


{"id":82415,"date":"2019-01-30T12:12:06","date_gmt":"2019-01-30T17:12:06","guid":{"rendered":"https:\/\/mrnf.gouv.qc.ca\/nos-publications\/interactions-atmospheric-deposition-with-mixed-hardwood-coniferous-forest-canopy\/"},"modified":"2019-01-30T12:12:06","modified_gmt":"2019-01-30T17:12:06","slug":"interactions-atmospheric-deposition-with-mixed-hardwood-coniferous-forest-canopy","status":"publish","type":"cpt_publication","link":"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/interactions-atmospheric-deposition-with-mixed-hardwood-coniferous-forest-canopy\/","title":{"rendered":"Interactions of atmospheric deposition with a mixed hardwood and a coniferous forest canopy at the Lake Clair Watershed (Duchesnay, Qu\u00e9bec)"},"content":{"rendered":"\n<p>Published in <strong>Canadian Journal of Forest Research 29: 1944-1957<\/strong><\/p> <p>From 1989 to 1996, ion deposition in precipitation, throughfall, and stemflow were measured under a deciduous and a coniferous stand, located in the Lake Clair Watershed, during the growing and the dormant seasons. During the growing season, throughfall deposition under both stands was significantly depleted in H<sup>+<\/sup> and NH<sub>4<\/sub><sup>+<\/sup> compared with wet deposition, and a significant uptake of NO<sub>3<\/sub><sup>&#8211;<\/sup> was observed under the coniferous canopy. Deposition of Ca<sup>2+<\/sup>, Mg<sup>2+<\/sup>, K<sup>+<\/sup>, Na<sup>+<\/sup>, Cl<sup>&#8211;<\/sup>, and S0<sub>4<\/sub><sup>2-<\/sup> was significantly higher in the throughfall than in the wet precipitation. During the growing season, the coniferous stand was more efficient in retaining nitrogen (NH<sub>4<\/sub><sup>+<\/sup> and N0<sub>3<\/sub><sup>&#8211;<\/sup>), while H<sup>+<\/sup> was more intensively retained in the deciduous stand. Significant interactions between precipitation and forest canopies were also observed during the dormant season: throughfall depositions of Ca<sup>2+<\/sup>, Mg<sup>2+<\/sup>, K<sup>+<\/sup>, Na<sup>+<\/sup>, and Cl<sup>&#8211;<\/sup> were significantly higher than wet precipitation under both canopies, while throughfall S0<sub>4<\/sub><sup>2-<\/sup> was significantly enriched only under the coniferous stand. Using a Na<sup>+<\/sup> ratio method, foliar leaching was found mostly responsible for the throughfall enrichment on a full-year basis in both stands, with values averaging 61, 73, and 96% of the total throughfall fluxes for Ca<sup>2+<\/sup>, Mg<sup>2+<\/sup>, and K<sup>+<\/sup>, respectively. Under both stands, net canopy exchange (NCE) of base cations, expressed on a monthly basis, were correlated to water volume and to H<sup>+<\/sup> and S0<sub>4<\/sub><sup>2-<\/sup> deposition. Multiple regression models including wet S0<sub>4<\/sub><sup>2-<\/sup> deposition and an estimate of dry S deposition, explained up to 88% (Ca<sup>2+<\/sup> in the coniferous stand) of the variance in base cation NCE under both stands.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Published in Canadian Journal of Forest Research 29: 1944-1957 From 1989 to 1996, ion deposition in precipitation, throughfall, and stemflow were measured under a deciduous and a coniferous stand, located in the Lake Clair Watershed, during the growing and the dormant seasons. During the growing season, throughfall deposition under both stands was significantly depleted in [&hellip;]<\/p>\n","protected":false},"template":"","format":"standard","cptt_secteur":[1179],"cptt_theme":[1183,1185,1180,1181],"cptt_categ_publi":[1149],"cptt_auteurs_ministeriels":[1102],"class_list":["post-82415","cpt_publication","type-cpt_publication","status-publish","format-standard","hentry","cptt_secteur-forests","cptt_theme-ecosystems-and-environment","cptt_theme-forest-ecology","cptt_theme-forestry-research","cptt_theme-forests","cptt_categ_publi-scientific-article","cptt_auteurs_ministeriels-r-ouimet"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Interactions of atmospheric deposition with a mixed hardwood and a coniferous forest canopy at the Lake Clair Watershed (Duchesnay, Qu\u00e9bec) - Minist\u00e8re des Ressources naturelles et des For\u00eats<\/title>\n<meta name=\"description\" content=\"During the growing season, throughfall deposition under both stands was significantly depleted in H+ and NH4+ compared with wet deposition...\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/interactions-atmospheric-deposition-with-mixed-hardwood-coniferous-forest-canopy\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Interactions of atmospheric deposition with a mixed hardwood and a coniferous forest canopy at the Lake Clair Watershed (Duchesnay, Qu\u00e9bec) - 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