{"help":"https://catalogue.cioos.ca/api/3/action/help_show?name=package_show","success":true,"result":{"id":"3a6e9472-1a85-48e5-8ac6-792945e03045","ecv":[],"eov":["dissolvedOrganicCarbon","other"],"url":null,"name":"ca-cioos_ff68a559-3de8-4ad0-9367-79697d7cc897","tags":[],"type":"dataset","notes":"Rapport scientifique sur les réponses des bassins versants et les flux de carbone organique pour sept rivières qui se déversent dans le chenal Kwakshua (île Calvert, Colombie-Britannique, Canada) à la suite d'un épisode pluvieux d'été et de début d'automne en 2014.\n\nLa forêt pluviale tempérée côtière de l'ouest de la Colombie-Britannique est un important réservoir de carbone et un contributeur important au cycle mondial du carbone. Le flux de carbone organique dissous à partir des sols dominés par les zones humides est d'une importance vitale pour les écosystèmes côtiers d'eau douce et marins. L'objectif de cette étude était d'étudier la relation entre le débit, la concentration de COD et le flux de carbone organique pour sept bassins versants dominés par les zones humides et les forêts de tourbières lors d'un épisode pluvieux d'été et de début d'automne. Des échantillons d'eau de cours d'eau ont été prélevés le long des branches ascendantes et descendantes des hydrogrammes de l'événement à la sortie des sept bassins versants et analysés pour déterminer la concentration de COD. La concentration de COD dans le courant a augmenté le long de la branche montante et a diminué pour revenir à une concentration stable dans les conditions d'écoulement La relation entre le débit et le flux de carbone organique a été caractérisée par une hystérésis ; il y a eu un retard dans le flux de carbone maximal par rapport au débit de pointe pour tous les bassins versants étudiés. La quantité de carbone organique exportée au cours d'un épisode de pluie était directement liée à la fraction de pluie exportée sous forme de ruissellement. La charge totale en carbone organique des événements pour six des sept bassins versants était de 233 kg km-2 pour l'événement estival et de 204 kg km-2 pour l'événement du début de l'automne. L'exportation de carbone organique par jour était deux fois plus élevée pour l'événement plus court et plus intensif du début de l'automne que pour l'événement estival.\n\nCitation recommandée pour l'article publié dans son intégralité : Korver, M.C., van Meerveld, H.J., Floyd, W.C., Waterloo, M.J. : Flux de carbone organique dissous de sept bassins versants dans un écosystème forestier de tourbière à l'île Calvert, en Colombie-Britannique, au Canada. Université libre d'Amsterdam et Institut Hakai. 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\\\"issued\\\": [{\\\"date-parts\\\": [\\\"2016\\\", \\\"01\\\", \\\"18\\\"]}], \\\"abstract\\\": \\\"Scientific report on catchment responses and organic carbon fluxes for seven rivers draining into Kwakshua Channel (Calvert Island, BC, Canada) for a summer and early fall rain event in 2014.\\n\\nThe coastal temperate rainforest of western British Columbia is a major store of carbon and an important contributor to the global carbon cycle. The flux of dissolved organic carbon from wetland-dominated soils is of vital importance for coastal freshwater and marine ecosystems. The objective of this study was to investigate the relation between discharge, DOC concentration and organic carbon flux for seven wetland and bog forest dominated watersheds for a summer and early fall rain event. Stream water samples were taken along the rising and falling limb of the event hydrographs at the outlets of all seven watersheds and analyzed for DOC concentration. Stream DOC concentration increased along the rising limb and decreased back to a stable concentration under base flow conditions. The relation between discharge and flux of organic carbon was characterized by hysteresis; there was a delay in peak carbon flux compared to peak discharge for all studied watersheds. The amount of organic carbon exported over the course of a rain event was directly related to the fraction of rain exported as runoff. Total event organic carbon load for six out of seven watersheds was 233 kg km-2 for the summer event and 204 kg km-2 for the early fall event. The export of organic carbon per day was twice as high for the shorter and more intensive early fall event than the summer event.