{"id":1438,"date":"2011-06-30T09:11:45","date_gmt":"2011-06-30T06:11:45","guid":{"rendered":"http:\/\/www.islamidavet.com\/kutuphane\/\/?p=1438"},"modified":"2011-07-02T11:35:00","modified_gmt":"2011-07-02T08:35:00","slug":"yeralti-sulari-ve-kaynaklar-2","status":"publish","type":"post","link":"https:\/\/www.islamidavet.com\/kutuphane\/yeralti-sulari-ve-kaynaklar-2\/","title":{"rendered":"Yeralt\u0131 Sular\u0131 ve Kaynaklar"},"content":{"rendered":"<p>Ya\u011f\u0131\u015flar sonucu yery\u00fcz\u00fcne d\u00fc\u015fen sular\u0131n bir k\u0131sm\u0131 y\u00fczeyden akarken bir k\u0131sm\u0131da yeralt\u0131na s\u0131zararak depolan\u0131rlar veya buralarda ak\u0131\u015f g\u00f6sterirler. Bunlara Yeralt\u0131 Sular\u0131 denir. Bu sular\u0131n kendili\u011finden yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yerlere de Kaynak denir.<br \/>\n Yeralt\u0131 suyunun miktar\u0131n\u0131;<br \/>\n Ya\u011f\u0131\u015f Miktar\u0131<br \/>\n Y\u00fczeyin E\u011fimi<br \/>\n Bitki \u00d6rt\u00fcs\u00fc<br \/>\n Zeminin \u00d6zelli\u011fi etkiler.<br \/>\n Al\u00fcvyal Ovalar, Karstik Araziler, Deniz ve G\u00f6l K\u0131y\u0131lar\u0131 yeralt\u0131 suyu bak\u0131m\u0131ndan zengin alanlard\u0131r.<br \/>\n Kaynaklar<br \/>\n Kaynaklar yery\u00fcz\u00fcne \u00e7\u0131k\u0131\u015f \u00f6zelliklerine g\u00f6re de\u011fi\u015firler;<br \/>\n1-Yama\u00e7 Kaynaklar\u0131: Da\u011f ve vadi yama\u00e7lar\u0131nda ge\u00e7irimli tabakan\u0131n yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yerdir.<br \/>\n2- Fay Kaynaklar\u0131: Yeralt\u0131 sular\u0131n\u0131n Fay \u00c7atlaklar\u0131ndan yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 kaynaklard\u0131r. Baz\u0131lar\u0131n\u0131n sular\u0131 derinlerden geldi\u011fi i\u00e7in s\u0131cak olur. Buralara Kapl\u0131ca, Il\u0131ca veya \u00c7ermik denir.<br \/>\n3- Karstik Kaynaklar: Kalkerli arazilerin \u00e7atlaklar\u0131ndan s\u0131zan sular\u0131n toplan\u0131p yery\u00fcz\u00fcne \u00e7\u0131kmas\u0131yla olu\u015fur. Bu sular\u0131n en \u00f6nemli \u00f6zelli\u011fi kire\u00e7li olu\u015flar\u0131d\u0131r.<br \/>\n4- Artezyen Kaynaklar\u0131: \u00d6zellikle k\u0131vr\u0131ml\u0131 sahalardaki \u00e7anakla\u015fm\u0131\u015f arazilerde 2 ge\u00e7irimsiz tabaka aras\u0131nda kalm\u0131\u015f yeralt\u0131 suyunun \u00e7ana\u011f\u0131n taban\u0131n\u0131n delinmesiyle \u00e7\u0131kan bas\u0131n\u00e7l\u0131 kaynakt\u0131r.<br \/>\n5- Gayzer Kaynaklar: Volkanik sahalarda ma\u011fman\u0131n etkisiyle yeralt\u0131 suyunun s\u0131cak su ve buhar olarak d\u0131\u015far\u0131 \u00e7\u0131kmas\u0131 ile olu\u015fan kaynaklard\u0131r. Denizli-Sarayk\u00f6y de \u00f6rne\u011fini g\u00f6rmek m\u00fcmk\u00fcnd\u00fcr.<\/p>\n<p>YER ALTI SULARI VE KAYNAKLAR <\/p>\n<p> Ya\u011f\u0131\u015flarla yer y\u00fcz\u00fcne inen sular\u0131n ge\u00e7irimli tabakadan yer alt\u0131na s\u0131zarak , yer alt\u0131nda olu\u015fturduklar\u0131 sulara yer alt\u0131 sular\u0131 denir.<br \/>\n Yer Alt\u0131 Sular\u0131n\u0131n Beslenmesinde Etkili Olan Fakt\u00f6rler<br \/>\n 1) Ya\u011f\u0131\u015f miktar\u0131,<br \/>\n 2) Ya\u011f\u0131\u015f t\u00fcr\u00fc (Kar ya\u011f\u0131\u015flar\u0131 ile beslenme fazla olur.)