Yer alt\u0131 Suyu (Taban Suyu)<\/p>\n
Ya\u011f\u0131\u015f olarak yery\u00fcz\u00fcne d\u00fc\u015fen ya da yery\u00fcz\u00fcnde bulunan sular\u0131n, yer\u00e7ekimi etkisiyle yerin alt\u0131na s\u0131z\u0131p, orada birikmesiyle olu\u015fan sulard\u0131r. Yer alt\u0131 suyunun olu\u015fabilmesi i\u00e7in beslenme ve depolanma ko\u015fullar\u0131n\u0131n uygun olmas\u0131 gerekir. Yer alt\u0131 suyunun beslenmesini etkileyen en \u00f6nemli etmen ya\u011f\u0131\u015flard\u0131r. Depolama ko\u015fullar\u0131 ise y\u00fczeyin e\u011fimine, bitki \u00f6rt\u00fcs\u00fcne ve y\u00fczeyin ge\u00e7irimlik \u00f6zelli\u011fine ba\u011fl\u0131d\u0131r. <\/p>\n
Yer alt\u0131 Sular\u0131n\u0131n Bulunu\u015f Bi\u00e7imleri<\/p>\n
Bol ya\u011f\u0131\u015fl\u0131 ve zemini ge\u00e7irimli ta\u015flardan olu\u015fan alanlarda yer alt\u0131 suyu fazlad\u0131r. Az ya\u011f\u0131\u015f alan, e\u011fimi fazla ve ge\u00e7irimsiz zeminlerde ise, yer alt\u0131 suyunun olu\u015fumu zordur. Kum, \u00e7ak\u0131l, kumta\u015f\u0131 konglomera, kalker, volkanik t\u00fcfler, al\u00fcvyonlar, ge\u00e7irimli zeminleri olu\u015fturur. Bu nedenle al\u00fcvyal ovalar ve karstik y\u00f6reler yer alt\u0131 suyu bak\u0131m\u0131ndan zengin alanlard\u0131r. Kil, marn, \u015fist, granit gibi ta\u015flar ise ge\u00e7irimsizdir. Yer alt\u0131 suyu olu\u015fumunu engeller. Yeralt\u0131nda biriken sular <\/p>\n
Taban suyu<\/p>\n
Artezyen<\/p>\n
Karstik Yeralt\u0131 Suyu<\/p>\n
olarak bulunur.<\/p>\n
Taban Suyu<\/p>\n
Altta ge\u00e7irimsiz bir tabaka ile s\u0131n\u0131rland\u0131r\u0131lan, ge\u00e7irimli tabaka i\u00e7indeki sulard\u0131r. Bu sular genellikle y\u00fczeye yak\u0131nd\u0131r. Marmara B\u00f6lgesi\u2019ndeki ovalar, Ege B\u00f6lgesi\u2019ndeki \u00e7\u00f6k\u00fcnt\u00fc ovalar\u0131, Mu\u015f, Erzurum ve Pasinler ovalar\u0131ndaki yer alt\u0131 sular\u0131 bu gruba girer.<\/p>\n
Artezyen <\/p>\n
Bu t\u00fcr sular bas\u0131n\u00e7l\u0131 yeralt\u0131 sular\u0131d\u0131r. \u0130ki ge\u00e7irimsiz tabaka aras\u0131ndaki ge\u00e7irimli tabaka i\u00e7inde bulunan sulard\u0131r. Tekne bi\u00e7imli ovalar ve vadi tabanlar\u0131nda bu t\u00fcr sular bulunmaktad\u0131r.<\/p>\n
\u0130\u00e7 Anadolu B\u00f6lgesi artezyen sular\u0131 bak\u0131m\u0131ndan zengindir.<\/p>\n
Karstik Yer alt\u0131 Suyu<\/p>\n
Karstik y\u00f6relerdeki kal\u0131n kalker tabakalar aras\u0131ndaki \u00e7atlak ve bo\u015fluklarda biriken yer alt\u0131 sular\u0131d\u0131r. En \u00f6nemli \u00f6zelli\u011fi birbirinden ba\u011f\u0131ms\u0131z taban sular\u0131 olu\u015fturmas\u0131d\u0131r. Karstik alanlar\u0131n geni\u015f yer kaplad\u0131\u011f\u0131 Akdeniz B\u00f6lgesi karstik yeralt\u0131 sular\u0131 bak\u0131m\u0131ndan zengindir.<\/p>\n
Kaynak <\/p>\n
Yeralt\u0131 sular\u0131n\u0131n kendili\u011finden yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131 yere kaynak denir. T\u00fcrkiye\u2019de kaynaklara p\u0131nar, e\u015fme, bulak ve g\u00f6ze gibi adlar da verilir.<\/p>\n
Kaynaklar, yer alt\u0131 suyunun bulunu\u015f bi\u00e7imine, y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yere ve sular\u0131n s\u0131cakl\u0131\u011f\u0131na g\u00f6re grupland\u0131r\u0131labilir. Sular\u0131n\u0131n s\u0131cakl\u0131\u011f\u0131na g\u00f6re kaynaklar, so\u011fuk ve s\u0131cak su kaynaklar\u0131 olarak iki gruba ayr\u0131l\u0131r :<\/p>\n
So\u011fuk Su Kaynaklar\u0131 <\/p>\n
Ya\u011f\u0131\u015f sular\u0131n\u0131n yeralt\u0131nda birikerek y\u00fczeye \u00e7\u0131kmas\u0131 sonucunda olu\u015furlar. Genellikle y\u00fczeye yak\u0131n olduklar\u0131 i\u00e7in d\u0131\u015f ko\u015fullardan daha \u00e7ok etkilenirler. Bu nedenle sular\u0131 so\u011fuktur. So\u011fuk su kaynaklar\u0131 yeralt\u0131nda bulunu\u015f bi\u00e7imine ve y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yere g\u00f6re \u00fc\u00e7 gruba ayr\u0131l\u0131r :<\/p>\n
