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<a href="http://dbpedia.org">dbpedia.org</a> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> Graphite (/ˈɡræfaɪt/) is a crystalline form of the element carbon. It consists of stacked layers of graphene. Graphite occurs naturally and is the most stable form of carbon under standard conditions. Synthetic and natural graphite are consumed on large scale (300 kton/year, in 1989) for uses in pencils, lubricants, and electrodes. Under high pressures and temperatures it converts to diamond. It is a weak conductor of heat and electricity. </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-233436.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;">El grafit és un mineral de la classe dels elementals, i en la seua composició concreta intervé un element semimetàl·lic. Està format quasi exclusivament per àtoms de carboni, i es tracta de fet d'una de les formes al·lotròpiques en què es pot presentar el carboni elemental, juntament amb el diamant, el ful·lerè i altres, com el grafè. El grafit és la forma més estable del carboni en condicions estàndard (o a pressions i temperatures baixes), motiu pel qual se l'utilitza en termoquímica per a definir l'estat estàndard respecte del qual es mesura la calor de formació dels compostos del carboni. També és polimorf de la chaoïta i la lonsdaleïta. Rep el seu nom per Abraham Gottlob Werner l'any 1789, i el terme grafit deriva del grec γραφειν (graphein) que significa escriure. Es pot considerar el grafit com el carbó de màxim contingut en carboni, trobant-se per damunt de l'antracita, de manera que se'l pot anomenar meta-antracita, encara que normalment no se l'empra com a combustible degut al fet que és molt difícil encendre'l. També és possible entendre el grafit com una successió de capes de grafè superposades. (ca)</li> <li style="display:none;">Grafit, chemický vzorec C, je šesterečný nekovový minerál. Starší, stále běžně používaný název pro grafit je tuha. (cs)</li> <li style="display:none;">الغرافيت هو معدن متوافر بشكل طبيعي بكثرة وهو أحد أشكال الكربون المتآصلة وذلك بالإضافة إلى الألماس والفوليرين. الغرافيت موصل للكهرباء ويمكن استخدامه على سبيل المثال في أقطاب الأقواس الكهربائية. يتبلور الغرافيت غالباً بنظام سداسي ونادراً ما يكون بالنظام الثلاثي، ويشكل بلورات بنية إلى سوداء أو رمادية لها شكل سداسي الأضلاع أو متوازي الأضلاع (لوح)، أو تكون على شكل قشور. وجود الغرافيت في حديد الزهر هو سبب ضعف هذا النوع من الحديد عندما يتعرض لشد. ولا يُعرف طريقة للتخلص منه. (ar)</li> <li style="display:none;">Ο γραφίτης (αγγλ. graphite) είναι ορυκτή πολυμορφική μορφή του άνθρακα. Το όνομά του προέρχεται από το αρχαίο ελληνικό γράφειν, λόγω της ιδιότητάς του να αποβάφει όταν τρίβεται σε μαλακή επιφάνεια. Τα άτομα του άνθρακα σχηματίζουν επίπεδα "φύλλα", με δεσμούς πολύ ισχυρούς μεταξύ των ατόμων του ίδιου φύλλου, οι δεσμοί, όμως, μεταξύ των φύλλων είναι ασθενείς. Ως συνέπεια, ο γραφίτης εμφανίζεται μαλακός και σχίζεται σε φυλλάρια (νιφάδες) πολύ εύκολα, ενώ οι συνήθεις σχηματισμοί του στη φύση είναι επίσης πλακώδεις. Εμφανίζεται, όμως, και σε στηλοειδείς, ακτινωτές και ακανόνιστες συμπαγείς μάζες. Ανευρίσκεται σε ζώνες καθολικής μεταμόρφωσης ή μεταμόρφωσης επαφής εντός γνευσίων, σχιστολίθων (κρυσταλλοσχιστώδη) αλλά και μεταμορφωμένων ασβεστολίθων. Ανευρίσκεται, επίσης, σε υδροθερμικές φλέβες και σε μερικούς σιδηρομετεωρίτες καθώς και σε ορισμένες περιφερειακές ζώνες ανθρακωρυχείων, προερχόμενος από μεταμόρφωση άλλων μορφών ορυκτού άνθρακα, ενώ έχει ανευρεθεί και ως συστατικό πυριγενών πετρωμάτων. Συνδέεται με χαλαζία, ασβεστίτη, μαρμαρυγίες και ορυκτά της ομάδας του τουρμαλίνη. Παρά το ότι χημικά είναι όμοιος σε σύσταση με το διαμάντι, οι διαφορές τους είναι αξιοσημείωτες και οφείλονται στην διαφορετική διάταξη των ατόμων του άνθρακα. Εκτός από τη σκληρότητα, ο γραφίτης είναι καλός αγωγός του ηλεκτρισμού, αδιαφανής, και χρησιμοποιείται ως πρόσθετο σε λιπαντικά (π.χ. γραφιτούχος βαλβολίνη, η οποία περιορίζει τους θορύβους σε συστήματα μετάδοσης οχημάτων). Χρησιμοποιείται, υπό μορφή παχέων πλακών, στους πυρηνικούς αντιδραστήρες, ως επιβραδυντής νετρονίων. Είναι, επίσης, το βασικό συστατικό για την κατασκευή των κοινών μολυβιών. Σημαντικές χρήσεις του είναι, επίσης, η κατασκευή ηλεκτροδίων (η ηλεκτρόλυση αλουμίνας για την παρασκευή αργιλίου πραγματοποιείται με ηλεκτρόδια από γραφίτη), στην βιομηχανία χάλυβα και ορειχάλκου, στην κατασκευή μπαταριών (οι κοινές μπαταρίες έχουν ηλεκτρόδιο ανόδου από γραφίτη) και στην κατασκευή πυρίμαχων υλικών. Απαντά σε πολλές περιοχές του κόσμου. Οι περιοχές που ανευρίσκονται μεγάλοι κρύσταλλοι και είναι, επίσης, οικονομικά εκμεταλλεύσιμος, είναι στην Καρελία και στο Τουρουκάνσκ (Turukhansk) (επί του ποταμού Ιενεσέη) της Ρωσίας, στο Κεμπέκ (Καναδάς), στην Σρι Λάνκα (μεγάλο κοίτασμα με εξαιρετικής ποιότητας γραφίτη), στο Μεξικό (περιοχή της Σονόρα), προερχόμενος από μεταμόρφωση λιθανθρακοφόρων