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45GJ/ton3.2tonsCO2/ton71kgCO2/GJ
55GJ/ton2.8tonsCO2/ton51kgCO2/GJ
Ifnotforthe35billiontonsperyear(Gta)ofCO2,fossilfuels
couldbeuClizedforthebenefitofsocietyunCltheybecamemore
expensivethanalternaCves.à“TransiRonOpRon”
20-30GJ/ton2.3tonsCO2/ton92kgCO2/GJ
−CHx + yO2 → CO2 + H2O + Heat
ThereisnoevidencethateconomicallysustainablealternaCvestofossilfuelsexisttoday;atmosphericCO2conCnuestorise
2016~17TW
Oil(5.3)
Coal(4.9)
Gas(3.6)
Sustainables(3.2)
2XXX??30+?TW
Hydro(44%CF)480GWelec(16%)14GWelec/y
Nuclear(90%CF)330GWelec(~11%)
13GWelec/yWind(39%CF)144GWelec(~4%)10GWelec/ySolar(21%CF)
13GWelec(~0.6%)3GWelec/y
Wave Geothermal
Someday,increasinglyrarefossilresourceswillbetoocostlytoburn.Probablybeforethen,theCO2emissionsfromcombusRonwillcause
harmtopartsofourglobalecosystemandpeople.
GlobalDiversifiedRiskManagement• ProtectAgainstFossilFuelPrice/SupplyRisk• AddressEnvironmentalandClimateRiskà IncreaseEfficiencyà IncreaseCO2-freepowergeneraRon
NoneofthetechnologyopRonsarenewAllrelyonsustainednuclearreacRons.
Withoutcost-effecRveopRons,significantCO2emissionreducRonswillnotbeachievable.
Ifsevereconsequencesoccur,
thepoorwillbeharmedfarworsethanthewealthy.
$0.1/kg20-30GJ/ton
$2-3/GJ
~9.5GtaofCinHydrocarbonsAreCombustedForLowCostHeat
−CH2x + yO2 → CO2 + xH2O + Heat
$0.3/kg45GJ/ton$7-8/GJ
$0.2/kg55GJ/ton$3-4/GJ
3.3MktaC 9.5MktaC9.5Gta
$80TrillionGlobalGDP
~35GtaCO2Emissions.
24%Heat
36%Transport
40%Electricity
Present“Strategy”:HydrocarbonCombusConForLowCostHeat
24%Heat
36%Transport
40%Electricity
$80+TrillionGlobalGDP
9.5++GtaC
35+GtaCO2Emissions
Gas
Coal
Oil
Reserves1,000Gt+
Reserves250Gt+
Reserves140Gt+++
MassiveExisRngInfrastructureGlobalTradeRelaRonsKnownScale-up
BUT,if…....
−CH2x + yO2 → CO2 + xH2O + Heat
PlanB:HydrocarbonsforLowCostHeatWithoutCO2−CH2x + yO2 → C + xH2O + Heat
24%Heat
36%Transport
40%Electricity
$80+TrillionGlobalGDP
19++GtaC
0CO2Emissions
Gas
Coal
Oil
Reserves1,000Gt+
Reserves250Gt+
Reserves140Gt+++
MassiveExisRngInfrastructureGlobalTradeRelaRonsKnownScale-up
CO2+xH2O
-CH2x
~35GtaCO2Emissions.
PlanB:~2xfossilresourcesForHeat
C+xH2O
ZeroCO2
19GtaC
MorestrategicuseofourfossilizedsolarresourcesmaybemorereasonablethannouseatallorCCS.
MassiveQuanRResofMethaneareAvailableWorldwide > 7000 tcf Natural Gas Reserves (non-hydrate) ~ 250 TW-y
Weareinterestedin
findingwaysofefficientlyusingCH4without
producingCO2
CO2+2H2O
~2Gtaofmethaneisburnedinabundantoxygentoproduceheat+smallcontribuRontothe0.4Gtaoforganicchemicalsmadelargelyfrompetroleum.
