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:	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 Great Slave Lake Northwest Territories Yellowknife Yellowknife Bay
Online Access:	https://doi.org/10.1371/journal.pone.0279412.g006

Description
Summary:	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.