\\n\\nRecommended citation for the full published article: Korver, M.C., van Meerveld, H.J., Floyd, W.C., Waterloo, M.J.: Dissolved organic carbon fluxes of seven watersheds in a bog forest ecosystem at Calvert Island, British Columbia, Canada. VU University Amsterdam and Hakai Institute. MSc thesis extension, 2015.\\\", \\\"edition-date\\\": \\\"\\\", \\\"publisher\\\": \\\"Hakai Institute\\\", \\\"title\\\": \\\"Dissolved organic carbon fluxes of seven watersheds in a bog forest ecosystem at Calvert Island, British Columbia, Canada\\\", \\\"version\\\": \\\"1.0\\\", \\\"DOI\\\": \\\"10.21966/1.715701\\\", \\\"language\\\": \\\"en\\\", \\\"URL\\\": \\\"https://catalogue.hakai.org/dataset/ca-cioos_ff68a559-3de8-4ad0-9367-79697d7cc897?local=en\\\"}]","fr":"[{\\\"type\\\": \\\"dataset\\\", \\\"id\\\": \\\"ca.cioos_ff68a559-3de8-4ad0-9367-79697d7cc897\\\", \\\"author\\\": [{\\\"given\\\": \\\"Maartje C.\\\", \\\"family\\\": \\\"Korver\\\"}, {\\\"given\\\": \\\"H.J.\\\", \\\"family\\\": \\\"van Meerveld\\\"}, {\\\"given\\\": \\\"William\\\", \\\"family\\\": \\\"Floyd\\\"}, {\\\"given\\\": \\\"M.J.\\\", \\\"family\\\": \\\"Waterloo\\\"}], \\\"issued\\\": [{\\\"date-parts\\\": [\\\"2016\\\", \\\"01\\\", \\\"18\\\"]}], \\\"abstract\\\": \\\"Rapport scientifique sur les r\\u00e9ponses des bassins versants et les flux de carbone organique pour sept rivi\\u00e8res qui se d\\u00e9versent dans le chenal Kwakshua (\\u00eele Calvert, Colombie-Britannique, Canada) \\u00e0 la suite d'un \\u00e9pisode pluvieux d'\\u00e9t\\u00e9 et de d\\u00e9but d'automne en 2014.\\n\\nLa for\\u00eat pluviale temp\\u00e9r\\u00e9e c\\u00f4ti\\u00e8re de l'ouest de la Colombie-Britannique est un important r\\u00e9servoir de carbone et un contributeur important au cycle mondial du carbone. Le flux de carbone organique dissous \\u00e0 partir des sols domin\\u00e9s par les zones humides est d'une importance vitale pour les \\u00e9cosyst\\u00e8mes c\\u00f4tiers d'eau douce et marins. L'objectif de cette \\u00e9tude \\u00e9tait d'\\u00e9tudier la relation entre le d\\u00e9bit, la concentration de COD et le flux de carbone organique pour sept bassins versants domin\\u00e9s par les zones humides et les for\\u00eats de tourbi\\u00e8res lors d'un \\u00e9pisode pluvieux d'\\u00e9t\\u00e9 et de d\\u00e9but d'automne. Des \\u00e9chantillons d'eau de cours d'eau ont \\u00e9t\\u00e9 pr\\u00e9lev\\u00e9s le long des branches ascendantes et descendantes des hydrogrammes de l'\\u00e9v\\u00e9nement \\u00e0 la sortie des sept bassins versants et analys\\u00e9s pour d\\u00e9terminer la concentration de COD. La concentration de COD dans le courant a augment\\u00e9 le long de la branche montante et a diminu\\u00e9 pour revenir \\u00e0 une concentration stable dans les conditions d'\\u00e9coulement La relation entre le d\\u00e9bit et le flux de carbone organique a \\u00e9t\\u00e9 caract\\u00e9ris\\u00e9e par une hyst\\u00e9r\\u00e9sis\\u00a0; il y a eu un retard dans le flux de carbone maximal par rapport au d\\u00e9bit de pointe pour tous les bassins versants \\u00e9tudi\\u00e9s. La quantit\\u00e9 de carbone organique export\\u00e9e au cours d'un \\u00e9pisode de pluie \\u00e9tait directement li\\u00e9e \\u00e0 la fraction de pluie export\\u00e9e sous forme de ruissellement. La charge totale en carbone organique des \\u00e9v\\u00e9nements pour six des sept bassins versants \\u00e9tait de 233 kg km-2 pour l'\\u00e9v\\u00e9nement estival et de 204 kg km-2 pour l'\\u00e9v\\u00e9nement du d\\u00e9but de l'automne. L'exportation de carbone organique par jour \\u00e9tait deux fois plus \\u00e9lev\\u00e9e pour l'\\u00e9v\\u00e9nement plus court et plus intensif du d\\u00e9but de l'automne que pour l'\\u00e9v\\u00e9nement estival.\\n\\nCitation recommand\\u00e9e pour l'article publi\\u00e9 dans son int\\u00e9gralit\\u00e9\\u00a0: Korver, M.C., van Meerveld, H.J., Floyd, W.C., Waterloo, M.J.\\u00a0: Flux de carbone organique dissous de sept bassins versants dans un \\u00e9cosyst\\u00e8me forestier de tourbi\\u00e8re \\u00e0 l'\\u00eele Calvert, en Colombie-Britannique, au Canada. Universit\\u00e9 libre d'Amsterdam et Institut Hakai. 