{"id":4089,"date":"2023-07-21T16:18:45","date_gmt":"2023-07-21T12:18:45","guid":{"rendered":"https:\/\/journal.geonatres.az\/?p=4089"},"modified":"2026-02-13T22:49:59","modified_gmt":"2026-02-13T18:49:59","slug":"h%c9%99k%c9%99ricay-hovz%c9%99sind%c9%99-yayilan-dag-mes%c9%99-torpaqlarinin-isgaldan-%c9%99vv%c9%99lki-v%c9%99ziyy%c9%99ti-v%c9%99-onlarin-b%c9%99rpasi-yollari","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/h%c9%99k%c9%99ricay-hovz%c9%99sind%c9%99-yayilan-dag-mes%c9%99-torpaqlarinin-isgaldan-%c9%99vv%c9%99lki-v%c9%99ziyy%c9%99ti-v%c9%99-onlarin-b%c9%99rpasi-yollari\/","title":{"rendered":"THE SITUATION OF THE MOUNTAINFOREST SOILS OF THE HAKARI RIVER BASIN BEFORE THE OCCUPATION AND THE WAYS OF THEIR RESTORATION"},"content":{"rendered":"<p><strong>M.A.Mammadov, A.M.Zulfugarova<\/strong><\/p>\n<p>DOI: <a href=\"https:\/\/r.mkt21.rads-doi.org\/tr\/cl\/lTu4KQmmKiXiFJNB587eKj0m1A2Rrhb7mzEJwN_TxnqRbyZNg6uY8-uC1ABVrBlrW63Ka1H1iFBEjwekM1Td5krBI7IWFLnt_mPxo_QXEdbBy10Fb8RJwrpRvGWrgF8QoFaCn2DLvvCB4ZiLGt4td2Do2xUxuL3IPxRVZik5iQ_p3ayE_elQeTvRz5N71NQUrbS434UllsNDUH_aCuQJ3TUq5e2o-5iIgdtGYQXLr0EwAQZNNilrWebUvj8\" target=\"_blank\" rel=\"noopener\" data-saferedirecturl=\"https:\/\/www.google.com\/url?q=https:\/\/r.mkt21.rads-doi.org\/tr\/cl\/lTu4KQmmKiXiFJNB587eKj0m1A2Rrhb7mzEJwN_TxnqRbyZNg6uY8-uC1ABVrBlrW63Ka1H1iFBEjwekM1Td5krBI7IWFLnt_mPxo_QXEdbBy10Fb8RJwrpRvGWrgF8QoFaCn2DLvvCB4ZiLGt4td2Do2xUxuL3IPxRVZik5iQ_p3ayE_elQeTvRz5N71NQUrbS434UllsNDUH_aCuQJ3TUq5e2o-5iIgdtGYQXLr0EwAQZNNilrWebUvj8&#038;source=gmail&#038;ust=1690888246308000&#038;usg=AOvVaw12QO8FuECLWAG-8AA9bx6b\">10.59423\/gnr.2023.36.30.005<\/a><\/p>\n<p style=\"text-align: justify;\">\n<strong>Annotation<\/strong>. Areas under different forest types and some physico-chemical characteristics of the barren mountain-forest, rotten mountain-forest and brown mountain-forest soils located in the upper reaches of the Hekari river basin were studied in the article. The research has been conducted on the impact of volcanic and landslide and landslide deposits on soil granulometric composition, water retention, drainage, and water permeability in the middle mountain belt at an altitude of 1000-2000 meters above sea level. In the research, the impact of the geomorphological structure of the area, its altitude above sea level, slope inclination, exposure, and changes within a wide range of climate factors on the formation of soil types is being investigated. The research has focused on examining the impact of the degree of fragmentation of the narrow river network and dry valleys, as well as the diversity and density of forest species composition, on the formation of various subtypes of barren mountainforest, degraded mountain-forest, and chestnut forest soils in the basin. Extensive research has been conducted on the widespread destruction of valuable Oak and Hornbeam forests in the area by the occupiers, the alteration of the lower boundary of forests, and the degree of soil degradation in deforested areas and areas that have emerged from under the forest cover.