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.

Bibliographic Details
Main Authors: Brittany C. Astles (14290341), John Chételat (529889), Michael J. Palmer (3189375), Jesse C. Vermaire (5464793)
Format: Still Image
Language:unknown
Published: 2022
Subjects:
Online Access:https://doi.org/10.1371/journal.pone.0279412.g006
id ftunivfreestate:oai:figshare.com:article/21765414
record_format openpolar
spelling 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