Photochemical Formation of volatile mercury in high Arctic lakes

Abstract Formation rates of dissolved gaseous mercury (DGM were measured in three high (74 °N) Arctic lakes and one wetland. The rate of formation of DGM was controlled by (1) the intensity of solar radiation, particularly ultraviolet‐B (280–320 nm) and ultraviolet‐A (320–400 nm) wavebands and (2) t...

Full description

Bibliographic Details
Published in:Environmental Toxicology and Chemistry
Main Authors: Amyot, Marc, Lean, David, Mierle, Greg
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1997
Subjects:
Online Access:http://dx.doi.org/10.1002/etc.5620161010
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fetc.5620161010
https://setac.onlinelibrary.wiley.com/doi/pdf/10.1002/etc.5620161010
id crwiley:10.1002/etc.5620161010
record_format openpolar
spelling crwiley:10.1002/etc.5620161010 2024-09-09T19:19:08+00:00 Photochemical Formation of volatile mercury in high Arctic lakes Amyot, Marc Lean, David Mierle, Greg 1997 http://dx.doi.org/10.1002/etc.5620161010 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fetc.5620161010 https://setac.onlinelibrary.wiley.com/doi/pdf/10.1002/etc.5620161010 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Environmental Toxicology and Chemistry volume 16, issue 10, page 2054-2063 ISSN 0730-7268 1552-8618 journal-article 1997 crwiley https://doi.org/10.1002/etc.5620161010 2024-07-04T04:31:15Z Abstract Formation rates of dissolved gaseous mercury (DGM were measured in three high (74 °N) Arctic lakes and one wetland. The rate of formation of DGM was controlled by (1) the intensity of solar radiation, particularly ultraviolet‐B (280–320 nm) and ultraviolet‐A (320–400 nm) wavebands and (2) the concentration of available photoreducible Hg(II) complexes. Additions of hydrogen peroxide and of fulvic acids did not enhance DGM formation rates in our experiments. This study illustrates that photoreduction of mercury occurs in a wide range of aquatic systems even in the high arctic where radiation levels are lower but continue for the entire day during the summer. Article in Journal/Newspaper Arctic Wiley Online Library Arctic Environmental Toxicology and Chemistry 16 10 2054 2063
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Formation rates of dissolved gaseous mercury (DGM were measured in three high (74 °N) Arctic lakes and one wetland. The rate of formation of DGM was controlled by (1) the intensity of solar radiation, particularly ultraviolet‐B (280–320 nm) and ultraviolet‐A (320–400 nm) wavebands and (2) the concentration of available photoreducible Hg(II) complexes. Additions of hydrogen peroxide and of fulvic acids did not enhance DGM formation rates in our experiments. This study illustrates that photoreduction of mercury occurs in a wide range of aquatic systems even in the high arctic where radiation levels are lower but continue for the entire day during the summer.
format Article in Journal/Newspaper
author Amyot, Marc
Lean, David
Mierle, Greg
spellingShingle Amyot, Marc
Lean, David
Mierle, Greg
Photochemical Formation of volatile mercury in high Arctic lakes
author_facet Amyot, Marc
Lean, David
Mierle, Greg
author_sort Amyot, Marc
title Photochemical Formation of volatile mercury in high Arctic lakes
title_short Photochemical Formation of volatile mercury in high Arctic lakes
title_full Photochemical Formation of volatile mercury in high Arctic lakes
title_fullStr Photochemical Formation of volatile mercury in high Arctic lakes
title_full_unstemmed Photochemical Formation of volatile mercury in high Arctic lakes
title_sort photochemical formation of volatile mercury in high arctic lakes
publisher Wiley
publishDate 1997
url http://dx.doi.org/10.1002/etc.5620161010
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fetc.5620161010
https://setac.onlinelibrary.wiley.com/doi/pdf/10.1002/etc.5620161010
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Environmental Toxicology and Chemistry
volume 16, issue 10, page 2054-2063
ISSN 0730-7268 1552-8618
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/etc.5620161010
container_title Environmental Toxicology and Chemistry
container_volume 16
container_issue 10
container_start_page 2054
op_container_end_page 2063
_version_ 1809759264889110528