<br \/>\n 3) Zeminin ge\u00e7irimlili\u011fi ( al\u00fcvyal ve karstik alanlarda ge\u00e7irimlilik fazlad\u0131r).<br \/>\n 4) Arazinin e\u011fimi :e\u011fimin az oldu\u011fu alanlarda beslenme daha fazlad\u0131r.<br \/>\n 5) Bitki \u00f6rt\u00fcs\u00fc: Y\u00fczeysel ak\u0131m\u0131 engelledi\u011fi i\u00e7in.<br \/>\n Taban Suyu: Al\u00fcvyal ovalar\u0131n taban\u0131nda bulunurlar. Altta ge\u00e7irimsiz tabaka ile<br \/>\n s\u0131n\u0131rland\u0131r\u0131lm\u0131\u015f ge\u00e7irimli tabaka \u00fczerinde biriken sulard\u0131r. Beslenme durumuna g\u00f6re taban sular\u0131 bazen y\u00fczeye kadar \u00e7\u0131kabilir. Yer alt\u0131 su seviyesinin d\u00fc\u015f\u00fck oldu\u011fu alanlarda ise<br \/>\n kuyu a\u00e7mak suretiyle bu sulardan faydalan\u0131l\u0131r.<br \/>\n T\u00fcrkiye taban sular\u0131 bak\u0131m\u0131ndan zengindir. \u00d6r: Ege B\u00f6lgesinin \u00e7\u00f6k\u00fcnt\u00fc ovalar\u0131, Konya,Kayseri, Erzurum, Erzincan, Elaz\u0131\u011f, Bursa, Adapazar\u0131 gibi.<br \/>\nKAYNAKLAR<br \/>\n Yer alt\u0131 sular\u0131n\u0131n tekrar yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yere kaynak denir.<br \/>\n Sular\u0131n\u0131n S\u0131cakl\u0131\u011f\u0131na G\u00f6re Kaynaklar 2 Grupta \u0130ncelenebilir:<br \/>\nA-SO\u011eUK SU KAYNAKLARI:<br \/>\n Sular\u0131n\u0131 ya\u011f\u0131\u015flarla yery\u00fcz\u00fcnden al\u0131rlar.<br \/>\n Sular\u0131n\u0131n s\u0131cakl\u0131\u011f\u0131 ve ak\u0131mlar\u0131 y\u0131l boyunca de\u011fi\u015fir.<br \/>\n1)Tabaka Kayna\u011f\u0131 (yama\u00e7): Ge\u00e7irimli tabaklar\u0131n u\u00e7 k\u0131sm\u0131ndan sular\u0131n y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yerdir.<br \/>\n2)Vadi Kayna\u011f\u0131: Vadi tabanlar\u0131ndan \u00e7\u0131kan kaynaklard\u0131r.<br \/>\n3)Karstik Kaynak (Vokl\u00fcz): Kalkerli arazilerde yer y\u00fcz\u00fcne \u00e7\u0131kan kaynaklard\u0131r. En fazla Akdeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr. \u00d6r: D\u00fcden suyu <\/p>\n<p> Bu kaynaklar\u0131n en \u00f6nemli \u00f6zelli\u011fi sular\u0131n\u0131n bol miktarda kire\u00e7 i\u00e7ermesidir.<br \/>\n4)Artezyen Kayna\u011f\u0131: Tekne bi\u00e7imindeki iki ge\u00e7irimsiz tabaka aras\u0131ndaki ge\u00e7irimli<br \/>\n tabakaya a\u00e7\u0131lan bir sondaj ile sular\u0131n p\u00fcsk\u00fcrerek yer y\u00fcz\u00fcne \u00e7\u0131kmas\u0131d\u0131r. Di\u011fer<br \/>\n kaynaklardan ayr\u0131lan yan\u0131 be\u015feri fakt\u00f6rlerin etkisiyle yer y\u00fcz\u00fcne \u00e7\u0131kmas\u0131d\u0131r. <\/p>\n<p>B-SICAK SU KAYNAKLARI<br \/>\n Sular\u0131n\u0131 ma\u011fmaya yak\u0131n alanlardan al\u0131rlar.<br \/>\n Sular\u0131 geldi\u011fi derinli\u011fe g\u00f6re s\u0131cak veya \u0131l\u0131kt\u0131r.<br \/>\n Sular\u0131n\u0131n s\u0131cakl\u0131\u011f\u0131 y\u0131l boyunca ayn\u0131d\u0131r.<br \/>\n Ak\u0131m de\u011fi\u015fikli\u011fi olmaz.<br \/>\n Bol miktarda eriyik madde i\u00e7erir.<br \/>\n1)Fay Kayna\u011f\u0131: Fay hatt\u0131 boyunca yery\u00fcz\u00fcne \u00e7\u0131kan kaynaklard\u0131r. Halk aras\u0131nda bu<br \/>\n kaynaklara \u0131l\u0131ca, kapl\u0131ca,\u00e7ermik, i\u00e7me ve maden sular\u0131 denilmektedir.