Experimental sediment metal(loid) fluxes in relation to temperature.
Metal(loid) fluxes from sediment to overlying water of Lower Martin Lake and Yellowknife Bay cores incubated at different temperatures. There are two points for each temperature which are measured fluxes of duplicate cores for each temperature treatment. Coefficients of determination are provided fo...
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2022
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Online Access: | https://doi.org/10.1371/journal.pone.0279412.g005 |
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ftunivfreestate:oai:figshare.com:article/21765411 2023-05-15T16:23:06+02:00 Experimental sediment metal(loid) 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.g005 unknown https://figshare.com/articles/figure/Experimental_sediment_metal_loid_fluxes_in_relation_to_temperature_/21765411 doi:10.1371/journal.pone.0279412.g005 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.g005 2022-12-23T00:20:49Z Metal(loid) fluxes from sediment to overlying water of Lower Martin Lake and Yellowknife Bay cores incubated at different temperatures. There are two points for each temperature which are measured fluxes of duplicate cores for each temperature treatment. Coefficients of determination are provided for statistically significant regressions. 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) Experimental sediment metal(loid) 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 |
Metal(loid) fluxes from sediment to overlying water of Lower Martin Lake and Yellowknife Bay cores incubated at different temperatures. There are two points for each temperature which are measured fluxes of duplicate cores for each temperature treatment. Coefficients of determination are provided for statistically significant regressions. |
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 |
Experimental sediment metal(loid) fluxes in relation to temperature. |
title_short |
Experimental sediment metal(loid) fluxes in relation to temperature. |
title_full |
Experimental sediment metal(loid) fluxes in relation to temperature. |
title_fullStr |
Experimental sediment metal(loid) fluxes in relation to temperature. |
title_full_unstemmed |
Experimental sediment metal(loid) fluxes in relation to temperature. |
title_sort |
experimental sediment metal(loid) fluxes in relation to temperature. |
publishDate |
2022 |
url |
https://doi.org/10.1371/journal.pone.0279412.g005 |
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/Experimental_sediment_metal_loid_fluxes_in_relation_to_temperature_/21765411 doi:10.1371/journal.pone.0279412.g005 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1371/journal.pone.0279412.g005 |
_version_ |
1766011278540668928 |