acetone and hydroperoxyl radical equilibrium certainly fascinating, but is it important to you?
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Acetone and Hydroperoxyl Radical Equilibrium Certainly Fascinating, But Is It Important To You?. Fred Grieman, Aaron Noell, Stan Sander, Mitchio Okumura Funding: NASA Upper Atmospheric Research Program NASA Senior Post-Doctoral Fellowship - PowerPoint PPT PresentationTRANSCRIPT
Acetone and Hydroperoxyl Radical Equilibrium
Certainly Fascinating, But Is It Important To You?
Fred Grieman, Aaron Noell, Stan Sander, Mitchio Okumura
Funding: NASA Upper Atmospheric Research Program NASA Senior Post-Doctoral Fellowship NASA Summer Faculty Research Fellow Program
HO2/OH Atmospheric ChemistryImportance to you?
Laboratory Study of and Atmospheric Observation of HOx Radicals
For example: Photochemical Ozone Production
Simplified Tropospheric Chemistry
Volatile Organic Compounds
Oxygenated Volatile Organic Compounds
Understanding Atmospheric Chemistry
Overall Picture
HO2 + Acetone HO2Acetone (CH3)2C(OH)OO?Acetone in the Upper Atmosphere• One of main OVOCs in the Upper Troposphere (UT)
• Key source of OH and HO2 (HOx) from photolysis
• Primary loss pathways in Upper Troposphere: Photolysis, Reaction with OH
• Recent experiments by Blitz, Orr-Ewing, Heard, Pilling suggest much lower photolysis yields at low T
An alternate oxidation pathway in the atmosphere? Possible Reaction with HO2?• Hydrogen radicals in Upper Troposphere: HOx = OH, HO2
• In the atmosphere, [HO2] >> [OH]
• HO2 is known to react rapidly with formaldehyde at room temperature
Literature?
So, YES!!! Determination of Acetone/Hydroperoxyl Radical Equilibrium IS Important to YOU!
Int. J. Chem. Kinet. 32, 573 (2000).
ADDUCT
PEROXY RADICAL HO(iPr)OO
REACTANTS
COMPUTED STATIONARY POINTSB3LYP/cc-pVTZ GeometriesG2Mc/DFT Energies
HO2 + Acetone HO2Acetone (CH3)2C(OH)OO?
MOLECULAR COMPLEX
Atmospheric Loss Process
1. HO2 + Acetone are in equilibrium with peroxy (H-bonded molecular complex is pre-equilibrium config)
HO2 + CH3C(O)CH3 → HOC(CH3)2OO
k(200K) = 6.9 10-12 cm3 s-1 Kc(210K) = 6.0 10-13 cm3
2. Peroxy radical reacts with HO2 or NO, leading to loss of HO2 (then important to include in HO2 / OH budget)
3. Acetone sink: If Herman’s et al. calculation correct, HO2 removal on par with photolysis & greater than from OH
Abstraction
Addition
Higher Barrier – NO REACTION!
Does this rxn occur at relevant atmospheric T?
Kc(T)
2.27E-172.32E-151.17E-133.05E-12
k+
4.50E-131.06E-122.20E-124.04E-12
k-
1.98E+044.58E+021.89E+011.33E+00
How?? Experimental Determination via Infrared Kinetics Spectroscopy (IRKS)
HO2 + CH3C(O)CH3 ⇌ HOC(CH3)2OOk+
k-
Because k- is so large, Keq is the quantity that determines effective rate of removal
Excimer laser308 nm
D2 lamp
diode laser
detector
low pass filter
monochromator
computer
6.8 MHz current modulator
2x/phase shifter
demodulated signal
FM signal
gas entranceexit exit
Herriott cellPD
Infrared Kinetic Spectroscopy Apparatus
UV
NIR{2ν(OH)}
T-controlled FLOW CELL
λ = 220 nm (near HO2 max)
Cl2 + hν → 2 ClCl + CH3OH → CH2OH + HClCH2OH + O2 → HO2 + CH2O
Herriot Cell Mirror
FM Detection of HO2 NIR Lines by Diode Laser InGaAs/InP single-mode DFB Diode Lasers 1.4 and 1.5 m fabricated at JPL,Selectivity for HO2
Detection of single rotational linesWavelength Modulation 2f detection at 7 MHz modulation Near shot-noise limited detectionHerriott Cell 30 passes, Leff = 2000 cmSensitivity (Minimum detectable absorption) 5x107 Hz or 2. 5x1010 cm1HzHO2 Detection Limit (6636 cm1, 295K, 100 Torr):
1.0 x 10 cm3 1 Hz 3 x 10 cm 10kHz, 1 shot