<\/p>\n<p>\u00d6r: Manisa (Kur\u015funlu, Urganl\u0131, Ala\u015fehir, Demirci), Denizli (Pamukkale, Karahay\u0131t,<br \/>\n Sarayk\u00f6y, Buldan), K\u00fctahya (Simav),Bal\u0131kesir (Edremit, G\u00f6nen), Sivas (Bal\u0131kl\u0131 \u00c7ermik)<br \/>\n gibi merkezlerde vard\u0131r. Bu yerlerin ortak \u00f6zelli\u011fi yer yap\u0131lar\u0131n\u0131n \u00f6zelli\u011fidir.<br \/>\n2)Gayzer Kayna\u011f\u0131: Etkin haldeki volkan da\u011flar\u0131ndan de\u011fi\u015fik aral\u0131klarla p\u00fcsk\u00fcrerek \u00e7\u0131kan kaynaklard\u0131r. T\u00fcrkiyede \u00f6rneklerine rastlanmaz. <\/p>\n<p>YER ALTI SULARI VE KAYNAKLAR<br \/>\n *Ya\u011f\u0131\u015flarla yer y\u00fcz\u00fcne inen sular\u0131n ge\u00e7irimli tabakadan yer alt\u0131na s\u0131zarak , yer alt\u0131nda olu\u015fturduklar\u0131 sulara yer alt\u0131 sular\u0131 denir.<br \/>\n Yer Alt\u0131 Sular\u0131n\u0131n Beslenmesinde Etkili Olan Fakt\u00f6rler:<br \/>\n 1) Ya\u011f\u0131\u015f miktar\u0131,<br \/>\n 2) Ya\u011f\u0131\u015f t\u00fcr\u00fc (Kar ya\u011f\u0131\u015flar\u0131 ile beslenme fazla olur.)<br \/>\n 3) Zeminin ge\u00e7irimlili\u011fi ( al\u00fcvyal ve karstik alanlarda ge\u00e7irimlilik fazlad\u0131r).<br \/>\n 4) Arazinin e\u011fimi :e\u011fimin az oldu\u011fu alanlarda beslenme daha fazlad\u0131r.<br \/>\n 5) Bitki \u00f6rt\u00fcs\u00fc: Y\u00fczeysel ak\u0131m\u0131 engelledi\u011fi i\u00e7in.<br \/>\n Taban Suyu:Al\u00fcvyal ovalar\u0131n taban\u0131nda bulunurlar. Altta ge\u00e7irimsiz tabaka ile s\u0131n\u0131rland\u0131r\u0131lm\u0131\u015f ge\u00e7irimli tabaka \u00fczerinde biriken sulard\u0131r. Beslenme durumuna g\u00f6re taban sular\u0131 bazen y\u00fczeye kadar \u00e7\u0131kabilir. Yer alt\u0131 su seviyesinin d\u00fc\u015f\u00fck oldu\u011fu alanlarda ise kuyu a\u00e7mak suretiyle bu sulardan faydalan\u0131l\u0131r.<br \/>\n *T\u00fcrkiye taban sular\u0131 bak\u0131m\u0131ndan zengindir. \u00d6r: Ege B\u00f6lgesinin \u00e7\u00f6k\u00fcnt\u00fc ovalar\u0131, Konya,Kayseri, Erzurum, Erzincan, Elaz\u0131\u011f, Bursa, Adapazar\u0131 gibi.<br \/>\nKAYNAKLAR: Yer alt\u0131 sular\u0131n\u0131n tekrar yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yere kaynak denir.<br \/>\n Sular\u0131n\u0131n S\u0131cakl\u0131\u011f\u0131na G\u00f6re Kaynaklar 2 Grupta \u0130ncelenebilir:<br \/>\nA-SO\u011eUK SU KAYNAKLARI: *Sular\u0131n\u0131 ya\u011f\u0131\u015flarla yery\u00fcz\u00fcnden al\u0131rlar. *Sular\u0131n\u0131n s\u0131cakl\u0131\u011f\u0131 ve ak\u0131mlar\u0131 y\u0131l boyunca de\u011fi\u015fir. <\/p>\n<p>1)Tabaka Kayna\u011f\u0131 (yama\u00e7): Ge\u00e7irimli tabaklar\u0131n u\u00e7 k\u0131sm\u0131ndan sular\u0131n y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yerdir.<br \/>\n2)Vadi Kayna\u011f\u0131: Vadi tabanlar\u0131ndan \u00e7\u0131kan kaynaklard\u0131r.<br \/>\n3)Karstik Kaynak (Vokl\u00fcz): Kalkerli arazilerde yer y\u00fcz\u00fcne \u00e7\u0131kan kaynaklard\u0131r. En fazla Akdeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr. \u00d6r: D\u00fcden suyu<br \/>\n Bu kaynaklar\u0131n en \u00f6nemli \u00f6zelli\u011fi sular\u0131n\u0131n bol miktarda kire\u00e7 i\u00e7ermesidir.