Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes

Autores
Osburn, Christopher L.; Zagarese, Horacio Ernesto; Morris, Donald P.; Hargreaves, Bruce R.; Cravero, Walter Ruben
Año de publicación
2001
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The effect of solar radiation on the dissolved absorption coefficient (aCDOM[λ]), which reflects the concentration of chromophoric dissolved organic matter (CDOM), was investigated in several lakes near Bariloche, Argentina and in northeastern Pennsylvania, USA. Samples of 0.2 μm filtered lake water were exposed in quartz tubes to different portions of the solar spectrum using optical cutoff filters to remove parts of the ultraviolet (UV) region of the solar spectrum. Changes in the spectral absorption in these samples and the absorbed incident energy were used to calculate spectral weighting functions (SWFs) for the photobleaching (PB) of CDOM. PB was measured as the loss of aCDOM(λ) (the aCDOM[λ] was averaged from 280 to 500 nm) per unit absorbed energy. CDOM from humic and clear lakes, as well as from a Sphagnum bog and an algal culture, was used in the experiments covering a wide range of carbon sources. We used an iterative, nonlinear optimization method to fit the measured results to a simple exponential function in order to generate each SWF. Comparing individual SWFs calculated for various CDOM sources, we computed a summary SWF from the experiments using epilimnial CDOM from our study lakes. Our summary SWF was able to explain 80-90% of the observed variance in our exposure experiments, and we were able to predict PB results obtained for other Argentine lakes (mean error 14.5%). Finally, we calculated that the effect of UV-B radiation on PB was small (<20% of total decrease in the absorption coefficient) compared to UV-A and blue light radiation. This suggested that increased UV-B radiation due to stratospheric ozone depletion would not greatly increase the photobleaching of whole water column CDOM in Patagonian lakes (<10%).
Fil: Osburn, Christopher L.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Zagarese, Horacio Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Morris, Donald P.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Hargreaves, Bruce R.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Cravero, Walter Ruben. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto de Física del Sur. Universidad Nacional del Sur. Departamento de Física. Instituto de Física del Sur; Argentina
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/71793

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spelling Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakesOsburn, Christopher L.Zagarese, Horacio ErnestoMorris, Donald P.Hargreaves, Bruce R.Cravero, Walter Rubenhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1The effect of solar radiation on the dissolved absorption coefficient (aCDOM[λ]), which reflects the concentration of chromophoric dissolved organic matter (CDOM), was investigated in several lakes near Bariloche, Argentina and in northeastern Pennsylvania, USA. Samples of 0.2 μm filtered lake water were exposed in quartz tubes to different portions of the solar spectrum using optical cutoff filters to remove parts of the ultraviolet (UV) region of the solar spectrum. Changes in the spectral absorption in these samples and the absorbed incident energy were used to calculate spectral weighting functions (SWFs) for the photobleaching (PB) of CDOM. PB was measured as the loss of aCDOM(λ) (the aCDOM[λ] was averaged from 280 to 500 nm) per unit absorbed energy. CDOM from humic and clear lakes, as well as from a Sphagnum bog and an algal culture, was used in the experiments covering a wide range of carbon sources. We used an iterative, nonlinear optimization method to fit the measured results to a simple exponential function in order to generate each SWF. Comparing individual SWFs calculated for various CDOM sources, we computed a summary SWF from the experiments using epilimnial CDOM from our study lakes. Our summary SWF was able to explain 80-90% of the observed variance in our exposure experiments, and we were able to predict PB results obtained for other Argentine lakes (mean error 14.5%). Finally, we calculated that the effect of UV-B radiation on PB was small (<20% of total decrease in the absorption coefficient) compared to UV-A and blue light radiation. This suggested that increased UV-B radiation due to stratospheric ozone depletion would not greatly increase the photobleaching of whole water column CDOM in Patagonian lakes (<10%).Fil: Osburn, Christopher L.. Lehigh University. Department of Earth and Environmental Sciences; Estados UnidosFil: Zagarese, Horacio Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Morris, Donald P.. Lehigh University. Department of Earth and Environmental Sciences; Estados UnidosFil: Hargreaves, Bruce R.. Lehigh University. Department of Earth and Environmental Sciences; Estados UnidosFil: Cravero, Walter Ruben. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto de Física del Sur. Universidad Nacional del Sur. Departamento de Física. Instituto de Física del Sur; ArgentinaAmerican Society of Limnology and Oceanography2001-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/71793Osburn, Christopher L.; Zagarese, Horacio Ernesto; Morris, Donald P.; Hargreaves, Bruce R.; Cravero, Walter Ruben; Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes; American Society of Limnology and Oceanography; Limnology and Oceanography; 46; 6; 12-2001; 1455-14670024-3590CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://aslopubs.onlinelibrary.wiley.com/doi/abs/10.4319/lo.2001.46.6.1455info:eu-repo/semantics/altIdentifier/doi/10.4319/lo.2001.46.6.1455info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:13:26Zoai:ri.conicet.gov.ar:11336/71793instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:13:26.747CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
title Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
spellingShingle Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
Osburn, Christopher L.
title_short Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
title_full Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
title_fullStr Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
title_full_unstemmed Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
title_sort Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes
dc.creator.none.fl_str_mv Osburn, Christopher L.
