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Space: <a href="http://dbpedia.org">dbpedia.org</a> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> Uraninite, formerly pitchblende, is a radioactive, uranium-rich mineral and ore with a chemical composition that is largely UO2 but because of oxidation typically contains variable proportions of U3O8. Radioactive decay of the uranium causes the mineral to contain oxides of lead and trace amounts of helium. It may also contain thorium and rare-earth elements. </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Pitchblende_schlema-alberoda.jpg?width=300" alt="thumbnail" class="img-fluid" /> </a> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="row"> <div class="table-responsive"> <table class="table table-hover table-sm table-light"> <thead> <tr> <th class="col-xs-3 ">Property</th> <th class="col-xs-9 px-3">Value</th> </tr> </thead> <tbody> <tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/abstract">dbo:abstract</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">اليورانينيت (Uraninite) أو البتشبلند (بالإنجليزية: pitchblende)‏ هو خام معدني نشط إشعاعياً يتكون بشكل أساسي من ثاني أكسيد اليورانيوم (UO2) مع نسب من ثالث أكسيد اليورانيوم (UO3) وأكاسيد الرصاص والثوريوم وعناصر أرضية نادرة كالروديوم. عرف خام اليورانينيت منذ القرن الخامس عشر الميلادي على أقل تقدير في مناجم الفضة في مرتفعات إرتسيبيرغه (بالألمانية Erzgebirge) بألمانيا، إلا أنه يتركز بشكل أكبر في ياتشيموف بجمهورية التشيك، وهو الموقع الذي وصف فيه بروكمان الخام سنة 1727. وقد استخلص كلابروث عنصر اليورانيوم من خام البتشبلند المستخرج من مدينة يوهانجورجنشتات (بالألمانية Johanngeorgenstadt) الألمانية سنة 1789. (ar)</li> <li style="display:none;">La uraninita és un mineral de la classe dels òxids. És un mineral conegut des del segle xv a les mines d'argent de les Muntanyes Metal·líferes, Alemanya, tot i que la localitat tipus des del punt de vista de la geologia és Jáchymov a la República Txeca. Franz Ernst Brückmann descrigué el mineral el 1727 a partir d'uns exemplars d'aquesta localitat txeca. Va ser anomenada així l'any 1845 per Wilhelm Karl von Haidinger per la seva composició. (ca)</li> <li style="display:none;">Uraninit (starší český název smolinec), chemický vzorec UO2 (oxid uraničitý), je krychlový minerál nazvaný podle prvku uranu. (cs)</li> <li style="display:none;">Ο ουρανινίτης (αγγλ. uraninite) ή και πισσουρανίτης (παραλλαγή με την οποία συχνά συγχέεται ή και ταυτίζεται) είναι ορυκτό οξείδιο του ουρανίου, από το οποίο λαμβάνει και το όνομά του. Σχηματίζει ισόμορφη σειρά με τον θοριανίτη (ThO2). Είναι ισχυρά ραδιενεργό ορυκτό, λόγω της ύπαρξης ουρανίου αλλά και ραδίου, του οποίου αποτελεί επίσης μετάλλευμα. Αξίζει να αναφερθεί ότι το στοιχείο ήλιο εντοπίστηκε για πρώτη φορά στη Γη σε δείγμα ουρανινίτη, καθώς αποτελεί προϊόν διάσπασης των περιεχόμενων ραδιενεργών στοιχείων. Ο ουρανινίτης εξαλλοιώνεται προς ωτουνίτη και τορμπερνίτη (Cu(UO2)2(PO4)2 . 8-12H2O) αλλά και ουρανιοπυριτικά ορυκτά, όπως ο (Mg(UO2)2Si2O7 . 6H2O) και ο (Cu(UO2)2Si2O7 . 6H2O). Η κρυσταλλική του δομή είναι ανάλογη προς του φθορίτη, με ισχυρή κυβική συμμετρία, αν και στον ουρανινίτη οι σχηματισμένοι κρύσταλλοι είναι σπάνιοι και δεν παρατηρείται σχισμός. Παραλλαγή του ουρανινίτη είναι ο πισσουρανίτης (pitchblende, εμπειρικού τύπου U3O8), μίγμα κυρίως ουρανινίτη και άλλων ουρανιούχων ορυκτών. Ο πισσουρανίτης είναι, εν γένει, μαλακότερος και χαμηλότερης πυκνότητας και έχει υφή γαιώδη. Πισσουρανίτης ανευρίσκεται, σε μικρές ποσότητες, στην Βόρεια Ελλάδα. Ένα μίγμα ορυκτών με το όνομα "Γκαμίτης" (Gummite) δεν είναι, όπως συχνά θεωρείται, παραλλαγή του ουρανινίτη, αλλά μίγμα του