O=C=O
O2(H2O)
H2O(O2)CO/CO2+H2
CH3OH
Olefins/Arom Paraffin’s,HC’s
+0.5-1tonsCO2/tonC
Ammonia
N2
+2.8tonsCO2/tonC
NaturalGasURlizaRon:Past=Present
CH4
H HO
O=O
Heat
Transport
Electricity9.5GtaC
Gas
Coal
Oil
OrganicChemicals(0.3GtaPlasCcs)Metals(1.5Gtasteel)
0.4Gta
~3GtaCO2Emissions
2.8Gta
SustainableChemicalProducRonIsARelaRvelyMinorProblemButpoten<allylargeopportunity
O2(H2O)
H2O(O2)CO/CO2+H2
CH3OH
Olefins/Arom Paraffin’s,HC’s
+0.5-1tonsCO2/tonC
Ammonia
N2
CH4
“SelecRve”ParRalOxidaRonofMethaneforChemicals
C(-4)
CH4
SelecRveParRalOxidaRonofMethaneforChemicals
CH4 + 12 O2 ⎯→⎯ 1
2 C2H4 + H2O
OxidaCveCouplingofMethane(OCM)
C2selecCvity
C2Yield
HCYield
ChemistryLe,ers,1986,3,p1981-1984
Academic“HolyGrail”
f = k2
k1= rate of secondary product oxidation with O
rate of first C-H bond transformation
f= k2k1
CAN'T BE SMALL !
ToDreamtheImpossibleDreamOCMWithO2:ThermochemicallyandKineCcallyNotSensible(Bell-Evans-Polanyi)
J.NaturalGasChem.2012Vol.21Issue(3):308-313
0 1 2 3 4 5f0.0
0.2
0.4
0.6
0.8
1.0Yield0.0 0.2 0.4 0.6 0.8 1.0
Conversion0.0
0.2
0.4
0.6
0.8
1.0Selectivity
f=0.5
f=2
f=1
CH 4
k1O−M⎯ →⎯⎯ C−2 k2
O−M⎯ →⎯⎯ →→COx + H2Ogas phase
O2⎯ →⎯⎯⎯ ⎯→⎯ →→→→COx + H2O
HighYieldsNotPossiblek1<k2
k2k1
≥ 21
→ S+C ≤ 100%
k2k1
≥ 110
→ Yield < 75%
S+C<100%Notgoodenough
CnHm
ΔH,ΔG700K,1atm
½C2H4+H2106,60CH4
MethaneforChemicals
WhatWeReallyWanttoDo
(1-x)/2C2H4+(1-x)H2O+xCO2WhatWeActuallyDo
CO2+2H2O-800,-800WhatWeDon’tWantToDo
½C2H4+H2O-139,-148
CH4+nO2
WhatWeHaveBeenTryingtoDo
H2
O=O
CH4
~2moles/s-kta
-4
~-1500kW/ktaHeat
Philosophicalapproachàmaintaintheelectron’schemicalpotenRal
C(-4)
CO2+2H2O
O=C=OO(-2)
O=O
-(C H2)- -2
-C- 0
OrganicChemicals
-C- +4
~1.5MillionAmps/ktaà
e- e- e- e- e- e- e- e-
CH4 -(C H2)- -4 -2
-C- 0
e- e- e- e-
DonotallowcompleteCoxidaRon:DifferentReacRonEnvironments
~-775kW/ktaHeat
O=C=O
CnHm
ΔH,ΔG700K,1atm
MethaneforOrganicChemicals
½C2H4+H2106,60
½C2H4+2HI94,36
½C2H4+2HCl-80,-137Cl2
I2 2HX
H2
CH4+nX2
½C2H4+H2O-139,-149O2
H2O
Oxygenisnottheonlyelectrophile!
HalogensSuppressCompleteOxidaConflameretardants:
1)OxidaBvedehydrogenaBon+2)SuppressesoxycombusBon
-CH2-CHBr-CH2---------CH2-CH2-CH2-
HBr+O2àHOO*+Br*HOO*+HBràH2O2+Br*H2O2à2OHOH+HBràH2O+Br*
HydrodebrominaCon(ODH)
-CHBr-CH2-à-CH=CH-+HBrT
HCl+O2àHOO*+Cl*
HBr+O2àHOO*+Br*
HI+O2àHOO*+l*HIisthefastest
FredrickRust,Industrial&engineeringchemistry1949vol:41iss:11pg:2595
AlkylhalidesareEasyToMakeandEasyToSeparateOxyhalogenaBon/DehydrohalogenaBonforParBalOxidaBon
Shell1960’s(I2-ODH)-90%Sel.,80%Conv.