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The flux of dissolved organic carbon from wetland-dominated soils is of vital importance for coastal freshwater and marine ecosystems. The objective of this study was to investigate the relation between discharge, DOC concentration and organic carbon flux for seven wetland and bog forest dominated watersheds for a summer and early fall rain event. Stream water samples were taken along the rising and falling limb of the event hydrographs at the outlets of all seven watersheds and analyzed for DOC concentration. Stream DOC concentration increased along the rising limb and decreased back to a stable concentration under base flow conditions. The relation between discharge and flux of organic carbon was characterized by hysteresis; there was a delay in peak carbon flux compared to peak discharge for all studied watersheds. The amount of organic carbon exported over the course of a rain event was directly related to the fraction of rain exported as runoff. Total event organic carbon load for six out of seven watersheds was 233 kg km-2 for the summer event and 204 kg km-2 for the early fall event. The export of organic carbon per day was twice as high for the shorter and more intensive early fall event than the summer event.\n\nRecommended citation for the full published article: Korver, M.C., van Meerveld, H.J., Floyd, W.C., Waterloo, M.J.: Dissolved organic carbon fluxes of seven watersheds in a bog forest ecosystem at Calvert Island, British Columbia, Canada. VU University Amsterdam and Hakai Institute. MSc thesis extension, 2015.","fr":"Rapport scientifique sur les réponses des bassins versants et les flux de carbone organique pour sept rivières qui se déversent dans le chenal Kwakshua (île Calvert, Colombie-Britannique, Canada) à la suite d'un épisode pluvieux d'été et de début d'automne en 2014.\n\nLa forêt pluviale tempérée côtière de l'ouest de la Colombie-Britannique est un important réservoir de carbone et un contributeur important au cycle mondial du carbone. Le flux de carbone organique dissous à partir des sols dominés par les zones humides est d'une importance vitale pour les écosystèmes côtiers d'eau douce et marins. L'objectif de cette étude était d'étudier la relation entre le débit, la concentration de COD et le flux de carbone organique pour sept bassins versants dominés par les zones humides et les forêts de tourbières lors d'un épisode pluvieux d'été et de début d'automne. Des échantillons d'eau de cours d'eau ont été prélevés le long des branches ascendantes et descendantes des hydrogrammes de l'événement à la sortie des sept bassins versants et analysés pour déterminer la concentration de COD. La concentration de COD dans le courant a augmenté le long de la branche montante et a diminué pour revenir à une concentration stable dans les conditions d'écoulement La relation entre le débit et le flux de carbone organique a été caractérisée par une hystérésis ; il y a eu un retard dans le flux de carbone maximal par rapport au débit de pointe pour tous les bassins versants étudiés. La quantité de carbone organique exportée au cours d'un épisode de pluie était directement liée à la fraction de pluie exportée sous forme de ruissellement. La charge totale en carbone organique des événements pour six des sept bassins versants était de 233 kg km-2 pour l'événement estival et de 204 kg km-2 pour l'événement du début de l'automne. L'exportation de carbone organique par jour était deux fois plus élevée pour l'événement plus court et plus intensif du début de l'automne que pour l'événement estival.\n\nCitation recommandée pour l'article publié dans son intégralité : Korver, M.C., van Meerveld, H.J., Floyd, W.C., Waterloo, M.J. : Flux de carbone organique dissous de sept bassins versants dans un écosystème forestier de tourbière à l'île Calvert, en Colombie-Britannique, au Canada. Université libre d'Amsterdam et Institut Hakai. Prolongation de thèse de maîtrise, 2015."