{"id":100,"date":"2020-04-23T10:29:35","date_gmt":"2020-04-23T10:29:35","guid":{"rendered":"http:\/\/localhost\/pelister\/?post_type=soils&#038;p=100"},"modified":"2020-09-09T05:43:49","modified_gmt":"2020-09-09T05:43:49","slug":"test-1","status":"publish","type":"soils","link":"https:\/\/park-pelister.com\/sq\/soils\/test-1\/","title":{"rendered":"Tok\u00ebs"},"content":{"rendered":"<p>Llojet e tok\u00ebs n\u00eb PK Pelister<\/p>\n<p>Parku Komb\u00ebtar Pelister ka nj\u00eb heterogjenitet t\u00eb madh t\u00eb faktor\u00ebve pedogjenik\u00eb, gj\u00eb q\u00eb kusht\u00ebzon nj\u00eb larmi t\u00eb madhe t\u00eb mbules\u00ebs s\u00eb tok\u00ebs. Formimi i tok\u00ebs \u00ebsht\u00eb i lidhur ngusht\u00eb me faktor\u00ebt pedogjenetik\u00eb, si\u00e7 \u00ebsht\u00eb substrati gjeologjik, pastaj biodiversiteti n\u00eb mjedis, njeriu, klima, terreni, epoka e terrenit, pjerr\u00ebsia, ekspozimi i terrenit dhe faktor\u00eb t\u00eb tjer\u00eb.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-33\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/pocva-300x201.jpg\" alt=\"\" width=\"337\" height=\"226\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pocva-300x201.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pocva.jpg 640w\" sizes=\"(max-width: 337px) 100vw, 337px\" \/>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0<img loading=\"lazy\" class=\"alignnone wp-image-378\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/pocva-1-300x210.jpg\" alt=\"\" width=\"323\" height=\"226\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pocva-1-300x210.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pocva-1.jpg 561w\" sizes=\"(max-width: 323px) 100vw, 323px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p>Substrati gjeologjik ka nj\u00eb ndikim t\u00eb madh n\u00eb pedogjenez\u00ebn e tok\u00ebs, sepse formimi i tokave varet drejtp\u00ebrdrejt nga produktet e dekompozimit t\u00eb tyre. Karakteristika kryesore e substratit gjeologjik \u00ebsht\u00eb se \u00ebsht\u00eb silikat. Granit\u00ebt q\u00eb mbizot\u00ebrojn\u00eb terrenin jan\u00eb shk\u00ebmbinj acidik, n\u00eb t\u00eb cilat p\u00ebrmbajtja e SiOZ arrin rreth 75%, dhe p\u00ebrmbajtja e A1Z03 rreth 13%. Oksidet e tjera jan\u00eb shum\u00eb pak t\u00eb p\u00ebrfaq\u00ebsuara.<\/p>\n<p><img loading=\"lazy\" class=\"wp-image-375 aligncenter\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/Pelister-Pedoloska-A1-20.000-300x212.jpg\" alt=\"\" width=\"430\" height=\"304\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/Pelister-Pedoloska-A1-20.000-300x212.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/Pelister-Pedoloska-A1-20.000-768x542.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/Pelister-Pedoloska-A1-20.000.jpg 800w\" sizes=\"(max-width: 430px) 100vw, 430px\" \/><\/p>\n<p>Gabro dhe diabaza jan\u00eb shk\u00ebmbinj themelor\u00eb magmatik n\u00eb t\u00eb cil\u00ebt p\u00ebrmbajtja SiOZ arrin deri n\u00eb 47%. Shk\u00ebmbinjt\u00eb e argjil\u00ebs (shistrat e gjelb\u00ebrta, shistrat serikite kuarc) jan\u00eb shk\u00ebmbinj tipik\u00eb me nj\u00eb struktur\u00eb gjethesh. Shk\u00ebmbinjt\u00eb e mbetur (depozitat glaciale dhe fluviglaciale) si shk\u00ebmbinj sedimentar\u00eb, u formuan