HO2 line6625.80 cm-1
-1.0
-0.5
0.0
0.5
1.0
1.5
-40 -30 -20 -10 0 10 20 30 40
Relative Frequency (milli-cm-1)
HO2 S
igna
l (m
icro
volt)
Association Reaction
HO2 + (CH3)2CO ⇄ (CH3)2CO---HO2
isomerization ↓ (CH3)2COH ← (CH3)2CO---H †
O▬O O▬O
MOLECULARCOMPLEX
2-hydroxyisopropylperoxy (2-HIPP)
0.16
0.14
0.12
0.10
0.08
0.06
0.04
0.02
0.00
1086420ms
IR05t [Ace] = 0 IR06t 2.24e15 IR09t 2.98e15 IR10t 3.50e15 IR13t 4.52e15 IR14t 5.62e15
HO2 NIR Decay Curves at Varying [Acetone]
T = 221 K T = 297 K
0.12
0.10
0.08
0.06
0.04
0.02
0.00
3020100ms
IR02t [Ace] = 0.0e15 IR03t 2.18 IR04t 4.06 IR05t 5.48 IR06t 5.41 IR07t 7.09 IR08t 9.93 IR09t 12.8 IR10t 17.5 IR11t 20.5
Time (msec)Time (msec)
HO
2 A
bsor
banc
e Dramatic decreasein [HO2] at lower T& same [Acetone]
Measuring [HO2] decay upon adding Acetone
Does not occur at room T, but may at lower T
Measure with increasing [Acetone]
Preliminary Result:
No HO2 + Acetone rxn !!! Must consider all chemistry Cl + Acetone HCl + CH3C(O)CH2
Decreases HO2 made Slows at Low T {k(297) = 2.1E-12 ; k(221) = 1.0E-12)}
Interpretation: 1) Complexation occurs at lower T 2) Equilibrium reached quickly followed by HO2 rxns
Fitting Rise and Fall of Short time decay not possible
Method Developed: • Fit Longer time decay with simple HO2 self-reaction• Determine [HO2] at time = 0, w/out & w/ [Acetone]• Correct for Cl + Acetone reaction• Determine Keq from equilibrium concentrations• Repeat for several [Acetone] at several T• Keq(T) ΔrH & ΔrS
First must determine Cl + Acetone reaction at T=298K
0.16
0.14
0.12
0.10
0.08
0.06
0.04
0.02
0.00
1086420ms
IR05t [Ace] = 0 IR06t 2.24e15 IR09t 2.98e15 IR10t 3.50e15 IR13t 4.52e15 IR14t 5.62e15
0.12
0.10
0.08
0.06
0.04
0.02
0.00
3020100ms
IR02t [Ace] = 0.0e15 IR03t 2.18 IR04t 4.06 IR05t 5.48 IR06t 5.41 IR07t 7.09 IR08t 9.93 IR09t 12.8 IR10t 17.5 IR11t 20.5
80
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
210
-1-2
x10-3
0.10
0.08
0.06
0.04
0.02
0.00
IR s
igna
l/ (V
)
1086420ms
3210
-1-2
x10-3
0.10
0.08
0.06
0.04
0.02
0.00
IR s
igna
l/ (V
)
1086420ms
3210
-1-2
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
210
-1
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
210
-1-2
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
210
-1
x10-3
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
3210
-1-2
x10-3
70
60
50
40
30
20
10
0
IR s
igna
l/ (V
x10
-3 )
1086420ms
2
0
-2
x10-3
Cl + CH3C(O)CH3 → HCl + CH3C(O)CH2 (~10 sec)
O2 + CH3C(O)CH2 → CH3C(O)CH2OO (fast excess O2)
HO2 + CH3C(O)CH2OO → Products (k12f)
HO2 + HO2 → H2O2 + O2 (k1f)
Fit with literature k12f and k1f from [Acetone] = 0 fit
Agree w/ lit. (no HO2 + Acetone reaction at Room T)
T =297 K
Fits of Cl chemistry with Acetone & O2
0.14
0.12
0.10
0.08
0.06
0.04
0.02
0.00
IR s
igna
l/ (V
)
3.53.02.52.01.51.00.50.0ms
43210
-1-2
x10-3
0.16
0.14
0.12
0.10
0.08
0.06
0.04
0.02
0.00
IR s
igna
l/ (V
)
3.02.52.01.51.00.50.0ms
3210
-1-2
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10-3
)
3.53.02.52.01.51.00.50.0ms
210
-1
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10-3
)
3.53.02.52.01.51.00.50.0ms
1.0
0.0
-1.0
x10-3
80
60
40
20
0
IR s
igna
l/ (V
x10-3
)
3.02.52.01.51.00.50.0ms
1.00.50.0
-0.5-1.0
x10-3
60
40
20
0
IR s
igna
l/ (V
x10-3
)
3.53.02.52.01.51.00.50.0ms
1.0
0.0
-1.0
x10-3
Preliminary objective: Determine thermodynamics
Family of NIR HO2 decay curves at T = 221Kat varying acetone concentrations
0.16
0.14
0.12
0.10
0.08
0.06
0.04
0.02
0.00
1086420ms
IR05t [Ace] = 0 IR06t 2.24e15 IR09t 2.98e15 IR10t 3.50e15 IR13t 4.52e15 IR14t 5.62e15
Cannot Fit Curves with Cl reactions
