{"id":2445,"date":"2018-05-31T13:38:48","date_gmt":"2018-05-31T12:38:48","guid":{"rendered":"http:\/\/www.earth-site.co.uk\/Education\/?page_id=2445"},"modified":"2024-10-01T13:53:23","modified_gmt":"2024-10-01T12:53:23","slug":"ozone-layer","status":"publish","type":"post","link":"https:\/\/www.earth-site.co.uk\/Education\/ozone-layer\/","title":{"rendered":"Ozone Layer"},"content":{"rendered":"<p>[et_pb_section admin_label=&#8221;section&#8221;][et_pb_row admin_label=&#8221;row&#8221;][et_pb_column type=&#8221;4_4&#8243;][et_pb_text admin_label=&#8221;Text&#8221; background_layout=&#8221;light&#8221; text_orientation=&#8221;left&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221;]<\/p>\n<h1 style=\"text-align: center;\">Ozone Layer<\/h1>\n<p>[\/et_pb_text][et_pb_text admin_label=&#8221;Text&#8221; background_layout=&#8221;light&#8221; text_orientation=&#8221;left&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221;]<\/p>\n<p style=\"text-align: justify;\"><span class=\"style80\">In the Stratosphere (between 10 and 50 kilometers high) is the layer containing most of the atmospheric ozone and this is mainly concentrated at about 25 kilometers up. <a href=\"https:\/\/www.earth-site.co.uk\/Education\/ozone\/\">Ozone<\/a> is produced in the ozone layer mainly through ultraviolet light from <\/span><span class=\"style80\">solar radiation (hn) colliding with diatomic oxygen (oxygen made of two <a href=\"https:\/\/www.earth-site.co.uk\/Education\/atoms\/\" title=\"Atoms\">atoms<\/a>). Diatomic oxygen in the stratosphere absorbs the majority of the harmful ultraviolet radiation (anything with a wavelength smaller than 240 nm) and in doing this the absorbed energy splits the molecule leaving two individual oxygen atoms.<\/span><\/p>\n<p>[\/et_pb_text][et_pb_image admin_label=&#8221;Image&#8221; src=&#8221;https:\/\/www.earth-site.co.uk\/Education\/wp-content\/uploads\/2018\/05\/Ozone-Layer.png&#8221; show_in_lightbox=&#8221;off&#8221; url_new_window=&#8221;off&#8221; use_overlay=&#8221;off&#8221; animation=&#8221;left&#8221; sticky=&#8221;off&#8221; align=&#8221;center&#8221; force_fullwidth=&#8221;off&#8221; always_center_on_mobile=&#8221;on&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; \/][et_pb_text admin_label=&#8221;Text&#8221; background_layout=&#8221;light&#8221; text_orientation=&#8221;left&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221;]<\/p>\n<p style=\"text-align: justify;\"><span class=\"style80\">In the Stratosphere (between 10 and 50 kilometers high) is the layer containing most of the atmospheric ozone and this is mainly concentrated at about 25 kilometers up. Ozone is produced in the ozone layer mainly through ultraviolet light from <\/span><span class=\"style80\">solar radiation (h<\/span><span class=\"style80\">n<\/span><span class=\"style80\">) colliding with diatomic oxygen (oxygen made of two atoms). Diatomic oxygen in the stratosphere absorbs the majority of the harmful ultraviolet radiation (anything with a wavelength smaller than 240 nm) and in doing this the absorbed energy splits the molecule leaving two individual oxygen atoms.<\/span><\/p>\n<p>[\/et_pb_text][et_pb_image admin_label=&#8221;Image&#8221; src=&#8221;https:\/\/www.earth-site.co.uk\/Education\/wp-content\/uploads\/2018\/05\/Ozone-Layer-Chemical-Reaction.png&#8221; show_in_lightbox=&#8221;off&#8221; url_new_window=&#8221;off&#8221; use_overlay=&#8221;off&#8221; animation=&#8221;left&#8221; sticky=&#8221;off&#8221; align=&#8221;center&#8221; force_fullwidth=&#8221;off&#8221; always_center_on_mobile=&#8221;on&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; \/][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ozone Layer In the Stratosphere (between 10 and 50 kilometers high) is the layer containing most of the atmospheric&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_edit_lock":["1707067109:1"],"_edit_last":["1"],"_wp_page_template":["default"],"ttr_page_title_checkbox":["false"],"ttr_page_foot_checkbox":["true"],"ttr_header_size_select":["None"],"ttr_background_repeat_enable_checkbox":["true"],"ttr_change_header_image_text":[""],"ttr_background_size_select":["None"],"ttr_header_repeat_enable_checkbox":["true"],"ttr_custom_style_text":[""],"_et_pb_use_builder":["on"],"_et_pb_ab_bounce_rate_limit":["5"],"_et_pb_ab_stats_refresh_interval":["hourly"],"_et_pb_old_content":[""],"_et_pb_enable_shortcode_tracking":[""],"_et_pb_custom_css":[""],"_et_pb_light_text_color":["#FFFFFF"],"_et_pb_dark_text_color":["#666666"],"_et_pb_content_area_background_color":[""],"_et_pb_section_background_color":["#FFFFFF"],"ampforwp-amp-on-off":["default"],"_et_builder_dynamic_assets_loading_attr_threshold":["2"],"rank_math_news_sitemap_robots":["index"],"rank_math_robots":["a:1:{i:0;s:5:\"index\";}"],"_et_dynamic_cached_shortcodes":["a:5:{i:0;s:13:\"et_pb_section\";i:1;s:9:\"et_pb_row\";i:2;s:12:\"et_pb_column\";i:31;s:11:\"et_pb_image\";i:50;s:10:\"et_pb_text\";}"],"_et_dynamic_cached_attributes":["a:1:{s:16:\"show_in_lightbox\";a:1:{i:0;s:3:\"off\";}}"]},"categories":[1],"tags":[],"class_list":["post-2445","post","type-post","status-publish","format-standard","hentry","category-generalknowledge"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - 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