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Co–Mn-oxide spinel catalysts for CO and propane
oxidation at mild temperature
Benjamin Faure, Pierre Alphonse
To cite this version:
Benjamin Faure, Pierre Alphonse. Co–Mn-oxide spinel catalysts for CO and propane oxidation at
mild temperature. Applied Catalysis B: Environmental, Elsevier, 2016, vol. 180, pp. 715-725.
�10.1016/j.apcatb.2015.07.019�. �hal-01308137�
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Eprints ID : 14529
To link to this article : DOI : 10.1016/j.apcatb.2015.07.019
URL :
http://dx.doi.org/10.1016/j.apcatb.2015.07.019
To cite this version : Faure, Benjamin and Alphonse, Pierre
Co–Mn-oxide spinel catalysts for CO and propane oxidation at mild
temperature. (2016) Applied Catalysis B: Environmental, vol. 180. pp.
715-725. ISSN 0926-3373
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Co–Mn-oxide
spinel
catalysts
for
CO
and
propane
oxidation
at
mild
temperature
Benjamin
Faure
faure.benjamin.n@gmail.com,
Pierre
Alphonse
∗CIRIMAT-UPS,UniversitédeToulouse,118routedeNarbonne31062Toulousecedex09,France
Keywords: Mixedoxalate Cobaltitespinel Totaloxidation Propane VOCsremoval
a
b
s
t
r
a
c
t
CoxMn3−xO4oxides(0≤x≤3)werepreparedbycontrolleddecompositionofmixedoxalatesnear200◦C,
followedbyacalcinationat300◦C.Theseoxidesareamorphousforx<0.9.Forhighercobaltfractionthey
haveacubicspinelstructureandtheircrystallitesizegrowswiththecobaltfraction.Thesematerials havealargesurfacearea;thehighestvalues,exceeding250m2/g,wereobtainedforx≈2.Thespinel
oxidesexhibitanoutstandingcatalyticactivityforpropaneoxidationatmildtemperature(20–200◦C).
TheyarealsoactiveforCOoxidationatambienttemperature.Thishighactivitywascorrelatedbothwith thesurfaceareaandthecobaltconcentration.ThemostefficientmaterialisCo2,3Mn0,7O4,whichhasa
betteractivitythancobaltoxidecatalystsreportedintheliterature.
1. Introduction
Catalyticoxidationisaveryeffectivemethodfortheabatement oflowconcentrationsofVolatileOrganicCompounds(VOCs). Cur-rently,themostactivecatalystsaresupportednoblemetals[1–3]. Howeverthesecatalystsareveryexpensiveandtheiractivitycanbe stronglyinhibitedbyCO[4],waterorchloride[5].Forlow tempera-tureapplications,likeVOCsremovalinindoorair,preciousmetals canbereplacedbytransitionmetaloxides[6].Especiallyspinel cobaltoxide(Co3O4)wasreportedtobethebestcatalystforthe totaloxidationofCO[7]andhydrocarbons[6,8].Spineloxides,with thegeneralformulaAB2O4,containcationsitesofdifferent coordi-nation(tetrahedralandoctahedral)withtheoxideanionsarranged in a cubicclose-packed lattice.Partialsubstitution of cobaltby
manganesegivesmixedCo–Mnspineloxides,whichcanbebetter
catalyststhanCo3O4fortheoxidationofVOCs[9–11].
Mostoftenthecatalystsreportedintheliteratureare synthe-sizedathightemperature(>500◦C).Thisrequirement,unavoidable
for automotive catalytic converters, becomes useless for VOCs
abatementatmildtemperature(<300◦C).Actuallyitisexpected thatmetastablenanocrystalline oxides,withverylargeporosity andsurfacearea,willbehighlyactivecatalysts.Thiskindof
mate-rialscanbeeasilyobtainedbythermaldecomposition ofmetal
oxalates.Indeedaclosecontrolofthedecompositionallows
prepar-∗ Correspondingauthor.
E-mailaddress:alphonse@chimie.ups-tlse.fr(P.Alphonse).
ing mixed oxides with very high surface area (300–500m2/g)
[12,13].Moreoverthiseasyandinexpensivemethodisalsovery convenienttoobtainmixedoxides[14].
Thegoalofthisstudywasthesynthesisoflargesurfacearea CoxMn3−xO4 oxides (0≤x≤ 3) by controlled decomposition of
mixedoxalates and theevaluationof thecatalytic performance
of these metastable materialsfor the total oxidation of carbon
monoxideandpropaneatmildtemperature(20–200◦C).Carbon
monoxideisproducedinlargeamountbytransportation,industrial anddomesticactivities.Itisextremelytoxicandcatalytic oxida-tionintoCO2 constitutesthebestsolutionforCO removalfrom indoorair[7].Thuslowcost,preciousmetalfreecatalysts,
work-ingatroomtemperaturearehighlydemanded.Propaneislargely
usedasdomesticandindustrialfuel.Besidesitisalsothethirdmost commonmotorvehiclefuelintheworldbehindgasolineandDiesel fuel.Ontheotherhanditisgenerallyadmittedthatalkanesarethe leastreactiveamongVOCsandacatalystabletoremovepropaneat mildtemperaturesisexpectedtobeactiveforotherVOCsaswell.
2. Experimental
2.1. Synthesisofoxides
2.1.1. Preparationofmixedoxalates
MixedoxalatesCox/3Mn(3−x)/3C2O4.2H2Owereprecipitatedat
roomtemperaturebyquickintroductionofanaqueoussolution
ofcobaltandmanganesenitrates(200mL;0.2M)intoanaqueous
solution of ammonium oxalate (200mL; 0.22M) under
ousstirring.After30min,theprecipitatewasfiltered,thoroughly washedwithdeionizedwateranddriedinairat70◦C.
2.1.2. Thermaldecompositionofoxalates
Thethermaldecompositionofoxalateswascarriedoutina ver-ticaltubularfixed-bedflowreactorunderatmosphericpressure. Theinternaldiameterofreactorwas1cm.Theflowrateoftheinlet gas(4%O2inAr)was100cm3/min.Theoutletgascompositionwas
followedusingamassspectrometer(HPR20-QICfromHiden
Ana-lytical).ThetemperatureofthereactingsolidwasrecordedbyaK
thermocouplepositionedinsidethepowderedsample.Thissetup
allowedcontrollingboth thetemperatureofthereacting
mate-rialandthecompositionoftheatmosphere.Thetemperaturewas
increasedat2.5◦C/minuntilCO
2emissionwasdetected;fromthen
thedecompositionwasdoneinisothermalconditions.For
exam-ple,inthecaseofmanganeseoxalatethistemperaturewasabout
210◦C.WhenCO
2emissionwasover,toensureatotal decompo-sition,eveninthecoreofparticles,thepartialpressureofO2was
augmentedgraduallyto20%;thenthetemperaturewasincreased
at5◦C/minupto300◦Candmaintainedtothisvaluefor1h.