κοιτών, και στην πολιτεία της Νέας Υόρκης (Μονρόε και Τικοντερόγκα) των ΗΠΑ. (el)</li> <li style="display:none;">Grafito (nomata de Abraham Gottlob Werner en 1789, el la greka γραφειν: "skribi/desegni" pro sia uzo en krajonoj) estas la ĉefa alotropo de karbono. Malsimile al diamanto, grafito estas konduktanto. Grafito estadas uzata kiel materialo de elektrodoj por fari elektran arkon (ekzemple en arkolampo, kvankam nun ĉi tiaj lampoj ne estas uzataj) kaj por glatantaj kontaktoj. Ĝi estas tre mola mineralo, nur 1-2 laŭ la Mohs-skalo. Grafito estas memstara mineralo kreata per pura karbono simile kiel la dua kaj tre diferenca formo de la karbono en la naturo – diamanto. La trian alotropon kreas fermitaj globformaj strukturoj kun 20 kaj pli multe da atomoj - fulereno (Kroto, Curl, Smalley 1985). Kristalografie sesangula grafito havas la atomojn ordigatajn en tavoloj, moveblaj unu trans la alia. Ĝi do lasas spuron sur papero kaj estas bonega lubrikaĵo, farbaĵo, elektro- kaj varmkondukanto, varme kaj ĥemie rezista materialo. La kubforma diamanto male havas ĉiun atomon firme ligitan kun kvar pluaj atomoj en regula strukturo. Fulereno C60 ankaŭ havas la kubforman sistemon. (Jehlička – Frank 2006). Grafito estas trovebla en multaj lokoj sur la terglobo. Grandaj grafitminejoj ekzistas en Usono (Texas kaj New York), Meksiko, Hindujo kaj Sovetio; gravaj estis ankaŭ la trovejoj en suda Bohemio (Český Krumlov, Netolice). La grafito estas samtempe parto de fulgoj, estiĝantaj per forbruligo de fosiliaj energiportantoj. Ĉiokaze la grafito ĉeestas en tiom malgrandaj eretoj, ke la fulgoj montras ecojn de amorfa karbono. La grafito aperas en la naturo tre ofte kiel parto de diversaj precipe metamorfintaj petroj. Ĝia enhavo en ili estas normale ne granda, do estiĝo de grafita kuŝejo estas natura escepto simile kiel metalerca kuŝejo. Por akiri altgrade puran grafiton oni devas rafini grafitercon plej ofte per flotado. Intereson pri diversaj specoj de koncentraĵoj, rafinaĵoj, lubrikaĵoj, pastoj, lakoj kaj suspensiaĵoj montras diversgrade preskaŭ ĉiu branĉo de industrio. La plej gravaj estas nigra keramiko (tigloj, metalurgiaj iloj), fandejoj, stalfabrikoj, elektroteĥniko (elektrodoj, baterioj, brosoj), fabrikado de varmrezistaj materialoj, ĥemio, glasfabrikoj, lubrikado de maŝinoj, kontaktolineoj, relkomutiloj, ferindustrio, krajonfabrikado (ekzemple ĉina inko estas koloida solvaĵo de grafito kaj fulgoj), nuklea energetiko (moderigiloj), raketa tekniko. Novaj produktoj baze de karbono – fibroj, fibroŝtofoj, fluorgrafito, elasta grafito servas por kalfatri movigantajn kaj aliajn maŝinpartojn anstataŭ la malsaniga asbesto. La esplorado kaj provado de novaj fabrikaĵoj ĉiam daŭras (fulerenoj C60 kaj aliaj, optiko, elektroniko, medicino).Plua grava uzebleco de grafito estas tiu en metalurgia industrio. Pro ĝia granda varmrezisto oni uzas ĝin por fabrikado de ujoj, t. n. muldujoj por fanditaj metaloj kaj ties kunfandaĵoj. Oni evitas tiel malpurigadon de la fandaĵo per metalo, el kiu la muldujo devus esti farita. El grafito estiĝas ankaŭ elektrodoj por elfandigi aluminion el kunfandaĵo de baŭksito kaj kriolito per la procezo Hall-Héroult aŭ silicion el fandita siliko. Artefarita formo de grafito estas t.n. glasa grafito (angle glassy carbon), distingiĝanta per alta denseco, malgranda poreco kaj grava ĥemia kaj meĥanika imuneco. Oni fabrikas ĝin per precize kontrolita longtempa alttemperatura disigo de organikaj materialoj ĉe la surfaco de ordinara grafito. Dank´ al eksterordinaraj fizikaj kaj ĥemiaj ecoj de glasa grafito ĝia praktika uzado ĉiam disvastiĝas malgraŭ ĝia relativa altprezo. Por elektroĥemio gravas la fakto, ke la surfaco de elektrodoj el la glasa grafito estas tre ĥemie imuna kaj oni povas atingi sur ili altan afirman potencialon sen ilia disfandiĝo, kiel ĉe ordinaraj metalaj elektrodoj.Tion oni povas bone eluzi kaj en analitika ĥemio dum la esploro de elektroĥemiaj ecoj de organikaj molekuloj, kaj por prepara oksidigo dum la preparo de kelkaj kombinaĵoj. Analitika metodo GFAAS (atoma spektrometrio kun senflama atomigo) uzas por liofilizado de prilaborata specimeno kuveton, varmiĝanta dum kelkaj sekundoj ĝis proks. 