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords<\/strong>: forest, soil, humus, nitrogen, degradation.<\/p>\n<p><strong>References<\/strong><\/p>\n<ol>\n<li>\u018fli\u00adyev H.\u018f., Mir\u00adz\u0259\u00adyev \u015e.\u0130. H\u0259\u00adk\u0259\u00adri\u00ad\u00e7ay h\u00f6v\u00adz\u0259\u00adsi\u00adnin da\u011f-me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131 v\u0259 on\u00adlar\u00addan s\u0259\u00adm\u0259\u00adr\u0259\u00adli is\u00adti\u00adfa\u00add\u0259 edil\u00adm\u0259\u00adsi. Ba\u00adk\u0131-1979, 126 s.<\/li>\n<li>\u018fli\u00adyev H.\u018f., La\u00ad\u00e7\u0131n me\u00ad\u015f\u0259 t\u0259\u00ads\u0259r\u00adr\u00fc\u00adfa\u00adt\u0131 ida\u00adr\u0259\u00adsi\u00adnin ta\u00adbe\u00adli\u00adyin\u00add\u0259 olan tor\u00adpaq\u00adla\u00adr\u0131n qe\u00adne\u00adtik x\u00fc\u00adsusiy\u00ady\u0259t\u00adl\u0259\u00adri v\u0259 ya\u00ady\u0131l\u00adma\u00ads\u0131\u00adn\u0131n \u00f6y\u00adr\u0259\u00adnil\u00adm\u0259\u00adsi. El\u00admi he\u00adsa\u00adbat, AMEA AK. H.\u018f.\u018fli\u00adyev ad. C\u0130 1980.\u00a0 91 s.<\/li>\n<li>Ge\u00adra\u00adsi\u00admov \u0130.P.\u00a0 M\u00fca\u00adsir tor\u00adpaq\u00ad\u015f\u00fc\u00adnas\u00adl\u0131\u00ad\u011f\u0131n\u00a0 ge\u00adne\u00adtik, co\u011f\u00adra\u00adfi v\u0259 ta\u00adri\u00adxi prob\u00adlem\u00adl\u0259\u00adri,\u00a0 Moskva,\u00a0 Elm-1976. 300 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>X\u0259\u00adli\u00adlov M.Y., R\u0259\u00adsu\u00adlov V.R., H\u0259\u00ads\u0259\u00adnov M. S., M\u0259m\u00adm\u0259\u00addov M.\u018f. Ki\u00ad\u00e7ik Qaf\u00adqa\u00adz\u0131n c\u0259\u00adnub-\u015f\u0259rq his\u00ads\u0259\u00adsin\u00add\u0259 da\u011f me\u00ad\u015f\u0259\u00adl\u0259\u00adri\u00adnin v\u0259 arid me\u00ad\u015f\u0259\u00adl\u0259\u00adrin \u0259sas edi\u00adfi\u00adka\u00adtor\u00adla\u00adr\u0131\u00adn\u0131n eko\u00adlo\u00adji area\u00adl\u0131\u00adn\u0131n \u00f6y\u00adr\u0259\u00adnil\u00adm\u0259\u00adsi. El\u00admi he\u00adsa\u00adbat, AMEA akad.. H.\u018f.\u018fli\u00adyev ad\u0131\u00adna Co\u011f\u00adra\u00adfi\u00adya ins\u00adti\u00adtu\u00adtu, Ba\u00adk\u0131, 1988, 268 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>Klo\u00adpo\u00adtovs\u00adki A.B, Sa\u00adla\u00adye\u00adv E. M,Zey\u00adna\u00adlov \u018f.K. Qo\u00adnur \u00e7\u00fc\u00adr\u00fcn\u00adt\u00fc\u00adl\u00fc kar\u00adbo\u00adnat\u00adl\u0131 da\u011f-me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131. Az\u0259r\u00adbay\u00adcan SSR tor\u00adpaq\u00adla\u00adr\u0131 Ba\u00adk\u0131 1953, s.163-167. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>Qor\u00ad\u00e7a\u00adruk L.G. Qaf\u00adqa\u00adz\u0131n D\u00f6v\u00adl\u0259t\u00a0 Bi\u00ados\u00adfer Qo\u00adru\u00ad\u011fu. Qaf\u00adqa\u00adz\u0131n m\u00fch\u00adafi\u00adz\u0259 ol\u00adunan da\u011f-me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131.