με πολλά ορυκτά των σπανίων γαιών. Ο ουρανινίτης ανευρίσκεται σε γρανιτικούς και πηγματίτες, σε υδροθερμικές φλέβες υψηλών θερμοκρασιών με κασσίτερο και μέσων θερμοκρασιών με σουλφίδια κοβαλτίου, νικελίου, αργύρου, βισμουθίου και αρσενικού. Επίσης, ως παρενεσπαρμένο ορυκτό, σε ψαμμιτικές - κροκαλοπαγείς αποθέσεις. Σχετίζεται με ζιρκόνιο, μοναζίτη, σιδηροπυρίτη, χαλκοπυρίτη, γαληνίτη, αυτοφυή άργυρο, νικελίνη και βαρύτη. Είναι σχετικά ευρέως διαδεδομένο ορυκτό. Εκμεταλλεύσιμα κοιτάσματά του βρίσκονται στην Τσεχία, τη Γερμανία, τη Βρετανία (Κορνουάλλη), την Ισπανία (περιοχή Sierra Albarrana, Κόρδοβα, μεγάλοι κρύσταλλοι). Επίσης στον Καναδά, τις ΗΠΑ, την Τανζανία και το Ζαΐρ. Υπενθυμίζεται ότι είναι ισχυρά ραδιενεργό ορυκτό (360 mRem/gr ετησίως) και πρέπει να αποφεύγεται η έκθεση σε αυτό για μεγάλα χρονικά διαστήματα. (el)</li> <li style="display:none;">Uraninito, antaŭe peĉblendo, estas radioaktiva, riĉa en uranio mineralo kaj erco kun kemia kompono kiu estas ĉefe UO2, sed pro oksidigo la mineralo tipe enhavas variajn proporciojn de U3O8. Aldone, pro efiko de radioaktiveco, la erco enhavas oksidojn el plumbo kaj eretojn el heliumo. Ĝi povas enhavi ankaŭ torion kaj rarajn terelementojn. (eo)</li> <li style="display:none;">Uraninit, unter anderem auch bekannt als Pechblende, ist ein häufig vorkommendes Mineral aus der Mineralklasse der „Oxide und Hydroxide“. Es kristallisiert im kubischen Kristallsystem mit der Zusammensetzung UO2, ist also chemisch gesehen ein Uran(IV)-oxid. Durch die radioaktive Zerfallsreihe von Uran enthält Uraninit stets einen gewissen Anteil Bleioxid (PbO), der in Abhängigkeit vom geologischen Alter bis zu 20 % betragen kann. Uraninit entwickelt meist würfelförmige oder oktaedrische Kristalle bzw. deren Kombinationen, aber auch nierige, körnige oder massige Aggregate in grauer, schwarzer und bräunlicher Farbe bei braunschwarzer bis grünlicher Strichfarbe. Im Allgemeinen ist Uraninit undurchsichtig, nur feine Splitter und dünnste Schichten sind rotbraun durchscheinend. Frische Proben weisen einen pech- bis fettartigen, gelegentlich auch schwach metallischen Glanz auf, der allerdings nach einiger Zeit durch Verwitterung matt wird. (de)</li> <li style="display:none;">La uraninita es un mineral radiactivo de la clase de los minerales óxidos según la clasificación de Strunz, rico en uranio, siendo la principal mena de este elemento. Su composición química es mayormente dióxido de uranio (UO2), pero también contiene (UO3), óxido de plomo, torio, y tierras raras.Es una principal mena de uranio la uraninita, dio lugar a su nombre en 1792. El mineral se conoce desde el siglo XV en las minas de plata en las montañas Erzgebirge, Alemania. Sin embargo, el es el de Jáchymov en la República Checa, que fue descrito por F.E.Brückmann en 1727. (es)</li> <li style="display:none;">Uraninita, edo honen aldaeratzat jo daitekeen pekblenda, mineral erradioaktibo bat da. Uranio, polonio, radio, torio, berun eta beste hainbat metal edo lur arraro izan ditzake. Izan ere, mineral hau finduz ibili ziren Pierre eta Marie Curie, polonioa eta radioa aurkitzeko. (eu)</li> <li style="display:none;">Ocsaíd úráiniam, UO2, príomh-mhianach úráiniam. Crua an-dlúth radaighníomhach. Faightear i bhféitheacha ardteochta i gcarraigeacha doigheartha í. (ga)</li> <li style="display:none;">Pitchblende merupakan bijih mineral bahan pembuat radium. Bijih ini dihasilkan dari uranium. Rumus pembuatan radium dari limbah pitchblende ini ditemukan oleh pasangan , yaitu Pierre Curie dan Marie Curie. * l * * s (in)</li> <li style="display:none;">La pechblende, également appelée uraninite, pechurane ou