


{"id":82193,"date":"2019-01-30T12:13:39","date_gmt":"2019-01-30T17:13:39","guid":{"rendered":"https:\/\/mrnf.gouv.qc.ca\/nos-publications\/ecosystem-carbon-accumulation\/"},"modified":"2019-01-30T12:13:39","modified_gmt":"2019-01-30T17:13:39","slug":"ecosystem-carbon-accumulation","status":"publish","type":"cpt_publication","link":"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ecosystem-carbon-accumulation\/","title":{"rendered":"Ecosystem carbon accumulation following fallow farmland afforestation with red pine in southern Qu\u00e9bec"},"content":{"rendered":"\n<p>Published in <b>Canadian Journal of Forest Research 37: 1118-1133<\/b><\/p>\n<p>We assessed the organic C stocks and inferred their changes in vegetation biomass, forest floor, and soil using a 50 year chronosequence of red pine (<em>Pinus resinosa<\/em> Ait.) plantations established on postagricultural fields in southern Qu\u00e9bec, Canada. The data come from soil and tree field surveys carried out in the 1970s in 348 sites. Organic C concentrations were usually measured in three major mineral soil horizons; for the remaining soil horizons, they were estimated using pedotransfer functions. The effect of soil order, drainage, and texture was analysed. Over 22 years, organic C accumulation rates (Mg C<sup>.<\/sup>ha<sup>-1.<\/sup>year<sup>-1<\/sup>) were 1.66 <u>+<\/u> 0.03 in vegetation biomass, 0.56 <u>+<\/u> 0.07 in forest floor, 0.86 <u>+<\/u> 0.47 in loamy soils (0-100 cm), and -0.18 <u>+<\/u> 0.24 in sandy soils (0-100 cm). The greater rate of C accumulation in loamy soils was due to the contribution of the 30-100 cm subsoil layer. The overall net accumulation of organic C in these plantation ecosystems was estimated to 51.4 <u>+<\/u> 4.8 Mg C<sup>.<\/sup>ha<sup>-1<\/sup> at 22 years. Soils of these plantations acted as a C sink in the first two decades, particularly in loamy soils compared with sandy soils, with no major differences among soil order or drainage.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Published in Canadian Journal of Forest Research 37: 1118-1133 We assessed the organic C stocks and inferred their changes in vegetation biomass, forest floor, and soil using a 50 year chronosequence of red pine (Pinus resinosa Ait.) plantations established on postagricultural fields in southern Qu\u00e9bec, Canada. The data come from soil and tree field surveys [&hellip;]<\/p>\n","protected":false},"template":"","format":"standard","cptt_secteur":[1179],"cptt_theme":[1183,1185,1180,1181],"cptt_categ_publi":[1149],"cptt_auteurs_ministeriels":[1102,1103,1108,1117],"class_list":["post-82193","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","cptt_auteurs_ministeriels-c-perie","cptt_auteurs_ministeriels-g-pregent","cptt_auteurs_ministeriels-syl-tremblay"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Ecosystem carbon accumulation following fallow farmland afforestation with red pine in southern Qu\u00e9bec - Minist\u00e8re des Ressources naturelles et des For\u00eats<\/title>\n<meta name=\"description\" content=\"We assessed the organic C stocks and inferred their changes in vegetation biomass, forest floor, and soil using a 50 year chronosequence\" \/>\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\/ecosystem-carbon-accumulation\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Ecosystem carbon accumulation following fallow farmland afforestation with red pine in southern Qu\u00e9bec - 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