at and near a metal (electrode) surface ionization of water in high...
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Ionization of Water in High Electric Fieldsat and near a Metal (Electrode) Surface
Valentin Medvedev
Chris Rothfuss
Eric M. Stuve
University of Washington
Gordon Research Conference on Electrochemistry
Ventura, California
14-19 January 2001
Sponsored by the Office of Naval Research
UW ELECTROCHEMICALSURFACE SCIENCE
Role of Electric Field in Electrochemistry
• High interfacial electric field(~1 V/Å)
• Field controlled by electrodepotential or chemical potential ofsolution species
• What is role of field inelectrochemical reactions?
• How to control fieldindependently?
+
–+
++– –
–
–
– +–
+
n–
Je
(IHP)
C–
C+
Sub strate Bulk Elect rolytDiffuse Layer
In te rface
In te rfacial Field
• Characteristic field for bond breaking– All bonds similar strength: 1-5 eV– All bonds similar length: 1-2 Å
• Field emitter tips– Concentrate field at tip– 100-1000 Å tip radius; ß ≈ 5– 1-5 kV => 1-5 V/Å
Use of Field Emitter Tips
Ft = Vt
βrt
1-3 V/Š�����
VtrtFEM
Tip
Field-Free Adsorbed Water
• Low temperature (< 170 K)– Variables: tw, T, Tads
• What can we study?– Ionization in ice layers– Dielectric properties
Dipole momentDielectric constant
– Crystalline vs. amorphous ice– Interaction of field and temp.
tw
Ice
Field Adsorbed/Condensed Water
• High temperatures (> 170 K)– Variables: pw, T, F
• What can we study?– Monolayer & multilayer water– Surface vs. bulk ionization– Cluster formation: (H2O)n·H+
– Interaction of field and temp.– Room temp. studies possible
H2O (H2O)n·H+
How Are Ions Detected?
• Use principles of field ionization microscopy (FIM)• Tip usually in positive bias (to avoid e– emission)• Positive ions detected by microchannel plates
– Ion images– Ionization rates
(+)1 V/Å
• Mass spectroscopy with singleion resolution– Time of flight (field pulse
initiated)– ExB (Wien) filter
(continuous signal)
Experimental Techniques
• Imaging methods for spatio-temporal correlation– Field ionization (static and video)– Mass resolved ion images– Field emission micr. (FEM)
• Quantitative methods– Ramped field desorption (RFD)
similar to thermal desorp. (TDS)– Stepped field desorption (SFD)
similar to isothermal kinetics– Thermo-cycling (TC)
cycle temp. at given field field
Ionrate
Gas Handling
Turbomolecular Pump
Mass Spectrometer
WienFilter
Drift Tube
LensFocus
Tip TranslationApparatus
Alternate Wien FilterConfiguration (no Drift Tube)
CoolantDown Tube
UHV ChamberConfiguration
Analytical Equipment• Rotatable Tip Assembly• FIM/FEM Imaging• Wien Filter• Pulsed Potential Time of Flight• Quadrupole Mass Spectrometer
20 - 56 mm Variable CounterElectrode-Lens Distance
LD
EntranceDiaphragm
FrontElectrode
CenterElectrode
BackElectrode
Lens Assembly
Tip Assembly
• Spatial Resolution of Ion Emission• Field Clean Pt Surface to Prevent
Possible Contamination
Field Ion Microscopy Neon on Pt107 K
1x10-4 Torr~3.75 V/Å
METAL (Pt)LATTICE STEPIMAGE GAS (Ne)ION (Ne+)
Adapted from Tsong,1990.
TIP
HV
MULTI-CHANNELPLATES
PHOSPHORSCREEN
PotentialEnergy of
Image GasElectron In
AppliedField Near
Tip Surface
Iφ X
V
FERMILEVEL
ElectricElectricField (E)Field (E)
MagneticMagneticField (B)Field (B)
Lens: G.F. Rempter, J. Appl. Phys. 57 (1985) 2385.