3000 °C. Ŝirmo de la interna surfaco de tiu kuveto per glasa grafito ege pligrandigas ties imunon kaj prilongigas ĝian uzeblon kompare kun klasika grafita kuveto. En metalurgia purigado de metaloj per la metodo de zona fandigo oni povas uzi tubojn ŝirmitajn de glasa grafito, en kiuj la fandigo okazas. Laboratoraj ujoj kun la surfaco el glasa grafito atingas la saman aŭ eĉ pli grandan ĥemian rezistemon kiel la ujoj el platino aŭ ties kunfandaĵo kun rhodio. * * * (eo)</li> <li style="display:none;">Graphit (auch Grafit) ist ein sehr häufig vorkommendes Mineral aus der Mineralklasse der „Elemente“. Er ist eine der natürlichen Erscheinungsformen des chemischen Elements Kohlenstoff in Reinform und kristallisiert äußerlich gesehen im hexagonalen Kristallsystem (genaueres siehe ). Graphit bildet undurchsichtige, graue bis schwarze Kristalle in sechseckiger, tafeliger, schuppiger oder stängeliger Form, die auf den Kristallflächen Metallglanz aufweisen. Massige oder körnige Aggregate sind dagegen matt. Seine Mohshärte beträgt zwischen 1 und 2, seine Dichte etwa 2,1 bis 2,3 g/cm³, und er hat eine grauschwarze Strichfarbe. (de)</li> <li>Graphite (/ˈɡræfaɪt/) is a crystalline form of the element carbon. It consists of stacked layers of graphene. Graphite occurs naturally and is the most stable form of carbon under standard conditions. Synthetic and natural graphite are consumed on large scale (300 kton/year, in 1989) for uses in pencils, lubricants, and electrodes. Under high pressures and temperatures it converts to diamond. It is a weak conductor of heat and electricity. (en)</li> <li style="display:none;">Grafitoa karbono puruaren forma kristaldua da. Karbonoaren era alotropiko bat da. Hexagonala da eta kolore beltzaxka eta distira metalikoa du. Eroale ona da, tenperatura handia jasateko gaitasuna du, eta azidoek ez dute desegiten. Izadian aurki daiteke (sedimentu harrietan batez ere) baina laborategian ere prestatzen da labe elektriko batean antrazita berotuta. Erabilera asko ditu industrian, eroale eta labaingarritarako, adibidez (azken honetarako olioekin nahastuz). Margo beltzak, arkatzak eta elektrodoak egiteko, eta beste hainbat gauzatarako ere erabiltzen da. (eu)</li> <li style="display:none;">Le graphite est une espèce minérale qui est, avec le diamant, la lonsdaléite et la chaoite, l'un des allotropes naturels du carbone. Sa formule chimique est « C » mais les formes natives permettent de retrouver des traces d'hydrogène (« H »), d'azote (« N »), d'oxygène (« O »), de silicium (« Si »), d'aluminium (« Al »), de fer (« Fe ») ou encore d'argile. (fr)</li> <li style="display:none;">El grafito es una de las formas alotrópicas en las que se puede presentar el carbono en la naturaleza. Otras formas son el diamante, la y la lonsdaleíta. A presión atmosférica y temperatura ambiente el polimorfo más estable es el grafito. Sin embargo, la transformación del diamante en grafito es tan extremadamente lenta que solo es apreciable a escala geológica. Fue nombrado por Abraham Gottlob Werner en el año 1789. El término grafito deriva del griego γραφειν (graphein) que significa "escribir", ya que se usa principalmente para crear la punta de los lápices. Antiguamente recibía otros muchos nombres, como plombagina y "molibundasna" (que no debe confundirse con el mineral molibdeno). (es)</li> <li style="display:none;">Foirm mhianrach carbóin a fhaightear i gcarraigeacha meiteamorfacha. Dubh bog, gréisceach le mothú. Seoltóir maith leictreachais, agus bealadh tirim maith. (ga)</li> <li style="display:none;">Grafit, sebagaimana berlian, adalah bentuk alotrop karbon, karena kedua senyawa ini mirip namun struktur atomnya mempengaruhi sifat kimiawi dan fisikanya. Grafit terdiri atas lapisan atom karbon, yang dapat menggelincir dengan mudah. Artinya, grafit amat lembut, dan dapat digunakan sebagai untuk membuat peralatan mekanis bekerja lebih lancar. Grafit sekarang umum digunakan sebagai "timbal" pada pensil. Grafit berwarna kelabu. Akibat delokalisasi elektron antar-permukannya, grafit dapat berfungsi sebagai konduktor listrik. Secara alamiah, grafit ditemukan di Sri Lanka, Kanada dan Amerika Serikat. Grafit juga disebut sebagai timbal hitam. Grafit dinamai oleh pada tahun 1789 dengan mengambil kata dari bahasa Yunani yang artinya menulis. Grafit juga bisa dibuat menjadi isi pensil. mineral grafit dapat di temukan di batuan metamorf yaitu sabak, filit, sekis, gneis. Wikimedia Commons memiliki media mengenai Graphite. * l * * s (in)</li> <li style="display:none;">グラファイト（graphite、石墨、黒鉛）は、炭素から成る元素鉱物。六方晶系（結晶対称性はP63/mmc）、六角板状結晶。構造は亀の甲状の層状物質、層毎の面内は強い共有結合（sp2的）で炭素間が繋がっているが、層と層の間（面間）は弱いファンデルワールス力で結合している。それゆえ、層状に剥離する（へき開完全）。電子状態は、半金属的である。グラファイトが剥がれて厚さが原子1個分しかない単一層となったものはグラフェンと呼ばれ、金属と半導体の両方の性質を持つ。採掘は、スリランカのサバラガムワ、メキシコのソノラ、カナダのオンタリオ州、北朝鮮、マダガスカル、アメリカのニューヨーク州などで商業的に行われている。日本でも、かつて富山県で千野谷黒鉛鉱山が稼働していた。 (ja)</li> <li style="display:none;">흑연(黑鉛, 영어: graphite) 또는 석묵(石墨)은 탄소의 동소체 중 하나이다. 천연에서 산출되기도 하고, 인공적으로 제조되기도 한다. 흑연의 영어 이름인 "graphite"는 "(글 따위를) 쓰다"라는 뜻을 가진 그리스어 "graphein"에서 유래되었다. (ko)</li> <li style="display:none;">Grafiet is een allotrope vorm van het element koolstof. Grafiet is een van de zachtste vaste elementaire materialen. De kristalstructuur is hexagonaal. Als allotroop van koolstof heeft grafiet een aantal opmerkelijke eigenschappen voor een niet-metaal. Zo is het een relatief goede elektrische geleider. (nl)</li> <li style="display:none;">Grafit – pospolity i szeroko rozpowszechniony minerał z gromady pierwiastków rodzimych. Stosowany jako naturalny suchy smar. Jest – obok diamentu i fulerytu – odmianą alotropową węgla. Nazwa pochodzi od gr. graphein = pisać, nawiązuje do tradycyjnego zastosowania tego minerału. (pl)</li> <li style="display:none;">La grafite è un minerale che rappresenta uno degli stati allotropici del carbonio. È un ottimo conduttore elettrico ed è il materiale con la più alta temperatura di fusione. Attraverso la grafitazione si può ottenere la grafite artificiale. (it)</li> <li style="display:none;">Графи́т (от др.