D\u00fcnya’n\u0131n y\u00fczeyinin derinliklerinde, manto i\u00e7inde, y\u00fczeydeki t\u00fcm okyanuslardan daha b\u00fcy\u00fck, engin bir su haznesi bulunmaktad\u0131r. Bu su s\u0131v\u0131 halde de\u011fildir, fakat \u00e7evreleyen kayaya kimyasal olarak ba\u011fl\u0131d\u0131r. Bununla birlikte, bilim insanlar\u0131 taraf\u0131ndan geli\u015ftirilen yeni bir model, bu suyun \u00f6nemli bir k\u0131sm\u0131n\u0131n ge\u00e7i\u015f halinde oldu\u011funu ve “manto ya\u011fmuru” ad\u0131 verilen bir s\u00fcre\u00e7le mantoyla y\u00fczey aras\u0131nda hareket etti\u011fini \u00f6ne s\u00fcrmektedir.<\/p>\n\n
Derin su d\u00f6ng\u00fcs\u00fc, D\u00fcnya’n\u0131n y\u00fczeyi ve i\u00e7 k\u0131sm\u0131 aras\u0131ndaki su de\u011fi\u015fimini ifade eder. Bu d\u00f6ng\u00fc, D\u00fcnya’n\u0131n y\u00fczey suyunun dengesinin ve ya\u015fanabilirli\u011finin korunmas\u0131nda \u00e7ok \u00f6nemli bir rol oynar. Su, D\u00fcnya’n\u0131n kabu\u011funun mantoya batt\u0131\u011f\u0131 tektonik plakalar taraf\u0131ndan mantoyla ta\u015f\u0131n\u0131r. Bu su daha sonra volkanik patlamalar, hidrotermal bacalar ve okyanus yay\u0131lma merkezlerinde yeni kabu\u011fun olu\u015fmas\u0131 gibi \u00e7e\u015fitli s\u00fcre\u00e7lerle y\u00fczeye geri getirilebilir.<\/p>\n\n
Manto ya\u011fmuru olay\u0131n\u0131n derin su d\u00f6ng\u00fcs\u00fcn\u00fcn \u00f6nemli bir bile\u015feni oldu\u011funa inan\u0131lmaktad\u0131r. Mantodaki kat\u0131 kaya suyla doygun hale geldi\u011finde, su a\u00e7\u0131s\u0131ndan zengin erimi\u015f bir bulamaca d\u00f6n\u00fc\u015febilir. Bu bulama\u00e7 daha sonra kabu\u011fa do\u011fru geri s\u0131z\u0131p \u00fcst mantoya su salar. Su, \u00fcst mantodaki minerallerle ba\u011flanarak erime noktalar\u0131n\u0131 d\u00fc\u015f\u00fcr\u00fcr ve daha fazla erimeye neden olur, bu da daha fazla su sal\u0131n\u0131m\u0131na yol a\u00e7ar. Bu d\u00f6ng\u00fc devam ederek suyu mantoyla y\u00fczey aras\u0131nda ta\u015f\u0131r.<\/p>\n\n
Manto ya\u011fmuru olay\u0131, D\u00fcnya’n\u0131n ya\u015fanabilirli\u011fi i\u00e7in \u00f6nemli etkilere sahiptir. Manto ya\u011fmuru, y\u00fczey suyunu yenileyerek, di\u011fer su kaynaklar\u0131 t\u00fckense bile D\u00fcnya’n\u0131n y\u00fczeyinde her zaman su bulunmas\u0131n\u0131 sa\u011flar. Bu, D\u00fcnya’daki ya\u015fam\u0131n s\u00fcrd\u00fcr\u00fclmesi i\u00e7in \u00e7ok \u00f6nemlidir.<\/p>\n\n
Manto ya\u011fmuru s\u00fcreci, bir kaya ve kaya ba\u011flant\u0131l\u0131 su levhas\u0131 mantoya daha derine batt\u0131\u011f\u0131nda ba\u015flar. Levha batt\u0131k\u00e7a, artan s\u0131cakl\u0131k ve bas\u0131n\u00e7 kayalar\u0131n erimesine ve suyun sal\u0131nmas\u0131na neden olur. Eriyik, \u00e7evreleyen kayadan daha hafif olan ve y\u00fckselmeye ba\u015flayan bulama\u00e7 bir s\u0131v\u0131 olu\u015fturur. Y\u00fckselirken, su \u00fcst mantodaki minerallerle ba\u011flanarak erime noktalar\u0131n\u0131 d\u00fc\u015f\u00fcr\u00fcr ve daha fazla erimeye neden olur. Bu d\u00f6ng\u00fc devam ederek suyu mantoyla y\u00fczey aras\u0131nda ta\u015f\u0131r.<\/p>\n\n
Manto ya\u011fmuru modeli, D\u00fcnya’n\u0131n ge\u00e7mi\u015fi ve gelece\u011fi hakk\u0131nda yeni bilgiler sa\u011flar. Derin su d\u00f6ng\u00fcs\u00fcn\u00fcn daha \u00f6nce anla\u015f\u0131landan daha karma\u015f\u0131k oldu\u011funu ve manto ya\u011fmurunun D\u00fcnya’n\u0131n y\u00fczey suyunu ve ya\u015fanabilirli\u011fini korumada hayati bir rol oynad\u0131\u011f\u0131n\u0131 \u00f6ne s\u00fcrmektedir. Manto ya\u011fmuru olay\u0131n\u0131 anlamak, bilim insanlar\u0131n\u0131n D\u00fcnya’n\u0131n su kaynaklar\u0131n\u0131n gelecekte nas\u0131l de\u011fi\u015fece\u011fini daha iyi tahmin etmelerine yard\u0131mc\u0131 olabilir; bu da su k\u0131tl\u0131\u011f\u0131n\u0131n y\u00f6netilmesi ve D\u00fcnya’daki ya\u015fam\u0131n s\u00fcrd\u00fcr\u00fclebilirli\u011finin sa\u011flanmas\u0131 i\u00e7in \u00e7ok \u00f6nemlidir.<\/p>","protected":false},"excerpt":{"rendered":"
D\u00fcnya’n\u0131n Mantosu: Gizli Su Haznesi Manto Ya\u011fmuru Olay\u0131 D\u00fcnya’n\u0131n y\u00fczeyinin derinliklerinde, manto i\u00e7inde, y\u00fczeydeki t\u00fcm okyanuslardan daha b\u00fcy\u00fck, engin bir su haznesi bulunmaktad\u0131r. Bu su s\u0131v\u0131 halde de\u011fildir, fakat \u00e7evreleyen…<\/p>\n","protected":false},"author":6,"featured_media":0,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[212],"tags":[669,207,210,5044,1974,23560,2309,572],"class_list":["post-17987","post","type-post","status-publish","format-standard","hentry","category-earth-science","tag-hydrothermal-vents","tag-geology","tag-plate-tectonics","tag-water-cycle","tag-volcanology","tag-mantle-rain","tag-habitability","tag-earth-science"],"_links":{"self":[{"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/posts\/17987","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/comments?post=17987"}],"version-history":[{"count":1,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/posts\/17987\/revisions"}],"predecessor-version":[{"id":17988,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/posts\/17987\/revisions\/17988"}],"wp:attachment":[{"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/media?parent=17987"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/categories?post=17987"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.lifescienceart.com\/tr\/wp-json\/wp\/v2\/tags?post=17987"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}