2.2. Thermalanalysis(TGA-DSC)
Thethermaldecompositionofoxalateswasstudiedby
thermo-gravimetricanalysis(TGA)anddifferentialscanningcalorimetry (DSC),usinga constantheatingrate(5◦C/min),ona TGA-DSC-1
Mettler–Toledodevicein thetemperaturerange30–600◦C. The
flowinggaswasamixture20%O2inAr.About5mgofoxalate
pow-derwereplacedina40mLaluminiumpanandthereferencewas
anemptyaluminiumpan.
2.3. PowderX-raydiffraction(PXRD)
ThecrystalstructurewasinvestigatedviapowderX-ray diffrac-tion.Datawascollected,atroomtemperature,withaBrukerAXS
D4–2 diffractometer,in theBragg–Brentanogeometry,using
filteredCuKaradiationandagraphitesecondary-beam monochro-mator.Diffractionintensitiesweremeasuredbyscanningfrom20 to80◦(2)withastepsizeof0.02◦(2).
Aquantitativeestimationofthelatticeparametersand peak
broadeningwasaccomplishedbyprofilefittingofthewholeXRD
patternsusingtheFullprofsoftware[15].Thepeakprofileswere
modeledbyThompson-Cox-Hastings[16]pseudo-Voigtfunctions.
The parameters refined were zero shift (2), background, cell
parametersandpeakshape.Thesizeandstraincontributiontothe integralbreadthofeachreflectionwerecalculatedbythesoftware.
Theinstrumentalbroadeningcontributionwasevaluatedbyusing
ana-aluminasample(NISTStandardReferenceMaterial1976b).
Thestructuralchangesversustemperaturewerefollowedby
HighTemperatureX-rayDiffraction(HTXRD)withaBrukerAXSD8
diffractometer(usingNi-filteredCuKaradiation)equippedwith
ahightemperaturechamber AntonPaarHTK1200N. Diffraction
intensitieswererecordedinsyntheticairflow(20%O2inN2),at fixedtemperature,every10◦C,intherange100–500◦C.The
heat-ingratebetweeneach stepwas10◦C/min.Thetime neededto
recordeachpatternwasabout15min.
2.4. Specificsurfacearea,poresizedistribution
Specificsurfaceareaandporesizedistributionwerecalculated fromnitrogenadsorption-desorptionisothermscollectedat77K, usinganadsorptionanalyzer(MicromeriticsTristarII3020).The
specificsurfaceareaswerecomputedfromadsorptionisotherms,
usingtheBrunauer–Emmett–Teller(BET)method[17].Thepore
sizedistributions(PSD)werecomputedfromdesorptionisotherms
bytheNLDFTmethod[18](withQuantachromeAutosorb-1
soft-wareusingsilicaequilibriumtransitionkernelat77K,basedona cylindricalporemodel).
Porevolume(Vpore)wascalculatedfromtheadsorbedvolume atarelativepressureof0.995(Vsat)by:
Vpore=
N2gasdensity N2liq.densityVsat
=0.00155Vsat
Priortoanalysis,toremovethespeciesadsorbedonthesurface, theoxalatesamples(about0.5g)weredegassedfor16hat70◦C whereastheoxidesamples(about0.1g)weredegassedfor16hat 90◦C(finalpressure<10−3Pa).
2.5. Electronmicroscopy
Transmission electron microscopy analyses were performed
withaJeolJEM-1400operatingat80kV.Sampleswereprepared
byputtingadropofanethanolsuspensionofparticlesona carbon-coatedcoppergrid.
Scanningelectronmicroscopyanalyseswereperformedwitha
SEMFEGFEIQuanta-250at20kV.Thesampleswerepreparedby
puttingadropofanethanolsuspensionofparticlesonanaluminum
sampleholder.Beforeanalysis,thesampleswerecoveredwitha
thinlayer(5nm)ofPtbysputtercoating.
2.6. ChemicalanalysisbyX-rayfluorescence
Theelementalcompositionwasdeterminedonpowder
sam-plesbyX-rayfluorescencewithaBrukerS2Rangerworkingwitha
maximumvoltageof50kVandacurrentof2mA.
2.7. Catalytictests
Theactivitiesofcatalystsweretested forCO andC3H8 total oxidation.Thesetestswereperformed,atambientpressure,ina tubularfixedbedflowglassreactor(internaldiameter=6mm).The catalystmasswasalwayscloseto0.05g.Thecatalystpowderwas
packedinthetubegivinga2–3mmbedlength.Thevolumetric
flowratewas1.63mLs−1givingacontacttimeof0.03s.Thesizeof catalystparticleswasabout10mm.Thereactoroperatesat differ-entialconditionsonlyforpropaneoxidation,atmildtemperatures (conversion<10%).Thereactantsweredosedbymassflow
con-trollers (Brooks5850).The catalysttemperaturewascontrolled
byaK-typethermocouplepositionedinsidethecatalystbed.For
COoxidationthetemperaturerangewas30–200◦Candtheinlet
gascompositionwas0.8%CO+20%O2inAr.ForC3H8 oxidation
thetemperaturerangewas30–300◦Candtheinletgas
composi-tionwas0.4%C3H8+20%O2 inAr.Thecatalysttemperaturewas increasedataheatingrateof200◦C/h.Thegasphasecomposition
duringthetestswasmonitoredbymassspectrometry(HPR20-QIC
fromHidenAnalytical).BeforetheCOoxidationtest,thecatalysts werefirstpretreatedwith20%O2inArfor60minat200◦C.The C3H8oxidationtestwasdoneafterCOtestwithoutany pretreat-ment.