nga transporti dhe depozitimi i materialit t\u00eb grimcuar nga llojet e shk\u00ebmbinjve t\u00eb p\u00ebrshkruara m\u00eb par\u00eb. Struktura e argjil\u00ebs e disa prej shk\u00ebmbinjve mund\u00ebsoi veprimin m\u00eb t\u00eb madh t\u00eb faktor\u00ebve aktiv pedogjenetik m\u00eb t\u00eb thell\u00eb t\u00eb substratit. Sasia e madhe e kuarcit dhe sasia e vog\u00ebl e materialit balt\u00eb n\u00eb p\u00ebrb\u00ebrjen e shk\u00ebmbinjve \u00ebsht\u00eb nj\u00eb nga arsyet kryesore p\u00ebr p\u00ebrb\u00ebrjen e leht\u00eb t\u00eb dheut.<\/p>\n<p><img loading=\"lazy\" class=\"size-medium wp-image-377 aligncenter\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/brajcino_pedoloska-232x300.jpg\" alt=\"\" width=\"232\" height=\"300\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/brajcino_pedoloska-232x300.jpg 232w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/brajcino_pedoloska.jpg 600w\" sizes=\"(max-width: 232px) 100vw, 232px\" \/><\/p>\n<p>N\u00eb Parkun Komb\u00ebtar &#8220;Pelister&#8221;, rr\u00ebz\u00eb shpateve, n\u00eb form\u00ebn e nj\u00eb seri kone aluviale &#8220;Ladala&#8221; jan\u00eb t\u00eb pranishme tokat koluviale. Ato mbulojn\u00eb nj\u00eb sip\u00ebrfaqe prej 271.80 ha nj\u00eb 1,58% t\u00eb sip\u00ebrfaqes s\u00eb parkut.<\/p>\n<p>N\u00eb format e relievit me onde-kodrinore dhe tarracat liqenore, gjenden zona n\u00ebn tok\u00ebsore t\u00eb lezionuara. Tokat e d\u00ebmtuara, si nj\u00eb lloj i pavarur i tok\u00ebs brenda parkut, mbulojn\u00eb nj\u00eb sip\u00ebrfaqe prej 41,90 ha me 0.24 \u00b0 \/ o. Nj\u00eb zon\u00eb shum\u00eb e vog\u00ebl n\u00eb parkun prej 1.23 ha \u00ebsht\u00eb gjetur si nj\u00eb kompleks me regosol.<\/p>\n<p><img loading=\"lazy\" class=\"wp-image-376 aligncenter\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/pedoloska_vrtuska-300x140.jpg\" alt=\"\" width=\"422\" height=\"197\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pedoloska_vrtuska-300x140.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pedoloska_vrtuska-768x358.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/pedoloska_vrtuska.jpg 800w\" sizes=\"(max-width: 422px) 100vw, 422px\" \/><\/p>\n<p>Rendit\u00ebsit mbulojn\u00eb nj\u00eb sip\u00ebrfaqe prej 6421.60 ha vet\u00ebm 37.4% t\u00eb sip\u00ebrfaqes s\u00eb p\u00ebrgjithshme t\u00eb parkut. Leptozolet, si nj\u00eb lloj i pavarur i tok\u00ebs, gjenden n\u00eb nj\u00eb sip\u00ebrfaqe prej 2537.61 ha me 14.78% t\u00eb sip\u00ebrfaqes totale t\u00eb parkut. N\u00eb nj\u00eb kompleks me regosol ato gjenden n\u00eb nj\u00eb sip\u00ebrfaqe prej 345.96 ha unu 2.01 \u00b0 \/ o, dhe n\u00eb nj\u00eb kompleks me toka pyjore dhe regosol gjenden n\u00eb nj\u00eb sip\u00ebrfaqe prej 7548.65 ha dhe 43,96%.<\/p>","protected":false},"featured_media":381,"template":"","_links":{"self":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/soils\/100"}],"collection":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/soils"}],"about":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/types\/soils"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media\/381"}],"wp:attachment":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media?parent=100"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}