-греч. γράφω «записывать, писать») — минерал из класса самородных элементов, одна из аллотропных модификаций углерода. Структура слоистая. Слои кристаллической решётки могут по-разному располагаться относительно друг друга, образуя целый ряд политипов, с симметрией от гексагональной сингонии (дигексагонально-дипирамидальный), до тригональной (дитригонально-скаленоэдрический). Слои слабоволнистые, почти плоские, состоят из шестиугольных слоёв атомов углерода. Кристаллы пластинчатые, чешуйчатые. Образует листоватые и округлые радиально-лучистые агрегаты, реже — агрегаты концентрически-зонального строения. У крупнокристаллических выделений часто треугольная штриховка на плоскостях (0001). Природный графит имеет разновидности: плотнокристаллические (жильный), кристаллический (чешуйчатый), скрытокристаллический (аморфный, микрокристаллический) и различается по размерам кристаллов. (ru)</li> <li style="display:none;">Grafit (nybildning av grekiska grạphein - skriva)är ett mineral som bara består av grundämnet kol. Grafit är en allotrop av kol där atomerna bildar plana skikt med kristaller av hexagonstruktur. I grafit binder en kolatom tre andra. Inom lagren sitter atomerna fast hårt, men mellan lagren mindre hårt. Det behövs alltså ingen större yttre påverkan för att lagren ska lossna från varandra.[källa behövs] Detta gör att när man drar ett stycke grafit mot något, så lämnar det ett gråsvart streck efter sig (något som brukar kallas streckfärg). (sv)</li> <li style="display:none;">Grafite (ou, raramente, grafita) é um mineral, um dos alótropos do carbono. Ao contrário do diamante, a grafite é um condutor elétrico. Por isso possui aplicações em eletrônica, como em eletrodos e baterias. Em razão do seu alto ponto de fusão, também possui aplicações como material refratário, como em cadinhos de fundição de aço. A grafite pode ser dissolvida em ácido clorossulfúrico. (pt)</li> <li style="display:none;">石墨（Graphite），又稱黑鉛（Black Lead），是碳的一種同素異形體（碳的其他同素異形體有很多，為人熟悉的例如鑽石）。作为最軟的礦物之一，石墨不透明且觸感油膩，顏色由鐵黑到鋼鐵灰不等，形狀可呈晶體狀、薄片狀、鱗狀、條紋狀、層狀體，或散佈在變質岩（由煤、碳質岩石或碳質沉積物，受到區域變質作用或是岩漿侵入作用形成）之中。化學性質不活潑，具有耐腐蝕性。 (zh)</li> <li style="display:none;">Графі́т (від грец. γραφο — писати) — мінерал класу самородних напівметалів, найстійкіший у земній корі кристалічний різновид вуглецю. Структура шарувата. Колір чорний, сірий. Сингонія гексагональна. Графіт — темно-сіра непрозора речовина, алотропна форма вуглецю. На відміну від алмазу графіт добре проводить електричний струм і тепло та дуже м'який. Графіт належить до найбільш легкофлотованих мінералів, але його флотованість залежить від величини кристалів, характеру домішок та ступеня окиснення поверхні. Флотацію графіту звичайно проводять з використанням гасу і спінювача у лужному або кислотному середовищі, яке створюється содою, вапном або сірчаною кислотою. Природний аполярний характер кристалів графіту, їхня луската форма і мала густина обумовлюють легку флотованість графіту і дозволяють флотувати досить великі частинки. 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href="http://dbpedia.org/resource/File:2005graphite.PNG">dbr:File:2005graphite.PNG</a></li> <li><a class="uri" rel="dbo:wikiPageWikiLink" resource="http://dbpedia.org/resource/File:Crane’s_Servants_Friend_series_no._3.jpg" href="http://dbpedia.org/resource/File:Crane’s_Servants_Friend_series_no._3.jpg">dbr:File:Crane’s_Servants_Friend_series_no._3.jpg</a></li> <li><a class="uri" rel="dbo:wikiPageWikiLink" resource="http://dbpedia.org/resource/File:Graphite-pV.svg" href="http://dbpedia.org/resource/File:Graphite-pV.svg">dbr:File:Graphite-pV.svg</a></li> <li><a class="uri" rel="dbo:wikiPageWikiLink" resource="http://dbpedia.org/resource/File:Kimmirut_Graphite.jpg" href="http://dbpedia.org/resource/File:Kimmirut_Graphite.jpg">dbr:File:Kimmirut_Graphite.jpg</a></li> <li><a class="uri" rel="dbo:wikiPageWikiLink" resource="http://dbpedia.org/resource/File:Naturalis_Biodiversity_Center_-_Museum_-_Exhibition_Nature_theatre_08_-_Graphite,_large_stone.jpg" href="http://dbpedia.org/resource/File:Naturalis_Biodiversity_Center_-_Museum_-_Exhibition_Nature_theatre_08_-_Graphite,_large_stone.jpg">dbr:File:Naturalis_Biodiversity_Center_-_M...heatre_08_-_Graphite,_large_stone.jpg</a></li> <li><a