3. Resultsanddiscussion
3.1. Characterizationofoxalateprecursors
3.1.1. XRD
TheXRDpattern(Fig.1)ofmanganeseoxalatecorrespondsto themonoclinicstructurewiththespacegroupC2/c(PDF# 00-025-0544)whereascobaltoxalatehastheorthorhombicstructurewith thespacegroupCccm(PDF#00-025-0250).Thestructureofmixed
Co–Mnoxalatesdependsontheirmanganesecontent.Foroxalates
Fig.1. ExamplesofXRDpatternsofCox/3Mn(3−x)/3C2O4.2H2OaftertheprofilefittingwiththeFULLPROFsoftware[15].Theupperpatternswereindexedforthemonoclinic
structure(PDF#00-025-0544)whereasthelowerpatternswereindexedfortheorthorhombicstructure(PDF#00-025-0250).
Table1
StructureparametersofCox/3Mn(3−x)/3C2O4.2H2Odeterminedbyprofilefittingof
XRDpatternswithFULLPROFsoftware[15].Disthecrystallitesize.
x Spacegroup a(nm) b(nm) c(nm) ˇ(◦) D(nm) 0 C2/c 1.200 0.565 0.998 128.3 52 0.6 C2/c 1.197 0.561 0.996 128.2 55 0.9 C2/c 1.194 0.557 0.996 128.1 51 1.6 Cccm 1.192 0.550 1.556 90 15 2.0 Cccm 1.188 0.545 1.557 90 17 2.3 Cccm 1.191 0.546 1.564 90 21 3 Cccm 1.187 0.542 1.557 90 32
structuregives abetteragreementwhereas,whenCoequalsor
exceedsMn,abestfitisobtainedwithorthorhombicstructure.The latticeparametersandthecrystallitesizearereportedinTable1. BothaandblatticeparametersdecreasewhentheproportionofCo increasesindicatingthatthesmallerCo2+ions(r=89pmHS) sub-stituteforthelargerMn2+ions(r=97pmHS).Thecrystallitesize isconstant,atabout50nm,forthemonoclinicstructureanddrops
near20nmwhenthestructurebecomesorthorhombic.However
thecrystallitesizeofcobaltoxalateislarger,atabout30nm,than thatofCo-richmixedoxalates.
3.1.2. Scanningelectronmicroscopy
TheSEMimagesforseveralcompositionsareshowninFig.2.
Theparticlemorphologychangesaccordingtothechemical
com-Table2
BETsurfacearea(SBET)andporevolume(Vpore)ofCox/3Mn(3−x)/3C2O4.2H2O
deter-minedfromN2adsorptionisothermsat77K.
x SBET(m2/g) CBET Vpore(cm3/g)
0 26±2 130 0.095±0.008 0.6 2.4±0.2 120 0.010±0.001 0.9 4.0±0.3 130 0.030±0.002 1.6 5.0±0.4 150 0.062±0.005 2.0 4.4±0.3 110 0.044±0.003 2.3 6.0±0.5 160 0.074±0.005 3 4.0±0.3 170 0.024±0.002
position.Theparticlesofmanganeserichoxalates(upperimages) areveryirregularinsizeandshapewhereastheparticlesofcobalt richoxalatesaremoreuniform.Theseparticlesareatleasttentimes largerthanthecrystallitesizedeterminedfromXRD.For2≤x<3 theparticlesaggregateinball-shapedunits(lowerleftimage).We didnotobservesuchaggregatesforcobaltoxalate,whichgivesrod likeparticles(lowerrightimage).
3.1.3. Specificsurfaceareaandporevolume
TheBETsurfacearea(SBET)andporevolume(Vpore)ofoxalates arereportedinTable2.Thesurfaceareasofallthecompounds con-tainingcobaltaresimilar,intherange4–6m2/g.Theyareatleast5 timeslowerthanthesurfaceareaofmanganeseoxalatewhichhas alsothelargestporevolume.Forthisoxalatewesuspectedthatthe
Fig.2. SEMimagesofsomeoxalates.
degassingprocedure(16hat70◦Cinvacuum)inducedthe begin-ningofdehydrationbecausetheonsettemperatureofdehydration waslowerthanformixedoxalates(seeSection3.2.1). Neverthe-lessdoublingtheevacuationtimedidnotchangesignificantlythe texturalproperties.
3.2. Decompositionofoxalateprecursors
3.2.1. Thermalanalysisofoxalatedecomposition
TheTGA-DSCanalysiscurvesforseveralcompositionsare
plot-tedin Fig.3.The decomposition occursin two main separated
stages:below200◦Ctheendothermicdehydrationgivingthe
anhy-drousoxalate,followed bythe exothermicdecomposition near
300◦C. Foran oxalatecontaining2H
2Opermole,themassloss duetodehydrationmustdecreaseslightlyfrom20.1%forx=0to 19.7%forx=3.Weobtaintheexpectedvalueformanganeseoxalate whereasthemasslossisonly19%forcobaltoxalate,indicatinga numberofwatermoleculesslightlylessthan2.Besides,forcobalt
oxalate,theendothermicdehydrationpeakhasasmallshoulder
ontherightsideequivalenttoabout10%ofthewholearea.This
peakisalwayspresentwhateverthemassofsampleanalyzedor
theheatingrate.Itcouldbetheindicationthatwehaveamixture
betweentheorthorhombicformandasmallamountofthe
mono-clinicpolymorphwiththespacegroupC2/c(PDF#00-025-0251)
notdetectedontheXRDpatterns.
Thermaldecompositionoftransitionmetaloxalateshydrates
hasbeenstudiedfor manyyears [19–33].It wasobserved that
the decomposition product for these oxalates depends on the
reducibilityofthemetalliccationinvolved[23,25,32].Withcations
presentingalowreducibility,likeMn2+,thedecompositionleads tothemetaloxidefollowingthereaction:
MnC2O4→MnO+CO+CO21H= 151kJ/mol (1)
WhereasformorereduciblecationslikeCo2+thedecomposition producesthemetal:
CoC2O4→ Co+2CO2H= 94kJ/mol (2)
Howeverinair,CoisoxidizedinCo3O4:
3Co+2O2→ Co3O41H=−891kJ/mol (3)
SimilarlyMnOwillbealsooxidizedinair.Accordingtothe reac-tionconditionstheproductwasreportedasMn3O4[34],Mn2O3
[22,35],MnO2[26]oramorphousMnOx[36].
Moreoverthemanganeseorcobaltoxidesformedareknownto
begoodcatalystsfortheCOoxidation[7]:
CO+1/2O2→ CO21H= −283kJ/mol (4)
Therefore,sincetheseoxidationreactionsareveryexothermic, theoveralldecompositionreactionislargelyexothermictoo.