\u00a0 Mosk\u00adva, Elm-1992, 240 s<\/li>\n<li>H\u0259\u00ads\u0259\u00adnov \u015e.G. C\u0259\u00adnub-q\u0259r\u00adbi Az\u0259r\u00adbay\u00adca\u00adn\u0131n tor\u00adpaq\u00adla\u00adr\u0131\u00adn\u0131n ge\u00adne\u00adtik x\u00fc\u00adsu\u00adsiy\u00ady\u0259t\u00adl\u0259\u00adri v\u0259 bo\u00adnit\u00adrov\u00adka\u00ads\u0131. Ba\u00adk\u0131-1978, 220 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>M\u0259m\u00adm\u0259\u00addov Q.\u015e. Az\u0259r\u00adbay\u00adca\u00adn\u0131n tor\u00adpaq eh\u00adti\u00adyat\u00adla\u00adr\u0131. Ba\u00adk\u0131-2002, 132 s.<\/li>\n<li>Mir\u00adz\u0259\u00adyev. \u015e.\u0130. Ki\u00ad\u00e7ik Qaf\u00adqa\u00adz\u0131n c\u0259\u00adnub-\u015f\u0259rq his\u00ads\u0259\u00adsin\u00add\u0259 da\u011f-me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131\u00adn\u0131n me\u00ad\u015f\u0259\u00adbit\u00adm\u0259 x\u00fc\u00adsu\u00adsiy\u00ady\u0259t\u00adl\u0259\u00adri\u00adnin \u00f6y\u00adr\u0259\u00adnil\u00adm\u0259\u00adsi (Z\u0259n\u00adgi\u00adlan, Qu\u00adbad\u00adl\u0131 v\u0259 C\u0259b\u00adra\u00ady\u0131l ra\u00adyon\u00adla\u00adr\u0131 \u0259ra\u00adzi\u00adl\u0259\u00adri da\u00adxi\u00adlin\u00add\u0259). El\u00admi-he\u00adsa\u00adbat. AMEA aka\u00adde\u00admik H.\u018f.\u018fli\u00adyev ad\u0131\u00adna Co\u011f\u00adra\u00adfi\u00adya ins\u00adti\u00adtu\u00adtu. Ba\u00adk\u0131-1985. 97 s.<\/li>\n<li>Sa\u00adla\u00adyev M.E. Ki\u00ad\u00e7ik Qaf\u00adqa\u00adz\u0131n tor\u00adpaq\u00adla\u00adr\u0131. Ba\u00adk\u0131: 1966, 329 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>Sa\u00adla\u00adyev E. Az\u0259r\u00adbay\u00adcan tor\u00adpaq\u00adla\u00adr\u0131\u00adn\u0131n\u00a0 di\u00adaq\u00adnos\u00adti\u00adka\u00ads\u0131 v\u0259 t\u0259s\u00adni\u00adfa\u00adt\u0131. Ba\u00adk\u0131: 1991, 240 s.<\/li>\n<li>Sa\u00adba\u015f\u00advi\u00adli N.M. G\u00fcr\u00adc\u00fcs\u00adta\u00adn\u0131n tor\u00adpaq\u00adla\u00adr\u0131. G\u00fcr\u00adc\u00fcs\u00adtan EA. Tor\u00adpaq\u00ad\u015f\u00fc\u00adnas\u00adl\u0131q ins\u00adti\u00adtu\u00adtu. Tbli\u00adsi -1948, 250 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>Sa\u00adla\u00admov G.A. Ki\u00ad\u00e7ik Qaf\u00adqa\u00adz\u0131n \u015fi\u00admal-q\u0259r\u00adbin\u00add\u0259 ya\u00ady\u0131\u00adlan me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131\u00adn\u0131n ge\u00adne\u00adtik-is\u00adteh\u00adsa\u00adlat xas\u00ads\u0259\u00adl\u0259\u00adri\u00adnin \u00f6y\u00adr\u0259\u00adnil\u00adm\u0259\u00adsi. El\u00admi he\u00adsa\u00adbat, AMEA akad. H.\u018f.\u018fli\u00adyev ad\u0131\u00adna Co\u011f\u00adra\u00adfi\u00adya ins\u00adti\u00adtu\u00adtu, Ba\u00adk\u0131 1983, 173 s.<\/li>\n<li>\u015e\u0259\u00adri\u00adfov F. Ki\u00ad\u00e7ik Qaf\u00adqa\u00adz\u0131n \u015f\u0259rq ya\u00adma\u00adc\u0131\u00adn\u0131n da\u011f-me\u00ad\u015f\u0259 tor\u00adpaq\u00adla\u00adr\u0131.\u00a0 1984. 193 s. (rus di\u00adlin\u00add\u0259).