{"id":7352,"date":"2021-11-28T00:00:00","date_gmt":"2021-11-27T23:00:00","guid":{"rendered":"https:\/\/instrid.sk\/uncategorized\/davemaoit-mineral-nemal-existovat-na-zemskom-povrchu\/"},"modified":"2021-11-28T00:00:00","modified_gmt":"2021-11-27T23:00:00","slug":"davemaoit-mineral-nemal-existovat-na-zemskom-povrchu","status":"publish","type":"post","link":"https:\/\/instrid.sk\/en\/archiv\/davemaoit-mineral-nemal-existovat-na-zemskom-povrchu\/","title":{"rendered":"Davemaoit \u2013 jeho n\u00e1lez prekvapil vedcov, nemal existova\u0165 na zemskom povrchu"},"content":{"rendered":"<h3>Vz\u00e1cny n\u00e1lez ukryt\u00fd v diamante<\/h3>\n<p>Geochemik <strong>Oliver Tschauner<\/strong> p\u00f4sobiaci na Nevadskej univerzite (<strong>UNLV<\/strong>) spolu so svoj\u00edm t\u00edmom zverejnil nezvy\u010dajn\u00fa \u0161t\u00fadiu. V\u010faka v\u00fdskumu sa im podarilo objavi\u0165 nov\u00fd<strong> miner\u00e1l, ktor\u00fd by sa v\u0161ak pod\u013ea doteraj\u0161\u00edch inform\u00e1cii na Zemi vyskytova\u0165 nemal.<\/strong><\/p>\n<p>Miner\u00e1l, ktor\u00fd sa <strong>ukr\u00fdval v\u00a0diamante,<\/strong> uzrel svetlo sveta pred desiatkami rokov v Botswane cez ba\u0148u<strong> Orapa &#8211; najv\u00e4\u010d\u0161iu povrchov\u00fa ba\u0148u na svete.<\/strong> \u0164a\u017e\u00ed sa zo sope\u010dn\u00e9ho \u201epotrubia\u201c, ktor\u00e9 vybuchlo pred viac ako 200 mili\u00f3nmi rokov. <strong>Diamanty sa priemerne nach\u00e1dzaj\u00fa 150 a\u017e 200 km v hlbin\u00e1ch Zeme.<\/strong> Priemern\u00e1 teplota tam dosahuje 900 a\u017e 1 300 stup\u0148ov Celzia a tlak 45 a\u017e 60 kilobarov (\u010do je asi 50 000-n\u00e1sobok atmosf\u00e9rick\u00e9ho tlaku na zemskom povrchu).<\/p>\n Kimberley v\u010faka diamantovej bani patr\u00ed medzi najunik\u00e1tnej\u0161ie a najautentickej\u0161ie historick\u00e9 destin\u00e1cie v Ju\u017enej Afrike. &#8222;The Big Hole&#8220; sa pova\u017euje za jedno z najhlb\u0161\u00edch miest. do ktor\u00e9ho zasiahla \u013eudsk\u00e1 ruka (200 m2). zdroj: pixabay.com\n<p>Za t\u00fdchto podmienok sa <strong>roztaven\u00fd lamproit a kimberlit<\/strong>\u00a0 tvoria aj vo vrchnom pl\u00e1\u0161ti Zeme a r\u00fdchlo sa roz\u0161iruj\u00fa. Expanzia sp\u00f4sobuje erupciu magmy, ktor\u00e1 ju vytla\u010d\u00ed na zemsk\u00fd povrch a vezme so sebou horniny s diamantmi. Magma, ktor\u00e1 sa pohybuje neuverite\u013enou r\u00fdchlos\u0165ou, prech\u00e1dza dr\u00e1hou s najmen\u0161\u00edm odporom a vytv\u00e1ra \u201er\u00faru\u201c k povrchu. Ako sa ochladzuje, <strong>magma tuhne na kimberlit.<\/strong> Postupne sa usadzuje vo vertik\u00e1lnych \u0161trukt\u00farach zn\u00e1mych ako kimberlitov\u00e9 r\u00fary. Tie s\u00fa najv\u00fdznamnej\u0161\u00edm zdrojom diamantov, no odhaduje sa, \u017ee<strong> iba 1 z 200 r\u00far obsahuje diamanty, ktor\u00e9 disponuj\u00fa drahokamovou kvalitou.