{"id":4,"date":"2024-04-04T09:08:02","date_gmt":"2024-04-04T06:08:02","guid":{"rendered":"https:\/\/sisu.ut.ee\/peatlandn2o\/about\/"},"modified":"2024-04-04T09:08:26","modified_gmt":"2024-04-04T06:08:26","slug":"about","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/peatlandn2o\/about\/","title":{"rendered":"About project"},"content":{"rendered":"<p>\n\t<strong>Problem:<\/strong>\n<\/p>\n<ul>\n<li>\n\t\tPowerful\u00a0 greenhouse gas \u2013 agent of<strong> global warming<\/strong>\n\t<\/li>\n<li>\n\t\tMost dangerous stratospheric O<sub><sup>3<\/sup><\/sub> depleting agent\n\t<\/li>\n<\/ul>\n<p>\n\t<strong>Knowledge\u00a0gap:<\/strong>\n<\/p>\n<ul>\n<li>\n\t\t<strong>N<sub>2<\/sub>O budget: <\/strong>highly variable and scarcely studied\n\t<\/li>\n<li>\n\t\t<strong>Canopy effect <\/strong>largely unknown\n\t<\/li>\n<li>\n\t\t<strong>Tropical fluxes<\/strong><strong> <\/strong>insufficiently studied\n\t<\/li>\n<\/ul>\n<p>\n\t<strong>Major novelties of N<sub>2<\/sub>O flux:<\/strong>\n<\/p>\n<ul>\n<li>\n\t\tSynchronous automated measurement of N<sub>2<\/sub>O fluxes in <strong>soil, plants &amp; whole ecosystem<\/strong>\n\t<\/li>\n<li>\n\t\tEddy covariance N<sub>2<\/sub>O above <strong>forest canopy in tropics<\/strong>\n\t<\/li>\n<li>\n\t\tIntegrated <strong>microbiome <\/strong>and <strong>isotope <\/strong>analysis of N<sub>2<\/sub>O fluxes\n\t<\/li>\n<\/ul>\n<p>\n\t<img loading=\"lazy\" decoding=\"async\" width=\"4088\" height=\"2382\" class=\"alignnone wp-image-17\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23.png\" title=\"conceptual_figure_webpage_04.10.23.png\" alt=\"concepts\" srcset=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23.png 4088w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-300x175.png 300w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-1024x597.png 1024w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-768x447.png 768w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-1536x895.png 1536w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-2048x1193.png 2048w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/659\/conceptual_figure_webpage_04.10.23-1920x1119.png 1920w\" sizes=\"auto, (max-width: 4088px) 100vw, 4088px\"><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Problem: Powerful\u00a0 greenhouse gas \u2013 agent of global warming Most dangerous stratospheric O3 depleting agent Knowledge\u00a0gap: N2O budget: highly variable and scarcely studied Canopy effect largely unknown Tropical fluxes insufficiently studied Major novelties of N2O flux: Synchronous automated measurement of &#8230;<\/p>\n","protected":false},"author":325,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-4","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/pages\/4","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/users\/325"}],"replies":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/comments?post=4"}],"version-history":[{"count":2,"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/pages\/4\/revisions"}],"predecessor-version":[{"id":83,"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/pages\/4\/revisions\/83"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/peatlandn2o\/wp-json\/wp\/v2\/media?parent=4"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}