. . . . "\u0426\u0435\u0440\u0443\u0441\u0441\u0438\u0301\u0442, \u0431\u0435\u043B\u0430\u044F \u0441\u0432\u0438\u043D\u0446\u043E\u0432\u0430\u044F \u0440\u0443\u0434\u0430 \u2014 \u043C\u0438\u043D\u0435\u0440\u0430\u043B, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u0430, \u0446\u0435\u043D\u043D\u0430\u044F \u0441\u0432\u0438\u043D\u0446\u043E\u0432\u0430\u044F \u0440\u0443\u0434\u0430. \u041D\u0430\u0437\u0432\u0430\u043D\u0438\u0435 \u043F\u0440\u043E\u0438\u0441\u0445\u043E\u0434\u0438\u0442 \u043E\u0442 \u0434\u0440.-\u0433\u0440\u0435\u0447. \u03BA\u03B7\u03C1\u03CC\u03C2 \u2014 \u0432\u043E\u0441\u043A, \u043B\u0430\u0442. cerussa \u2014 \u0431\u0435\u043B\u0438\u043B\u0430, \u043F\u043E \u0441\u0445\u043E\u0436\u0435\u0441\u0442\u0438 \u0446\u0432\u0435\u0442\u0430 (\u043F\u0440\u0435\u0436\u0434\u0435 \u0446\u0435\u0440\u0443\u0441\u0441\u0438\u0442 \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u043E\u0432\u0430\u043B\u0441\u044F \u0432 \u043A\u043E\u0441\u043C\u0435\u0442\u0438\u043A\u0435 \u043A\u0430\u043A \u043F\u0443\u0434\u0440\u0430), \u0434\u0430\u043D\u043E \u0432 1845 \u0433\u043E\u0434\u0443 \u0430\u0432\u0441\u0442\u0440\u0438\u0439\u0441\u043A\u0438\u043C \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0433\u043E\u043C \u0412. \u0413\u0430\u0439\u0434\u0438\u043D\u0433\u0435\u0440\u043E\u043C."@ru . "Pnma [62]"@en . "\u0426\u0435\u0440\u0443\u0441\u0438\u0301\u0442, \u0431\u0456\u043B\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430 \u2014 \u043C\u0456\u043D\u0435\u0440\u0430\u043B, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u044E \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438.; \u0446\u0456\u043D\u043D\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430. \u0412\u0456\u0434 \u043B\u0430\u0442. cerussa \u2014 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0456 \u0431\u0456\u043B\u0438\u043B\u0430 (W.K.Haidinger, 1845). \u0421\u0438\u043D\u043E\u043D\u0456\u043C\u0438: \u0431\u0456\u043B\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430, \u0430\u043A\u0440\u0443\u0437\u0438\u0442, \u0448\u043F\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0438\u0439."@uk . "Brittle conchoidal"@en . "Massive granular, reticulate, tabular to equant crystals"@en . "\u0426\u0435\u0440\u0443\u0441\u0441\u0438\u0442"@ru . "Adamantine, vitreous, resinous"@en . . . . "Cerussit, PbCO3, \u00E4r ett av best\u00E5ende mineral med 77,5% bly (83,5 % PbO). Dess densitet \u00E4r 6,5 och h\u00E5rdhet enligt Moh 3,5. Mineralet \u00E4r starkt gl\u00E4nsande och starkt ljusbrytande med f\u00E4rgl\u00F6st streck. Det \u00E4r en ganska vanlig, god , som ofta p\u00E5 grund av en mindre silverhalt, ocks\u00E5 \u00E4r en viktig . F\u00F6rekomster finns p\u00E5 flera platser i Mellan- och Sydeuropa samt Tunisien, Marocko, Namibia, USA och Australien."@sv . . "Kerusit (dari bahasa Latin cerussa artinya \"timbal putih\"), adalah mineral yang terdiri dari timbal karbonat, PbCO3, dan merupakan bijih timbal yang penting. Pada 1565 senyawa ini disebut cerussa nativa (oleh ), pada 1832 menamainya cruse, sedangkan nama kerusit (cerussite) dimulai oleh . Wikimedia Commons memiliki media mengenai Cerussite."