MoreSeparableIntermediatesReactforShow,SeparateforDough
CH4+XYàH3C-X/HnCm+HY
XY Intermediates HYO2 CH4,N2,COxCHyOx H2O,H2
S CH4CH3SHCS2 H2S,H2
NOx CH4N2,NO,COx H2O
SOx CH4SO2CH3SO3H H2OSO2H2SO4
I,Br,Cl CH4CHn-Xm HX,H2
Less“efficient”orlessdirectreacConpathwayswithmoreseparableproductsareoqenmoredesirablethanmorereacConefficientanddirectpathways.
CH4 -(C H2)- e- e--4 -2
OrganicChemicals
+ 2HX
-C- e- e- 0
+ 4HX
TransferofHydrogen(e-)toHydrogenHalideOffersSignificantProcessFlexibilityandPreservesChemicalPotenRal
X2
Heatout+/-eV
O2
eV+/-Heatinput
1-2H22HI
2HBr2HCl
0.2−1.5Volt⎯ →⎯⎯⎯ H2 +I2
Br2
Cl2
2HI2HBr2HCl
+ 12
O2 ⎯→⎯ H2O+I2
Br2
Cl2
+ Heat (or eV)
SAPOàLightOlefins(ethylene/propylene)
ZSM5àAromaCcs
CH3OHà(-CH2-)+HOH
0%
5%
10%
15%
20%
25%
30%
35%
40%
Benzene Toluene Xylene Mesitylene Durene Naphthalenes
Wei
ght P
erce
ntag
e, %
Chem.Com.2004,566,658Phys.Chem.Chem.Phys.2011,13,2550
CH3Brà(-CH2-)+HBr
AlkylhalidesAreReadilyTransformedIntoOrganicChemicalsUsingKnownAlcoholPathways(MTO,MTG)
Polyhalides?InteresRngNew(old)Chemistry
CH2Br2H2⎯ →⎯ CH3Br H2⎯ →⎯ CH4
ACSCatal.(2012),2,479−486
CH2Br2H2⎯ →⎯ *CH −HBr⎯ →⎯⎯ *C2H5 −HBr⎯ →⎯⎯ *CnHm
Pd/SiO2
nCH2Br2à-CnHm+2nHBr
hsps://www.youtube.com/watch?v=44OU4JxEK4k
Whatyouwantonsurfacesforoligomersare-CHand-CH2(Fischer-Tropsch)
ACSCatal.(2012),2,479−486
Methane
EthanePropane
Methanol/DMEOlefinsBTX+
EthanolGlycolEthyleneBTX+
OlefinsEthoxylates
PropanolPropyleneBTX
AcRvaRon:R-H+Br2àR-Br+HBr
Conversion:R-BràR’+HBr
RegeneraRon:O2+HBràBr2+H2OHBràBr2+H2
HBrBr2
O2/Electricity/PhotonsH2O/H2
DemonstratedBr2/HBrPlayorm
WithoutCO2
But…....
Chem.Com.2004,2100
CatalysisToday2004,98,317
Chem.Com.2004,566,658
Phys.Chem.Chem.Phys.2011,13,2550
ACSCatal.2012,2,479−486
3Fe0
H - Cl
1FeCl2
8
2FeCl3
3C0
2
3
3CH4 + 2FeCl3+ FeCl2 → 3C + 3Fe + 8HCl + 2H2
HalogenFacilitatedThermalReducRon
Heat
Transport
Electricity
$80TrillionGlobalGDP
9.5GtaC
35GtaCO2Emissions
Gas
Coal
Oil
InteresRngchemistry,butthefewGtaofCO2fromchemicalproducRonisNOTtheproblem
ΔH,ΔG700K,1atm
C+4HCl-228/-382Cl2
C+4HI60/-34I2
2HX
C+2H2106,60 H2
CH4+nX2
C+2H2O-406/-405
O2
H2O
WeWantCO2-freeLowCostFuelsandHeat
NH3C+NH3+½H215/44
N2
C+NH3+HCl-62,-59N2+Cl2
1943BelgiumNH3Bus
X-15NH3Supersonic
NH3ToyotaGT86-R
KoreanNH3Subcompact
CO2 free combustion32
O2 + 2NH3 → N2 + 3H2O
HeatofCombusCon~Methanol
2 moles CH4
sec
1kta CH4
4 moles H2Osec
+ 2 moles CO2
sec
+ 1500 kW Heat → 750kWelec
LessHeatbutNoCO2
2CH4 + 4O2 → 2CO2 + 4H2O
2XoperaRngcost.Howmuchmorecapital?