class="uri" rel="dbo:wikiPageWikiLink" resource="http://dbpedia.org/resource/File:“Orgy_of_the_Growl_Devils_“_“Graphited_Wood_Grease”_1908_ad_-_Electric_railway_review_(IA_electricrailwayr19amer)_(page_50_crop).jpg" href="http://dbpedia.org/resource/File:“Orgy_of_the_Growl_Devils_“_“Graphited_Wood_Grease”_1908_ad_-_Electric_railway_review_(IA_electricrailwayr19amer)_(page_50_crop).jpg">dbr:File:“Orgy_of_the_Growl_Devils_“_“Grap...ricrailwayr19amer)_(page_50_crop).jpg</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/caption">dbp:caption</a> </td><td class="col-10 text-break"><ul> <li>Graphite specimen (en)</li> </ul></td></tr><tr class="odd"><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/Native_mineral" href="http://dbpedia.org/resource/Native_mineral">dbr:Native_mineral</a></li> </ul></td></tr><tr class="even"><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><a class="uri" rel="dbp:class" resource="http://dbpedia.org/resource/Hermann–Mauguin_notation" href="http://dbpedia.org/resource/Hermann–Mauguin_notation">dbr:Hermann–Mauguin_notation</a></li> <li>Dihexagonal dipyramidal (en)</li> </ul></td></tr><tr class="odd"><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>Basal – perfect on {0001} (en)</li> </ul></td></tr><tr class="even"><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>Iron-black to steel-gray; deep blue in transmitted light (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/density">dbp:density</a> </td><td class="col-10 text-break"><ul> <li>2.090000 (xsd:double)</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 only in extremely thin flakes (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><a class="uri" rel="dbp:formula" resource="http://dbpedia.org/resource/Carbon" href="http://dbpedia.org/resource/Carbon">dbr:Carbon</a></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>Flaky, otherwise rough when not on cleavage (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>1.900000 (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>Tabular, six-sided foliated masses, granular to compacted masses (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>170 (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>Gr (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>Metallic, earthy (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>1 (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>Graphite (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>Uniaxial (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>strongly anisotropic, conducts electricity, greasy feel, readily marks (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/pleochroism">dbp:pleochroism</a> </td><td class="col-10 text-break"><ul> <li>Strong (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/solubility">dbp:solubility</a> </td><td class="col-10 text-break"><ul> <li>Soluble in molten nickel, warm chlorosulfuric acid (en)</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>Black (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>1 (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>P63mc P63/mmc (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/Hexagonal_crystal_system" href="http://dbpedia.org/resource/Hexagonal_crystal_system">dbr:Hexagonal_crystal_system</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/tenacity">dbp:tenacity</a> </td><td class="col-10 text-break"><ul> <li>Flexible non-elastic, sectile (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/twinning">dbp:twinning</a> </td><td class="col-10 text-break"><ul> <li>Present (en)</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 = 2.461, c = 6.708 [Å]; Z = 4 (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" 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rel="dbp:wikiPageUsesTemplate" resource="http://dbpedia.org/resource/Template:Toclimit" href="http://dbpedia.org/resource/Template:Toclimit">dbt:Toclimit</a></li> <li><a class="uri" rel="dbp:wikiPageUsesTemplate" resource="http://dbpedia.org/resource/Template:Infobox_mineral" href="http://dbpedia.org/resource/Template:Infobox_mineral">dbt:Infobox_mineral</a></li> <li><a class="uri" rel="dbp:wikiPageUsesTemplate" resource="http://dbpedia.org/resource/Template:Allotropes_of_carbon" href="http://dbpedia.org/resource/Template:Allotropes_of_carbon">dbt:Allotropes_of_carbon</a></li> <li><a class="uri" rel="dbp:wikiPageUsesTemplate" resource="http://dbpedia.org/resource/Template:Coal" href="http://dbpedia.org/resource/Template:Coal">dbt:Coal</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/wordnet_type">dbp:wordnet_type</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbp:wordnet_type nofollow" 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:Industrial_minerals" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Industrial_minerals">dbc:Industrial_minerals</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Dry_lubricants" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Dry_lubricants">dbc:Dry_lubricants</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Electrical_conductors" 