},"title_translated":{"en":"Dissolved organic carbon fluxes of seven watersheds in a bog forest ecosystem at Calvert Island, British Columbia, Canada","fr":"Flux de carbone organique dissous de sept bassins versants dans un écosystème forestier de tourbière à l'île Calvert, en Colombie-Britannique, au Canada"},"xml_location_url":"https://metadata-generator-proxy.server.hakai.app/metadata/hakai/dissolved_organic_carbon_fluxe_ff68a.xml","metadata-language":"en","metadata_modified":"2026-09-16T20:22:50.959789","frequency-of-update":"asNeeded","dataset-reference-date":[{"type":"creation","value":"2014-08-01"},{"type":"publication","value":"2016-01-18"}],"cited-responsible-party":[{"role":["author","distributor","owner","pointOfContact"],"individual-name":"Korver, Maartje C.","organisation-name":"Hakai Institute","contact-info_email":"maartje.korver@hakai.org","individual-uri_code":"https://orcid.org/0000-0003-1062-4864","organisation-uri_code":"https://ror.org/02pry0c91","individual-uri_version":"","individual-uri_authority":"","organisation-uri_version":"","individual-uri_code-space":"","organisation-uri_authority":"","organisation-uri_code-space":"","contact-info_online-resource":""},{"role":"author","individual-name":"van Meerveld, H.J.","organisation-name":"","contact-info_email":"","individual-uri_code":"https://orcid.org/0000-0002-7547-3270","individual-uri_version":"","individual-uri_authority":"","individual-uri_code-space":"","contact-info_online-resource":""},{"role":"author","individual-name":"Floyd, William","organisation-name":"Vancouver Island University","contact-info_email":"","individual-uri_code":"https://orcid.org/0000-0001-7487-5721","organisation-uri_code":"https://ror.org/033wcvv61","individual-uri_version":"","individual-uri_authority":"","organisation-uri_version":"","individual-uri_code-space":"","organisation-uri_authority":"","organisation-uri_code-space":"","contact-info_online-resource":""},{"role":"author","individual-name":"Waterloo, M.J.","organisation-name":"","contact-info_email":"","contact-info_online-resource":""},{"role":"publisher","individual-name":"","organisation-name":"Hakai Institute","contact-info_email":"data@hakai.org","organisation-uri_code":"https://ror.org/02pry0c91","organisation-uri_version":"","organisation-uri_authority":"","organisation-uri_code-space":""}],"metadata-reference-date":[{"type":"publication","value":"2022-03-25"},{"type":"revision","value":"2026-06-22"}],"relationships_as_object":[],"notes_translation_method":{"en":"","fr":"text translated using the Amazon translate service / texte traduit à l'aide du service de traduction Amazon"},"relationships_as_subject":[],"title_translation_method":{"en":"","fr":"text translated using the Amazon translate service / texte traduit à l'aide du service de traduction Amazon"},"metadata-point-of-contact":[{"role":"custodian","individual-name":"Henderson, Matthew","organisation-name":"Hakai Institute","contact-info_email":"","individual-uri_code":"","organisation-uri_code":"https://ror.org/02pry0c91","organisation-uri_version":"","organisation-uri_authority":"","organisation-uri_code-space":"","contact-info_online-resource":""},{"role":"pointOfContact","individual-name":"Hakai Geospatial","organisation-name":"Hakai Institute","contact-info_email":"data@hakai.org","individual-uri_code":"","organisation-uri_code":"https://ror.org/02pry0c91","organisation-uri_version":"","organisation-uri_authority":"","organisation-uri_code-space":"","contact-info_online-resource":""},{"role":"funder","individual-name":"","organisation-name":"Tula Foundation","contact-info_email":"","individual-uri_code":"","organisation-uri_code":"https://ror.org/02pry0c91","organisation-uri_version":"","organisation-uri_authority":"","organisation-uri_code-space":""}],"included_in_data_catalogue":[{"url":"https://catalogue.cioos.ca","name":{"en":"CIOOS Catalogue","fr":"Catalogue du SIOOC"},"description":""},{"url":"https://catalogue.hakai.org","name":{"en":"Hakai Data Catalogue","fr":"Hakai Data Catalogue"},"description":{"en":"Science on the Coastal Margin","fr":"Science on the Coastal Margin"}},{"url":"https://temp_cat.cioospacific.ca","name":{"en":"CIOOS Pacific","fr":"SIOOC Pacifique"},"description":{"en":"A description of the Catalogue","fr":"Une description du catalogue"}}],"keywords_translation_method":{"en":""},"unique-resource-identifier-full":[{"code":"https://doi.org/10.21966/1.715701","version":"","authority":"","code-space":""}]}}