[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:470929":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":6,"elements":14,"sigelements":19,"key_elements":6,"impurities":6,"cim":6,"ima_status":20,"ima_notes":6,"ima_history":6,"approval_year":6,"publication_year":6,"discovery_year":6,"strunz10ed1":22,"strunz10ed2":23,"strunz10ed3":24,"strunz10ed4":6,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":25,"cclass":26,"spacegroup":27,"spacegroupset":28,"a":29,"b":30,"c":31,"alpha":6,"beta":32,"gamma":6,"aerror":33,"berror":34,"cerror":35,"alphaerror":6,"betaerror":36,"gammaerror":6,"va3":6,"z":33,"csmetamict":12,"commentcrystal":37,"twinning":6,"tranglide":6,"parting":6,"epitaxidescription":6,"morphology":6,"tlform":38,"hmin":35,"hmax":39,"hardtype":6,"vhnmin":6,"vhnmax":6,"vhnerror":6,"vhng":6,"vhns":6,"commenthard":6,"dmeas":40,"dmeas2":6,"dcalc":41,"dmeaserror":11,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":42,"commentluster":6,"diapheny":6,"streak":6,"colour":43,"commentcolor":6,"colors":44,"streak_colors":6,"luminescence":6,"uv":6,"cleavage":45,"cleavagetype":46,"fracturetype":47,"tenacity":48,"commentbreak":6,"opticaltype":49,"opticalsign":6,"opticalalpha":50,"opticalalpha2":6,"opticalalphaerror":11,"opticalbeta":51,"opticalbeta2":6,"opticalbetaerror":11,"opticalgamma":52,"opticalgamma2":6,"opticalgammaerror":53,"opticalomega":6,"opticalomega2":6,"opticalomegaerror":6,"opticalepsilon":6,"opticalepsilon2":6,"opticalepsilonerror":6,"opticaln":6,"opticaln2":6,"opticalnerror":6,"optical2vcalc":6,"optical2vcalc2":6,"optical2vcalcerror":6,"optical2vmeasured":54,"optical2vmeasured2":6,"optical2vmeasurederror":53,"rimin":55,"rimax":56,"opticaldispersion":57,"opticalpleochroism":58,"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":59,"industrial":6,"occurrence":60,"otheroccurrence":6,"type_specimen_store":61,"description_short":62,"aboutname":63,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":64,"reviewed_at":6,"variety_of":6,"varieties":65,"group_members":66,"associates":67,"confused_with":68,"type_localities":69,"occurrence_total":11,"citations":76,"images":87,"structures":88,"synonyms":89,"language_names":92,"wikidata_qid":101,"texts":102},470929,"1:1:470929:5",null,"Sarvodaite","Svd",0,"mineral",2,false,"Al\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>·5H\u003Csub>2\u003C\u002Fsub>O",[15,16,17,18],"Al","O","S","H",[15,16,17,18],[21],"APPROVED","7","C","B","Monoclinic",5,15,"0","5.4862","10.8029","20.841","96.416",4,8,1,7,"Space Group P21\u002Fn","white spherolites of thin colorless prismatic crystals up to 500 μm in maximum dimension",1.5,"2.33","2.349","Vitreous","white",[43],"{100}","Perfect","Splintery","brittle","Biaxial","1.529","1.537","1.545",3,"90",1.529,1.545,"is weak, r > v","Non-pleochroic","The mineral is non-soluble in water and ethanol and dissolves\r\nslowly at room temperature in HCl.","Sarvodaite is a fumarolic mineral formed directly from gas from a natural underground coal fire.","collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 6041\u002F1","Known synthetic analogue. The lower-hydrate counterpart of alunogen and meta-alunogen. The higher-hydrate counterpart of UM1976-22-SO:AlFeH. Yet another hydrate counterpart of millosevichite (the anhydrate phase of aluminum sulfate).","The new mineral is named after the ancient Sarvoda fortress, the remains of which are situated in the vicinity to the place where sarvodaite was found, the village of Zeravshan-Sarvoda. In the Middle Ages, this fortress served as an outpost on the route to the \"burning mines\", which were referred to by various names at different eras (Kan-Tag, Ravat, Kukhi-Malik). The region was the source of the extraction of ammonia, native sulfur, potassium nitrate, alum, and iron sulfate from ancient times until the mid-40s of the 20th century.","2026-04-14 13:23:44",[],[],[],[],[70],{"id":71,"txt":72,"latitude":73,"longitude":74,"country":75},122085,"Kukhi-Malik tract, Fan-Jagnob coal deposit, Ayni District, Sughd, Tajikistan",39.1952124,68.5708352,"Tajikistan",[77,82],{"id":78,"year":79,"html":80,"doi":81},16954804,2023,"Bosi, Ferdinando, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2023) Newsletter 76. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 1-5 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2023.89'>doi:10.1180\u002Fmgm.2023.89\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fservices\u002Faop-cambridge-core\u002Fcontent\u002Fview\u002F4A99F4833FEF3FA8AC6BEE25185C4D4D\u002FS0026461X23000890a.pdf\u002Fnewsletter-76.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fmgm.2023.89",{"id":83,"year":84,"html":85,"doi":86},19100876,2025,"Makhmadsharif, Saimudasir; Pautov, Leonid A.; Siidra, Oleg I.; Mirakov, Mirak A.; Karpenko, Vladimir Yu.; Shodibekov, Manuchekhr A. (2025) Sarvodaite Al2(SO4)3⸱5H2O, a new mineral from the Fan-Yagnob coal deposit, Tajikistan. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 1-19 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2025.10165'>doi:10.1180\u002Fmgm.2025.10165\u003C\u002Fa>","10.1180\u002Fmgm.2025.10165",[],[],[90,91],"Sarvodaiet","Unnamed (Al Sulphate-Hydrate)",[93,97],{"lang":94,"names":95},"ca",[96],"sarvodaïta",{"lang":98,"names":99},"de",[100],"Sarvodait","Q123998412",{"history":6,"applications":6}]