@in . . . "Cerussite"@en . "280"^^ . . . "Kerusit (dari bahasa Latin cerussa artinya \"timbal putih\"), adalah mineral yang terdiri dari timbal karbonat, PbCO3, dan merupakan bijih timbal yang penting. Pada 1565 senyawa ini disebut cerussa nativa (oleh ), pada 1832 menamainya cruse, sedangkan nama kerusit (cerussite) dimulai oleh . Kerusit umum terdapat dalam bentuk kristal. Kerusit mengkristal dalam sistem dan ber dengan aragonit. Mirip seperti aragonit, kerusit juga sering mengalami , dan berbentuk pseudo-heksagonal. Tiga kristal biasanya berkembar pada dua muka prisma, menghasilkan kelompok bergaris-enam dengan masing-masing kristal saling bersilangan dengan sudut sekitar 60\u00B0. Kristal kerusit biasanya memiliki penampilan yang terang dan halus. Kerusit juga terdapat dalam bentuk kelompok butiran yang kompak, atau kadang-kadang dalam bentuk serat. Biasanya kerusit berwarna putih atau tidak berwarna, kadang-kadang juga abu-abu atau kehijauan. Mineral ini sangat rapuh, dan memiliki retakan . Mineral ini memiliki tingkat kekerasan 3 hingga 3.75 dalam skala Mohs, dan massa jenis 6.5 g/cm3. Iglesiasit adalah kerusit yang memiliki kandungan 7% seng karbonat, dinamai menurut tempatnya ditemukan, yaitu Iglesias di Sardinia. Senyawa ini dikenali melalui pengembarannya yang khas, serta sifat pemantulan cahayanya yang disebut adamantine lustre, serta massa jenisnya yang tinggi. Mineral ini tidak larut dalam air, namun larut dalam asam nitrat encer berbuih. Dalam tes blowpipe, mineral ini melebur dengan cepat, yang mengindikasikan kandungan timbal. Wikimedia Commons memiliki media mengenai Cerussite."@in . . . "Cerusit"@cs . "\u039F \u03BA\u03B5\u03C1\u03BF\u03C5\u03C3\u03AF\u03C4\u03B7\u03C2 (\u03B1\u03B3\u03B3\u03BB. cerussite) \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B1\u03BD\u03B8\u03C1\u03B1\u03BA\u03B9\u03BA\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC \u03C4\u03BF\u03C5 \u03BC\u03BF\u03BB\u03CD\u03B2\u03B4\u03BF\u03C5. \u03A4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03BF\u03C5 \u03C0\u03C1\u03BF\u03AD\u03C1\u03C7\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BB\u03B1\u03C4\u03B9\u03BD\u03B9\u03BA\u03AE \u03BB\u03AD\u03BE\u03B7 cerussa, \u03C0\u03BF\u03C5 \u03C3\u03B7\u03BC\u03B1\u03AF\u03BD\u03B5\u03B9 \u00AB\u03BB\u03B5\u03C5\u03BA\u03CC\u03C2 \u03BC\u03CC\u03BB\u03C5\u03B2\u03B4\u03BF\u03C2\u00BB. \u03A3\u03C4\u03B7\u03BD \u03B1\u03B3\u03B3\u03BB\u03BF\u03C3\u03B1\u03BE\u03BF\u03BD\u03B9\u03BA\u03AE \u03B2\u03B9\u03B2\u03BB\u03B9\u03BF\u03B3\u03C1\u03B1\u03C6\u03AF\u03B1 \u03B1\u03BD\u03B1\u03C6\u03AD\u03C1\u03B5\u03C4\u03B1\u03B9, \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2, \u03BA\u03B1\u03B9 \u03C9\u03C2 \"Horn Silver\" \u03BA\u03B1\u03B9 \"Lead spar\", \u03B5\u03BD\u03CE \u03C3\u03C5\u03C7\u03BD\u03AC \u03B1\u03BD\u03B1\u03B3\u03C1\u03AC\u03C6\u03B5\u03C4\u03B1\u03B9 (\u03B5\u03C3\u03C6\u03B1\u03BB\u03BC\u03AD\u03BD\u03B1) \u03BA\u03B1\u03B9 \"cerrussite\" \u03BA\u03B1\u03B9 \"cerusite\"."@el . . . . . "Cerussite"@en . . "La cerussita \u00E9s un mineral de la classe dels carbonats. Wilhelm Karl von Haidinge li va donar nom el 1845 del llat\u00ED cerussa ('blanc de plom'). Pertany al grup de l'aragonita."