{"id":467,"date":"2025-11-02T00:11:23","date_gmt":"2025-11-01T19:11:23","guid":{"rendered":"http:\/\/npzaamin.uz\/?page_id=467"},"modified":"2025-11-05T13:58:42","modified_gmt":"2025-11-05T08:58:42","slug":"tuprogi","status":"publish","type":"page","link":"https:\/\/npzaamin.uz\/en\/tabiat\/tuprogi\/","title":{"rendered":"Soils"},"content":{"rendered":"<p><\/p>\n<p class=\"p1\"><span class=\"s1\">The diversity of <\/span><b>physical-geographical factors<\/b><span class=\"s1\">, <\/span><b>geomorphological structure<\/b><span class=\"s1\">, <\/span><b>climatic conditions<\/b><span class=\"s1\">, and <\/span><b>altitudinal variation of relief<\/b><span class=\"s1\"> contributes to the formation of various <\/span><b>soil types<\/b><span class=\"s1\">, corresponding to specific <\/span><b>bio-climatic zones and landscapes<\/b><span class=\"s1\">.<\/span><\/p>\n<p class=\"p3\">The main soil types of the Zomin National Nature Park include:<\/p>\n<ul>\n<li>\n<p class=\"p1\"><span class=\"s1\">In the <\/span><b>foothill zone<\/b><span class=\"s1\"> \u2014 <\/span><b>dark brown soils<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><span class=\"s1\">In the <\/span><b>sub-foothill zone<\/b><span class=\"s1\"> \u2014 <\/span><b>light brown soils<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><span class=\"s1\">In the <\/span><b>mountain forest zone<\/b><span class=\"s1\"> \u2014 <\/span><b>forest and sparse-forest soils<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><span class=\"s1\">In the <\/span><b>high-mountain zone<\/b><span class=\"s1\"> \u2014 <\/span><b>subalpine soils<\/b><span class=\"s1\">.<\/span><\/p>\n<\/li>\n<\/ul>\n<p class=\"p3\">The <span class=\"s3\"><b>continental environment<\/b><\/span> and <span class=\"s3\"><b>semi-desert climate<\/b><\/span> determine the diversity of soil cover.<\/p>\n<p class=\"p3\">On <span class=\"s3\"><b>northern slopes<\/b><\/span>, clear zonality is observed, whereas <span class=\"s3\"><b>southern slopes<\/b><\/span> are drier and lack a full vertical sequence of soil zones.<\/p>\n<p class=\"p1\"><span class=\"s1\">Hence, <\/span><b>northern slopes<\/b><span class=\"s1\"> are dominated by <\/span><b>alluvial-hydromorphic soils<\/b><span class=\"s1\">, while <\/span><b>southern slopes<\/b><span class=\"s1\"> contain <\/span><b>alluvial-xeromorphic soils<\/b><span class=\"s1\">.<\/span><\/p>\n<p class=\"p3\"><span class=\"s3\"><b>Biological factors<\/b><\/span>, <span class=\"s3\"><b>soil-forming rocks<\/b><\/span>, and <span class=\"s3\"><b>topographic deformations<\/b><\/span> play an important role in the soil formation process.<\/p>\n<p class=\"p3\">Closer to <span class=\"s3\"><b>valleys<\/b><\/span>, stronger <span class=\"s3\"><b>surface runoff and erosion<\/b><\/span> reduce moisture and nutrients, resulting in <span class=\"s3\"><b>sparse vegetation cover<\/b><\/span>.<\/p>\n<p class=\"p1\"><span class=\"s1\">The <\/span><b>morphological characteristics<\/b><span class=\"s1\"> of the soils are determined by the diversity of <\/span><b>mountain rocks<\/b><span class=\"s1\">, <\/span><b>erosional processes<\/b><span class=\"s1\">, and <\/span><b>hydrological activity<\/b><span class=\"s1\">.<\/span><\/p>\n<p class=\"p1\"><span class=\"s1\">Soils undergo continuous <\/span><b>degradation, regeneration, and renewal<\/b><span class=\"s1\">.<\/span><\/p>\n<p class=\"p3\">After <span class=\"s3\"><b>rock weathering<\/b><\/span>, stable soils develop, allowing <span class=\"s3\"><b>new vegetation<\/b><\/span> to form.<\/p>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>The diversity of physical-geographical factors, geomorphological structure, climatic conditions, and altitudinal variation of relief contributes to the formation of various soil types, corresponding to specific bio-climatic zones and landscapes. The main soil types of the Zomin National Nature Park include: In the foothill zone \u2014 dark brown soils; In the sub-foothill zone \u2014 light brown [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":465,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-467","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/467","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/comments?post=467"}],"version-history":[{"count":2,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/467\/revisions"}],"predecessor-version":[{"id":621,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/467\/revisions\/621"}],"up":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/465"}],"wp:attachment":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/media?parent=467"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}