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resource="http://dbpedia.org/resource/Category:Shades_of_black" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Shades_of_black">dbc:Shades_of_black</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Non-petroleum_based_lubricants" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Non-petroleum_based_lubricants">dbc:Non-petroleum_based_lubricants</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://purl.org/linguistics/gold/hypernym">gold:hypernym</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="gold:hypernym" resource="http://dbpedia.org/resource/Form" prefix="gold: http://purl.org/linguistics/gold/" href="http://dbpedia.org/resource/Form">dbr:Form</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://dbpedia.org/class/yago/WikicatArtMaterials" href="http://dbpedia.org/class/yago/WikicatArtMaterials">yago:WikicatArtMaterials</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" 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Starší, stále běžně používaný název pro grafit je tuha. (cs)</li> <li style="display:none;">الغرافيت هو معدن متوافر بشكل طبيعي بكثرة وهو أحد أشكال الكربون المتآصلة وذلك بالإضافة إلى الألماس والفوليرين. الغرافيت موصل للكهرباء ويمكن استخدامه على سبيل المثال في أقطاب الأقواس الكهربائية. يتبلور الغرافيت غالباً بنظام سداسي ونادراً ما يكون بالنظام الثلاثي، ويشكل بلورات بنية إلى سوداء أو رمادية لها شكل سداسي الأضلاع أو متوازي الأضلاع (لوح)، أو تكون على شكل قشور. وجود الغرافيت في حديد الزهر هو سبب ضعف هذا النوع من الحديد عندما يتعرض لشد. ولا يُعرف طريقة للتخلص منه. (ar)</li> <li>Graphite (/ˈɡræfaɪt/) is a crystalline form of the element carbon. It consists of stacked layers of graphene. Graphite occurs naturally and is the most stable form of carbon under standard conditions. Synthetic and natural graphite are consumed on large scale (300 kton/year, in 1989) for uses in pencils, lubricants, and electrodes. Under high pressures and temperatures it converts to diamond. It is a weak conductor of heat and electricity. (en)</li> <li style="display:none;">Grafitoa karbono puruaren forma kristaldua da. Karbonoaren era alotropiko bat da. Hexagonala da eta kolore beltzaxka eta distira metalikoa du. Eroale ona da, tenperatura handia jasateko gaitasuna du, eta azidoek ez dute desegiten. Izadian aurki daiteke (sedimentu harrietan batez ere) baina laborategian ere prestatzen da labe elektriko batean antrazita berotuta. Erabilera asko ditu industrian, eroale eta labaingarritarako, adibidez (azken honetarako olioekin nahastuz). Margo beltzak, arkatzak eta elektrodoak egiteko, eta beste hainbat gauzatarako ere erabiltzen da. (eu)</li> <li style="display:none;">Le graphite est une espèce minérale qui est, avec le diamant, la lonsdaléite et la chaoite, l'un des allotropes naturels du carbone. Sa formule chimique est « C » mais les formes natives permettent de retrouver des traces d'hydrogène (« H »), d'azote (« N »), d'oxygène (« O »), de silicium (« Si »), d'aluminium (« Al »), de fer (« Fe ») ou encore d'argile. (fr)</li> <li style="display:none;">Foirm mhianrach carbóin a fhaightear i gcarraigeacha meiteamorfacha. Dubh bog, gréisceach le mothú. Seoltóir maith leictreachais, agus bealadh tirim maith. (ga)</li> <li style="display:none;">グラファイト（graphite、石墨、黒鉛）は、炭素から成る元素鉱物。六方晶系（結晶対称性はP63/mmc）、六角板状結晶。構造は亀の甲状の層状物質、層毎の面内は強い共有結合（sp2的）で炭素間が繋がっているが、層と層の間（面間）は弱いファンデルワールス力で結合している。それゆえ、層状に剥離する（へき開完全）。電子状態は、半金属的である。グラファイトが剥がれて厚さが原子1個分しかない単一層となったものはグラフェンと呼ばれ、金属と半導体の両方の性質を持つ。採掘は、スリランカのサバラガムワ、メキシコのソノラ、カナダのオンタリオ州、北朝鮮、マダガスカル、アメリカのニューヨーク州などで商業的に行われている。日本でも、かつて富山県で千野谷黒鉛鉱山が稼働していた。 (ja)</li> <li style="display:none;">흑연(黑鉛, 영어: graphite) 또는 석묵(石墨)은 탄소의 동소체 중 하나이다. 천연에서 산출되기도 하고, 인공적으로 제조되기도 한다. 흑연의 영어 이름인 "graphite"는 "(글 따위를) 쓰다"라는 뜻을 가진 그리스어 "graphein"에서 유래되었다. (ko)</li> <li style="display:none;">Grafiet is een allotrope vorm van het element koolstof. Grafiet is een van de zachtste vaste elementaire materialen. De kristalstructuur is hexagonaal. Als allotroop van koolstof heeft grafiet een aantal opmerkelijke eigenschappen voor een niet-metaal. Zo is het een relatief goede elektrische geleider. (nl)</li> <li style="display:none;">Grafit – pospolity i szeroko rozpowszechniony minerał z gromady pierwiastków rodzimych. Stosowany jako naturalny suchy smar. Jest – obok diamentu i fulerytu – odmianą alotropową węgla. Nazwa pochodzi od gr. graphein = pisać, nawiązuje do tradycyjnego zastosowania tego minerału. (pl)</li> <li style="display:none;">La grafite è un minerale che rappresenta uno degli stati allotropici del carbonio. È un ottimo conduttore elettrico ed è il materiale con la più alta temperatura di fusione. Attraverso la grafitazione si può ottenere la grafite artificiale. (it)</li> <li style="display:none;">Grafit (nybildning av grekiska grạphein - skriva)är ett mineral som bara består av grundämnet kol. Grafit är en allotrop av kol där atomerna bildar plana skikt med kristaller av hexagonstruktur. I grafit binder en kolatom tre andra. Inom lagren sitter atomerna fast hårt, men mellan lagren mindre hårt. Det behövs alltså ingen större yttre påverkan för att lagren ska lossna från varandra.