[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:470773":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":6,"synid":6,"polytypeof":6,"groupid":6,"weighting":11,"nolocadd":12,"blacklisted":12,"mindat_formula":13,"mindat_formula_note":6,"ima_formula":14,"elements":15,"sigelements":20,"key_elements":6,"impurities":6,"cim":6,"ima_status":21,"ima_notes":6,"ima_history":23,"approval_year":24,"publication_year":6,"discovery_year":6,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":6,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":28,"cclass":29,"spacegroup":29,"spacegroupset":30,"a":31,"b":32,"c":33,"alpha":34,"beta":35,"gamma":36,"aerror":37,"berror":38,"cerror":39,"alphaerror":40,"betaerror":40,"gammaerror":29,"va3":41,"z":29,"csmetamict":12,"commentcrystal":6,"twinning":6,"tranglide":6,"parting":6,"epitaxidescription":6,"morphology":42,"tlform":43,"hmin":6,"hmax":6,"hardtype":6,"vhnmin":6,"vhnmax":6,"vhnerror":6,"vhng":6,"vhns":6,"commenthard":6,"dmeas":6,"dmeas2":6,"dcalc":44,"dmeaserror":6,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":45,"commentluster":6,"diapheny":6,"streak":46,"colour":47,"commentcolor":6,"colors":48,"streak_colors":50,"luminescence":6,"uv":51,"cleavage":52,"cleavagetype":53,"fracturetype":6,"tenacity":54,"commentbreak":6,"opticaltype":55,"opticalsign":56,"opticalalpha":57,"opticalalpha2":6,"opticalalphaerror":37,"opticalbeta":58,"opticalbeta2":6,"opticalbetaerror":37,"opticalgamma":59,"opticalgamma2":6,"opticalgammaerror":60,"opticalomega":6,"opticalomega2":6,"opticalomegaerror":6,"opticalepsilon":6,"opticalepsilon2":6,"opticalepsilonerror":6,"opticaln":6,"opticaln2":6,"opticalnerror":6,"optical2vcalc":61,"optical2vcalc2":6,"optical2vcalcerror":6,"optical2vmeasured":62,"optical2vmeasured2":6,"optical2vmeasurederror":63,"rimin":64,"rimax":65,"opticaldispersion":6,"opticalpleochroism":6,"opticalpleochorismdesc":6,"opticalbirefringence":6,"opticalcomments":6,"opticalcolour":6,"opticalinternal":6,"opticaltropic":6,"opticalanisotropism":6,"opticalbireflectance":6,"opticalextinction":6,"opticalr":6,"specdispm":6,"ir":6,"electrical":6,"magnetism":6,"thermalbehaviour":6,"other":66,"industrial":6,"occurrence":67,"otheroccurrence":6,"type_specimen_store":68,"description_short":69,"aboutname":70,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":71,"reviewed_at":6,"variety_of":6,"varieties":72,"group_members":73,"associates":74,"confused_with":75,"type_localities":76,"occurrence_total":29,"citations":83,"images":92,"structures":103,"synonyms":110,"language_names":113,"wikidata_qid":125,"texts":126},470773,"1:1:470773:4",null,"Batoniite","Bato",0,"mineral",7,false,"Al\u003Csub>8\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>14\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>18\u003C\u002Fsub>·5H\u003Csub>2\u003C\u002Fsub>O","Al\u003Csub>8\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>14\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>18\u003C\u002Fsub> · 5H\u003Csub>2\u003C\u002Fsub>O",[16,17,18,19],"Al","O","S","H",[16,17,18,19],[22],"APPROVED","IMA no. 2023-008",2023,"7","D","A","Triclinic",2,"0","9.1757","12.0886","20.9218","82.901","87.334","86.999",6,9,15,3,2295.7," ","hemispherical aggregates composed of brittle tabular crystals, up to 1 mm in size","1.949","Vitreous,Greasy","white","white to colorless",[46,49],"colorless",[46],"none"," shows a {011} perfect cleavage; there are other less distinct cleavage surfaces, but their crystallographic orientation was not determined.","Perfect","very brittle","Biaxial","-","1.4833","1.4948","1.5019",5,"75.8","71",1,1.4833,1.5019,"Batoniite is slowly soluble in H2O; it is affected by dehydration of under chamber vacuum.