Theeffectofcobaltfractiononsomecharacteristicsofmixed oxalatedehydrationanddecompositionisillustratedinFig.4.Four featuresarefollowed,theonsettemperatureofdehydration(Ti), thewidthofthedecompositionpeak(in◦C),theenthalpyof
dehy-drationand theenthalpyof decomposition.The upper-leftplot
shows thattheTi ofmixed oxalatesis closetotheTi ofcobalt
oxalate(130◦C) whereas thedehydration ofMn oxalatebegins
atleast30◦Cbelow.Thelower-leftplotshowsthattheenthalpy ofdehydrationis rathersimilarforallthesamplesanalyzed,at
Fig.3.TGA-DSCcurvesforsomeoxalates.
about520J/g(95kJ/moloxalate);onlytheenthalpyobservedfor manganeseoxalateisslightlylower.Thisvalueisveryclosetothe enthalpyreportedbyMaciejewskietal.[30].
Weobservedthattheonsettemperatureofdecomposition
aug-mentslinearly withthe cobalt content of oxalates, goingfrom
230◦C for manganese oxalate to255◦C for cobalt oxalate.The upper-rightplotshowsthatthewidthofthedecompositionpeak, whichislinkedtotherateofthereaction,markedlydecreaseswhen theproportionofcobaltincreases.Neverthelesstheenthalpyof
decomposition,estimatedbyintegrationoftheexothermicpeak,
doesnotrisemuchwiththecobaltfractionasshownbythe lower-rightplot.Thisis confirmedby theredlinein this plot,which
correspondstothe valuescalculated fromthermodynamicdata
(1fH◦298)[37,38]assumingtheformationofanidealsolidsolution havingthespinelstructure(cf.§3.2.2).Thereforewethinkthatthe increaseofthedecompositionratewiththeproportionofcobalt couldbeexplainedbytheveryhighreactivityofmetalcobaltin oxygencontainingatmospheres.Thustoavoidatemperature over-shoot,leadingtoafastgrowthofcrystallites,thedecompositionof cobalt-richoxalatesshallbeperformedinisothermalconditionand lowoxygenpartialpressure.
3.2.2. HT-XRDofoxalatedecomposition
Thethermaldecompositionoftheoxalateswasalsofollowed
byHT-XRD.Thesampleswereheatedbystepof10◦Cat5◦C/min. Takingintoaccountthetimerequiredtorecordeachpattern,the heatingrateontheaveragewasabout0.5◦C/min.Thus,compared withTGA-DSCforwhichtheheatingratewas5◦C/min,apeakshift
towardlowertemperaturecanbeexpected.
TherelevantXRDpatternsforseveralcompositionsareplotted inFig.5.Theupper-leftchartcorrespondstomanganeseoxalate.
Thefirstpattern,recordedat150◦C,correspondstotheanhydrous oxalatewhichhasanorthorhombicstructurewiththespacegroup
Pmna(PDF#00-032-0646).Thisanhydrousoxalatedecomposes
from230◦Ctogiveanamorphousphasewhichcrystallizesonlyat 400◦CincubicMn
2O3(bixbyite)withthespacegroupIa3(PDF#
00-041-1442).Thistransformationgivesasmallexothermalpeak
togetherwithaslightmasslossat450◦ContheTGA-DSCplot(see
Fig.3,x=0).
The upper-right plot corresponds to the mixed oxalate
Co0.2Mn0.8C2O4.2H2O(xCo=0.6).Theanhydrousoxalatepatternis observedfrom140◦C.Likeformanganeseoxalate,thisanhydrous oxalatedecomposesfrom220◦Ctogiveanamorphousphasewhich crystallizesat450◦Cinatetragonallydeformedspinel(spacegroup I41/amd)likeMn3O4(hausmannite,PDF#00-024-0734).Mn3O4 isa “normal”spinelbecauseallMn3+cationsarelocatedin the octahedralsites,givingthecationdistributionMn2+[Mn3+]
2O4[39]. Bordeneuveetal.[40],fromneutrondiffractiondatarecordedon CoxMn3-xO4ceramics,showedthat,forx<1,thesubstitutionoccurs onlyinthetetrahedralsitewhereCo2+replacesMn2+.
Thedeformationofthecubicspinelstructureiscorrelatedwith adistortionofthecoordinationoctahedronaroundMn3+,usually interpretedasaconsequenceofthecooperativeJahn–Tellereffect
[41].
The lattice parameters of hausmannite are a=0.576nm and
c=0.944nm[41].Profilematching(usingFullProfsoftware[15])
gives a=0.575nm and c=0.938nm for the pattern recorded at
450◦Canda=0.576nmandc=0.938nmforthepatternrecordedat 500◦C.Thelowercvalueinoursamplescouldoriginatefrom par-tialoxidationofMn3+intonon-distortingMn4+intheoctahedral sitesbecause,inhausmannitestructure,thecoordination octahe-dronaroundMn3+areelongatedapproximatelyparallelto[001].
Fig.4.EffectofcobaltfractionontheonsettemperatureofdehydrationTi(upper-left),thewidthofthedecompositionpeak(upper-right),theenthalpyofdehydration
(lower-left)andtheenthalpyofdecomposition(lower-right).
Profilematchingalsoprovidesanestimationofthecrystallitesize D;wefoundD=12nmfor450◦CandD=14nmfor500◦C.
Itisworthnoticingthatthecrystallizationobservedat450◦C isassociatedwithasmallmasslossonTGcurvebut,unlike man-ganeseoxalate,givesnodetectablethermalevent(Fig3,x=0.6). Thiscouldbeanindicationthat,inthis case,thecrystallization involvesonlylittlechangeinthestructuralarrangementofatoms, becausetheamorphousstatehasaproto-spinelstructureasitwas
previouslyassumedfornickelmanganitespinelspreparedbylow
temperaturedecompositionofmixedoxalates[42].
The lower-left plot corresponds to the mixed oxalate
Co0.3Mn0.7C2O4.2H2O (x=0.9). The dehydration occurs above
130◦C giving a compound with a XRD pattern similar to the
monocliniccobaltoxalatewiththespacegroupP21/n(PDF#
00-037-0719). This compound decomposes at 240◦C generating a
poorlycrystallinephasecorrespondingtothecubicspinel(space groupFd-3m).Then,from350◦C,thisphaseisprogressively con-vertedinthetetragonalspinel.Profilematchinggivesa=0.574nm, c=0.930nmandD=16nmforthepatternrecordedat500◦C.