E x B Mass Separator: M. Kato and K. Tsuno, Nucl. Instr. Methods A298 (1990) 296.
Wien Filter IonCharacterization
L1L
m
m0
Lens
Drift TubeE x BMass
Separator
Ion Detector
Tip
∆xVt
VCE VL
IonIon
m+m+δδmmm-m-δδmm
mm
• Continuous Mode Ion Massto Charge Resolution
• Easily Separate Distinct IonSignals without DisturbingFormation Conditions
00 BeeE ν=0
000
2
m
eBE
φ= ∆x =
E02φ0
L2
2+ LL1
1−m0m
WIEN SEPARATION Masses 19 and 37
Click here to playvideo of separation of
masses 19 (H3O+)and 37 (H2O)2H+
Field Distribution in Water
• Modeled water layer on tip• Ice like (low dielectric) water near
surface• Liquid like water far from surface• Field concentration at interface• Thin layer behavior (tw < rt)
Field at water/vacuum interf.Vacuum limit
• Thick layer behavior (tw > rt)Field at metal/water interf.Electrochem. Limit
rt tw
Field
Distance
3 80ε
H2O
+Vt
rt
Scovell et al., Chem. Phys. Lett. 294 (1998) 255.
Ramped Field Desorption of Ice
• Field-free adsorbed water• x = tw/rt = 3 (thick layer)• Increase field linearly in time• Measure ionization/desorption
of all ions
• Increasing temp. decreases fieldneeded for ionization
• Changes in peak shape withtemperature
0 0.4 0.8 1.2 1.6
Ion
Curre
nt (A
rb. U
nits
)
Fapp / V Å-1
148 K
138 K
128 K
118 K
103 K
x = 3.0 ± 0.3
Flash
Pinkerton, et al., Langmuir, 15 (1999) 851.
Onset Ionization Fields
• Phase transitions in ice layers• Amorphous ice (solid line)• Crystalline ice (dashed line)• Ionization at only
0.2 – 0.5 V/Å !
Temp. Dipole Permittivity
Amorph. < 130 K 3.9 D 10
Cryst. > 130 K 5.1 D 2.5
EEE
EE E
E
EEE
EEE E
EE
E
0.0
0.2
0.4
0.6
100 120 140 160 180 200 220T / K
H2O / Ptx 0
Ons
et F
ield
, F (V
Å-1
)
Scovell, et al., Surface Sci., 457 (2000) 365.
Thermal Activation Barrier of Ionization
• Gomer charge-exchange model
• Hydrogen motion alonghydrogen bond (red curve)
Field dependent barrier
Thermal activation barrier
0V(xc)
xc
∆Eres
H3O
H+·(H 2O)mF
PiF
HO–H … OH2
xO–H
E
QHa
Ionization in Thin and Thick FilmsThick Layers
– Ionization at metal surface
– Ions must diffuse through ice layerbefore detection
– less sensitive to ice layer structure
Pt FieldEmitter Tip
Water Layer
Pt - H20 InterfaceIon Formation
H20 -Vacuum InterfaceIon Formation
Thin Layers
– Easy detection of ions
– Sensitive to ice layer structure
108 K
rt
rw =1.7 rt
rw =5 rt
rw =7
108 K 133 K
Ramped Field Desorption of IceImaged in Total Ion Mode
Click here to playRFD video of thin,amorphous waterlayer adsorbed at
108 K
Click here to playRFD video of thick,amorphous waterlayer adsorbed at
108 K
Click here to playRFD video of thick,
crystalline waterlayer adsorbed at
133 K
Ion Cluster Formation
• Field condensed water layer on Pt• Ion clusters mass resolved with Wien
filter• Clusters of (H2O) n·H+ with n = 1-8• Trade-off between:
– Ionization potential(favors high n); lower ∆Hrxn
– Kinetics (favors low n);entropic effects
• Cluster field independent of temp.
