{"id":14554,"date":"2013-08-27T17:21:31","date_gmt":"2013-08-27T14:21:31","guid":{"rendered":"https:\/\/www.enerjigazetesi.ist\/?p=14554"},"modified":"2013-08-27T17:21:31","modified_gmt":"2013-08-27T14:21:31","slug":"jeotermal-enerji-depreme-sebep-olabilir","status":"publish","type":"post","link":"https:\/\/www.enerjigazetesi.ist\/en\/jeotermal-enerji-depreme-sebep-olabilir\/","title":{"rendered":"(Turkish) Jeotermal Enerji Depreme Sebep Olabilir…"},"content":{"rendered":"

Sorry, this entry is only available in Turkish<\/a>. For the sake of viewer convenience, the content is shown below in the alternative language. You may click the link to switch the active language.<\/p>

Topra\u011f\u0131n derinlerindeki birikmi\u015f \u0131s\u0131n\u0131n \u00e7\u0131kar\u0131lmas\u0131na dayanan jeotermal enerji, yaratt\u0131\u011f\u0131 sismik dalgalarla depremleri tetikleme riski bar\u0131nd\u0131r\u0131rken, a\u00e7\u0131\u011fa \u00e7\u0131kan s\u0131v\u0131daki kimyasallar da canl\u0131 ya\u015fam\u0131n\u0131 tehlikeye sokuyor. Bilim insanlar\u0131, jeotermal enerji ama\u00e7l\u0131 yap\u0131lan kaz\u0131lar\u0131n, yer sars\u0131nt\u0131lar\u0131na neden oldu\u011funu tespit etti. \u0130svi\u00e7re\u2019nin kuzeydo\u011fusunda meydana gelen deprem sars\u0131nt\u0131lar\u0131, jeotermal yat\u0131r\u0131m i\u00e7in yap\u0131lan kaz\u0131lar\u0131n durmas\u0131na neden oldu.<\/strong><\/p>\n

\u0130sve\u00e7 Sismoloji Merkezi bu sars\u0131nt\u0131lar\u0131n yerin derinliklerindenki birikmi\u015f \u0131s\u0131 kaynaklar\u0131n\u0131n olu\u015fturdu\u011fu enerjiyi ortaya \u00e7\u0131karmak i\u00e7in kullan\u0131lan Jeotermal Enerjinin yol a\u00e7t\u0131\u011f\u0131n\u0131 tespit ettiler.<\/p>\n

ntvmsnbc\u2019deki habere g\u00f6re, sars\u0131nt\u0131lar ilk olarak Colorado\u2019da Rock Flats alan\u0131nda 3000 m derinli\u011fe at\u0131k suyun enjeksiyonundan sonra b\u00f6lgeye yak\u0131n \u015fehirlerde pek \u00e7ok say\u0131da depremin hissedilmesi ile saptand\u0131. Ayr\u0131ca, Wairakei\u2019de jeotermal sahas\u0131nda y\u00fcksek bas\u0131n\u00e7 alt\u0131nda reenjeksiyon, b\u00f6lgede depremlerin hissedildi\u011finde durdurulmak zorunda kal\u0131nd\u0131\u011f\u0131 belirlendi.<\/p>\n

Ohaaki sahas\u0131nda 1987-1992 y\u0131llar\u0131 aras\u0131nda sismik \u00f6l\u00e7\u00fcmler de ise \u00fcretim s\u0131ras\u0131nda sismik aktivitenin d\u00fc\u015f\u00fck ol\"\"<\/a>du\u011fu saptanm\u0131\u015f.<\/p>\n

Bunun yan\u0131 s\u0131ra jeotermal s\u0131v\u0131da bulunan kimyasallar hava,y\u00fczey sular\u0131 ve yer alt\u0131 sular\u0131na kar\u0131\u015farak insan, hayvan ve tar\u0131msal ya\u015fam\u0131 \u00f6nemli \u00f6l\u00e7\u00fcde etkileme tehlikesinin de oldu\u011fu belirtiliyor.<\/p>\n

Sars\u0131nt\u0131lar\u0131n sebepleri<\/h2>\n

Jeotermal alanlarda \u00e7ekim ve tekrar basma i\u015fleminden dolay\u0131 d\u00fc\u015f\u00fck ve orta \u015fiddete sahip mikro-depremlerin meydana gelme nedenleri \u015fu \u015fekilde s\u0131ralanabilir:<\/p>\n