@ca . "\u0426\u0435\u0440\u0443\u0441\u0438\u0301\u0442, \u0431\u0456\u043B\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430 \u2014 \u043C\u0456\u043D\u0435\u0440\u0430\u043B, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u044E \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438.; \u0446\u0456\u043D\u043D\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430. \u0412\u0456\u0434 \u043B\u0430\u0442. cerussa \u2014 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0456 \u0431\u0456\u043B\u0438\u043B\u0430 (W.K.Haidinger, 1845). \u0421\u0438\u043D\u043E\u043D\u0456\u043C\u0438: \u0431\u0456\u043B\u0430 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0430 \u0440\u0443\u0434\u0430, \u0430\u043A\u0440\u0443\u0437\u0438\u0442, \u0448\u043F\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u0435\u0432\u0438\u0439."@uk . . . . "Cerussit, PbCO3, \u00E4r ett av best\u00E5ende mineral med 77,5% bly (83,5 % PbO). Dess densitet \u00E4r 6,5 och h\u00E5rdhet enligt Moh 3,5. Mineralet \u00E4r starkt gl\u00E4nsande och starkt ljusbrytande med f\u00E4rgl\u00F6st streck. Det \u00E4r en ganska vanlig, god , som ofta p\u00E5 grund av en mindre silverhalt, ocks\u00E5 \u00E4r en viktig . F\u00F6rekomster finns p\u00E5 flera platser i Mellan- och Sydeuropa samt Tunisien, Marocko, Namibia, USA och Australien."@sv . "Cerusit je koso\u010Dtvere\u010Dn\u00FD miner\u00E1l V. t\u0159\u00EDdy (karbon\u00E1ty), z \u0159ady aragonitu, s n\u00EDm\u017E je izotypn\u00ED, chemicky jde o uhli\u010Ditan olovnat\u00FD (PbCO3), m\u00EDsty hojn\u00FD. Pojmenoval jej Fran\u00E7ois Sulpice Beudant (1832) podle latinsk\u00E9ho slova cerussa, kter\u00E9 v roce 1565 pou\u017Eil Konrad Gessner pro olovnatou b\u011Blobu. Vysok\u00FD obsah olova (t\u00E9m\u011B\u0159 78 %) se projevuje zna\u010Dnou m\u011Brnou hmotnost\u00ED."@cs . . "\u039A\u03B5\u03C1\u03BF\u03C5\u03C3\u03AF\u03C4\u03B7\u03C2"@el . . "\u0627\u0644\u0633\u064A\u0631\u0648\u0633\u064A\u062A \u064A\u062A\u0643\u0648\u0646 \u0627\u0644\u0645\u0639\u062F\u0646 \u0645\u0646 \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0631\u0635\u0627\u0635 \u0648\u0647\u0648 \u0633\u0647\u0644 \u0627\u0644\u0627\u0646\u0635\u0647\u0627\u0631 \u0648\u064A\u0639\u0637\u064A \u0639\u0646\u062F \u062A\u0633\u062E\u064A\u0646\u0647 \u0645\u0639 \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0635\u0648\u062F\u064A\u0648\u0645 \u0639\u0644\u0649 \u0645\u0643\u0639\u0628 \u0627\u0644\u0641\u062D\u0645 \u0643\u0631\u0629 \u0635\u063A\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0631\u0635\u0627\u0635."@ar . "Cerussit, auch unter seiner bergm\u00E4nnischen Bezeichnung Wei\u00DFbleierz bekannt, ist ein h\u00E4ufig vorkommendes Mineral aus der Mineralklasse der \u201ECarbonate und Nitrate\u201C mit der chemischen Zusammensetzung Pb[CO3] und ist damit chemisch gesehen Blei(II)-carbonat. Cerussit kristallisiert im orthorhombischen Kristallsystem und entwickelt meist prismatische, plattige oder pyramidale Kristalle, aber auch feink\u00F6rnige bis derbe, b\u00FCschelige, ger\u00FCstartige und pulvrige Mineral-Aggregate. Durch Zwillingsbildung entstehen zudem pseudohexagonale Kristallformen mit oft gitterartiger Struktur."@de . "Cerussit"@sv . "\u0426\u0435\u0440\u0443\u0441\u0438\u0442"@uk . . . "Cerussit"@de . "Cerussita karbonato motako minerala da eta aragonite taldearen kidea da."