uranochre, est un minéral radioactif qui représente le principal minerai d'uranium. Le gisement de Jachymov (comté de Karlovy Vary, République tchèque), aujourd'hui épuisé, est le plus connu ; c'est lui qui a fourni la pechblende dont Pierre et Marie Curie ont extrait le radium. (fr)</li> <li>Uraninite, formerly pitchblende, is a radioactive, uranium-rich mineral and ore with a chemical composition that is largely UO2 but because of oxidation typically contains variable proportions of U3O8. Radioactive decay of the uranium causes the mineral to contain oxides of lead and trace amounts of helium. It may also contain thorium and rare-earth elements. (en)</li> <li style="display:none;">Het mineraal uraniniet, gewoonlijk pekblende genoemd, is het belangrijkste oxide van uranium, met de chemische formule UO2, maar vanwege oxidatie bevat het mineraal meestal variabele verhoudingen U3O8. Als gevolg van radioactief verval bevat het erts bovendien oxiden van lood en sporen van helium. Het kan ook thorium- en zeldzame aardelementen bevatten. (nl)</li> <li style="display:none;">우라니나이트(Uraninite) 혹은 역청 우라늄석, 섬우라늄석은 방사성을 띤 광물로, 우라늄 산화물이 많이 함유된 광석(UO2으로 대다수 구성)이나, 때때로 UO3, 납이나 토륨, 그리고 다른 희토류 원소들의 산화물을 포함하고 있기도 한다. 우라니나이트의 우라늄 함량은 U3O8으로 환산하자면, 약 50에서 80%정도로 추산된다. 보통 괴상의 우라니나이트를 가리켜 피치블렌드(Pitchblende)라고 부른다. 피치블렌드의 어원은 독일어(Pechblende)로 Pech는 타르, 불운을 가리키며, Blende는 광물을 가리킨다. 이 이름이 붙여지게 된 계기는 15세기 독일의 에르츠 산맥에 위치한 은광에서 광부들이 채광하면서 이 광석이 나타났기 때문인데, 이 광석은 돈으로 바꾸기가 힘들거나 불가능했기 때문이다. 그 후 1789년 피치블렌드에서 마르틴 하인리치 클라프로트(Martin Heinrich Klaproth)가 세인트요하인스틸에서 나온 폐기물을 조사하다 우라늄을 발견하게 되었다. 모든 우라니나이트에는 우라늄의 붕괴 생성물로 인해 소량의 라듐이 함유되어 있다. 또한 모든 우라니나이트엔 우라늄의 최종 붕괴형태인 Pb-206과 Pb-207이 소량 들어있다. 또한 알파 붕괴로 인해 소량의 헬륨도 들어 있다. 헬륨의 경우 첫 발견은 태양의 대기에서 발견되었으나, 그 후 우라니나이트를 분광하면서 지구상에서 발견하게 되었다. 또한 우라늄 238의 자연적인 분열로 인해 극미량(약 0.2 ng/kg)의 테크네슘도 찾을 수 있다. (ko)</li> <li style="display:none;">L'uraninite o, se in forma colloidale, pechblenda (da pitchblende = blenda picea - un termine usato dai minatori tedeschi) è un minerale ed è una delle principali fonti naturali di uranio. (it)</li> <li style="display:none;">閃ウラン鉱（せんウランこう、uraninite）は、二酸化ウラン (UO2) よりなる鉱物。等軸晶系、硬度は 5 - 6、比重は 7.5 - 10。硫酸、硝酸、フッ化水素酸に可溶。全ての閃ウラン鉱は、ウランが崩壊した結果として少量のラジウムを含む。また、少量のトリウム、希土類なども含む。ウランは、1789年にマルティン・ハインリヒ・クラプロートによりこの鉱物から初めて発見された。 (ja)</li> <li style="display:none;">Uraninit – minerał promieniotwórczy z gromady tlenków. Należy do minerałów rzadkich. Nazwa pochodzi od składnika uranu. Badania tego minerału doprowadziły Marię Skłodowską-Curie do odkrycia polonu i radu, za co otrzymała w 1911 r. drugą Nagrodę Nobla. (pl)</li> <li style="display:none;">Настуран (от др.-греч. ναστός — уплотнённый и лат. uranium — уран; синонимы: уранинит, урановая смоляная руда, урановая смолка, урановая смоляная обманка; Уранинит) — наиболее распространённый минерал урана. С точки зрения современной минералогии — устаревшее название, соответствующее скрытокристаллической морфологической разновидности минерального вида уранинит. (ru)</li> <li style="display:none;">Descoberta por Antoine Henri Becquerel, a pechblenda é uma variedade, provavelmente impura, de uraninita. Dela é retirado o urânio, que é constituinte de muitas rochas. É extraído do minério, purificado e concentrado sob a forma de um sal de cor amarela, conhecido como "yellowcake". Yellowcake significa, literalmente, “bolo amarelo”. Deve seu nome à intensa coloração amarela, característica dos compostos secundários de urânio, como pode ser visto na figura que ilustra esta página. O minério de urânio é retirado da mina e, após processos de extração, é enviado para usina de beneficiamento para obtenção do concentrado de