Thermo-Cycling: Ion Cluster Formation
RESULTS•Ion cluster emission thermally deactivatedfor given cluster size.
•Termination of cluster n emissioncoincides with beginning of cluster (n – 1)decay.
•Deactivation energies comparable to protonsolvation energies for the nth solvatingwater molecule.
PROCEDURE•Tip at optimum pot. for desired cluster•Background H2O pressure: 5 x 10-6 Torr•Temperature cycled linearly with time,remaining above 165 K to avoidcondensation
•Mass selected ion signal measured andimaged with MCPs; for mass 73 (n = 4),etc.
3.0 3.5 4.0 4.5 5.0 5.5 6.0
1000/T (K-1)
Lo
g o
f Io
n S
ign
al
∆E = 0.85 ± 0.03 ∆E = 0.76 ± 0.02
H+(H2O)4H+(H2O)3
∆E = 0.55 ± 0.02
H+(H2O)5
300K 250K 200K 167K
Time
Lo
g Io
n S
ign
al
150
160
170
180
190
200
210
220
230
240
250
Tip
Tem
per
atu
re, K
10 Minutes
H+(H2O)n H+(H2O)n–1
H+(H2O)n+1
H+(H2O)n*
H2O
Ion Emission(Field Dependent)
Desorption of nth
Solvating H2O(Thermally Activated)
Solvation byAdditional H2O(Positive ∆E)
ThermalDeactivation ofIon ClusterEmission
aOptimal observed applied field for cluster formation.
bH+ solvation energy associated with n-1 to n transition. [Meot-Ner]
cExperimentally observed solvation energies.
dCalculated emission energy based on ∆Esolv+lvap
(e.g. ∆Eemit(n=3) = 4.83eV - 0.82eV + 0.44eV = 4.45eV)
Lit ExpFapp
a ∆Esolv b ∆Esolv
c ∆Eemitd
V/Å eV eV eV
H+ n/a n/a - 12.55H+(H2O) 1.00 -7.22 - 5.77
H+(H2O)2 0.64 -1.38 - 4.83
H+(H2O)3 0.45 -0.82 -0.85 4.45
H+(H2O)4 0.34 -0.76 -0.76 4.12
H+(H2O)5 0.29 -0.50 -0.55 4.07
H+(H2O)6 0.27 -0.48 - 4.02
H+(H2O)7 0.26 -0.46 - 4.00
H2O*
(c)
180K
230K
Direct Imaging of Ion Clusters
PROCEDURE• Ion signal
directly imagedby FIM
• pw = 5x10-6 Torr• Tip at optimum
potential fordesired cluster
• 10 sec averagedpixel intensity
n>4 n=4 n=3
n=2 n=1 H2O+
n=2 n=1 Ne
Dissociation HumpFormation
Emission
Pt Pt Pt+ + + + + + + + + + +
Water Ion Cluster FormationProposed Mechanism
DecreasedLocal Radiusof Curvature
0.00
0.25
0.50
0.75
1.00
100 150 200 250
Temperature, K
Ap
plie
d F
ield
(V
/Å)
H2O+
H+(H2O)n1
234 - 6
Dissociation
RFD 1
RFD 2
FIEL
D F
REE
CO
ND
ENSA
TIO
N
Field dissociation (~ 0.7 eV)– Strong temperature dependence– Field-free dissociation at ~ 220K (Extrap)
Field ion emission (~ 4+ eV)– Not significantly temperature dependent
Ramped Field Desorption 1– Amorphous ice deposition– Field ramp passes through
emission fields for all clusters n≥ 2 before dissociation
– When ramp reaches dissociationfield, clusters n ≥ 2 are emittedsimultaneously.
Ramped Field Desorption 2– Field adsorbed layer– Field ramp activates dissociation
before emission– Cluster n emission observed,
each in turn.
Separating Ion Dissociation and Ion Emission
+
+
+
+
+
Field
DissociationRegion
•Shifting proton along the H-bond requires~0.6 V/Å
•Field in dissociation region is muchlower than applied field or field at watervacuum interface.