<br \/>\n4)Artezyen Kayna\u011f\u0131: Tekne bi\u00e7imindeki iki ge\u00e7irimsiz tabaka aras\u0131ndaki ge\u00e7irimli tabakaya a\u00e7\u0131lan bir sondaj ile sular\u0131n p\u00fcsk\u00fcrerek yer y\u00fcz\u00fcne \u00e7\u0131kmas\u0131d\u0131r. Di\u011fer kaynaklardan ayr\u0131lan yan\u0131 be\u015feri fakt\u00f6rlerin etkisiyle yer y\u00fcz\u00fcne \u00e7\u0131kmas\u0131d\u0131r.<br \/>\nB-SICAK SU KAYNAKLARI<br \/>\n *Sular\u0131n\u0131 ma\u011fmaya yak\u0131n alanlardan al\u0131rlar.<br \/>\n *Sular\u0131 geldi\u011fi derinli\u011fe g\u00f6re s\u0131cak veya \u0131l\u0131kt\u0131r.<br \/>\n *Sular\u0131n\u0131n s\u0131cakl\u0131\u011f\u0131 y\u0131l boyunca ayn\u0131d\u0131r.<br \/>\n *Ak\u0131m de\u011fi\u015fikli\u011fi olmaz.<br \/>\n *Bol miktarda eriyik madde i\u00e7erir.<br \/>\n1)Fay Kayna\u011f\u0131:Fay hatt\u0131 boyunca yery\u00fcz\u00fcne \u00e7\u0131kan kaynaklard\u0131r. Halk aras\u0131nda bu kaynaklara \u0131l\u0131ca, kapl\u0131ca,\u00e7ermik, i\u00e7me ve maden sular\u0131 denilmektedir. \u00d6r: Manisa (Kur\u015funlu, Urganl\u0131, Ala\u015fehir, Demirci), Denizli (Pamukkale, Karahay\u0131t, Sarayk\u00f6y, Buldan), K\u00fctahya (Simav),Bal\u0131kesir (Edremit, G\u00f6nen), Sivas (Bal\u0131kl\u0131 \u00c7ermik) gibi merkezlerde vard\u0131r. Bu yerlerin ortak \u00f6zelli\u011fi yer yap\u0131lar\u0131n\u0131n \u00f6zelli\u011fidir.<br \/>\n2)Gayzer Kayna\u011f\u0131: Etkin haldeki volkan da\u011flar\u0131ndan de\u011fi\u015fik aral\u0131klarla p\u00fcsk\u00fcrerek \u00e7\u0131kan kaynaklard\u0131r. T\u00fcrkiyede \u00f6rneklerine rastlanmaz.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ya\u011f\u0131\u015flar sonucu yery\u00fcz\u00fcne d\u00fc\u015fen sular\u0131n bir k\u0131sm\u0131 y\u00fczeyden akarken bir k\u0131sm\u0131da yeralt\u0131na s\u0131zararak depolan\u0131rlar veya buralarda ak\u0131\u015f g\u00f6sterirler. Bunlara Yeralt\u0131 Sular\u0131 denir. Bu sular\u0131n kendili\u011finden yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yerlere de Kaynak denir. Yeralt\u0131 suyunun miktar\u0131n\u0131; Ya\u011f\u0131\u015f Miktar\u0131 Y\u00fczeyin E\u011fimi Bitki \u00d6rt\u00fcs\u00fc Zeminin \u00d6zelli\u011fi etkiler. Al\u00fcvyal Ovalar, Karstik Araziler, Deniz ve G\u00f6l K\u0131y\u0131lar\u0131 yeralt\u0131 suyu bak\u0131m\u0131ndan zengin &hellip;<\/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":[2926,2878,3977,3272],"class_list":["post-1438","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-bitki-ortusu","tag-fay","tag-gayzer","tag-yeralti-sulari-ve-kaynaklar"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1438","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=1438"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1438\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1438"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1438"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1438"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}