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Phenomenon:OxidationofIron Thissimpledemonstrationcanbeusedasa phenomenonduringaunitonchemicalweatheringof rockstoactivatestudentthinkingabouthowchemical reactionsmaychangerocksattheEarth’ssurface. Oxidationisachemicalreactionwhereanelement lossesoneormoreelectronsandresultsinan increaseinitsoxidationstate(ex.Fe2+→Fe3+).For example,ironrustformswhenironisoxidized (formingironoxide).Thetopimageshowsthe oxidationofironnailsformingrust.Theoxidationof ironandtheformationofironoxidesisresponsible fortherustyredcolorcommonlyfoundin sedimentaryrockssuchasthesandstoneinthe secondimage.Somemineralsinrocks(suchasolivine, pyroxeneandmagnetite)containironandoxidizein thepresenceofoxygenfromtheatmosphereand waterattheEarth’ssurface.Theoxidationofironis acceleratedinthepresenceofacidandsalt. Inthisdemonstration,soakapieceoffinesteelwool invinegarandapinchofsaltforafewminutes. NationalParkServicePhoto Shakeofftheexcessvinegarandinsertthesteelwool intoanErlenmeyerflask(1000mlflaskworkswell).Putaballoonontopoftheflasktosealthe steelwoolinsidetheflask(bottomleftfigure).Afteraboutanhour,theballoonwillbedrawn downintotheflaskastheoxygenintheair reactswiththeironinthesteelwoolto formironoxide(bottomrightfigure).This activitydemonstratesthatironreactswith oxygenintheatmospheretoformiron oxide.Likewise,iron-bearingmineralsin theEarth’scrustmayreactwithoxygento formironoxide.Aftertheexperiment,the steelwoolcanberemovedfromtheflask. Itwillbenoticeablyrustyinappearance duetotheoxidationofironandthe formationofironoxide.