[källa behövs] Detta gör att när man drar ett stycke grafit mot något, så lämnar det ett gråsvart streck efter sig (något som brukar kallas streckfärg). (sv)</li> <li style="display:none;">Grafite (ou, raramente, grafita) é um mineral, um dos alótropos do carbono. Ao contrário do diamante, a grafite é um condutor elétrico. Por isso possui aplicações em eletrônica, como em eletrodos e baterias. Em razão do seu alto ponto de fusão, também possui aplicações como material refratário, como em cadinhos de fundição de aço. A grafite pode ser dissolvida em ácido clorossulfúrico. (pt)</li> <li style="display:none;">石墨（Graphite），又稱黑鉛（Black Lead），是碳的一種同素異形體（碳的其他同素異形體有很多，為人熟悉的例如鑽石）。作为最軟的礦物之一，石墨不透明且觸感油膩，顏色由鐵黑到鋼鐵灰不等，形狀可呈晶體狀、薄片狀、鱗狀、條紋狀、層狀體，或散佈在變質岩（由煤、碳質岩石或碳質沉積物，受到區域變質作用或是岩漿侵入作用形成）之中。化學性質不活潑，具有耐腐蝕性。 (zh)</li> <li style="display:none;">El grafit és un mineral de la classe dels elementals, i en la seua composició concreta intervé un element semimetàl·lic. Està format quasi exclusivament per àtoms de carboni, i es tracta de fet d'una de les formes al·lotròpiques en què es pot presentar el carboni elemental, juntament amb el diamant, el ful·lerè i altres, com el grafè. El grafit és la forma més estable del carboni en condicions estàndard (o a pressions i temperatures baixes), motiu pel qual se l'utilitza en termoquímica per a definir l'estat estàndard respecte del qual es mesura la calor de formació dels compostos del carboni. També és polimorf de la chaoïta i la lonsdaleïta. Rep el seu nom per Abraham Gottlob Werner l'any 1789, i el terme grafit deriva del grec γραφειν (graphein) que significa escriure. Es pot considerar e (ca)</li> <li style="display:none;">Ο γραφίτης (αγγλ. graphite) είναι ορυκτή πολυμορφική μορφή του άνθρακα. Το όνομά του προέρχεται από το αρχαίο ελληνικό γράφειν, λόγω της ιδιότητάς του να αποβάφει όταν τρίβεται σε μαλακή επιφάνεια. Τα άτομα του άνθρακα σχηματίζουν επίπεδα "φύλλα", με δεσμούς πολύ ισχυρούς μεταξύ των ατόμων του ίδιου φύλλου, οι δεσμοί, όμως, μεταξύ των φύλλων είναι ασθενείς. Ως συνέπεια, ο γραφίτης εμφανίζεται μαλακός και σχίζεται σε φυλλάρια (νιφάδες) πολύ εύκολα, ενώ οι συνήθεις σχηματισμοί του στη φύση είναι επίσης πλακώδεις. Εμφανίζεται, όμως, και σε στηλοειδείς, ακτινωτές και ακανόνιστες συμπαγείς μάζες. (el)</li> <li style="display:none;">Graphit (auch Grafit) ist ein sehr häufig vorkommendes Mineral aus der Mineralklasse der „Elemente“. Er ist eine der natürlichen Erscheinungsformen des chemischen Elements Kohlenstoff in Reinform und kristallisiert äußerlich gesehen im hexagonalen Kristallsystem (genaueres siehe ). (de)</li> <li style="display:none;">Grafito (nomata de Abraham Gottlob Werner en 1789, el la greka γραφειν: "skribi/desegni" pro sia uzo en krajonoj) estas la ĉefa alotropo de karbono. Malsimile al diamanto, grafito estas konduktanto. Grafito estadas uzata kiel materialo de elektrodoj por fari elektran arkon (ekzemple en arkolampo, kvankam nun ĉi tiaj lampoj ne estas uzataj) kaj por glatantaj kontaktoj. Ĝi estas tre mola mineralo, nur 1-2 laŭ la Mohs-skalo. En metalurgia purigado de metaloj per la metodo de zona fandigo oni povas uzi tubojn ŝirmitajn de glasa grafito, en kiuj la fandigo okazas. * * * (eo)</li> <li style="display:none;">El grafito es una de las formas alotrópicas en las que se puede presentar el carbono en la naturaleza. Otras formas son el diamante, la y la lonsdaleíta. A presión atmosférica y temperatura ambiente el polimorfo más estable es el grafito. Sin embargo, la transformación del diamante en grafito es tan extremadamente lenta que solo es apreciable a escala geológica. (es)</li> <li style="display:none;">Grafit, sebagaimana berlian, adalah bentuk alotrop karbon, karena kedua senyawa ini mirip namun struktur atomnya mempengaruhi sifat kimiawi dan fisikanya. Grafit terdiri atas lapisan atom karbon, yang dapat menggelincir dengan mudah. Artinya, grafit amat lembut, dan dapat digunakan sebagai untuk membuat peralatan mekanis bekerja lebih lancar. Grafit sekarang umum digunakan sebagai "timbal" pada pensil. Grafit berwarna kelabu. Akibat delokalisasi elektron antar-permukannya, grafit dapat berfungsi sebagai konduktor listrik. Wikimedia Commons memiliki media mengenai Graphite. * l * * s (in)</li> <li style="display:none;">Графи́т (от др.