{"id":750,"date":"2024-03-07T10:21:57","date_gmt":"2024-03-07T08:21:57","guid":{"rendered":"https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/?p=750"},"modified":"2024-03-07T10:22:00","modified_gmt":"2024-03-07T08:22:00","slug":"post-fire-soil-greenhouse-gas-fluxes-in-boreal-scots-pine-forests-are-they-affected-by-surface-fires-with-different-severities","status":"publish","type":"post","link":"https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/2024\/03\/07\/post-fire-soil-greenhouse-gas-fluxes-in-boreal-scots-pine-forests-are-they-affected-by-surface-fires-with-different-severities\/","title":{"rendered":"Post-fire soil greenhouse gas fluxes in boreal Scots pine forests\u2013Are they affected by surface fires with different severities?"},"content":{"rendered":"\n<p>A new paper by K\u00f6ster et al (2024) gives information regarding surface fires (dominant in Northern Europe), and how surface fires of different severities could affect post-fire soil greenhouse gas emissions.\u00a0The results of the study show that fire severity, time since fire and post-fire changes in soil temperature were the main factors driving forest floor ecosystem respiration (soil CO<sub>2<\/sub>\u00a0flux) from burned boreal forest soils. In the case of CH4, time since fire and post-fire changes in soil temperatures were the main factors driving soil CH4\u00a0fluxes from burned boreal forest soils. Unburned study areas were sinks of CH4\u00a0through the entire measurement period, while immediately after the fire, the burned areas turned from CH4\u00a0sinks to CH4\u00a0sources, and areas with higher fire severity showed significantly higher CH<sub>4<\/sub>\u00a0emissions compared to areas with lower fire severity. For N<sub>2<\/sub>O, measurement time (time since fire) was the only factor that significantly affected soil N<sub>2<\/sub>O fluxes. Shortly after the fire, the N<sub>2<\/sub>O emissions increased significantly, but at later stages of post-fire succession, there was no difference between the N<sub>2<\/sub>O fluxes from both unburned and burned areas. Throughout the entire summer measurement period (until the end of August), all areas were acting as a source of N<sub>2<\/sub>O, but from September, all areas turned from N<sub>2<\/sub>O sources to N<sub>2<\/sub>O sinks. We also observed an increase in post-fire soil C and N content (two days after the fire) within the first 5 cm of the soil mineral layer, showing that after the fire disturbance, part of the pyrogenic material created during the combustion is transported quickly through different soil horizons in the form of C and N.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"841\" src=\"https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/wp-content\/uploads\/sites\/178\/2024\/03\/AgrForMet-2024-1024x841.jpg\" alt=\"\" class=\"wp-image-753\" srcset=\"https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/wp-content\/uploads\/sites\/178\/2024\/03\/AgrForMet-2024-1024x841.jpg 1024w, https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/wp-content\/uploads\/sites\/178\/2024\/03\/AgrForMet-2024-300x247.jpg 300w, https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/wp-content\/uploads\/sites\/178\/2024\/03\/AgrForMet-2024-768x631.jpg 768w, https:\/\/blogs.uef.fi\/disturbances-and-biogeochemistry\/wp-content\/uploads\/sites\/178\/2024\/03\/AgrForMet-2024.jpg 1066w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>A new paper by K\u00f6ster et al (2024) gives information regarding surface fires (dominant in Northern Europe), and how surface fires of different severities could affect post-fire soil greenhouse gas emissions.\u00a0The results of the study show that fire severity, time since fire and post-fire changes in soil temperature were the main factors driving forest floor [&hellip;]<\/p>\n","protected":false},"author":535,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-750","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.1.1 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Post-fire soil greenhouse gas fluxes in boreal Scots pine forests\u2013Are they affected by surface fires with different severities? - Disturbances and Biogeochemistry for Ecosystem Services<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" 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