urânio, cuja composição química é o octóxido de urânio, conhecido como yellowcake (U3O8). O Brasil tem a quinta maior reserva de urânio do mundo, de aproximadamente 300 mil toneladas. Foi a base da descoberta da radioatividade, após experimentos de Becquerel, que notou que essa pedra emitia uma forte luz, capaz de atravessar objetos opacos. Também foi base de estudo do casal Curie. Foi numa amostra de pechblenda que Marie Curie e Pierre Curie conseguiram isolar 2 elementos muito mais radioativos que o urânio, que foram o Polônio (Bem mais radioativo que o urânio), e o Rádio (Cerca de um milhão de vezes mais radioativo que o urânio). Mineiros de pechblenda apresentavam alta incidência de câncer de pulmão às pessoas que mantinham contato. (pt)</li> <li style="display:none;">Uraninit är ett radioaktivt uranoxidmineral som i regel bildar en glänsande svart till brunsvart eller grönsvart massa. Uraninit förekommer ofta i mikrokristallin form, så kallat pechblände. Namnet uraninit används för kristalliserade varianter av UO2. I sällsynta fall uppträder det som kristaller, företrädesvis i formerna 100 (kub) 111 (oktaeder) och 110. Det är ett viktigt malmmineral för utvinning av uran. På grund av uranatomernas långsamma sönderfall men även vittring, varierar den kemiska sammansättningen. (sv)</li> <li style="display:none;">晶質鈾礦（英語：Uraninite），曾被稱為瀝青鈾礦（英語：Pitchblende），是一种放射性的，富含铀的矿石，主要成分为二氧化铀，同时因氧化含有不同比例的八氧化三铀。鈾的放射性衰變導致礦物含有鉛的氧化物和微量的氦。它還可能含有釷和稀土元素。 (zh)</li> <li style="display:none;">Ураніні́т (настуран, уранова смоляна руда, уранова смолка, уранова смоляна обманка) — мінерал класу оксидів і гідрооксидів, діоксид урану координаційної будови. Руда урану й радію. Утворює ряд з торіанітом. Синоніми: кірхіт, настуран, обманка смоляна, уранін, уранопісит, уранатемніт, ульріхіт. 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class="col-2"><a class="uri" href="http://dbpedia.org/property/caption">dbp:caption</a> </td><td class="col-10 text-break"><ul> <li>Pitchblende from Niederschlema-Alberoda deposit, Germany (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/category">dbp:category</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbp:category" resource="http://dbpedia.org/resource/Oxide_minerals" href="http://dbpedia.org/resource/Oxide_minerals">dbr:Oxide_minerals</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/class">dbp:class</a> </td><td class="col-10 text-break"><ul> <li>H-M symbol: (en)</li> <li>Hexoctahedral (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/cleavage">dbp:cleavage</a> </td><td class="col-10 text-break"><ul> <li>Indistinct (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/color">dbp:color</a> </td><td class="col-10 text-break"><ul> <li>Steel-black to velvet-black, brownish black, pale gray to pale green; in transmitted light, pale green, pale yellow to deep brown and green-gray (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/diaphaneity">dbp:diaphaneity</a> </td><td class="col-10 text-break"><ul> <li>Opaque; transparent in thin fragments (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/formula">dbp:formula</a> </td><td class="col-10 text-break"><ul> <li>Uranium dioxide or uranium(IV) oxide (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/fracture">dbp:fracture</a> </td><td class="col-10 text-break"><ul> <li>Conchoidal to uneven (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/gravity">dbp:gravity</a> </td><td class="col-10 text-break"><ul> <li>10.630000 (xsd:double)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/habit">dbp:habit</a> </td><td class="col-10 text-break"><ul> <li>Massive, botryoidal, granular. Octahedral