<\/strong> N\u00e1zov \u201eKimberlit\u201c bol odvoden\u00fd od juhoafrick\u00e9ho mesta Kimberley, kde sa v\u00a0druhej polovici\u00a019. storo\u010dia na\u0161li prv\u00e9 diamanty.<\/p>\n<h3>\u00a0Davemaoit a jeho anal\u00fdza<\/h3>\n<p>Predajca drahokamov predal diamant v roku 1987 mineral\u00f3govi z Kalifornsk\u00e9ho technologick\u00e9ho in\u0161tit\u00fatu v Pasadene. Ned\u00e1vno k nemu z\u00edskal pr\u00edstup Tschauner a jeho kolegovia. \u010cakal ich neuverite\u013en\u00fd objav, ktor\u00fd nazvali <strong>davemaoit<\/strong>. <strong>Miner\u00e1l bol pomenovan\u00fd po<\/strong> \u010d\u00ednsko-americkom geol\u00f3govi<strong> Ho-Kwangovi<\/strong> (americk\u00e9 meno &#8211; Dave) <strong>Maovi<\/strong> za jeho \u0161t\u00fadie o typoch vysokotlakov\u00fdch prvkov, ktor\u00e9 sa nach\u00e1dzaj\u00fa iba medzi zemskou k\u00f4rou a jej jadrom.<\/p>\n<p>Nezvykl\u00fd n\u00e1lez vznikol stovky kilometrov pod zemsk\u00fdm povrchom. <strong>Davemaoit cestoval z h\u013abky najmenej 660 kilometrov v spodnom pl\u00e1\u0161ti Zeme,<\/strong> dok\u00fdm ho nevy\u0165a\u017eili. Miner\u00e1ly spodn\u00e9ho pl\u00e1\u0161\u0165a sa v\u00e4\u010d\u0161inou rozpadn\u00fa sk\u00f4r, ne\u017e dosiahnu povrch Zeme. V\u00a0tomto pr\u00edpade v\u0161ak bol <strong>miner\u00e1l zachyten\u00fd v\u00a0zelenkavom diamante,<\/strong> v\u010faka ktor\u00e9mu sa<strong> bezpe\u010dne dostal na zemsk\u00fa plochu.<\/strong><\/p>\n V\u00fdskumn\u00edci \u0161tudovali zelenkast\u00fd diamant vykopan\u00fd z najv\u00e4\u010d\u0161ej povrchovej diamantovej bane na svete. zdroj: pinterest.com\n<p>V\u00fdsledky anal\u00fdzy tvrdia, \u017ee mohol vznikn\u00fa\u0165 v d\u00f4sledku vysok\u00e9ho tepl\u00f4t a tlaku v spodnom pl\u00e1\u0161ti Zeme. Ke\u010f sa na tomto miner\u00e1li vykonal v\u00fdskum a chemick\u00e1 anal\u00fdza, preuk\u00e1zala sa pr\u00edtomnos\u0165 r\u00e1dioakt\u00edvnych izotopov r\u00f4znych prvkov, ako je drasl\u00edk, ur\u00e1n a t\u00f3rium, ktor\u00e9 sa nenach\u00e1dzaj\u00fa v hornom pl\u00e1\u0161ti. <strong>&#8222;Davemaoit m\u00f4\u017ee by\u0165 hostite\u013eom troch hlavn\u00fdch prvkov produkuj\u00facich teplo (ur\u00e1n a t\u00f3rium boli predt\u00fdm experiment\u00e1lne preuk\u00e1zan\u00e9), ktor\u00e9 ovplyv\u0148uj\u00fa tvorbu tepla v dolnom pl\u00e1\u0161ti Zeme,&#8220;<\/strong> uv\u00e1dza sa v \u0161t\u00fadi\u00ed.<\/p>\n<p>Davemaoit je len druh\u00fdm vysokotlakov\u00fdm kremi\u010ditanom, ktor\u00fd bol kedy na Zemi viden\u00fd. Druh\u00fd zn\u00e1my pr\u00edpad je <strong>meteorit, ktor\u00fd tak\u00fdto kremi\u010ditan ukr\u00fdval.