[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:38700":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":11,"ima_formula":16,"elements":17,"sigelements":21,"key_elements":22,"impurities":11,"cim":11,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":11,"discovery_year":11,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":29,"dana8ed1":30,"dana8ed2":31,"dana8ed3":31,"dana8ed4":11,"csystem":32,"cclass":11,"spacegroup":11,"spacegroupset":33,"a":34,"b":35,"c":36,"alpha":11,"beta":37,"gamma":11,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":38,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":39,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":40,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":41,"colour":41,"commentcolor":11,"colors":42,"streak_colors":44,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":45,"description_short":46,"aboutname":47,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":48,"reviewed_at":11,"variety_of":11,"varieties":49,"group_members":50,"associates":66,"confused_with":67,"type_localities":68,"occurrence_total":75,"citations":76,"images":100,"structures":101,"synonyms":102,"language_names":106,"wikidata_qid":124,"texts":125},38700,"1:1:38700:2","642b20fe-6fb3-4613-9e9c-527564b5f408","Paulscherrerite","Psc",0,"mineral",null,40555,34,false,"UO\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","(UO\u003Csub>2\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>",[18,19,20],"O","H","U",[18,19,20],[20],[24],"APPROVED",2008,"4","G","A","20","5","2","Monoclinic","0","4.281","10.230","6.865","90.35","pseudo-orthorhombic","Powdery, pseudomorphs.  intimately admixed with significant amounts of metaschoepite","6.66","canary yellow",[43],"yellow",[43],"Holotype material (G31382) is deposited in the South Australian Museum, North Terrace, 5000 Adelaide, Australia, and cotype material (MGL 79287) in the Musée Géologique, UNIL-Anthropole, 1015 Lausanne, Switzerland.","Occurs as a dehydration product of metaschoepite.\r\nPreviously, generally called 'dehydrated schoepite.'","Named in 2011 by Joël Brugger, Nicolas Meisser, Barbara Etschmann, Stefan Ansermet, Allan Pring in honor of Paul Scherrer [February 3, 1890 Saint Gallen, Switzerland – September 25, 1969 Zürich, Switzerland], Swiss physicist, professor of experimental physics in the Eidgenössische Technische Hochschule of Zürich, Switzerland, and president of the Swiss Atomic Energy Commission. In 1918, together with Paul Debye, he developed a technique for crystal structure determination by X-ray diffraction on powders (Debye-Scherrer technique). He is also known for the Scherrer equation, which describes the dependence of line broadening of reflected X-rays on crystal size for small particles.","2026-04-18 16:17:19",[],[51,57],{"id":52,"name":53,"entrytype":9,"csystem":54,"ima_formula":55,"mindat_formula":56,"hmin":11,"hmax":11,"dmeas":33,"dcalc":33,"primary_image_id":11},2684,"Metaschoepite","Orthorhombic","(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>12\u003C\u002Fsub> &middot; 10H\u003Csub>2\u003C\u002Fsub>O","(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>12\u003C\u002Fsub>&middot;10H\u003Csub>2\u003C\u002Fsub>O",{"id":58,"name":59,"entrytype":9,"csystem":54,"ima_formula":60,"mindat_formula":61,"hmin":62,"hmax":62,"dmeas":63,"dcalc":64,"primary_image_id":65},3574,"Schoepite","(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>O(OH)\u003Csub>6\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>","(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>12\u003C\u002Fsub>&middot;12H\u003Csub>2\u003C\u002Fsub>O",2.5,"4.8","4.918",78506,[],[],[69],{"id":70,"txt":71,"latitude":72,"longitude":73,"country":74},16646,"Mount Painter No. 2 workings, Mount Painter area, Arkaroola (Arkaroola Wilderness Sanctuary; Arkaroola Station), Pastoral Unincorporated Area, South Australia, Australia",-30.2208333,139.3322222,"Australia",3,[77,82,86,91,96],{"id":78,"year":79,"html":80,"doi":81},13253746,1997,"Finch, Robert J., Hawthorne, Frank C., Miller, M. L., Ewing, R. C. (1997) Distinguishing among schoepite, [(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>12\u003C\u002Fsub>](H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>12\u003C\u002Fsub>, and related minerals by X-ray powder diffraction. \u003Ci>Powder Diffraction\u003C\u002Fi>,  12 (4) 230-238 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1017\u002Fs0885715600009799'>doi:10.1017\u002Fs0885715600009799\u003C\u002Fa>","10.1017\u002Fs0885715600009799",{"id":83,"year":84,"html":85,"doi":11},16137539,1998,"Finch, R.J., Hawthorne, F.C. and Ewing, R.C. (1998): Structural relations among schoepite, metaschoepite and \"dehydrated schoepite\". Canadian Mineralogist 36, 831-845.",{"id":87,"year":88,"html":89,"doi":90},9391519,1999,"Sowder, A. G., Clark, S. B., Fjeld, R. A. (1999) The Transformation of Uranyl Oxide Hydrates:  The Effect of Dehydration on Synthetic Metaschoepite and Its Alteration to Becquerelite. \u003Ci>Environmental Science & Technology\u003C\u002Fi>, 33 (20). 3552-3557 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1021\u002Fes9901516'>doi:10.1021\u002Fes9901516\u003C\u002Fa>","10.1021\u002Fes9901516",{"id":92,"year":93,"html":94,"doi":95},396691,2011,"Brugger, J., Meisser, N., Etschmann, B., Ansermet, S., Pring, A. (2011) Paulscherrerite from the Number 2 Workings, Mount Painter Inlier, Northern Flinders Ranges, South Australia: \"Dehydrated schoepite\" is a mineral after all. \u003Ci>American Mineralogist\u003C\u002Fi>,  96 (2) 229-240 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2011.3601'>doi:10.2138\u002Fam.2011.3601\u003C\u002Fa>","10.2138\u002Fam.2011.3601",{"id":97,"year":98,"html":99,"doi":11},16966603,2021,"(2021) Paulscherrerite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FPaulscherrerite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[103,104,105],"Dehydrated schoepite","IMA2008-022","Paulscherreriet",[107,111,116,120],{"lang":108,"names":109},"ca",[110],"paulscherrerita",{"lang":112,"names":113},"de",[114,115],"IMA 2008-022","Paulscherrerit",{"lang":117,"names":118},"eu",[119],"Paulscherrerita",{"lang":121,"names":122},"it",[123],"paulscherrerite","Q7155354",{"history":11,"applications":11}]