crystals uncommon. (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/imagesize">dbp:imagesize</a> </td><td class="col-10 text-break"><ul> <li>260 (xsd:integer)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/imasymbol">dbp:imasymbol</a> </td><td class="col-10 text-break"><ul> <li>Urn (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/luster">dbp:luster</a> </td><td class="col-10 text-break"><ul> <li>Submetallic, greasy, dull (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/mohs">dbp:mohs</a> </td><td class="col-10 text-break"><ul> <li>5 (xsd:integer)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/name">dbp:name</a> </td><td class="col-10 text-break"><ul> <li>Uraninite (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/opticalprop">dbp:opticalprop</a> </td><td class="col-10 text-break"><ul> <li>Isotropic (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/other">dbp:other</a> </td><td class="col-10 text-break"><ul> <li>25 (xsd:integer)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/streak">dbp:streak</a> </td><td class="col-10 text-break"><ul> <li>Brownish black, gray, olive-green (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/strunz">dbp:strunz</a> </td><td class="col-10 text-break"><ul> <li>4 (xsd:integer)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/symmetry">dbp:symmetry</a> </td><td class="col-10 text-break"><ul> <li>Fmm (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/system">dbp:system</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbp:system" resource="http://dbpedia.org/resource/Cubic_(crystal_system)" href="http://dbpedia.org/resource/Cubic_(crystal_system)">dbr:Cubic_(crystal_system)</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/unitCell">dbp:unitCell</a> </td><td class="col-10 text-break"><ul> <li>a = 5.4682 Å; Z = 4 (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/var">dbp:var</a> </td><td class="col-10 text-break"><ul> <li>Pitchblende (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/var1text">dbp:var1text</a> </td><td class="col-10 text-break"><ul> <li>Massive (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" 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resource="http://www.w3.org/2006/03/wn/wn20/instances/synset-mineral-noun-1" href="http://www.w3.org/2006/03/wn/wn20/instances/synset-mineral-noun-1">http://www.w3.org/2006/03/wn/wn20/instances/synset-mineral-noun-1</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://purl.org/dc/terms/subject">dcterms:subject</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Uranium(IV)_minerals" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Uranium(IV)_minerals">dbc:Uranium(IV)_minerals</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Cubic_minerals" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Cubic_minerals">dbc:Cubic_minerals</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Minerals_in_space_group_225" 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href="http://dbpedia.org/resource/Mineral">dbr:Mineral</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/1999/02/22-rdf-syntax-ns#type">rdf:type</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="rdf:type" resource="http://www.w3.org/2002/07/owl#Thing" href="http://www.w3.org/2002/07/owl#Thing">owl:Thing</a></li> <li><a class="uri" rel="rdf:type" resource="http://www.ontologydesignpatterns.org/ont/dul/DUL.owl#ChemicalObject" href="http://www.ontologydesignpatterns.org/ont/dul/DUL.owl#ChemicalObject">dul:ChemicalObject</a></li> <li><a class="uri" rel="rdf:type" resource="http://dbpedia.org/ontology/ChemicalSubstance" href="http://dbpedia.org/ontology/ChemicalSubstance">dbo:ChemicalSubstance</a></li> <li><a