Thecriticalconcentrationof distortingMn3+required inthe octahedralsitestotriggertheJahn–Tellereffectisabout55%[41]. Thusthetransientformationofthecubicspinelcouldbeexplained bythepartialoxidation,aftertheoxalatedecomposition,ofmore
than45% of Mn3+ into non-distorting Mn4+
. From 350◦C Mn4+ cationsarereducedinMn3+inducingtheprogressiveconversion inthetetragonalspinel.
Inthecaseofcobaltoxalate(lower-rightplot)thedehydration occursabove140◦C,givingthemonocliniccobaltoxalate(PDF#
00-037-0719),which startstodecomposeat230◦C toyieldthe
cubicspinelCo3O4(spacegroupFd-3m,PDF#00-042-1467). Pro-filematching,forthepatternrecordedat300◦C,givesa=0.809nm andD=12nm.
3.3. Characterizationofoxidesusedascatalysts
3.3.1. XRD
Whatever the decomposition temperature of oxalates, the
oxidesusedascatalystswereheatedinairat300◦Cfor1h.The crystal structure, latticeparameter and crystallite sizeof these materialsarereportedinTable3.Asshownintheprevious sec-tion,theoxidesforwhichx<0.9areamorphous.TheXRDpattern ofCo0.9Mn2.1O4showsverybroadlinescorrespondingtoacubic spinelcompoundbutisistoopoorlycrystallizedtoevaluateitscell parameterandcrystallitesize.Forx>0.9alltheproductshavea cubicspinelstructure.Thecellparametersofthemixedoxidesare slightlylargerthanthecellparameterofCo3O4.Neutrondiffraction dataonceramicsshowedthat,for1<x<2,thetetrahedralsitesare fullyoccupiedbyCo2+andthesubstitutionnowoccursin octahe-dralsiteswhereMn3+isreplacedbothbyCo2+andCo3+bearing inmindthateachCo2+alsoimpliestheoxidationofoneMn3+in Mn4+topreservetheglobalelectroneutrality[40].BecauseCo2+ andMn3+ionshavealargerdiameter(respectively,79and72pm)
Fig.5. XRDpatternsrecordedatincreasingtemperatureduringthedecompositionofoxalatesinair.
thanLSCo3+ions(55pm)itisexpectedthatthecellparameterof mixedoxidesbelargerthanthatofCo3O4.Thebiggestcell param-eterisobservedforx=2probablybecausethisoxidecontainsthe largestamountofCo2+.Furthermoretheincreaseofcobaltcontent isassociatedwithasignificantgrowthofthecrystallite.
3.3.2. Electronmicroscopy
Atmediummagnification,theSEMimagesofoxalatesbefore
and after decomposition are similar as shown in the case of
Co2.3Mn0.7O4 in Fig.6(left andcenter images). Thus, despitea masslosscloseto60%,whenthereactionconditionsallows
con-Table3
Microstructuralandtexturalpropertiesofmixedoxides(CoxMn3−xO4)obtainedafterheatinginairat300◦C.StructuralparameterswasdeterminedbyprofilefittingofXRD
patternswithFULLPROFsoftware[15];Disthecrystallitesize.BETsurfacearea(SBET)andporevolume(Vpore)werecalculatedfromN2adsorptionisothermsat77K.The
valuesofSBETandVporearetheaverageofseveralmeasurements.
x Structure a(nm) D(nm) SBET(m2/g) CBET Vpore(cm3/g)
0 Amorphous 90±5 110 0.16±0.01 0.6 Amorphous 100±10 140 0.21±0.02 0.9 Cubicspinel 230±20 160 0.28±0.03 1.6 Cubicspinel 8.11 6 270±30 50 0.33±0.04 2.0 Cubicspinel 8.12 7 260±30 40 0.48±0.05 2.3 Cubicspinel 8.10 9 220±20 35 0.29±0.03 3 Cubicspinel 8.09 16 60±5 50 0.27±0.01
Fig.6.SEMimagesofCo0.77Mn0.23C2O4.2H2Ooxalate(leftimage)andCo2.3Mn0.7O4oxide(middleimage).TEMmicrographofCo2.3Mn0.7O4oxide(rightimage). trollingthedecompositionrate,theexternalshapeoftheoxalate
particlesiskept.Itispossibleonthecentralmicrographytomake outmanycracksindicatingthattheoxideparticlesarehighly frac-turedbuttheporosityismoreeasilyevidencedontheTEMimage whichclearlyshowsthevoidbetweencrystallites(rightimage). Thecrystallitesizeisin goodagreementwiththesizeobtained
fromXRD.
3.3.3. Specificsurfacearea,porevolumeandporesize
distribution(PSD)
TheBETspecificsurfaceareas(SBET)andtheporevolume(Vpore) ofthematerialsheatedat300◦C,calculatedfromtheN
2
adsorp-tionisotherms,arereportedinTable3.Inthecaseofmixedoxides, weobservethatSBETisstronglydependentofthedecomposition conditionssothat,forseveralpreparationsdoneinsimilar condi-tions,SBETcandifferbyabout20%.Monometallicandamorphous oxideshavethelowestsurfaceandporevolume.ThehighestSBETis obtainedforx≈2;abovethisvaluetheincreaseofcobaltcontentis associatedwithadiminutionofthesurfaceareaandporevolume. Thehighsurfaceareaandporosityofoxidesstronglycontrast withthelowtexturalpropertiesmeasuredonoxalates(seeTable2). Thislargeinterfaceiscreatedbecausethereisalmostno shrink-ageoftheoxalateparticlesinducedbythebigmasslossoccurring
duringdecompositionprocess.