<\/li>\n<li>Zonn S.V. Tor\u00adpaq\u00a0 \u00f6r\u00adt\u00fc\u00ady\u00fc v\u0259\u00a0\u00a0 SSSR-nin subt\u00adro\u00adpik\u00adl\u0259\u00adri\u00adnin\u00a0 t\u0259\u00adbi\u0259\u00adti\u00adnin\u00a0 v\u0259 t\u0259\u00ads\u0259r\u00adr\u00fc\u00adfa\u00adt\u0131\u00adn\u0131n\u00a0 d\u0259\u00adyi\u015f\u00addi\u00adril\u00adm\u0259\u00adsi prob\u00adlem\u00adl\u0259\u00adri. (rus di\u00adlin\u00add\u0259), Mosk\u00adva,\u00a0 Elm-1987, 166.s.<\/li>\n<\/ol>\n<p><strong>\u00c7apa q\u0259bul olunub:<\/strong>\u00a018 may 2023<\/p>\n<p><strong>M\u0259qal\u0259ni y\u00fckl\u0259<\/strong><\/p>\n<p style=\"text-align: justify;\"><strong>M.A.Mammadov, A.M.Zulfugarova<\/strong> &#8211; The situat\u0131on of the mountain-forest soils of the Hakari river basin before the occupation and the ways of their restoration. Geography and Natural Resources, \u21161 (19), 2023, pp.\u00a0 31-38.<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>M.A.Mammadov, A.M.Zulfugarova DOI: 10.59423\/gnr.2023.36.30.005 Annotation. Areas under different forest types and some physico-chemical characteristics of the barren mountain-forest, rotten mountain-forest and brown mountain-forest soils located in the upper reaches of the Hekari river basin were studied in the article. The research has been conducted on the impact of volcanic and landslide and landslide deposits on [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-4089","post","type-post","status-publish","format-standard","hentry","category-mqallr"],"blocksy_meta":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>THE SITUATION OF THE MOUNTAINFOREST SOILS OF THE HAKARI RIVER BASIN BEFORE THE OCCUPATION AND THE WAYS OF THEIR RESTORATION<\/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\/h\u0259k\u0259ricay-hovz\u0259sind\u0259-yayilan-dag-mes\u0259-torpaqlarinin-isgaldan-\u0259vv\u0259lki-v\u0259ziyy\u0259ti-v\u0259-onlarin-b\u0259rpasi-yollari\/\" \/>\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 SITUATION OF THE MOUNTAINFOREST SOILS OF THE HAKARI RIVER BASIN BEFORE THE OCCUPATION AND THE WAYS OF THEIR RESTORATION\" \/>\n<meta property=\"og:description\" content=\"M.A.Mammadov, A.M.Zulfugarova DOI: 10.59423\/gnr.2023.36.30.005 Annotation. Areas under different forest types and some physico-chemical characteristics of the barren mountain-forest, rotten mountain-forest and brown mountain-forest soils located in the upper reaches of the Hekari river basin were studied in the article. The research has been conducted on the impact of volcanic and landslide and landslide deposits on [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/journal.geonatres.az\/en\/h\u0259k\u0259ricay-hovz\u0259sind\u0259-yayilan-dag-mes\u0259-torpaqlarinin-isgaldan-\u0259vv\u0259lki-v\u0259ziyy\u0259ti-v\u0259-onlarin-b\u0259rpasi-yollari\/\" \/>\n<meta property=\"og:site_name\" content=\"Geography and Natural Resources\" \/>\n<meta property=\"article:published_time\" content=\"2023-07-21T12:18:45+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-02-13T18:49:59+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\" content=\"1024\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"Sarkhan 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