{"id":312,"date":"2019-03-21T11:07:57","date_gmt":"2019-03-21T07:07:57","guid":{"rendered":"http:\/\/journal.geonatres.az\/?p=312"},"modified":"2019-07-19T00:05:00","modified_gmt":"2019-07-18T20:05:00","slug":"l%c9%99ng%c9%99biz-silsil%c9%99si-v%c9%99-%c9%99traf-%c9%99razi-torpaqlarinin-fiziki-kimy%c9%99vi-s%c9%99ciyy%c9%99si","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/l%c9%99ng%c9%99biz-silsil%c9%99si-v%c9%99-%c9%99traf-%c9%99razi-torpaqlarinin-fiziki-kimy%c9%99vi-s%c9%99ciyy%c9%99si\/","title":{"rendered":"THE PHYSICAL AND CHEMICAL CHARACTERISTICS OF THE SOIL COVER OF THE LANGABIZ RIDGE AND SURROUNDING AREAS"},"content":{"rendered":"

G.A.Imanova<\/strong><\/p>\n

Abstract.\u00a0<\/strong>The soil cover of the Langabiz ridge and surrounding areas has been studied, the boundaries of its develop\u00adment were specified, and the morphogenetic features and phy\u00adsicochemical properties of these soils were cha\u00adrac\u00adte\u00adri\u00adzed.<\/p>\n

Within the research object the following soils are de\u00adveloped: typical brown mountain-forest, carbonate brown-mountain-forest, typical brown-mountain, car\u00adbo\u00adnate-mountain-brown, steppe-mountain-brown, dark-gray-brown, ordinary gray-brown, light gray-brown, gray and gray – brown.<\/p>\n

A soil map of the Langabiz Ridge and the sur\u00adro\u00adun\u00adding territories is drawn up at a scale of 1: 100 000.<\/p>\n

REFERENCES<\/strong><\/p>\n

    \n
  1. Az\u0259rbaycan d\u00f6vl\u0259t torpaq x\u0259rit\u0259sinin le\u00adgen\u00addas\u0131. Q.\u015e.M\u0259mm\u0259dov, M.P.Baba\u00adyev, \u015e.Q.H\u0259\u00ads\u0259novun redakt\u0259si il\u0259. Bak\u0131: Elm, 2003, 68 s.<\/li>\n
  2. Az\u0259rbaycan Respubliks\u0131n\u0131n torpaq atlas\u0131. Bak\u0131: Bak\u0131 Kartoqrafiya Fabriki, 2007, 102 s.<\/li>\n
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  4. M\u0259mm\u0259dov Q.\u015e. Torpaq\u015f\u00fcnasl\u0131q v\u0259 tor\u00adpaq co\u011frafiyas\u0131n\u0131n \u0259saslar\u0131. Bak\u0131: Elm, 2007, 644 s.<\/li>\n
  5. M\u0259mm\u0259dov Q.\u015e., Babayev M.P., \u0130smay\u0131\u00adlov A.\u0130. Az\u0259rbaycan\u0131n torpaq t\u0259snifat\u0131n\u0131n \u00dcRB sis\u00adtemi il\u0259 korrelyasiyas\u0131. Bak\u0131: Elm, 2002, 225 s.<\/li>\n
  6. M\u0259mm\u0259dov Q.\u015e. Az\u0259rbaycan\u0131n torpaq eh\u00adtiyatlar\u0131. Bak\u0131: Elm, 2002, 131 s.<\/li>\n
  7. \u0410\u043b\u0438\u0435\u0432 \u0413.\u0410. \u041f\u043e\u0447\u0432\u044b \u0411\u043e\u043b\u044c\u0448\u043e\u0433\u043e \u041a\u0430\u0432\u043a\u0430\u0437\u0430 (\u0432 \u043f\u0440\u0435\u00ad\u0434\u0435\u043b\u0430\u0445 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0441\u043a\u043e\u0439 \u0421\u0421\u0420). \u0427.I. \u0411\u0430\u043a\u0443: \u042d\u043b\u043c, 1978, 156 \u0441.<\/li>\n
  8. \u0410\u043b\u0438\u0435\u0432 \u0413.\u0410. \u041f\u043e\u0447\u0432\u044b \u0411\u043e\u043b\u044c\u0448\u043e\u0433\u043e \u041a\u0430\u0432\u043a\u0430\u0437\u0430 (\u0432 \u043f\u0440\u0435\u00ad\u0434\u0435\u043b\u0430\u0445 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0441\u043a\u043e\u0439 \u0421\u0421\u0420). \u0427.II. \u0411\u0430\u043a\u0443: \u042d\u043b\u043c, 1994, 310 \u0441.<\/li>\n
  9. \u0410\u043b\u0438\u0435\u0432 \u0413.\u0410., \u0413\u0430\u0441\u0430\u043d\u043e\u0432 \u0428.\u0413., \u0418\u0441\u043a\u0435\u043d\u0434\u0435\u0440\u043e\u0432 \u0418.\u0428., \u0411\u0430\u0431\u0430\u0435\u0432 \u041c.\u041f., \u041c\u0430\u043c\u0435\u0434\u043e\u0432 \u0413.\u0428. \u041f\u043e\u0447\u0432\u0435\u043d\u043d\u0430\u044f \u043a\u0430\u0440\u0442\u0430 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0441\u043a\u043e\u0439 \u0421\u0421\u0420 (1:600000). \u2013\u041c., 1991<\/li>\n
  10. \u0411\u0443\u0434\u0430\u0433\u043e\u0432 \u0411.\u0410., \u041c\u0430\u043c\u0435\u0434\u043e\u0432 \u0413.\u0428. \u0411\u043e\u043d\u0438\u0442\u0438\u00ad\u0440\u043e\u0432\u043a\u0430 \u0442\u0438\u043f\u043e\u0432 \u043b\u0430\u043d\u0434\u0448\u0430\u0444\u0442\u043e\u0432 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0441\u043a\u043e\u0439 \u0421\u0421\u0420 \/\/ \u0414\u043e\u043a\u00ad\u043b\u0430\u00ad\u0434\u044b \u0410\u041d \u0410\u0437\u0435\u0440\u0431.\u0421\u0421\u0420, \u0442.XVIII, 1987, \u21167, \u0441.67-71..<\/li>\n
  11. \u0421\u0430\u043b\u0430\u0435\u0432 \u041c.\u042d. \u0414\u0438\u0430\u0433\u043d\u043e\u0441\u0442\u0438\u043a\u0430 \u0438 \u043a\u043b\u0430\u0441\u00ad\u0441\u0438\u00ad\u0444\u0438\u00ad\u043a\u0430\u0446\u0438\u044f \u043f\u043e\u0447\u0432 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0430. \u0411\u0430\u043a\u0443: \u042d\u043b\u043c, 1991, 240 \u0441.<\/li>\n
  12. \u0428\u0438\u0445\u043b\u0438\u043d\u0441\u043a\u0438\u0439 \u042d.\u041c., \u041c\u0430\u0434\u0430\u0442\u0437\u0430\u0434\u0435 \u0410.\u0410. \u041a\u043b\u0438\u00ad\u043c\u0430\u0442 \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0430. \u0411\u0430\u043a\u0443: \u0410\u041d \u0410\u0437\u0435\u0440\u0431.\u0421\u0421\u0420, 1968, 200.<\/li>\n<\/ol>\n