Somerepresentativeisothermsand theirassociatedPSD,
cal-culatedusingNLDFTmethod,areplottedinFig.7.Theporosityof thesematerialspansawiderange,frommicroporestomacropores; howevertheirPSDvariesconsiderablyaccordingtothecobalt frac-tion.Theapproximatecorrelationbetweenthecrystallitesizeand thepositionofthemainpeakofPSDletssupposethatthe meso-porescorrespondtotheinter-crystallitespaces.Theporesinthe
macroporerangeareprobablyduetotheinter-granularporosity
correspondingforexampletothevoidbetweentheparticles. 3.4. Catalyticactivity
Thecatalyticactivityofthemonometallicand mixedoxides,
forCOandC3H8totaloxidation,ispresentedinFig.8.These
mea-surementswerenotdoneatsteadystatebutwithadynamicramp
rateoftemperature(200◦C/h)andon-linemonitoringusingmass
spectrometry.For COoxidation,toreachthemaximumactivity,
thecatalystswereheated ina drygasflow (20%O2 inAr).For
propaneoxidationthispre-treatmentwasnotrequiredtoobtain
optimumactivity.WedetectedonlyCO2 andH2Oasproductsof oxidationandthecarbonbalancewascloseto100%within2%.All thecatalystsweretestedoverthetemperaturerange(20tests). SomerepresentativeCO(left)andC3H8(right)conversioncurves versustemperature(light-offcurves)areshownontheupperplots
ofFig.8.Wenoticedthatthesameoxalatedecomposedinwhat
Fig.7.N2adsorption-desorptionisothermsandtheirassociatedporesize
distribu-tion(PSD)calculatedusingNLDFTmethod[18].
seemstobethesameconditionscouldproducetwocatalysts hav-ingsignificantdifferencesinactivity.Thisisillustratedinthelower chartswheretheconversionobservedat60◦CforCO (left)and 200◦CforC
3H8 (right)areplotted versustheamountofcobalt. Despitethescatteringoftheresults,theeffectofthesubstitutionof manganesebycobaltseemsrathersimilarforbothreactions. Espe-ciallyweobservethat,forx<0.9,thesubstitutiondoesnotchange theactivitywhereasforx=0.9theactivityisclearlybetter(about3 times).BesidesCo3O4hasaloweractivitythanCo2.3Mn0.7O4which seemstobethebestcomposition.
The boost of activity for x=0.9 is associated with a strong increaseofSBETwhichrisesfrom100to230m2/g.Inanattempt todissociatetheeffectofspecificareafromtheinfluenceofcobalt concentration,wecalculated,fromtheconversionrateandSBET, theintrinsicactivity,Ai,definedasthenumberofreactantmmoles convertedpersecondandperm2ofcatalyst.Thisintrinsic activ-ity,plottedagainstthecobaltfraction,isshowninFig.9.Inthe caseofCOoxidationAidoesnotappeartobedirectlydependentof cobaltfractionbelowx=1.5.Thenastrongimprovementof
activ-Fig.8. ExamplesoftheCO(upper-left)andC3H8(upper-right)conversioncurvesversustemperature(light-offcurves).Effectofcobaltfractionontheconversionobserved
at60◦CforCO(lower-left)and200◦CforC
3H8(lower-right).
Figure10.CO(left)andpropane(right)conversionwithtimeonstreamforCo2.3Mn0.7O4catalyst.
Table4
Comparisonofcatalystactivityforpropaneoxidationat200◦C.
Ref. Catalyst Catalystmass(g) Flowrate(cm3/min) InletC
3H8concentration(%) %C3H8conv.at175◦C Activityat175◦C(mmols−1g−1)
[49] Co3O4 0.25 50 0.80 21 0.25
[50] 4%Au/Co3O4 0.25 50 0.80 32 0.38
[51] Co3O4 0.05 98 0.37 5 0.27
thiswork Co2,3Mn0,7O4 0.05 98 0.37 8 0.43 ityisobservedforhighercobaltcontent.Forpropaneoxidation,a
similarcorrelationbetweenAiandcobaltfractionisobservedfor x>1.5.Belowx=1.5,thecorrelationislessclear.
Severalworkshavedemonstratedthattheoctahedralsitesare
almost exclusivelyexposed at the surface of the spinel oxides
[43–45].Moreoverit wasalsoshown thatthe catalyticactivity ofcobaltoxideswasduetoCo3+ionsinoctahedralsites[45,46]. Hence,forlowcobaltcontent,itisexpectedthatthecatalytic activ-itydoesnotchangemuchbecausethesubstitutionoccursonlyin theinactivetetrahedralsiteswhereCo2+replacesMn2+.Whenthe tetrahedralsitesarefullyoccupiedbyCo2+(x>1)thesubstitution occursinoctahedralsitescreatingactiveCo3+ions[40].
Theapparentactivationenergyforpropaneoxidationwas deter-minedfromArrheniusplotsintheconversionrange0–10%.Except formanganeseoxide,itwasfoundalmostconstantat60±10kJ/mol whateverthecobaltconcentration.ForMnOxtheactivationenergy isslightlyhigherat75±10kJ/mol.
InthecaseoftheCOoxidationtheconversionistoohightoallow thecalculationofactivationenergy.
Forthebestcatalyst(Co2.3Mn0.7O4)wefollowedtheeffectofthe
oxalatedecompositiontemperature(intherange220–300◦C)on
thecatalyticactivityforpropaneoxidation.Althoughthevariations inactivitywereofthesameorderofmagnitudeasthedifferences
betweenreplicatesitseemsthattheoptimumdecomposition
tem-peratureis280◦C.
Thelong-termstabilityoftheconversionwastestedwiththe bestcatalyst(Co2.3Mn0.7O4).TheleftplotofFig.10showsthatthe COconversiondecreasesbyabout8%duringthefirsthalfofthe test.Thenitseemstoremainstableuntiltheendofthetest.
Unex-pectedlyweobservedvariationsoftemperatureassociatedwith
variationsofconversion.Wecouldnotdetermineifitwasthe
tem-peraturechangethatinducedconversionchangeortheconverse.
Asregardspropaneoxidation,therightplotofFig.10indicatesthat theconversionwasstableformorethan14hat160◦C.
Tocomparethecatalyticactivityofourmaterialswiththedata reportedintheliteraturewecalculatedthespecificactivitydefined
asthenumberofreactantmmolesconvertedpersecondandper
gramofcatalyst.
AsitwasdemonstratedthatCOconversionwasstrongly depen-dentupontheamountofwaterintheinletgas[46–48]welimited
ourcomparisontopropaneoxidation.Thiscomparisonrevealed
(Table4)thatCo2.3Mn0.7O4activitywasmorethan50%higherthan thatofCo3O4catalystsfoundinthemostrecentpublicationsand wassimilartocatalystsforwhichpreciousmetalhavebeenadded toenhancetheactivity.
4. Conclusion
Cobalt-manganesemixedoxalatedihydratescrystallizeinthe
monoclinicstructurewhenthecobaltfractionis lowerthan0.5
andinorthorhombicstructureotherwise.Thecontrolled
decom-positionoftheseoxalatesnear200◦C,followedbyacalcinationat 300◦C,stronglyrestrainstheshrinkageofparticlesandthe crys-tallitesintering,producingmixedoxidesCoxMn3−xO4withavery largesurfacearea.Forx<0.9thesematerialsareamorphous.For x≥0.9theyhaveacubicspinelstructureandtheircrystallitesize increaseswiththecobaltfraction.