Zagarese, Horacio Ernesto
Morris, Donald P.
Hargreaves, Bruce R.
Cravero, Walter Ruben
author Osburn, Christopher L.
author_facet Osburn, Christopher L.
Zagarese, Horacio Ernesto
Morris, Donald P.
Hargreaves, Bruce R.
Cravero, Walter Ruben
author_role author
author2 Zagarese, Horacio Ernesto
Morris, Donald P.
Hargreaves, Bruce R.
Cravero, Walter Ruben
author2_role author
author
author
author
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The effect of solar radiation on the dissolved absorption coefficient (aCDOM[λ]), which reflects the concentration of chromophoric dissolved organic matter (CDOM), was investigated in several lakes near Bariloche, Argentina and in northeastern Pennsylvania, USA. Samples of 0.2 μm filtered lake water were exposed in quartz tubes to different portions of the solar spectrum using optical cutoff filters to remove parts of the ultraviolet (UV) region of the solar spectrum. Changes in the spectral absorption in these samples and the absorbed incident energy were used to calculate spectral weighting functions (SWFs) for the photobleaching (PB) of CDOM. PB was measured as the loss of aCDOM(λ) (the aCDOM[λ] was averaged from 280 to 500 nm) per unit absorbed energy. CDOM from humic and clear lakes, as well as from a Sphagnum bog and an algal culture, was used in the experiments covering a wide range of carbon sources. We used an iterative, nonlinear optimization method to fit the measured results to a simple exponential function in order to generate each SWF. Comparing individual SWFs calculated for various CDOM sources, we computed a summary SWF from the experiments using epilimnial CDOM from our study lakes. Our summary SWF was able to explain 80-90% of the observed variance in our exposure experiments, and we were able to predict PB results obtained for other Argentine lakes (mean error 14.5%). Finally, we calculated that the effect of UV-B radiation on PB was small (<20% of total decrease in the absorption coefficient) compared to UV-A and blue light radiation. This suggested that increased UV-B radiation due to stratospheric ozone depletion would not greatly increase the photobleaching of whole water column CDOM in Patagonian lakes (<10%).
Fil: Osburn, Christopher L.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Zagarese, Horacio Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Morris, Donald P.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Hargreaves, Bruce R.. Lehigh University. Department of Earth and Environmental Sciences; Estados Unidos
Fil: Cravero, Walter Ruben. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto de Física del Sur. Universidad Nacional del Sur. Departamento de Física. Instituto de Física del Sur; Argentina
description The effect of solar radiation on the dissolved absorption coefficient (aCDOM[λ]), which reflects the concentration of chromophoric dissolved organic matter (CDOM), was investigated in several lakes near Bariloche, Argentina and in northeastern Pennsylvania, USA. Samples of 0.2 μm filtered lake water were exposed in quartz tubes to different portions of the solar spectrum using optical cutoff filters to remove parts of the ultraviolet (UV) region of the solar spectrum. Changes in the spectral absorption in these samples and the absorbed incident energy were used to calculate spectral weighting functions (SWFs) for the photobleaching (PB) of CDOM. PB was measured as the loss of aCDOM(λ) (the aCDOM[λ] was averaged from 280 to 500 nm) per unit absorbed energy. CDOM from humic and clear lakes, as well as from a Sphagnum bog and an algal culture, was used in the experiments covering a wide range of carbon sources. We used an iterative, nonlinear optimization method to fit the measured results to a simple exponential function in order to generate each SWF. Comparing individual SWFs calculated for various CDOM sources, we computed a summary SWF from the experiments using epilimnial CDOM from our study lakes. Our summary SWF was able to explain 80-90% of the observed variance in our exposure experiments, and we were able to predict PB results obtained for other Argentine lakes (mean error 14.5%). Finally, we calculated that the effect of UV-B radiation on PB was small (<20% of total decrease in the absorption coefficient) compared to UV-A and blue light radiation. This suggested that increased UV-B radiation due to stratospheric ozone depletion would not greatly increase the photobleaching of whole water column CDOM in Patagonian lakes (<10%).
publishDate 2001
dc.date.none.fl_str_mv 2001-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/71793
Osburn, Christopher L.; Zagarese, Horacio Ernesto; Morris, Donald P.; Hargreaves, Bruce R.; Cravero, Walter Ruben; Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes; American Society of Limnology and Oceanography; Limnology and Oceanography; 46; 6; 12-2001; 1455-1467
0024-3590
CONICET Digital
CONICET
url http://hdl.handle.net/11336/71793
identifier_str_mv Osburn, Christopher L.; Zagarese, Horacio Ernesto; Morris, Donald P.; Hargreaves, Bruce R.; Cravero, Walter Ruben; Calculation of spectral weighting functions for the solar photobleaching of chromophoric dissolved organic matter in temperate lakes; American Society of Limnology and Oceanography; Limnology and Oceanography; 46; 6; 12-2001; 1455-1467
0024-3590
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://aslopubs.onlinelibrary.wiley.com/doi/abs/10.4319/lo.2001.46.6.1455
info:eu-repo/semantics/altIdentifier/doi/10.4319/lo.2001.46.6.1455
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv American Society of Limnology and Oceanography
publisher.none.fl_str_mv American Society of Limnology and Oceanography
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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