\r\n\r\n","action of H2SO4 on Al-bearing rocks of Paleozoic age","collections of the Museo di Storia Naturale, Università di Pisa, Via Roma 79, Calci (PI), Italy, catalogue number 20028","New structure type. Among the most structurally complex minerals to date (see also: ewingite, morrisonite, and ilmajokite-(Ce)).\r\n\r\nBears a most likely unique octameric [Al8(OH)14(H2O)18]10+ cluster.\r\n\r\nIts genesis is likely due to interaction of sulfu...","Named in honour of Massimo Batoni (born 6 April 1948), vice-president of AMI - Associazione Micromineralogica Italiana.","2025-08-11 12:15:25",[],[],[],[],[77],{"id":78,"txt":79,"latitude":80,"longitude":81,"country":82},2164,"Le Cetine di Cotorniano mine, Chiusdino, Siena Province, Tuscany, Italy",43.231978,11.1682997,"Italy",[84,88],{"id":85,"year":24,"html":86,"doi":87},16099192,"Bosi, Ferdinando; Hatert, Frédéric; Pasero, Marco; Mills, Stuart J. (2023) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 73. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  35 (3). 397-402 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-35-397-2023'>doi:10.5194\u002Fejm-35-397-2023\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F35\u002F397\u002F2023\u002Fejm-35-397-2023.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-35-397-2023",{"id":89,"year":24,"html":90,"doi":91},17062578,"Mauro, Daniela, Biagioni, Cristian, Sejkora, Jiří, Dolníček, Zdeněk, Škoda, Radek (2023) Batoniite, [Al\u003Csub>8\u003C\u002Fsub>(OH)\u003Csub>14\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>18\u003C\u002Fsub>](SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>  ⋅  5H\u003Csub>2\u003C\u002Fsub>O, a new mineral with the [Al\u003Csub>8\u003C\u002Fsub>(OH)\u003Csub>14\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>18\u003C\u002Fsub>]\u003Csup>10+\u003C\u002Fsup> polyoxocation from the Cetine di Cotorniano Mine, Tuscany, Italy. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  35 (5) 703-714 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-35-703-2023'>doi:10.5194\u002Fejm-35-703-2023\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F35\u002F703\u002F2023\u002Fejm-35-703-2023.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-35-703-2023",[93],{"id":94,"source_url":95,"license_code":96,"credit_html":97,"title":98,"description":99,"author":100,"original_width":101,"original_height":102},2853,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=136759374","CC BY 4.0","Daniela Mauro, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=136759374\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Batoniite.jpg","Batoniite, aggregate of white tabular crystals with colorless prismatic crystals of gypsum and orange-brown resinous unidentified Al–Fe sulfate. Garibaldi Tunnel, Cetine di Cotorniano Mine, Chiusdino, Siena, Tuscany, Italy. Type material. Catalogue number 20028, Museo di Storia Naturale, Università di Pisa. Photo: Daniela Mauro.","Daniela Mauro",2067,2544,[104],{"id":105,"url":106,"label":107,"formula":108,"spacegroup":109,"year":24},1298,"\u002Fcif\u002F1298.cif","Mauro 2023","Al8 S5 O57 H60","P -1",[111,112],"Batoniiet","IMA2023-008",[114,118,122],{"lang":115,"names":116},"ca",[117],"batoniïta",{"lang":119,"names":120},"de",[121],"Batoniit",{"lang":123,"names":124},"it",[7],"Q120333830",{"history":6,"applications":6}]