class="uri" rel="rdf:type" resource="http://www.wikidata.org/entity/Q7946" href="http://www.wikidata.org/entity/Q7946">wikidata:Q7946</a></li> <li><a class="uri" rel="rdf:type" resource="http://dbpedia.org/ontology/Mineral" href="http://dbpedia.org/ontology/Mineral">dbo:Mineral</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#comment">rdfs:comment</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">اليورانينيت (Uraninite) أو البتشبلند (بالإنجليزية: pitchblende)‏ هو خام معدني نشط إشعاعياً يتكون بشكل أساسي من ثاني أكسيد اليورانيوم (UO2) مع نسب من ثالث أكسيد اليورانيوم (UO3) وأكاسيد الرصاص والثوريوم وعناصر أرضية نادرة كالروديوم. عرف خام اليورانينيت منذ القرن الخامس عشر الميلادي على أقل تقدير في مناجم الفضة في مرتفعات إرتسيبيرغه (بالألمانية Erzgebirge) بألمانيا، إلا أنه يتركز بشكل أكبر في ياتشيموف بجمهورية التشيك، وهو الموقع الذي وصف فيه بروكمان الخام سنة 1727. وقد استخلص كلابروث عنصر اليورانيوم من خام البتشبلند المستخرج من مدينة يوهانجورجنشتات (بالألمانية Johanngeorgenstadt) الألمانية سنة 1789. (ar)</li> <li style="display:none;">La uraninita és un mineral de la classe dels òxids. És un mineral conegut des del segle xv a les mines d'argent de les Muntanyes Metal·líferes, Alemanya, tot i que la localitat tipus des del punt de vista de la geologia és Jáchymov a la República Txeca. Franz Ernst Brückmann descrigué el mineral el 1727 a partir d'uns exemplars d'aquesta localitat txeca. Va ser anomenada així l'any 1845 per Wilhelm Karl von Haidinger per la seva composició. (ca)</li> <li style="display:none;">Uraninit (starší český název smolinec), chemický vzorec UO2 (oxid uraničitý), je krychlový minerál nazvaný podle prvku uranu. (cs)</li> <li style="display:none;">Uraninito, antaŭe peĉblendo, estas radioaktiva, riĉa en uranio mineralo kaj erco kun kemia kompono kiu estas ĉefe UO2, sed pro oksidigo la mineralo tipe enhavas variajn proporciojn de U3O8. Aldone, pro efiko de radioaktiveco, la erco enhavas oksidojn el plumbo kaj eretojn el heliumo. Ĝi povas enhavi ankaŭ torion kaj rarajn terelementojn. (eo)</li> <li style="display:none;">La uraninita es un mineral radiactivo de la clase de los minerales óxidos según la clasificación de Strunz, rico en uranio, siendo la principal mena de este elemento. Su composición química es mayormente dióxido de uranio (UO2), pero también contiene (UO3), óxido de plomo, torio, y tierras raras.Es una principal mena de uranio la uraninita, dio lugar a su nombre en 1792. El mineral se conoce desde el siglo XV en las minas de plata en las montañas Erzgebirge, Alemania. Sin embargo, el es el de Jáchymov en la República Checa, que fue descrito por F.E.Brückmann en 1727. (es)</li> <li style="display:none;">Uraninita, edo honen aldaeratzat jo daitekeen pekblenda, mineral erradioaktibo bat da. Uranio, polonio, radio, torio, berun eta beste hainbat metal edo lur arraro izan ditzake. Izan ere, mineral hau finduz ibili ziren Pierre eta Marie Curie, polonioa eta radioa aurkitzeko. (eu)</li> <li style="display:none;">Ocsaíd úráiniam, UO2, príomh-mhianach úráiniam. Crua an-dlúth radaighníomhach. Faightear i bhféitheacha ardteochta i gcarraigeacha doigheartha í. (ga)</li> <li style="display:none;">Pitchblende merupakan bijih mineral bahan pembuat radium. Bijih ini dihasilkan dari uranium. Rumus pembuatan radium dari limbah pitchblende ini ditemukan oleh pasangan , yaitu Pierre Curie dan Marie Curie. * l * * s (in)</li> <li style="display:none;">La pechblende, également appelée uraninite, pechurane ou uranochre, est un minéral radioactif qui représente le principal minerai