AKARSU: Yer alt\u0131nda yada yer y\u00fcz\u00fcnde belirli bir do\u011fal yatak i\u00e7inde,s\u00fcrekli yada d\u00f6nemli ak\u0131\u015f\u0131 bulunan su k\u00fctlelerine akarsu denir.Akarsular;okyanus,deniz ve g\u00f6llerle,atmosfer ve karalar aras\u0131ndaki su dola\u015f\u0131m\u0131n\u0131n \u00f6nemli bir unsurudur.<\/p>\n
T\u00dcRK\u0130YE’DE K\u0130 AKARSULARIN GENEL \u00d6ZELL\u0130KLER\u0130<\/p>\n
T\u00fcrkiye, iklim ko\u015fullar\u0131 ve yer \u015fekillerinin do\u011fal yap\u0131s\u0131na ba\u011fl\u0131 olarak s\u0131k bir akarsu a\u011f\u0131na sahiptir.ancak akarsular\u0131m\u0131z\u0131n uzunluklar\u0131 fazla de\u011fildir.T\u00fcrkiye’nin bir yar\u0131mada olu\u015fu ve da\u011flar\u0131n genellikle k\u0131y\u0131lara paralel s\u0131ralar halinde uzanmas\u0131, uzun akarsular\u0131n olu\u015fma\u0131n\u0131 engellemi\u015ftir.K\u0131y\u0131lardaki da\u011flardan kayna\u011f\u0131n\u0131 alan akrsular, k\u0131sa bir yol ald\u0131ktan sonra denize ula\u015f\u0131r.En uzun akarsuyumuz olan K\u0131z\u0131l \u0131rmak’\u0131n boyu (\u0130\u00e7 Anadolu’da geni\u015f\u00e7e bir kavis \u00e7izdi\u011fi halde)1355 km’yi ancak bulur.
\n Akarsular\u0131m\u0131z\u0131n di\u011fer bir \u00f6zelli\u011fi de, ta\u015f\u0131d\u0131klar\u0131 su miktar\u0131n\u0131n az olmas\u0131d\u0131r.T\u00fcrkiye’nin b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcn\u00fcn yar\u0131 kurak iklimin etkisinde olmas\u0131 nedeniyle az ya\u011f\u0131\u015f almas\u0131 bunun ba\u015fl\u0131ca nedenidir.Akarsular\u0131m\u0131z\u0131n ta\u015f\u0131d\u0131klar\u0131 su miktar\u0131 azl\u0131\u011f\u0131n\u0131n di\u011fer nedeni de,akarsu havzalar\u0131n\u0131n dar olu\u015fudur.Akarsular\u0131m\u0131z\u0131n
\nboylar\u0131 k\u0131sa,kollar\u0131 da az oldu\u011fundan do\u011fal olarak ta\u015f\u0131d\u0131klar\u0131 su,
\nfazla olmamaktad\u0131r.Ancak, ya\u011f\u0131\u015fs\u0131z mevsimi olmayan Do\u011fu Karadeniz b\u00f6l\u00fcm\u00fcn\u00fcn akarsular\u0131 her zaman bol su ta\u015f\u0131maktad\u0131r.
\n Akarsular\u0131m\u0131z\u0131n rejimleri d\u00fczenli de\u011fildir.T\u00fcrkiye’de ya\u011f\u0131\u015f rejimin
\nd\u00fczensiz olu\u015fu, ilkbahardaki kar erimeleri ve yaz\u0131n buharla\u015fman\u0131n fazla olmas\u0131, akarsular\u0131m\u0131z\u0131n ta\u015f\u0131d\u0131klar\u0131 su miktr\u0131n\u0131n y\u0131l boyunca b\u00fcy\u00fck de\u011fi\u015fikliklere u\u011framas\u0131n\u0131n ba\u015fl\u0131ca nedenlerindendir.Akarsular\u0131m\u0131z\u0131n b\u00fcy\u00fck bir k\u0131sm\u0131nda su seviyesinin en y\u00fcksek d\u00fczeyde oldu\u011fu d\u00f6nem ilkbahara rastlar.
\nYataklar\u0131n e\u011fiminin yazla olu\u015fu, akarsular\u0131m\u0131z\u0131n bir di\u011fer \u00f6zelli\u011fidir.Bu nedenle ak\u0131\u015f h\u0131zlar\u0131, dolay\u0131s\u0131 ile erozyonu h\u0131zland\u0131r\u0131c\u0131 etkileri fazlad\u0131r.Bol al\u00fcvyon ta\u015f\u0131r ve denizlere d\u00f6kt\u00fckleri yerlerde deltalar olu\u015ftururlar.T\u00fcrkiye’deki akarsular\u0131n genellikle denge profilini almam\u0131\u015f olmalar\u0131, T\u00fcrkiyenin son jeolojik d\u00f6nemde \u015fekillenmi\u015f olmas\u0131ndan, ba\u015fka bir de\u011fi\u015fle “gen\u00e7 arazi” yap\u0131s\u0131ndan kaynaklanmaktad\u0131r.Akarsular\u0131mz\u0131n hidroelektrik enrji \u00fcretimine \u00e7ok
\nelveri\u015fli olmalar\u0131 da dar ve derin vadiler olu\u015fturmalar\u0131n\u0131n bir sonucudur.Bu nedenle \u00fclkemizde \u00e7ok say\u0131da baraj yap\u0131lm\u0131\u015f ve hidroelektrik santirali kurulmu\u015ftur.
\n Akarsular\u0131m\u0131z\u0131n \u00e7o\u011fu da\u011fl\u0131k kesimlerden inmektedir.Ta\u015f\u0131d\u0131klar\u0131 kum ve \u00e7ak\u0131llarla yataklar\u0131n\u0131 doldurduklar\u0131 i\u00e7in denize yak\u0131n k\u0131s\u0131mlar\u0131nda bile ula\u015f\u0131ma elveri\u015fli de\u011fildir.<\/p>\n","protected":false},"excerpt":{"rendered":"
AKARSU: Yer alt\u0131nda yada yer y\u00fcz\u00fcnde belirli bir do\u011fal yatak i\u00e7inde,s\u00fcrekli yada d\u00f6nemli ak\u0131\u015f\u0131 bulunan su k\u00fctlelerine akarsu denir.Akarsular;okyanus,deniz ve g\u00f6llerle,atmosfer ve karalar aras\u0131ndaki su dola\u015f\u0131m\u0131n\u0131n \u00f6nemli bir unsurudur. T\u00dcRK\u0130YE’DE K\u0130 AKARSULARIN GENEL \u00d6ZELL\u0130KLER\u0130 T\u00fcrkiye, iklim ko\u015fullar\u0131 ve yer \u015fekillerinin do\u011fal yap\u0131s\u0131na ba\u011fl\u0131 olarak s\u0131k bir akarsu a\u011f\u0131na sahiptir.ancak akarsular\u0131m\u0131z\u0131n uzunluklar\u0131 fazla de\u011fildir.T\u00fcrkiye’nin bir yar\u0131mada …<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[2993,2796,2798,2925],"class_list":["post-1007","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akarsu-ve-ozellikleri","tag-atmosfer","tag-hidroelektrik","tag-iklim"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1007","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=1007"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1007\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1007"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1007"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1007"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}