Thesespineloxidesexhibitanoutstandingcatalyticactivityfor propaneoxidation.TheyarealsoactiveforCOoxidationevenat
ambienttemperature.Thishighactivityiscorrelated both with
the surface area and the cobalt concentration. For manganese
oxide the apparent activation energy for propane oxidation is
75±10kJ/molwhereasitis60±10kJ/molandnearlyindependent ofcobaltfractionfortheothercatalysts.Themostefficientmaterial isCo2,3Mn0,7O4,whichhasanactivitymorethan50%higherthan thebestCo3O4catalystsreportedintheliterature.
Acknowledgments
ThisworkwasfinanciallysupportedbytheDGEandtheRegional CouncilofMidi-PyrénéesintheframeworkoftheSOFTAIRproject. References
[1]L.F.Liotta,Catalyticoxidationofvolatileorganiccompoundsonsupported noblemetals,Appl.Catal.B:Environ.100(2010)403–412.
[2]M.Ousmane,L.F.Liotta,G.Carlo,Di,G.Pantaleo,A.M.Venezia,G.Deganello,L. Retailleau,A.Boreave,A.Giroir-Fendler,SupportedAuCatalystsFor Low-TemperatureAbatementofPropeneandToluene,AsModelVOCs: SupportEffect,Appl.Catal.B:Environ.101(2011)629–637.
[3]V.P.Santos,S.A.C.Carabineiro,P.B.Tavares,M.F.R.Pereira,J.J.M.Orfao,J.L. Figueiredo,OxidationofCO,ethanolandtolueneoverTiO2supportednoble
metalcatalysts,Appl.Catal.B:Environ.99(2010)198–205.
[4]M.J.Patterson,D.E.Angove,N.W.Cant,Theeffectofcarbonmonoxideonthe oxidationoffourC6–C8hydrocarbonsoverplatinum,palladiumand rhodium,Appl.Catal.B:Environ.26(2000)47–57.
[5]P.Marecot,A.Fakche,B.Kellali,G.Mabilon,P.Prigent,J.Barbier,Propaneand propeneoxidationoverplatinumandpalladiumonalumina:effectsof chlorideandwater,Appl.Catal.BEnviron.3(1994)283–294.
[6]G.Busca,M.Daturi,E.Finocchio,V.Lorenzelli,G.Ramis,R.J.Willey,Transition metalmixedoxidesascombustioncatalysts:preparation,characterization andactivitymechanisms,Catal.Today33(1997)239–249.
[7]S.Royer,D.Duprez,Catalyticoxidationofcarbonmonoxideovertransition metaloxides,ChemCatChem3(2011)24–65.
[8]B.Solsona,I.Vazquez,T.Garcia,T.E.Davies,S.H.Taylor,Completeoxidationof shortchainalkanesusingananocrystallinecobaltoxidecatalyst,Catal.Lett. 116(3–4)(2007)116–121.
[9]J.Zhu,QiumingGao,MesoporousMCo2O4(M=Cu,MnandNi)spinels:
structuralreplication,characterizationandcatalyticapplicationinCO oxidation,Micropor.Mesopor.Mater.124(2009)144–152.
[10]S.Todorova,H.Kolev,J.P.Holgado,G.Kadinov,Ch.Bonev,R.Pereniguez,A. Caballero,Completen-hexaneoxidationoversupportedMn–Cocatalysts, Appl.Catal.B:Environ.94(2010)46–54.
[11]B.Puertolas,A.Smith,I.Vazquez,A.Dejoz,A.Moragues,T.Garcia,B.Solsona, Thedifferentcatalyticbehaviourinthepropanetotaloxidationofcobaltand manganeseoxidespreparedbyawetcombustionprocedure,Chem.Eng.J. 229(2013)547–558.
[12]C.Drouet,P.Alphonse,Synthesisofmixedmanganiteswithhighsurfacearea bythermaldecompositionofoxalates,J.Mater.Chem.12(2002)3058–3063. [13]V.Iablokov,K.Frey,O.Geszti,N.Kruse,HighcatalyticactivityinCOoxidation
overMnOxnanocrystals,Catal.Lett.134(2010)210–216.
[14]J.Robin,Etudedesoxalatesmétalliquescommematièrespremièrespourla preparationdesolutionsolidesd’oxydes,BulletindelaSociétéChimiquede France20(1953)1078–1084.
[15]J.Rodríguez-Carvajal,RecentdevelopmentsoftheprogramFULLPROF, Commissiononpowderdiffraction(IUCr)Newsletter26,12–19.
[16]P.Thompson,D.E.Cox,J.B.Hastings,RietveldrefinementofDebye-Scherrer synchrotronX-raydatafromAl2O3,J.Appl.Crystallogr.20(1987)79–83.
[17]S.Brunauer,P.Hemmett,E.Teller,Adsorptionofgasesinmultimolecular layers,J.Am.Chem.Soc.60(1938)309–319.
[18]N.Seaton,J.Walton,N.Quirke,Anewanalysismethodforthedetermination oftheporesizedistributionofporouscarbonsfromnitrogenadsorption measurements,Carbon27(1989)853–861.
[19]D.Dollimore,D.Nicholson,Thethermaldecompositionofoxalates:partI, Var.Surf.AreaTemp.Treat.AirJ.Chem.Soc.96(1962)0–96.
[20]D.Broadbent,D.Dollimore,J.Dollimore,Thethermaldecompositionof oxalates.partVII.Theeffectofpriordehydrationconditionsuponthe subsequentdecompositionofcobaltoxalate,J.Chem.Soc.A.(1966) 1491–1493.
[21]D.Dollimore,J.Dollimore,J.Little,Thethermaldecompositionofoxalates. PartX.Nitrogenadsorptiondataonsolidresiduesfromtheisothermalheat treatmentofmanganese(II)oxalatedihydrate,J.Chem.Soc.A.(1969) 2946–2951.
[22]M.E.Brown,D.Dollimore,A.K.Galwey,Thermaldecompositionof manganese(II)oxalateinvacuumandinoxygen,J.Chem.Soc.FaradayTrans. 170(1974)1316–1324.
[23]K.Nagase,K.Sato,N.Tanaka,Thermaldehydrationanddecomposition reactionsofbivalentmetaloxalatesinthesolidstate,Bull.Chem.Soc.Jpn.48 (1975)439–442.