@eu . . . . "\u03B4 = 0.273"@en . . . "Simple or cyclic contact twins"@en . "Cerusit je koso\u010Dtvere\u010Dn\u00FD miner\u00E1l V. t\u0159\u00EDdy (karbon\u00E1ty), z \u0159ady aragonitu, s n\u00EDm\u017E je izotypn\u00ED, chemicky jde o uhli\u010Ditan olovnat\u00FD (PbCO3), m\u00EDsty hojn\u00FD. Pojmenoval jej Fran\u00E7ois Sulpice Beudant (1832) podle latinsk\u00E9ho slova cerussa, kter\u00E9 v roce 1565 pou\u017Eil Konrad Gessner pro olovnatou b\u011Blobu. Vysok\u00FD obsah olova (t\u00E9m\u011B\u0159 78 %) se projevuje zna\u010Dnou m\u011Brnou hmotnost\u00ED."@cs . "Cer"@en . . "Cerussite"@en . "Cerusita"@es . "La cerusita (conocida como sin\u00F3nimo del carbonato de plomo o mena blanca de plomo) es un mineral del grupo V seg\u00FAn la clasificaci\u00F3n de Strunz, consistente en carbonato de plomo (PbCO3), y constituye una de las menas m\u00E1s importantes del elemento plomo. El nombre procede etimol\u00F3gicamente del lat\u00EDn cerussa (\"plomo blanco\"). El mineral se conoce desde muy antiguo, fue mencionado por el naturalista suizo Conrad von Gesner en 1565, y en 1832 por Fran\u00E7ois Sulpice Beudant aplicado el nombre ceruse al mineral, mientras que la actual forma, cerusita se debe a W. Haidinger en 1845."@es . . . . . . . "Cerusyt"@pl . . "Cerusyt (gr. keros \u2013 \"wosk\"; \u0142ac. cereus \u2013 \"o barwie wosku\" lub cerrusa \u2013 \"bia\u0142y o\u0142\u00F3w\") \u2013 rzadki minera\u0142 z grupy w\u0119glan\u00F3w."@pl . . . "617624"^^ . . "\u767D\u94C5\u77FF"@zh . . . . "Cerussita karbonato motako minerala da eta aragonite taldearen kidea da."@eu . "Transparent to translucent"@en . . "1123735621"^^ . . "Cerussit, auch unter seiner bergm\u00E4nnischen Bezeichnung Wei\u00DFbleierz bekannt, ist ein h\u00E4ufig vorkommendes Mineral aus der Mineralklasse der \u201ECarbonate und Nitrate\u201C mit der chemischen Zusammensetzung Pb[CO3] und ist damit chemisch gesehen Blei(II)-carbonat. Cerussit kristallisiert im orthorhombischen Kristallsystem und entwickelt meist prismatische, plattige oder pyramidale Kristalle, aber auch feink\u00F6rnige bis derbe, b\u00FCschelige, ger\u00FCstartige und pulvrige Mineral-Aggregate. Durch Zwillingsbildung entstehen zudem pseudohexagonale Kristallformen mit oft gitterartiger Struktur. In reiner Form ist Cerussit farblos und durchsichtig. Durch vielfache Lichtbrechung aufgrund von Gitterbaufehlern oder polykristalliner Ausbildung kann er aber auch wei\u00DF erscheinen und durch Fremdbeimengungen eine hellgelbe, rauch- bis dunkelgraue oder schwarze Farbe annehmen, wobei die Transparenz entsprechend abnimmt. Seine Strichfarbe ist allerdings immer wei\u00DF. Mit einer Mohsh\u00E4rte von 3 bis 3,5 geh\u00F6rt Cerussit zu den mittelharten Mineralen, die sich \u00E4hnlich wie das Referenzmineral Calcit noch mit einer Kupferm\u00FCnze ritzen lassen."@de . . . . . "La c\u00E9rusite (ou cerussite) est une esp\u00E8ce min\u00E9rale compos\u00E9e de carbonate naturel de plomb de formule (PbCO3), pouvant contenir comme impuret\u00E9s des traces de Sr, Zn, Cu ; cristallisant dans le syst\u00E8me cristallin orthorhombique, groupe d'espace Pmcn. La c\u00E9rusite est normalement presque membre terminal pur, le calcium pouvant remplacer le plomb jusqu'\u00E0 3 mol % environ.C'est un min\u00E9ral hautement toxique car le plomb de ce compos\u00E9 devient en phase de digestion (ou dans un sol acide) tr\u00E8s bio accessible et bioassimilable ."