2 moles Csec
4 moles H2Osec
+ 1,000 kW Heat- 225 kW= 775 kW→ 387 kWelec
4 moles H2
sec
2CH4 → 2C + 4H2
4H2 + 2O2 → 4H2O-225kW
83
moles NH3
sec
43
moles N2
sec
+142kW
4 moles H2Osec
+ 43
mole N2
sec
+ 842 kW Heat- 225 kW+ 142 kW Heat= 760 kW→ 380 kWelec
83
NH3 + 2O2 → 4H2O + 43
N2
UnderstandingandControllingReacRonsandProcessesinComplexMelts
R- 103R- 102
S- 101
SPL- 102
E- 102A
T- 101
E- 101
D- 101
SPL- 101
E- 103
E- 104
T- 201
R- 101A R- 101B
E- 102B
P- 201
SPL- 103
E- 201A
T- 202
C- 201
E- 202
MIX101
MIX-102
E- 201B
MCOMPR
C- 101
NG IN
BRO UTOR OUT2
W HR
S20
W HRTO V
CR OUT
RW ATER1
RW ATER2
LIG HTGAS
W HB
OILIN
OW OW IN
W ATER
W ATER2
NG F
ACO MOU T
CO MSUC
OILLEAN
OW OU T
OILR2
W HV
W HL
HO TAIR
OR OUT1
HPO ILOILTCOO L
W ATER1
OILR1
CO MDIS RG AS
C4
C5+BTX
S5
OM AKEUP
W PROD
S2
S1
S3
AIR
0.0
0.5
1.0
1.5
2.0
2.5
0 200 400 600 800 1,000 1,200
Equilibriu
mCom
posiC
on(m
ole
basis)
Temperature(C)
H2(g) CH4(g) C
H2_withI2 CH4_withI2 C_withI2 H2
CH4
C(graphite)
Equilibriumforpyrolysisfavoredatlowertemperaturewhenhalogenspresent
H2(remainderHI)
HighercarbonyieldwhenI2ispresent(highermethaneconversion)
MoltensaltsusedforenvironmentalcontrolofreacCvesurfacesites
Ethane Ethylene Oxygen Water
J.Phys.Chem.C,2015,119(16),pp8681–8691
CH 4heat /catalyst⎯ →⎯⎯⎯ C + 2H2
H2 −>Heat⎯ →⎯⎯⎯ C + 53 H2 +
13 H2O
SubmizedChemicalEngineeringJournal
0
5
10
15
20
25
0 10 20 30 40 50
IRR
(%
)
CO2 Charge ($/tonne)
EAF Catalytic Pyrolysis
SMRSMR”adjustedpriceofH2forInternalRateofReturn(IRR)=10%.Other’susesameH2price.
ThermochemicalHydrogenProducRonCanBeatSMRSMRvsPyrolysisUSGasPrice$2/GJ
ACarof“thefuture”:OnBoardThermalPyrolysis?
H2
CCH4
OrotherHC
ICE/Hybrid
CarbonHoldingTank
Today’s~48mpghybrid
Tomorrow’s~0CO2~24mpghybrid**
Challenge:CosteffecRvemodularreactorsystemCatalyBcconverters~$100.
CH4 + 12
N2 + nX → NH3 +C + HX
500ktaHaberBoschAmmoniaFacility
OurGrandChallenge:DirectMethanetoAmmonia(FuelandFoods)
CH4 + H2O → 3H2 + CO 2N2 + 3H2 → 2NH3
Summary
• FossilhydrocarbonsremainthelowestcostsourceofpowerandorganicchemicalsandconRnuetomakepossibleglobalprosperity.
• Wedonot,presently,havecostcompeRRvealternaRves.• IftheglobalsocietyeverplacesameaningfulcostoncarbondioxideemissionsandconRnuestounnecessarilyrestrictinnovaRonincommercialnuclearpower,alternaRvemeansofusingfossilresourcesmayprovidetheleastcostlyprocessesforCO2emissionsreducRonsunRltheinevitableincreasingscarcitydrivesuptheircost.
• AlternaRveconversionpathwayshavemanyinteresRngfundamentalmechanisRcquesRonsandpracRcalchallengesthatshouldbeinteresRngtochemicalscienRsts,engineers,andstudents.