Field Induced Ion Dissociation
OH
H OH
H
~ 1.1Å
H
~ 0.7eV
+
+
+
+
+
Field
DissociationRegion
•Emission of ion cluster fromwater covered surface requires
∆Eemit / eV H+(H2O)n5.77 14.832 24.453 34.124 44.075 5
•Ion cluster can protrude nearsurface and experience enhancedlocal field
•Protrusion results in extendedlocal dissociation region
Field Induced Ion Emission
Summary of Results (I)• Moderate fields (0.2-0.5 V/Å) promote
water ionization
• Ionization occurs at electrode surface orin water adlayer
• Ionization and dielectric properties ofwater accessible
• Thermal activation barrier forionization: 0.7 eV
E
EE
EE E
EE
EEE
EE
EE
E
E
0.00.2
0.40.6
100 120 140 160 180 200 220
Onset F
ield Fo / V
Å-1
T / K
H2O / Pt
x 0
Temp. Dipole Permittivity
Amorph. < 130 K 3.9 D 10
Cryst. > 130 K 5.1 D 2.5
0V(xc)
xc
∆Eres
H3O
H+·(H 2O)mF
PiF
HO–H … OH2
xO–H
E
QHa
Summary II
• Water ion clusters H+(H2O)n fromfield adsorbed water detected for n upto 7 for temps. of 170-300 K
• Low fields favor large clusters(energetically favorable)
• High fields favor small clusters(kinetically favorable)
3.0 3.5 4.0 4.5 5.0 5.5 6.0
1000/T (K-1)
Lo
g o
f Io
n S
ign
al
∆E = 0.85 ± 0.03 ∆E = 0.76 ± 0.02
H+(H2O)4H+(H2O)3
∆E = 0.55 ± 0.02
H+(H2O)5
300K 250K 200K 167K
Summary III
• Ion emission of large clustersdeactivated at high temperatures due todesorption of solvating molecules
• Ion emission locally enhanced, possiblydue to hump formation.
H+(H2O)nH+(H2O)n–1
H+(H2O)n*
H2O*
Looking Ahead: E-Field Induced Ionization
• Ionic strength sensitive to electricfield– Small fields (0.2-0.5 V/Å)
required for ionization– Fields obtainable at several
hundred mV from PZC– Ionic strength near electrode
surface could be greatlydifferent than in bulkelectrolyte
• Enhance reactions that depend onH+ or OH– concentrations
• Hydrated ions may impedetransport of species to/from surface
Greater ionicstrength in regionof high field
E-Field Effects in Electrocatalysis
• Increased ionic strength nearsurface can increase OH–
concentration• Increased OH– can help remove
CO poison from fuel cell anodes• Catalyst design, i.e. addition of
other elements, should be thoughtin terms of influence on localelectric fields
O–C–O
Pt
Ru
–C–O
Future Experiments
• Temperature / flux dependence– Quantify ionization rates– Examine surface diffusion vs.
ionization– Adlayer thickness– Ionic diffusion through ice layer
• Field ionization of methanol– Pure methanol– Methanol/water mixtures– Consider methanol
adsorption/ionization for DMFC
• Ion energy deficit of waterionization– Measure appearance potential– ∆H of ionization– Influence of surface bonding– Combine with activation energy
results
• Negative field ionization– Probe OH– formation,
energetics, and hydration– Work function measurements
UniversityUniversityofof
WashingtonWashington
Top (l-r)Nallakkan (Arvind) Arvindan,
Chris Rothfuss, Eric Stuve
Bottom (l-r)Tom Madden,
Valentin Medvedev,Seng-Woon (David) Lim
Not shown: Laura Roen
Former members:Tim Pinkerton (Intel)Dawn Scovell (Intel)
UW ELECTROCHEMICALSURFACE SCIENCE
World’s LargestField Emitter Tip