@fr . . . "\u767D\u94C5\u77FF\uFF08\u82F1\u8A9E\uFF1ACerussite\uFF09\u662F\u4E00\u79CD\u7531\u78B3\u9178\u94C5\uFF08PbCO3\uFF09\u7EC4\u6210\u7684\u77FF\u7269\uFF0C\u662F\u4E00\u79CD\u91CD\u8981\u7684\u94C5\u77FF\u77F3\u3002\u767D\u94C5\u77FF\u7684\u82F1\u6587\u540D\u6765\u81EA\u62C9\u4E01\u8BED\u201Ccerussa\u201D\uFF0C\u610F\u4E3A\u201C\u767D\u94C5\u201D\u3002 \u767D\u94C5\u77FF\u4EE5\u659C\u65B9\u6676\u7CFB\u7ED3\u6676\uFF0C\u4E0E\u9730\u77F3\u540C\u6676\u3002\u50CF\u971E\u77F3\u4E00\u6837\uFF0C\u5B83\u7ECF\u5E38\u4EA7\u751F\u5B6A\u6676\uFF0C\u590D\u5408\u6676\u4F53\u5448\u5047\u516D\u89D2\u5F62\u3002\u4E09\u4E2A\u6676\u4F53\u901A\u5E38\u5728\u68F1\u955C\u7684\u4E24\u4E2A\u9762\u4E0A\u5B6A\u751F\u5728\u4E00\u8D77\uFF0C\u4EA7\u751F\u516D\u5C04\u7EBF\u661F\u72B6\u7FA4\uFF0C\u5404\u4E2A\u6676\u4F53\u4EE5\u63A5\u8FD160\u00B0\u7684\u89D2\u5EA6\u4EA4\u53C9\u3002\u6676\u4F53\u7ECF\u5E38\u51FA\u73B0\uFF0C\u5B83\u4EEC\u901A\u5E38\u5177\u6709\u975E\u5E38\u660E\u4EAE\u548C\u5149\u6ED1\u7684\u8868\u9762\u3002\u8BE5\u77FF\u7269\u8FD8\u4EE5\u81F4\u5BC6\u7684\u9897\u7C92\u72B6\u5B58\u5728\uFF0C\u6709\u65F6\u4EE5\u7EA4\u7EF4\u72B6\u5F62\u5F0F\u5B58\u5728\u3002\u8BE5\u77FF\u7269\u901A\u5E38\u4E3A\u65E0\u8272\u6216\u767D\u8272\uFF0C\u6709\u65F6\u5448\u7070\u8272\u6216\u7EFF\u8272\uFF0C\u4ECE\u900F\u660E\u5230\u534A\u900F\u660E\u4E0D\u7B49\uFF0C\u5E26\u6709\u91D1\u521A\u5149\u6CFD\u3002\u5B83\u975E\u5E38\u8106\uFF0C\u5E76\u4E14\u6709\u8D1D\u58F3\u72B6\u65AD\u53E3\u3002\u5B83\u7684\u83AB\u6C0F\u786C\u5EA6\u4E3A3 - 3.75\uFF0C\u6BD4\u91CD\u4E3A6.5\u3002 \u8BE5\u77FF\u7269\u53EF\u4EE5\u901A\u8FC7\u5176\u7279\u6709\u7684\u5B6A\u6676\u7279\u5F81\u4EE5\u53CA\u91D1\u521A\u5149\u6CFD\u548C\u9AD8\u6BD4\u91CD\u6765\u8F7B\u677E\u8BC6\u522B\u3002\u5728\u7A00\u785D\u9178\u4E2D\u8D77\u6CE1\u6EB6\u89E3\u3002\u4F1A\u5BFC\u81F4\u5B83\u5F88\u5BB9\u6613\u7194\u65AD\uFF0C\u5E76\u7ED9\u51FA\u94C5\u7684\u6307\u793A\u3002 \u767D\u94C5\u77FF\u7ECF\u5E38\u88AB\u5927\u91CF\u53D1\u73B0\uFF0C\u94C5\u542B\u91CF\u9AD8\u8FBE77.5%\u3002"@zh . "7830"^^ . . . . "La cerusita (conocida como sin\u00F3nimo del carbonato de plomo o mena blanca de plomo) es un mineral del grupo V seg\u00FAn la clasificaci\u00F3n de Strunz, consistente en carbonato de plomo (PbCO3), y constituye una de las menas m\u00E1s importantes del elemento plomo. El nombre procede etimol\u00F3gicamente del lat\u00EDn cerussa (\"plomo blanco\"). El mineral se conoce desde muy antiguo, fue mencionado por el naturalista suizo Conrad von Gesner en 1565, y en 1832 por Fran\u00E7ois Sulpice Beudant aplicado el nombre ceruse al mineral, mientras que la actual forma, cerusita se debe a W. Haidinger en 1845."@es . . "La c\u00E9rusite (ou cerussite) est une esp\u00E8ce min\u00E9rale compos\u00E9e de carbonate naturel de plomb de formule (PbCO3), pouvant contenir comme impuret\u00E9s des traces de Sr, Zn, Cu ; cristallisant dans le syst\u00E8me cristallin orthorhombique, groupe d'espace Pmcn. La c\u00E9rusite est normalement presque membre terminal pur, le calcium pouvant remplacer le plomb jusqu'\u00E0 3 mol % environ.C'est un min\u00E9ral hautement toxique car le plomb de ce compos\u00E9 devient en phase de digestion (ou dans un sol acide) tr\u00E8s bio accessible et bioassimilable ."