     <\/p>\n

    Download the article<\/strong><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

    G.A.Imanova Abstract.\u00a0The soil cover of the Langabiz ridge and surrounding areas has been studied, the boundaries of its develop\u00adment were specified, and the morphogenetic features and phy\u00adsicochemical properties of these soils were cha\u00adrac\u00adte\u00adri\u00adzed. Within the research object the following soils are de\u00adveloped: typical brown mountain-forest, carbonate brown-mountain-forest, typical brown-mountain, car\u00adbo\u00adnate-mountain-brown, steppe-mountain-brown, dark-gray-brown, ordinary gray-brown, light […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-312","post","type-post","status-publish","format-standard","hentry","category-article"],"blocksy_meta":[],"yoast_head":"\nTHE PHYSICAL AND CHEMICAL CHARACTERISTICS OF THE SOIL COVER OF THE LANGABIZ RIDGE AND SURROUNDING AREAS<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/journal.geonatres.az\/en\/l\u0259ng\u0259biz-silsil\u0259si-v\u0259-\u0259traf-\u0259razi-torpaqlarinin-fiziki-kimy\u0259vi-s\u0259ciyy\u0259si\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:locale:alternate\" content=\"az\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"THE PHYSICAL AND CHEMICAL CHARACTERISTICS OF THE SOIL COVER OF THE LANGABIZ RIDGE AND SURROUNDING AREAS\" \/>\n<meta property=\"og:description\" content=\"G.A.Imanova Abstract.\u00a0The soil cover of the Langabiz ridge and surrounding areas has been studied, the boundaries of its develop\u00adment were specified, and the morphogenetic features and phy\u00adsicochemical properties of these soils were cha\u00adrac\u00adte\u00adri\u00adzed. Within the research object the following soils are de\u00adveloped: typical brown mountain-forest, carbonate brown-mountain-forest, typical brown-mountain, car\u00adbo\u00adnate-mountain-brown, steppe-mountain-brown, dark-gray-brown, ordinary gray-brown, light […]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/journal.geonatres.az\/en\/l\u0259ng\u0259biz-silsil\u0259si-v\u0259-\u0259traf-\u0259razi-torpaqlarinin-fiziki-kimy\u0259vi-s\u0259ciyy\u0259si\/\" \/>\n<meta property=\"og:site_name\" content=\"Geography and Natural Resources\" \/>\n<meta property=\"article:published_time\" content=\"2019-03-21T07:07:57+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2019-07-18T20:05:00+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/journal.geonatres.az\/wp-content\/uploads\/2026\/03\/ChatGPT-Image-27-\u043c\u0430\u0440.-2026-\u0433.-01_39_18.png\" \/>\n\t<meta property=\"og:image:width\" content=\"1536\" \/>\n\t<meta property=\"og:image:height\" 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