Tabaka Kayna\u011f\u0131 : Ge\u00e7irimli tabakalar\u0131n topo\u011frafya y\u00fczeyi ile kesi\u015ftikleri yerden sular\u0131n y\u00fczeye \u00e7\u0131kmas\u0131yla olu\u015fan kaynaklara tabaka kayna\u011f\u0131 denir.<\/p>\n
Vadi Kayna\u011f\u0131 : Yeralt\u0131na s\u0131zan sular\u0131n bulundu\u011fu tabakan\u0131n bir vadi taraf\u0131ndan kesilmesi ile olu\u015fan kaynakt\u0131r. Genellikle vadi yama\u00e7lar\u0131nda g\u00f6r\u00fcl\u00fcr. <\/p>\n
Karstik Kaynak (Vokl\u00fcz) : Kal\u0131n kalker tabakalar\u0131 aras\u0131ndaki bo\u015fluklar\u0131 doldurmu\u015f olan yer alt\u0131 sular\u0131n\u0131n y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 kaynakt\u0131r. Bol miktarda kire\u00e7 i\u00e7eren bu kaynaklar\u0131n sular\u0131 genellikle s\u00fcrekli de\u011fildir. Ya\u011f\u0131\u015flarla beslendikleri i\u00e7in karstik kaynaklar\u0131n sular\u0131 so\u011fuktur. Toroslar \u00fczerindeki \u015eekerp\u0131nar\u0131 en tan\u0131nm\u0131\u015f karstik kaynak \u00f6rneklerinden biridir.<\/p>\n
S\u0131cak Su Kaynaklar\u0131 <\/p>\n
Yerkabu\u011fundaki fay hatlar\u0131 \u00fczerinde bulunan kaynaklard\u0131r. Fay kaynaklar\u0131 da denir. Sular\u0131 yerin derinliklerinden geldi\u011fi i\u00e7in s\u0131cakt\u0131r ve d\u0131\u015f ko\u015fullardan etkilenmez. Sular ge\u00e7tikleri ta\u015f ve tabakalardaki \u00e7e\u015fitli mineralleri eriterek b\u00fcnyelerine ald\u0131klar\u0131 i\u00e7in mineral bak\u0131m\u0131ndan zengindir. Bu t\u00fcr kaynaklara; kapl\u0131ca, \u0131l\u0131ca, i\u00e7me gibi adlar verilir. S\u0131cak su kaynaklar\u0131n\u0131n \u00f6zel bir t\u00fcr\u00fcne gayzer denir.<\/p>\n
Gayzer : Volkanik y\u00f6relerde yeralt\u0131ndaki s\u0131cak suyun belirli aral\u0131klarla f\u0131\u015fk\u0131rmas\u0131 ile olu\u015fan kaynaklard\u0131r.<\/p>\n
UYARI : Yerin derinliklerinde bulunan sular\u0131n s\u0131cakl\u0131\u011f\u0131 y\u0131l i\u00e7inde fazla bir de\u011fi\u015fme g\u00f6stermez. Fay kaynaklar\u0131 volkanik ve k\u0131r\u0131kl\u0131 b\u00f6lgelerde g\u00f6r\u00fcl\u00fcr.<\/p>\n
T\u00fcrkiye\u2019de S\u0131cak Su Kaynaklar\u0131n\u0131n Da\u011f\u0131l\u0131\u015f\u0131<\/p>\n
T\u00fcrkiye kapl\u0131ca ve \u0131l\u0131ca bak\u0131m\u0131ndan zengin bir \u00fclkedir. Bursa, \u0130neg\u00f6l, Yalova, Bolu, Haymana, K\u0131z\u0131lcahamam, Sar\u0131kaya, Erzurum, Sivas Bal\u0131kl\u0131 \u00c7ermik, Afyon, K\u00fctahya, Denizli \u00e7evresindeki kapl\u0131ca ve \u0131l\u0131calar en \u00fcnl\u00fcleridir.<\/p>\n","protected":false},"excerpt":{"rendered":"
Yer alt\u0131 Suyu (Taban Suyu) Ya\u011f\u0131\u015f olarak yery\u00fcz\u00fcne d\u00fc\u015fen ya da yery\u00fcz\u00fcnde bulunan sular\u0131n, yer\u00e7ekimi etkisiyle yerin alt\u0131na s\u0131z\u0131p, orada birikmesiyle olu\u015fan sulard\u0131r. Yer alt\u0131 suyunun olu\u015fabilmesi i\u00e7in beslenme ve depolanma ko\u015fullar\u0131n\u0131n uygun olmas\u0131 gerekir. Yer alt\u0131 suyunun beslenmesini etkileyen en \u00f6nemli etmen ya\u011f\u0131\u015flard\u0131r. Depolama ko\u015fullar\u0131 ise y\u00fczeyin e\u011fimine, bitki \u00f6rt\u00fcs\u00fcne ve y\u00fczeyin ge\u00e7irimlik \u00f6zelli\u011fine …<\/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":[10930,3977,10932,10931,10929,10442,3221,3272],"class_list":["post-5246","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-artezyen","tag-gayzer","tag-sicak-su-kaynaklari","tag-soguk-su-kaynaklari","tag-taban-suyu","tag-turkiyede-sicak-su-kaynaklarinin-dagilisi","tag-vokluz","tag-yeralti-sulari-ve-kaynaklar"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5246","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=5246"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5246\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5246"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5246"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5246"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}