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闪锌矿和方铅矿的沉淀顺序:以中国西南铅锌矿床为例(英文) PrecipitationOrderofSphaleriteandGalena:ACaseStudyofSouthwestChinaLead-ZincDeposits Introduction Lead-zincoresareimportantresourcesintheresourcesindustryfortheirvaluablemetals.But,theprecipitationorderofmineralsinlead-zincdepositsisofgreatconcerninthemineralprocessingsector.Inthispaper,wewilldiscusstheprecipitationorderofsphaleriteandgalenawiththesouthwestChinalead-zincdepositsasanexample.Theprecipitationorderissignificant,asitdetermineswhattypesofmethodscanbeusedinmineralseparationandhowtoachieveeffectiveseparationoflead-zincores. GeologicalBackground Thelead-zincdepositsinsouthwestChinamainlyoccurintheUpperPermiansedimentaryrocks.Thedepositsmainlyconsistofsixtypesofmineralization,includingvein-type,stratiform,replacement,cave-filling,sedimentary,andresidual.Thesphaleriteandgalenaarethemostimportantminerals.Thesphaleriteisrichinzinc,whereasgalenaisrichinlead.Thesetwomineralsaretypicallyassociatedwitheachother,whichmakestheseparationoftheleadandzincmineralsdifficult. PrecipitationOrderofSphaleriteandGalena Theprecipitationorderofsphaleriteandgalenainthelead-zincdepositshasbeenstudiedextensively.Accordingtoresearch,theprecipitationofsphaleritegenerallyprecedestheprecipitationofgalena.Thisordercanbeexplainedbasedontheprinciplesofthermodynamics.SphaleritehasalowerGibbsfreeenergythangalena,whichmeansthatitismorestableandwillformfirst.Theprecipitationofsphaleritealsoconsumesmoreoftheavailablemetalionsandleavesfewerionsavailabletoformgalena. Ingeneral,therearethreemainfactorsthataffecttheprecipitationorderofsphaleriteandgalena:temperature,metalconcentration,andpHvalue.Highertemperaturespromotetheprecipitationofgalena,whereaslowertemperaturespromotetheprecipitationofsphalerite.Ahighermetalconcentrationleadstotheformationofmoresulfideminerals,includingsphaleriteandgalena.AhigherpHvaluealsopromotestheprecipitationofgalena,whereaslowerpHvaluespromotetheprecipitationofsphalerite. ImplicationforMineralProcessing Inmineralprocessing,theprecipitationo

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