@fr . . . . "May fluoresce yellow under LW UV"@en . . . "Cerussite"@it . "C\u00E9rusite"@fr . "Dipyramidal"@en . "n\u03B1 = 1.803, n\u03B2 = 2.074, n\u03B3 = 2.076"@en . "Spencer"@en . . . . . "Het mineraal cerussiet is een lood(II)carbonaat met de chemische formule PbCO3."@nl . . . . . . "\u767D\u94C5\u77FF\uFF08\u82F1\u8A9E\uFF1ACerussite\uFF09\u662F\u4E00\u79CD\u7531\u78B3\u9178\u94C5\uFF08PbCO3\uFF09\u7EC4\u6210\u7684\u77FF\u7269\uFF0C\u662F\u4E00\u79CD\u91CD\u8981\u7684\u94C5\u77FF\u77F3\u3002\u767D\u94C5\u77FF\u7684\u82F1\u6587\u540D\u6765\u81EA\u62C9\u4E01\u8BED\u201Ccerussa\u201D\uFF0C\u610F\u4E3A\u201C\u767D\u94C5\u201D\u3002 \u767D\u94C5\u77FF\u4EE5\u659C\u65B9\u6676\u7CFB\u7ED3\u6676\uFF0C\u4E0E\u9730\u77F3\u540C\u6676\u3002\u50CF\u971E\u77F3\u4E00\u6837\uFF0C\u5B83\u7ECF\u5E38\u4EA7\u751F\u5B6A\u6676\uFF0C\u590D\u5408\u6676\u4F53\u5448\u5047\u516D\u89D2\u5F62\u3002\u4E09\u4E2A\u6676\u4F53\u901A\u5E38\u5728\u68F1\u955C\u7684\u4E24\u4E2A\u9762\u4E0A\u5B6A\u751F\u5728\u4E00\u8D77\uFF0C\u4EA7\u751F\u516D\u5C04\u7EBF\u661F\u72B6\u7FA4\uFF0C\u5404\u4E2A\u6676\u4F53\u4EE5\u63A5\u8FD160\u00B0\u7684\u89D2\u5EA6\u4EA4\u53C9\u3002\u6676\u4F53\u7ECF\u5E38\u51FA\u73B0\uFF0C\u5B83\u4EEC\u901A\u5E38\u5177\u6709\u975E\u5E38\u660E\u4EAE\u548C\u5149\u6ED1\u7684\u8868\u9762\u3002\u8BE5\u77FF\u7269\u8FD8\u4EE5\u81F4\u5BC6\u7684\u9897\u7C92\u72B6\u5B58\u5728\uFF0C\u6709\u65F6\u4EE5\u7EA4\u7EF4\u72B6\u5F62\u5F0F\u5B58\u5728\u3002\u8BE5\u77FF\u7269\u901A\u5E38\u4E3A\u65E0\u8272\u6216\u767D\u8272\uFF0C\u6709\u65F6\u5448\u7070\u8272\u6216\u7EFF\u8272\uFF0C\u4ECE\u900F\u660E\u5230\u534A\u900F\u660E\u4E0D\u7B49\uFF0C\u5E26\u6709\u91D1\u521A\u5149\u6CFD\u3002\u5B83\u975E\u5E38\u8106\uFF0C\u5E76\u4E14\u6709\u8D1D\u58F3\u72B6\u65AD\u53E3\u3002\u5B83\u7684\u83AB\u6C0F\u786C\u5EA6\u4E3A3 - 3.75\uFF0C\u6BD4\u91CD\u4E3A6.5\u3002 \u8BE5\u77FF\u7269\u53EF\u4EE5\u901A\u8FC7\u5176\u7279\u6709\u7684\u5B6A\u6676\u7279\u5F81\u4EE5\u53CA\u91D1\u521A\u5149\u6CFD\u548C\u9AD8\u6BD4\u91CD\u6765\u8F7B\u677E\u8BC6\u522B\u3002\u5728\u7A00\u785D\u9178\u4E2D\u8D77\u6CE1\u6EB6\u89E3\u3002\u4F1A\u5BFC\u81F4\u5B83\u5F88\u5BB9\u6613\u7194\u65AD\uFF0C\u5E76\u7ED9\u51FA\u94C5\u7684\u6307\u793A\u3002 \u767D\u94C5\u77FF\u7ECF\u5E38\u88AB\u5927\u91CF\u53D1\u73B0\uFF0C\u94C5\u542B\u91CF\u9AD8\u8FBE77.5%\u3002"@zh . "762"^^ . "\u0633\u064A\u0631\u0648\u0633\u064A\u062A"@ar . . . . . . . . "Cerusyt (gr. keros \u2013 \"wosk\"; \u0142ac. cereus \u2013 \"o barwie wosku\" lub cerrusa \u2013 \"bia\u0142y o\u0142\u00F3w\") \u2013 rzadki minera\u0142 z grupy w\u0119glan\u00F3w."@pl . . . "Het mineraal cerussiet is een lood(II)carbonaat met de chemische formule PbCO3."@nl . . . . "\u0627\u0644\u0633\u064A\u0631\u0648\u0633\u064A\u062A \u064A\u062A\u0643\u0648\u0646 \u0627\u0644\u0645\u0639\u062F\u0646 \u0645\u0646 \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0631\u0635\u0627\u0635 \u0648\u0647\u0648 \u0633\u0647\u0644 \u0627\u0644\u0627\u0646\u0635\u0647\u0627\u0631 \u0648\u064A\u0639\u0637\u064A \u0639\u0646\u062F \u062A\u0633\u062E\u064A\u0646\u0647 \u0645\u0639 \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0635\u0648\u062F\u064A\u0648\u0645 \u0639\u0644\u0649 \u0645\u0643\u0639\u0628 \u0627\u0644\u0641\u062D\u0645 \u0643\u0631\u0629 \u0635\u063A\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0631\u0635\u0627\u0635."