
Brittany C. Astles (14290341) John Chételat (529889) Michael J. Palmer (3189375) Jesse C. Vermaire (5464793) |
author_sort |
Brittany C. Astles (14290341) |
title |
Predicted versus observed sediment arsenic fluxes in relation to temperature. |
title_short |
Predicted versus observed sediment arsenic fluxes in relation to temperature. |
title_full |
Predicted versus observed sediment arsenic fluxes in relation to temperature. |
title_fullStr |
Predicted versus observed sediment arsenic fluxes in relation to temperature. |
title_full_unstemmed |
Predicted versus observed sediment arsenic fluxes in relation to temperature. |
title_sort |
predicted versus observed sediment arsenic fluxes in relation to temperature. |
publishDate |
2022 |
url |
https://doi.org/10.1371/journal.pone.0279412.g006 |
long_lat |
ENVELOPE(-114.001,-114.001,61.500,61.500) ENVELOPE(-114.336,-114.336,62.367,62.367) |
geographic |
Great Slave Lake Northwest Territories Yellowknife Yellowknife Bay |
geographic_facet |
Great Slave Lake Northwest Territories Yellowknife Yellowknife Bay |
genre |
Great Slave Lake Northwest Territories Yellowknife |
genre_facet |
Great Slave Lake Northwest Territories Yellowknife |
op_relation |
https://figshare.com/articles/figure/Predicted_versus_observed_sediment_arsenic_fluxes_in_relation_to_temperature_/21765414 doi:10.1371/journal.pone.0279412.g006 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1371/journal.pone.0279412.g006 |
_version_ |
1766011277325369344 |