d'uranium. Le gisement de Jachymov (comté de Karlovy Vary, République tchèque), aujourd'hui épuisé, est le plus connu ; c'est lui qui a fourni la pechblende dont Pierre et Marie Curie ont extrait le radium. (fr)</li> <li>Uraninite, formerly pitchblende, is a radioactive, uranium-rich mineral and ore with a chemical composition that is largely UO2 but because of oxidation typically contains variable proportions of U3O8. Radioactive decay of the uranium causes the mineral to contain oxides of lead and trace amounts of helium. It may also contain thorium and rare-earth elements. (en)</li> <li style="display:none;">Het mineraal uraniniet, gewoonlijk pekblende genoemd, is het belangrijkste oxide van uranium, met de chemische formule UO2, maar vanwege oxidatie bevat het mineraal meestal variabele verhoudingen U3O8. Als gevolg van radioactief verval bevat het erts bovendien oxiden van lood en sporen van helium. Het kan ook thorium- en zeldzame aardelementen bevatten. (nl)</li> <li style="display:none;">L'uraninite o, se in forma colloidale, pechblenda (da pitchblende = blenda picea - un termine usato dai minatori tedeschi) è un minerale ed è una delle principali fonti naturali di uranio. (it)</li> <li style="display:none;">閃ウラン鉱（せんウランこう、uraninite）は、二酸化ウラン (UO2) よりなる鉱物。等軸晶系、硬度は 5 - 6、比重は 7.5 - 10。硫酸、硝酸、フッ化水素酸に可溶。全ての閃ウラン鉱は、ウランが崩壊した結果として少量のラジウムを含む。また、少量のトリウム、希土類なども含む。ウランは、1789年にマルティン・ハインリヒ・クラプロートによりこの鉱物から初めて発見された。 (ja)</li> <li style="display:none;">Uraninit – minerał promieniotwórczy z gromady tlenków. Należy do minerałów rzadkich. Nazwa pochodzi od składnika uranu. Badania tego minerału doprowadziły Marię Skłodowską-Curie do odkrycia polonu i radu, za co otrzymała w 1911 r. drugą Nagrodę Nobla. (pl)</li> <li style="display:none;">Настуран (от др.-греч. ναστός — уплотнённый и лат. uranium — уран; синонимы: уранинит, урановая смоляная руда, урановая смолка, урановая смоляная обманка; Уранинит) — наиболее распространённый минерал урана. С точки зрения современной минералогии — устаревшее название, соответствующее скрытокристаллической морфологической разновидности минерального вида уранинит. (ru)</li> <li style="display:none;">Uraninit är ett radioaktivt uranoxidmineral som i regel bildar en glänsande svart till brunsvart eller grönsvart massa. Uraninit förekommer ofta i mikrokristallin form, så kallat pechblände. Namnet uraninit används för kristalliserade varianter av UO2. I sällsynta fall uppträder det som kristaller, företrädesvis i formerna 100 (kub) 111 (oktaeder) och 110. Det är ett viktigt malmmineral för utvinning av uran. På grund av uranatomernas långsamma sönderfall men även vittring, varierar den kemiska sammansättningen. (sv)</li> <li style="display:none;">晶質鈾礦（英語：Uraninite），曾被稱為瀝青鈾礦（英語：Pitchblende），是一种放射性的，富含铀的矿石，主要成分为二氧化铀，同时因氧化含有不同比例的八氧化三铀。鈾的放射性衰變導致礦物含有鉛的氧化物和微量的氦。它還可能含有釷和稀土元素。 (zh)</li> <li style="display:none;">Ураніні́т (настуран, уранова смоляна руда, уранова смолка, уранова смоляна обманка) — мінерал класу оксидів і гідрооксидів, діоксид урану координаційної будови. Руда урану й радію. Утворює ряд з торіанітом. Синоніми: кірхіт, настуран, обманка смоляна, уранін, уранопісит, уранатемніт, ульріхіт. (uk)</li> <li style="display:none;">Ο ουρανινίτης (αγγλ. uraninite) ή και πισσουρανίτης (παραλλαγή με την οποία συχνά συγχέεται ή και ταυτίζεται) είναι ορυκτό οξείδιο του ουρανίου, από το οποίο λαμβάνει και το όνομά του. Σχηματίζει ισόμορφη σειρά με τον θοριανίτη (ThO2). Η κρυσταλλική του δομή είναι ανάλογη προς του φθορίτη, με ισχυρή κυβική συμμετρία, αν και στον ουρανινίτη οι σχηματισμένοι κρύσταλλοι είναι σπάνιοι και δεν παρατηρείται σχισμός. Υπενθυμίζεται ότι