Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments
The sources, sinks, fluxes, spatial distributions, and temporal variations of dissolved organic carbon (DOC) in subarctic fen catchments as well as the temporal patterns of DOC in streams draining subarctic fen catchments in the region of Schefferville, Quebec were investigated. In June to August sa...
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McGill University
1991
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ftcanadathes:oai:collectionscanada.gc.ca:QMM.60045 2023-05-15T18:28:07+02:00 Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments Koprivnjak, Jean-François Master of Science (Department of Geography.) 1991 application/pdf http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60045 en eng McGill University alephsysno: 001237861 proquestno: AAIMM67757 Theses scanned by UMI/ProQuest. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60045 All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. Fens -- Québec (Province) Carbon cycle (Biogeochemistry) Soils -- Carbon content -- Québec (Province) Electronic Thesis or Dissertation 1991 ftcanadathes 2014-02-16T01:01:26Z The sources, sinks, fluxes, spatial distributions, and temporal variations of dissolved organic carbon (DOC) in subarctic fen catchments as well as the temporal patterns of DOC in streams draining subarctic fen catchments in the region of Schefferville, Quebec were investigated. In June to August sampling, DOC concentrations averaged 17 mg/L in peat water, 2-16 m/L in stream water, 49-56 mg/L in canopy throughfall, 14-19 mg/L in understory throughfall, 122-187 mg/L in stemflow, 25-39 mg/L in lichen and moss mat water, and 35-42 mg/L in soil A horizon water. Precipitation and canopy and understory throughfall were all significant DOC sources with seasonal DOC fluxes to the forest floor of 0.1-0.4, 0.5-1.3, and 0.8-1.7 g DOC/m$ sp2$ of forest, respectively. The lichen and moss mats and the A soil horizon were also found to be DOC sources, whereas the B soil horizon was a DOC sink. The soil column was estimated to export 0.4-0.5 g DOC/m$ sp2$. Peat, also a DOC source, released 1.2-2.1 g DOC/m$ sp2$. DOC concentrations in streams draining ten fen catchments were found to be positively correlated with the percentage of fen area in the catchments. Thesis Subarctic Theses Canada/Thèses Canada (Library and Archives Canada) |
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Open Polar |
collection |
Theses Canada/Thèses Canada (Library and Archives Canada) |
op_collection_id |
ftcanadathes |
language |
English |
topic |
Fens -- Québec (Province) Carbon cycle (Biogeochemistry) Soils -- Carbon content -- Québec (Province) |
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Fens -- Québec (Province) Carbon cycle (Biogeochemistry) Soils -- Carbon content -- Québec (Province) Koprivnjak, Jean-François Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
topic_facet |
Fens -- Québec (Province) Carbon cycle (Biogeochemistry) Soils -- Carbon content -- Québec (Province) |
description |
The sources, sinks, fluxes, spatial distributions, and temporal variations of dissolved organic carbon (DOC) in subarctic fen catchments as well as the temporal patterns of DOC in streams draining subarctic fen catchments in the region of Schefferville, Quebec were investigated. In June to August sampling, DOC concentrations averaged 17 mg/L in peat water, 2-16 m/L in stream water, 49-56 mg/L in canopy throughfall, 14-19 mg/L in understory throughfall, 122-187 mg/L in stemflow, 25-39 mg/L in lichen and moss mat water, and 35-42 mg/L in soil A horizon water. Precipitation and canopy and understory throughfall were all significant DOC sources with seasonal DOC fluxes to the forest floor of 0.1-0.4, 0.5-1.3, and 0.8-1.7 g DOC/m$ sp2$ of forest, respectively. The lichen and moss mats and the A soil horizon were also found to be DOC sources, whereas the B soil horizon was a DOC sink. The soil column was estimated to export 0.4-0.5 g DOC/m$ sp2$. Peat, also a DOC source, released 1.2-2.1 g DOC/m$ sp2$. DOC concentrations in streams draining ten fen catchments were found to be positively correlated with the percentage of fen area in the catchments. |
format |
Thesis |
author |
Koprivnjak, Jean-François |
author_facet |
Koprivnjak, Jean-François |
author_sort |
Koprivnjak, Jean-François |
title |
Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
title_short |
Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
title_full |
Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
title_fullStr |
Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
title_full_unstemmed |
Sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
title_sort |
sources, sinks, and fluxes of dissolved organic carbon in subarctic fen catchments |
publisher |
McGill University |
publishDate |
1991 |
url |
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60045 |
op_coverage |
Master of Science (Department of Geography.) |
genre |
Subarctic |
genre_facet |
Subarctic |
op_relation |
alephsysno: 001237861 proquestno: AAIMM67757 Theses scanned by UMI/ProQuest. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60045 |
op_rights |
All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
_version_ |
1766210468018388992 |