\u2022 Rezervuardan do\u011fal beslenme miktar\u0131ndan fazla miktarda ak\u0131\u015fkan \u00e7ekiminden kaynakl\u0131 yeralt\u0131ndaki k\u00fctle miktar\u0131n\u0131n azalmas\u0131,<\/p>\n

\u2022 Rezervuara so\u011fuk suyun bas\u0131lmas\u0131 sonucu k\u0131zg\u0131n olan kaya\u00e7lar\u0131n bir anda enerjilerini kaybetmesi,<\/p>\n

\u2022 Bas\u0131lan ak\u0131\u015fkan bas\u0131nc\u0131n\u0131n, normal bas\u0131nc\u0131 artt\u0131rmas\u0131 sonucu, fay ve \u00e7atlaklar\u0131n kar\u015f\u0131l\u0131kl\u0131 y\u00fczeyleri aras\u0131ndaki s\u00fcrt\u00fcnme direncini azaltmas\u0131.<\/p>\n

Herhangi bir jeotermal sahadan b\u00fcy\u00fck \u00e7apta konut ve i\u015fyeri \u0131s\u0131t\u0131lacaksa, \u00f6nce jeotermal kuyular\u0131n a\u00e7\u0131lmas\u0131, a\u00e7\u0131lan t\u00fcm kuyular\u0131n ayn\u0131 anda \u00fcretime tabii tutulmas\u0131 ve en az 1.5 ay test edilmesi gerekir. Testler sonucunda kuyulardan \u00f6l\u00e7\u00fclen debi de\u011ferlerine g\u00f6re sahan\u0131n kapasitesi ve s\u00fcreklili\u011fi hakk\u0131nda bilgi sahibi olmak m\u00fcmk\u00fcnd\u00fcr.<\/p>\n

T\u00fcrkiye\u2019de jeotermal enerji<\/h2>\n

D\u00fcnya jeotermal enerji rezervinin 5 x 10\u00b2\u00ba ton ta\u015fk\u00f6m\u00fcr\u00fcne e\u015fde\u011fer oldu\u011fu tahmin ediliyor. T\u00fcrkiye\u2019de 1962\u2032den bu yana MTA taraf\u0131ndan yap\u0131lan \u00e7al\u0131\u015fmalar sonucunda, T\u00fcrkiye\u2019nin zengin jeotermal enerji kaynaklar\u0131na sahip oldu\u011fu belirlendi. T\u00fcrkiye jeotermal kaynak bak\u0131m\u0131ndan d\u00fcnyada yedinci s\u0131rada yer al\u0131yor. \u00d6zellikle, Bat\u0131 Anadolu (Denizli \u2013 K\u0131z\u0131ldere, \u0130zmir \u2013 Seferihisar, Ayd\u0131n -Germencik, \u00c7anakkale \u2013 Tuzla, Afyon \u2013 Gerek, Manisa, Bal\u0131kesir, K\u00fctahya-Simav) ve Orta Anadolu\u2019da (K\u0131z\u0131lcahamam \u2013 Kozakl\u0131) dolaylar\u0131nda enerji imkan\u0131 oldu\u011fu g\u00f6r\u00fclm\u00fc\u015ft\u00fcr.<\/p>\n

Kaynak: Enerji Enstit\u00fcs\u00fc<\/a><\/p>","protected":false},"excerpt":{"rendered":"

Sorry, this entry is only available in Turkish. For the sake of viewer convenience, the content is shown below in the alternative language. You may click the link to switch the active language.Topra\u011f\u0131n derinlerindeki birikmi\u015f \u0131s\u0131n\u0131n \u00e7\u0131kar\u0131lmas\u0131na dayanan jeotermal enerji, yaratt\u0131\u011f\u0131 sismik dalgalarla depremleri tetikleme riski bar\u0131nd\u0131r\u0131rken, a\u00e7\u0131\u011fa \u00e7\u0131kan s\u0131v\u0131daki kimyasallar da canl\u0131 ya\u015fam\u0131n\u0131 tehlikeye […]<\/p>\n","protected":false},"author":1,"featured_media":14555,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[53,48],"tags":[7957,63,67,1009,165,58,56,7956],"views":1023,"_links":{"self":[{"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/posts\/14554"}],"collection":[{"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/comments?post=14554"}],"version-history":[{"count":1,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/posts\/14554\/revisions"}],"predecessor-version":[{"id":14556,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/posts\/14554\/revisions\/14556"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/media\/14555"}],"wp:attachment":[{"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/media?parent=14554"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/categories?post=14554"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.enerjigazetesi.ist\/en\/wp-json\/wp\/v2\/tags?post=14554"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}