{"id":5429,"date":"2022-06-23T10:58:15","date_gmt":"2022-06-23T08:58:15","guid":{"rendered":"https:\/\/ist.blogs.inrae.fr\/afs\/?p=5429"},"modified":"2022-06-23T10:58:15","modified_gmt":"2022-06-23T08:58:15","slug":"potential-soil-methane-oxidation-in-naturally-regenerated-oak-dominated-temperate-deciduous-forest-stands-responds-to-soil-water-status-regardless-of-their-age-an-intact-core-incubation-study","status":"publish","type":"post","link":"https:\/\/ist.blogs.inrae.fr\/afs\/2022\/06\/23\/potential-soil-methane-oxidation-in-naturally-regenerated-oak-dominated-temperate-deciduous-forest-stands-responds-to-soil-water-status-regardless-of-their-age-an-intact-core-incubation-study\/","title":{"rendered":"Potential soil methane oxidation in naturally regenerated oak-dominated temperate deciduous forest stands responds to soil water status regardless of their age\u2014an intact core incubation study"},"content":{"rendered":"<script type='text\/javascript' src='https:\/\/d1bxh8uas1mnw7.cloudfront.net\/assets\/embed.js'><\/script><p><strong><a href=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2022\/06\/Bras-2022.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-5432 alignright\" src=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2022\/06\/Bras-2022-157x300.png\" alt=\"\" width=\"157\" height=\"300\" srcset=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2022\/06\/Bras-2022-157x300.png 157w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2022\/06\/Bras-2022.png 452w\" sizes=\"auto, (max-width: 157px) 100vw, 157px\" \/><\/a>Key message<\/strong><\/p>\n<p align=\"justify\">Potential CH4 oxidation in the top soil layer increased with decreasing soil water content in spring but was inhibited during severe summer drought in naturally-regenerated oak-dominated temperate deciduous forest stands regardless of their age. No direct effect of mineral nitrogen on soil CH4 oxidation was found. Soil CH4 oxidation in temperate forests could be reduced by extreme climatic events.<\/p>\n<p><strong>Keywords<\/strong><br \/>\nMethane oxidation; Naturally regenerated forest; Air-filled porosity; Mineral nitrogen; Water stress; Chronosequence<\/p>\n<div class='altmetric-embed' data-badge-type='donut' data-doi='10.1186\/s13595-022-01145-9'  style='float: right; ' ><\/div>\n<p><strong>Publication<\/strong><br \/>\nBras, N., Plain, C. &amp; Epron, D. Potential soil methane oxidation in naturally regenerated oak-dominated temperate deciduous forest stands responds to soil water status regardless of their age\u2014an intact core incubation study. Annals of Forest Science 79, 29 (2022). <a href=\"https:\/\/annforsci.biomedcentral.com\/articles\/10.1186\/s13595-022-01145-9\">https:\/\/doi.org\/10.1186\/s13595-022-01145-9<\/a><\/p>\n<p><strong>Data and\/or Code availability<\/strong><br \/>\nThe datasets analysed during the current study are available in the dorel repository (<a href=\"https:\/\/dorel.univ-lorraine.fr\/\">https:\/\/dorel.univ-lorraine.fr\/<\/a>), <a href=\"https:\/\/doi.org\/10.12763\/B5ETNU\">https:\/\/doi.org\/10.12763\/B5ETNU<\/a><\/p>\n<p><strong>Handling Editor<\/strong><br \/>\nAlexia Stokes<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Key message Potential CH4 oxidation in the top soil layer increased with decreasing soil water content in spring but was inhibited during severe summer drought in naturally-regenerated oak-dominated temperate deciduous forest stands regardless of their age. No direct effect of mineral nitrogen on soil CH4 oxidation was found. Soil CH4 oxidation in temperate forests could [&hellip;]<\/p>\n","protected":false},"author":109,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[14,110,109,15],"tags":[],"class_list":["post-5429","post","type-post","status-publish","format-standard","hentry","category-article-type","category-data-in-repository","category-open-access","category-research-paper","cat-14-id","cat-110-id","cat-109-id","cat-15-id"],"_links":{"self":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/5429","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/users\/109"}],"replies":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/comments?post=5429"}],"version-history":[{"count":4,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/5429\/revisions"}],"predecessor-version":[{"id":5434,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/5429\/revisions\/5434"}],"wp:attachment":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/media?parent=5429"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/categories?post=5429"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/tags?post=5429"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}