-греч. γράφω «записывать, писать») — минерал из класса самородных элементов, одна из аллотропных модификаций углерода. Структура слоистая. Слои кристаллической решётки могут по-разному располагаться относительно друг друга, образуя целый ряд политипов, с симметрией от гексагональной сингонии (дигексагонально-дипирамидальный), до тригональной (дитригонально-скаленоэдрический). Слои слабоволнистые, почти плоские, состоят из шестиугольных слоёв атомов углерода. Кристаллы пластинчатые, чешуйчатые. Образует листоватые и округлые радиально-лучистые агрегаты, реже — агрегаты концентрически-зонального строения. У крупнокристаллических выделений часто треугольная штриховка на плоскостях (0001). Природный графит имеет разновидности: плотнокристаллические (жильный), кристаллический (че (ru)</li> <li style="display:none;">Графі́т (від грец. γραφο — писати) — мінерал класу самородних напівметалів, найстійкіший у земній корі кристалічний різновид вуглецю. Структура шарувата. Колір чорний, сірий. Сингонія гексагональна. Графіт — темно-сіра непрозора речовина, алотропна форма вуглецю. На відміну від алмазу графіт добре проводить електричний струм і тепло та дуже м'який. Графіт належить до найбільш легкофлотованих мінералів, але його флотованість залежить від величини кристалів, характеру домішок та ступеня окиснення поверхні. Флотацію графіту звичайно проводять з використанням гасу і спінювача у лужному або кислотному середовищі, яке створюється содою, вапном або сірчаною кислотою. Природний аполярний характер кристалів графіту, їхня луската форма і мала густина обумовлюють легку флотованість графіту і дозволяю (uk)</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>Graphite (en)</li> <li style="display:none;">غرافيت (ar)</li> <li style="display:none;">Grafit (ca)</li> <li style="display:none;">Grafit (cs)</li> <li style="display:none;">Graphit (de)</li> <li style="display:none;">Γραφίτης (el)</li> <li style="display:none;">Grafito (eo)</li> <li style="display:none;">Grafito (es)</li> <li style="display:none;">Grafito (eu)</li> <li style="display:none;">Graifít (ga)</li> <li style="display:none;">Grafit (in)</li> <li style="display:none;">Graphite (fr)</li> <li style="display:none;">Grafite (it)</li> <li style="display:none;">グラファイト (ja)</li> <li style="display:none;">흑연 (ko)</li> <li style="display:none;">Grafiet (nl)</li> <li style="display:none;">Grafit (pl)</li> <li style="display:none;">Grafite (pt)</li> <li style="display:none;">Графит (ru)</li> <li style="display:none;">Grafit (sv)</li> <li style="display:none;">Графіт (uk)</li> <li style="display:none;">石墨 (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.037vk" href="http://rdf.freebase.com/ns/m.037vk">freebase:Graphite</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://d-nb.info/gnd/4158067-9" href="http://d-nb.info/gnd/4158067-9">http://d-nb.info/gnd/4158067-9</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://commons.dbpedia.org/resource/Graphite" href="http://commons.dbpedia.org/resource/Graphite">dbpedia-commons:Graphite</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://www.wikidata.org/entity/Q5309" 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resource="http://commons.wikimedia.org/wiki/Special:FilePath/CaC6structure.jpg" href="http://commons.wikimedia.org/wiki/Special:FilePath/CaC6structure.jpg">wiki-commons:Special:FilePath/CaC6structure.jpg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Crane’s_Servants_Friend_series_no._3.jpg" href="http://commons.wikimedia.org/wiki/Special:FilePath/Crane’s_Servants_Friend_series_no._3.jpg">wiki-commons:Special:FilePath/Crane’s_Servants_Friend_series_no._3.jpg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-233436.jpg" href="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-233436.jpg">wiki-commons:Special:FilePath/Graphite-233436.jpg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-layers-side-3D-balls.png" href="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-layers-side-3D-balls.png">wiki-commons:Special:FilePath/Graphite-layers-side-3D-balls.png</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-layers-top-3D-balls.png" href="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-layers-top-3D-balls.png">wiki-commons:Special:FilePath/Graphite-layers-top-3D-balls.png</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-pV.svg" href="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-pV.svg">wiki-commons:Special:FilePath/Graphite-pV.svg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Graphite-unit-cell-3D-balls.png" 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href="http://commons.wikimedia.org/wiki/Special:FilePath/Naturalis_Biodiversity_Center_-_Museum_-_Exhibition_Nature_theatre_08_-_Graphite,_large_stone.jpg">wiki-commons:Special:FilePath/Naturalis_Biodiversit...heatre_08_-_Graphite,_large_stone.jpg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Pencils_hb.jpg" href="http://commons.wikimedia.org/wiki/Special:FilePath/Pencils_hb.jpg">wiki-commons:Special:FilePath/Pencils_hb.jpg</a></li> <li><a class="uri" rel="foaf:depiction" resource="http://commons.wikimedia.org/wiki/Special:FilePath/“Orgy_of_the_Growl_Devils_“_“Graphited_Wood_Grease”_1908_ad_-_Electric_railway_review_(IA_electricrailwayr19amer)_(page_50_crop).jpg" 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