είναι ισχυρά ραδιενεργό ορυκτό (360 mRem/gr ετησίως) και πρέπει να αποφεύγεται η έκθεση σε αυτό για μεγάλα χρονικά διαστήματα. (el)</li> <li style="display:none;">Uraninit, unter anderem auch bekannt als Pechblende, ist ein häufig vorkommendes Mineral aus der Mineralklasse der „Oxide und Hydroxide“. Es kristallisiert im kubischen Kristallsystem mit der Zusammensetzung UO2, ist also chemisch gesehen ein Uran(IV)-oxid. Durch die radioaktive Zerfallsreihe von Uran enthält Uraninit stets einen gewissen Anteil Bleioxid (PbO), der in Abhängigkeit vom geologischen Alter bis zu 20 % betragen kann. (de)</li> <li style="display:none;">우라니나이트(Uraninite) 혹은 역청 우라늄석, 섬우라늄석은 방사성을 띤 광물로, 우라늄 산화물이 많이 함유된 광석(UO2으로 대다수 구성)이나, 때때로 UO3, 납이나 토륨, 그리고 다른 희토류 원소들의 산화물을 포함하고 있기도 한다. 우라니나이트의 우라늄 함량은 U3O8으로 환산하자면, 약 50에서 80%정도로 추산된다. 보통 괴상의 우라니나이트를 가리켜 피치블렌드(Pitchblende)라고 부른다. 피치블렌드의 어원은 독일어(Pechblende)로 Pech는 타르, 불운을 가리키며, Blende는 광물을 가리킨다. 이 이름이 붙여지게 된 계기는 15세기 독일의 에르츠 산맥에 위치한 은광에서 광부들이 채광하면서 이 광석이 나타났기 때문인데, 이 광석은 돈으로 바꾸기가 힘들거나 불가능했기 때문이다. 그 후 1789년 피치블렌드에서 마르틴 하인리치 클라프로트(Martin Heinrich Klaproth)가 세인트요하인스틸에서 나온 폐기물을 조사하다 우라늄을 발견하게 되었다. (ko)</li> <li style="display:none;">Descoberta por Antoine Henri Becquerel, a pechblenda é uma variedade, provavelmente impura, de uraninita. Dela é retirado o urânio, que é constituinte de muitas rochas. É extraído do minério, purificado e concentrado sob a forma de um sal de cor amarela, conhecido como "yellowcake". Yellowcake significa, literalmente, “bolo amarelo”. Deve seu nome à intensa coloração amarela, característica dos compostos secundários de urânio, como pode ser visto na figura que ilustra esta página. O Brasil tem a quinta maior reserva de urânio do mundo, de aproximadamente 300 mil toneladas. (pt)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#label">rdfs:label</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">يورانينيت (ar)</li> <li style="display:none;">Uraninita (ca)</li> <li style="display:none;">Uraninit (cs)</li> <li style="display:none;">Uraninit (de)</li> <li style="display:none;">Ουρανινίτης (el)</li> <li style="display:none;">Uraninito (eo)</li> <li style="display:none;">Uraninita (es)</li> <li style="display:none;">Uraninita (eu)</li> <li style="display:none;">Úráininít (ga)</li> <li style="display:none;">Uraninit (in)</li> <li style="display:none;">Pechblende (fr)</li> <li style="display:none;">Uraninite (it)</li> <li style="display:none;">우라니나이트 (ko)</li> <li style="display:none;">閃ウラン鉱 (ja)</li> <li style="display:none;">Uraniniet (nl)</li> <li style="display:none;">Uraninit (pl)</li> <li style="display:none;">Pechblenda (pt)</li> <li>Uraninite (en)</li> <li style="display:none;">Настуран (ru)</li> <li style="display:none;">Uraninit (sv)</li> <li style="display:none;">Уранініт (uk)</li> <li style="display:none;">晶质铀矿 (zh)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2002/07/owl#sameAs">owl:sameAs</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="owl:sameAs" resource="http://rdf.freebase.com/ns/m.0bxnx" href="http://rdf.freebase.com/ns/m.0bxnx">freebase:Uraninite</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://www.wikidata.org/entity/Q206467" href="http://www.wikidata.org/entity/Q206467">wikidata:Uraninite</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://af.dbpedia.org/resource/Uraniniet" href="http://af.dbpedia.org/resource/Uraniniet">dbpedia-af:Uraninite</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://ar.dbpedia.org/resource/يورانينيت" href="http://ar.dbpedia.org/resource/يورانينيت">dbpedia-ar:Uraninite</a></li> <li><a class="uri" 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