[24]J.Mu,D.D.Perlmutter,Thermaldecompositionofcarbonates,carboxylates, oxalates,acetatesformatesandhydroxides,Thermochim.Acta49(1981) 207–218.
[25]D.Dollimore,Thethermaldecompositionofoxalates.Areview,Thermochim. Acta117(1987)331–363.
[26]X.Gao,D.Dollimore,Thethermaldecompositionofoxalates.Part26.A kineticstudyofthethermaldecompositionofmanganese(II)oxalate dihydrate,Thermochim.Acta215(1993)47–63.
[27]A.Coetzee,M.E.Brown,D.J.Eve,C.A.Strydom,Kineticsofthethermal dehydrationsanddecompositionsofsomemixedmetaloxalates,J.Therm. Anal.41(1994)357–385.
[28]A.K.H.Nohman,H.M.Ismail,G.A.M.Hussein,Thermalandchemicaleventsin thedecompositioncourseofmanganesecompounds,J.Anal.Appl.Pyrolysis 34(2)(1995)265–278.
[29]A.K.Nikumbh,A.E.Athare,S.K.Pardeshi,Thermalandelectricalpropertiesof manganese(II)oxalatedihydrateandcadmium(II)oxalatemonohydrate, Thermochim.Acta326(1999)187–192.
[30]M.Maciejewski,E.Ingier-Stocka,W.D.Emmerich,A.Baiker,Monitoringofthe gasphasecomposition:aprerequisiteforunravellingthemechanismof decompositionofsolids.Thermaldecompositionofcobaltoxalatedihydrate, J.Therm.Anal.Calorim.60(2000)735–758.
[31]B.V.L’vov,Kineticsandmechanismofthermaldecompositionofnickel, manganese,silver,mercuryandleadoxalates,Thermochim.Acta364(2000) 99–109.
[32]B.Malecka,E.Drozdz-Cielsa,P.K.Olszewski,Kineticsofthermal
decompositionofmanganese(II)oxalate,J.Therm.Anal.Calorim.74(2003) 485–490.
[33]M.A.Mohamed,A.K.Galwey,S.A.Halawy,Acomparativestudyofthethermal reactivitiesofsometransitionmetaloxalatesinselectedatmospheres, Thermochim.Acta429(2005)57–72.
[34]B.Donkova,D.Mehandjiev,Mechanismofdecompositionofmanganese(II) Oxalatedihydrateandmanganese(II)oxalatetrihydrate,Thermochim.Acta 421(2004)141–149.
[35]M.E.Brown,D.Dollimore,A.K.Galwey,Thermochemistryofdecompositionof manganese(II)oxalatedihydrate,Thermochim.Acta21(1977)103–110. [36]V.Iablokov,K.Frey,O.Geszti,N.Kruse,HighcatalyticactivityinCOoxidation
overMnOxnanocrystals,Catal.Lett.134(2010)210–216.
[37]N.B.S.The,Tablesofchemicalthermodynamicproperties,J.Phys.Chem.Ref. Data11(supplementno.2)(1982).
[38]O.Kubaschewski,C.B.Alcock,P.J.Spencer,MaterialsThermochemistry,6th ed.,PergamonPress,1993.
[39]Y.Xiao,D.E.Wittmer,F.Izumi,S.Mini,T.Graber,P.J.Viccaro,Determinationof cationsdistributioninMn3O4byanomalousX-raypowderdiffraction,Appl.
Phys.Lett.85(2004)736–738.
[40]H.Bordeneuve,C.Tenailleau,S.Guillemet-Fritsch,R.Smith,E.Suard,A. Rousset,StructuralvariationsandcationdistributionsinMn3−xCoxO4
(0<x<3)denseceramicsusingneutrondiffractiondata,SolidStateSci.12 (2010)379–386.
[41]D.Jarosch,Crystalstructurerefinementandreflectancemeasurementsof hausmannite,Mn3O4,Mineral.Petrol.37(1987)15–23.
[42]C.Laberty,M.Verelst,P.Lecante,P.Alphonse,A.Mosset,A.Rousset,Awide angleX-rayscattering(WAXS)studyofnonstoichiometricnickelmanganite spinelsNiMn2h3ı/4O4+ı,J.SolidStateChem.129(1997)271–276.
[43]M.Shelef,M.A.Z.Wheeler,H.C.Yao,Ionscatteringspectrafromspinel surfaces,Surf.Sci.47(1975)697–703.
[44]J.P.Jacobs,A.Maltha,J.G.H.Reintjes,J.Drimal,V.Ponec,H.H.Brongersma,The surfaceofcatalyticallyactivespinels,J.Catal.147(1994)294–300.
[45]K.Omata,T.Takada,S.Kasahara,M.Yamada,Activesiteofsubstitutedcobalt spine1oxideforselectiveoxidationofCO/H2.PartII,Appl.Cata.A:Gen.146
(1996)255–267.
[46]X.Xie,Y.Li,Z.Q.Liu,M.Haruta,W.Shen,Low-temperatureoxidationofCO catalysedbyCo3O4nanorods,Nature458(2009)746–749.
[47]Y.F.YuYao,TheoxidationofhydrocarbonsandCOovermetaloxides:III. Co3O4,J.Catal.33(1974)108–122.
[48]F.Grillo,M.M.Natile,A.Glisenti,Lowtemperatureoxidationofcarbon monoxide:theinfluenceofwaterandoxygenonthereactivityofaCo3O4
powdersurface,Appl.Catal.B:Environ.48(2004)267–274.
[49]T.Garcia,S.Agouram,J.F.Sanchez-Royo,R.Murillo,A.M.Mastral,A.Aranda,I. Vazquez,A.Dejoz,B.Solsona,Deepoxidationofvolatileorganiccompounds usingorderedcobaltoxidespreparedbyananocastingroute,Appl.Cata.A: Gen.386(2010)16–27.
[50]B.Solsona,E.Aylon,R.Murillo,A.M.Mastral,A.Monzonis,S.Agouram,T.E. Davies,S.H.Taylor,T.Garcia,Deepoxidationofpollutantsusinggold depositedonahighsurfaceareacobaltoxidepreparedbyananocasting route,J.Hazard.Mater.187(2011)544–552.
[51]G.Salek,P.Alphonse,P.Dufour,S.Guillemet-Fritsch,C.Tenailleau, Low-temperaturecarbonmonoxideandpropanetotaloxidationby nanocrystallinecobaltoxides,Appl.Catal.B:Environ.147(2014)1–7.