@ar . "Biaxial"@en . "Leonard James"@en . "Cerussite"@en . . . "La cerussita \u00E9s un mineral de la classe dels carbonats. Wilhelm Karl von Haidinge li va donar nom el 1845 del llat\u00ED cerussa ('blanc de plom'). Pertany al grup de l'aragonita."@ca . "6.53"^^ . "Cerussite (also known as lead carbonate or white lead ore) is a mineral consisting of lead carbonate (PbCO3), and is an important ore of lead. The name is from the Latin cerussa, white lead. Cerussa nativa was mentioned by Conrad Gessner in 1565, and in 1832 F. S. Beudant applied the name c\u00E9ruse to the mineral, whilst the present form, cerussite, is due to W. Haidinger (1845). Miners' names in early use were lead-spar and white-lead-ore. Lead(II) carbonate is practically insoluble in neutral water (solubility product [Pb2+][CO32\u2212] \u2248 1.5\u00D710\u221213 at 25 \u00B0C), but will dissolve in dilute acids."@en . . . . . . "La cerussite \u00E8 un minerale costituito da carbonato di piombo appartenente al gruppo dell'aragonite."@it . . . "Good [110] and [021]"@en . . "Cerussiet"@nl . . . . "Lead carbonate: PbCO3"@en . "Cerussita"@ca . "\u039F \u03BA\u03B5\u03C1\u03BF\u03C5\u03C3\u03AF\u03C4\u03B7\u03C2 (\u03B1\u03B3\u03B3\u03BB. cerussite) \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B1\u03BD\u03B8\u03C1\u03B1\u03BA\u03B9\u03BA\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC \u03C4\u03BF\u03C5 \u03BC\u03BF\u03BB\u03CD\u03B2\u03B4\u03BF\u03C5. \u03A4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03BF\u03C5 \u03C0\u03C1\u03BF\u03AD\u03C1\u03C7\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BB\u03B1\u03C4\u03B9\u03BD\u03B9\u03BA\u03AE \u03BB\u03AD\u03BE\u03B7 cerussa, \u03C0\u03BF\u03C5 \u03C3\u03B7\u03BC\u03B1\u03AF\u03BD\u03B5\u03B9 \u00AB\u03BB\u03B5\u03C5\u03BA\u03CC\u03C2 \u03BC\u03CC\u03BB\u03C5\u03B2\u03B4\u03BF\u03C2\u00BB. \u03A3\u03C4\u03B7\u03BD \u03B1\u03B3\u03B3\u03BB\u03BF\u03C3\u03B1\u03BE\u03BF\u03BD\u03B9\u03BA\u03AE \u03B2\u03B9\u03B2\u03BB\u03B9\u03BF\u03B3\u03C1\u03B1\u03C6\u03AF\u03B1 \u03B1\u03BD\u03B1\u03C6\u03AD\u03C1\u03B5\u03C4\u03B1\u03B9, \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2, \u03BA\u03B1\u03B9 \u03C9\u03C2 \"Horn Silver\" \u03BA\u03B1\u03B9 \"Lead spar\", \u03B5\u03BD\u03CE \u03C3\u03C5\u03C7\u03BD\u03AC \u03B1\u03BD\u03B1\u03B3\u03C1\u03AC\u03C6\u03B5\u03C4\u03B1\u03B9 (\u03B5\u03C3\u03C6\u03B1\u03BB\u03BC\u03AD\u03BD\u03B1) \u03BA\u03B1\u03B9 \"cerrussite\" \u03BA\u03B1\u03B9 \"cerusite\"."@el . "5"^^ . . . "White"@en . . . . . . "Colorless, white, gray, blue, or green"@en . "Cerussita"@eu . "3"^^ . . "La cerussite \u00E8 un minerale costituito da carbonato di piombo appartenente al gruppo dell'aragonite."@it . . . . . . "Leonard James Spencer"@en . . . . . . "Cerussite (also known as lead carbonate or white lead ore) is a mineral consisting of lead carbonate (PbCO3), and is an important ore of lead. The name is from the Latin cerussa, white lead. Cerussa nativa was mentioned by Conrad Gessner in 1565, and in 1832 F. S. Beudant applied the name c\u00E9ruse to the mineral, whilst the present form, cerussite, is due to W. Haidinger (1845). Miners' names in early use were lead-spar and white-lead-ore. Cerussite crystallizes in the orthorhombic