<\/strong> Exempl\u00e1r davemaoitu je prv\u00fdm miner\u00e1lom svojho druhu z kremi\u010ditanu v\u00e1penat\u00e9ho (CaSiO3), ktor\u00fd vznikol pod vysok\u00fdm tlakom na Zemi.<\/p>\n<h3>B\u00e1danie pokra\u010duje<\/h3>\n<p>Pre vedcov bolo objavenie miner\u00e1lu nepochybne prekvapen\u00edm. Keby sa k\u00a0nemu dostali sk\u00f4r, mali by v\u00a0s\u00fa\u010dasnosti lep\u0161iu predstavu o\u00a0tom, \u010do skr\u00fdva zemsk\u00e9 jadro. V\u00fdskum tie\u017e predpoved\u00e1, \u017ee <strong>v\u00a0Zemi m\u00f4\u017ee by\u0165 ukryt\u00fdch viac ako 1000 r\u00f4znych miner\u00e1lov,<\/strong> ktor\u00e9 e\u0161te neboli n\u00e1jden\u00e9. <strong>Odhalenie davemaoitu od\u0161tartovalo nov\u00fa \u00e9ru v\u00fdskumu.<\/strong> Po jeho n\u00e1jden\u00ed vedci vedia, \u017ee h\u013eadanie miner\u00e1lov v spodnom pl\u00e1\u0161ti zemsk\u00e9ho vn\u00fatra m\u00f4\u017ee znamena\u0165 \u010fal\u0161ie vedeck\u00e9 \u00faspechy.<\/p>\n<p>Doteraz existovala predstava o mimozemsk\u00fdch svetoch a prvkoch, ktor\u00e9 sa na Zemi nenach\u00e1dzaj\u00fa. Nikto v\u0161ak nevie s \u00faplnou presnos\u0165ou odhadn\u00fa\u0165 ko\u013eko \u017eiv\u00fdch druhov alebo ne\u017eiv\u00fdch elementov na na\u0161ej plan\u00e9te skuto\u010dne existuje. V <strong>oce\u00e1noch s\u00fa tis\u00edcky a\u017e mili\u00f3ny nepoznan\u00fdch organizmov.<\/strong> V roku<strong> 2017 bolo v Amazonskom pralese objaven\u00fdch dohromady 381 nov\u00fdch druhov<\/strong> rastl\u00edn a\u00a0\u017eivo\u010d\u00edchov. Preto nie je mo\u017en\u00e9 vyl\u00fa\u010di\u0165, \u017ee v\u00a0nasleduj\u00facich rokoch sa bude po\u010det objavov zvy\u0161ova\u0165.<\/p>\n<p><strong>Zdroje: www.indiatoday.in, www.thebighole.co.za \u00a0\u00a0, www.scitechdaily.com<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p>Vz\u00e1cny n\u00e1lez ukryt\u00fd v diamante Geochemik Oliver Tschauner p\u00f4sobiaci na Nevadskej univerzite (UNLV) spolu so svoj\u00edm t\u00edmom zverejnil nezvy\u010dajn\u00fa \u0161t\u00fadiu. V\u010faka v\u00fdskumu sa im podarilo<\/p>","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[51],"tags":[],"class_list":["post-7352","post","type-post","status-publish","format-standard","hentry","category-archiv","two-columns"],"_links":{"self":[{"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/posts\/7352","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/comments?post=7352"}],"version-history":[{"count":0,"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/posts\/7352\/revisions"}],"wp:attachment":[{"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/media?parent=7352"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/categories?post=7352"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/instrid.sk\/en\/wp-json\/wp\/v2\/tags?post=7352"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}