crystal system and is isomorphous with aragonite. Like aragonite it is very frequently twinned, the compound crystals being pseudo-hexagonal in form. Three crystals are usually twinned together on two faces of the prism, producing six-rayed stellate groups with the individual crystals intercrossing at angles of nearly 60\u00B0. Crystals are of frequent occurrence and they usually have very bright and smooth faces. The mineral also occurs in compact granular masses, and sometimes in fibrous forms. The mineral is usually colorless or white, sometimes grey or greenish in tint and varies from transparent to translucent with an adamantine lustre. It is very brittle, and has a conchoidal fracture. It has a Mohs hardness of 3 to 3.75 and a specific gravity of 6.5. A variety containing 7% of zinc carbonate, replacing lead carbonate, is known as iglesiasite, from Iglesias in Sardinia, where it is found. The mineral may be readily recognized by its characteristic twinning, in conjunction with the adamantine lustre and high specific gravity. It dissolves with effervescence in dilute nitric acid. A blowpipe test will cause it to fuse very readily, and gives indications for lead. Finely crystallized specimens have been obtained from the Friedrichssegen mine in Lahnstein in Rhineland-Palatinate, Johanngeorgenstadt in Saxony, St\u0159\u00EDbro in the Czech Republic, Phoenixville in Pennsylvania, Broken Hill in New South Wales, and several other localities. Delicate acicular crystals of considerable length were found long ago in the Pentire Glaze mine near St Minver in Cornwall. Cerussite is often found in considerable quantities, and has a lead content of up to 77.5%. Lead(II) carbonate is practically insoluble in neutral water (solubility product [Pb2+][CO32\u2212] \u2248 1.5\u00D710\u221213 at 25 \u00B0C), but will dissolve in dilute acids."@en . "5"^^ . . . "\u0426\u0435\u0440\u0443\u0441\u0441\u0438\u0301\u0442, \u0431\u0435\u043B\u0430\u044F \u0441\u0432\u0438\u043D\u0446\u043E\u0432\u0430\u044F \u0440\u0443\u0434\u0430 \u2014 \u043C\u0438\u043D\u0435\u0440\u0430\u043B, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442 \u0441\u0432\u0438\u043D\u0446\u0430, \u0446\u0435\u043D\u043D\u0430\u044F \u0441\u0432\u0438\u043D\u0446\u043E\u0432\u0430\u044F \u0440\u0443\u0434\u0430. \u041D\u0430\u0437\u0432\u0430\u043D\u0438\u0435 \u043F\u0440\u043E\u0438\u0441\u0445\u043E\u0434\u0438\u0442 \u043E\u0442 \u0434\u0440.-\u0433\u0440\u0435\u0447. \u03BA\u03B7\u03C1\u03CC\u03C2 \u2014 \u0432\u043E\u0441\u043A, \u043B\u0430\u0442. cerussa \u2014 \u0431\u0435\u043B\u0438\u043B\u0430, \u043F\u043E \u0441\u0445\u043E\u0436\u0435\u0441\u0442\u0438 \u0446\u0432\u0435\u0442\u0430 (\u043F\u0440\u0435\u0436\u0434\u0435 \u0446\u0435\u0440\u0443\u0441\u0441\u0438\u0442 \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u043E\u0432\u0430\u043B\u0441\u044F \u0432 \u043A\u043E\u0441\u043C\u0435\u0442\u0438\u043A\u0435 \u043A\u0430\u043A \u043F\u0443\u0434\u0440\u0430), \u0434\u0430\u043D\u043E \u0432 1845 \u0433\u043E\u0434\u0443 \u0430\u0432\u0441\u0442\u0440\u0438\u0439\u0441\u043A\u0438\u043C \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0433\u043E\u043C \u0412. \u0413\u0430\u0439\u0434\u0438\u043D\u0433\u0435\u0440\u043E\u043C."@ru . "Kerusit"@in . .