Initial analysis: find [HO2]o([Ace]) at t = 0 s to determine equilibrium concentration prior to
subsequent kinetics
60
40
20
0
IR s
igna
l/ (V
x10
-3 )
3.53.02.52.01.51.00.50.0ms
1.0
0.0
-1.0
x10-3
1) [HO2]o(0) determined from fit & corrected for Cl rxn with Acetone
2) [HO2]eq = [HO2]o([Ace]) determined from fit
3) [Complex] = [HO2]o(0) – [HO2]o([Ace]) [Complex]Keq = [Ace] [HO2]o([Ace]) (excess)
Measure Keq at several atmospherically relevant temperatures
T(K) (2 Kc(cm3/molec) (pph)
215.6 2.957E-16 12.7220.7 1.506E-16 6.9222.5 1.227E-16 9.9226.8 9.087E-17 13.7227.6 7.856E-17 17.3231.9 7.177E-17 22.5232.3 5.977E-17 9.5237.1 3.955E-17 5.8242.7 2.589E-17 12.6243.5 2.451E-17 17.4245.9 2.961E-17 1.6249.6 2.898E-17 5.2254.5 1.335E-17 16.9266.2 1.408E-17 23.7272.3 7.671E-18 18.3
Kc(T) (cm3 molec-1) Van’t Hoff Plot: Rln(Kp) vs. 1/T slope = -ΔrH°; intercept = ΔrS°
ΔrH° = -31 1.7 kJ/molΔrS° = -70 7.2 J/mol/K
ΔrG° = ΔrH° - T ΔrS° Keq(T) = exp (- ΔrG° /RT)
Van't Hoff Plot (not weighted)
y = 30.97x - 0.0700R2 = 0.9614
0.040
0.045
0.050
0.055
0.060
0.065
0.070
0.075
0.080
0.00360 0.00380 0.00400 0.00420 0.00440 0.004601/T(K-1)
Rln
Kp
Comparison of Equilibrium ConstantsKc, cm3 molec-1
More ComparisonsReaction Thermodynamics Compared to Calculated Values
Aloisio product:
Like complex!!!
Reaction to Complex
HO2 + (CH3)2CO ⇄ (CH3)2CO---HO2
↓ (CH3)2CO---H †
O▬O
MOLECULARCOMPLEX
Herman et al.
Cours et al.
Aloisio et al.
Both Planar
Perpendicular
Calculations
Comparison with Methanol and Water
Source ΔrHo (kJ/mol) Do (kJ/mol)
HO2 + Acetone(This Work)
-31
HO2 + Methanol(Christiensen et al., 2006)
-36.8
H2O + H2O(Curtiss et al., 1979)
-15.0
HO2Acetone(Aloisio et al., 2000)
37.3
HO2Methanol(Christiensen et al., 2006)
35.7
H2OH2O(Klopper et al., 1995)
21.0
Atmospheric Implications(Just a taste.)
Analysis by Hermans et al.: Acetone removal (keff) from UT Keq
At 190 K, keff = 5 x 10-6 s-1 which is greater than acetone photolysis (4 x 10-7 s-1)
However, if our results are correct and 2-HIPP is product: Keq = 1.9 x 10-15
compared to Hermans et al. Keq = 2.0 x 10-11
keff = 4.3 x 10-10 s-1
Summary
• Discovered reaction between HO2 + Acetone
• Developed Method to Determine Keq for HO2/Carbonyl Reactions
• Able to Measure Keq Over Wide Temperature Range Including Atmospherically Relevant Temperatures
• Thermodynamic Parameters Determined: Possible Clues to Reaction Product and Its Structure
• Will Be Able to Determine Its Impact on the Atmosphere
Future Work
1) Search for products (acetonylperoxy, 2-HIPP, Molecular Complex)
We have done some of this: T = 297 K acetonylperoxy: CH3C(O)CH2OO
12
10
8
6
4
2
0
-2
-4
x10-3
2520151050ms
12
10
8
6
4
2
0
-2
-4
x10-3
2520151050ms
σ(cm2/molec) at λuv = 280 nm
2.07E-18 acetonylperoxy
0 HO2
2.00E-20 H2O2
[Ace] = 0 [Ace] = 2.05E16
For (CH3)2C(OH)OO and (CH3)2C(O)OOH
No spectrum observed in uv; Calculations underway to estimate OH stretching frequency and A-X transition
2) Measure forward rate constant
Very difficult work; has been accomplished for HO2 + methanol
3) Apply this method to many HO2 / Carbonyl systems: MEK, Acetaldehyde, Formaldehyde
Acknowledgements
HarryKroto
AaronNoell
StanSander
MitchioOkumura
The research described in this paper was carried out at the Jet Propulsion Laboratory, California Institute of Technology under contract to the National Aeronautics and Space Administration
*This research was supported by an appointment of Fred Grieman to the NASA Postdoctoral Program at the Jet Propulsion Laboratory, administered by Oak Ridge Associated Universities through a contract with NASA.
The Future
KiraWatson
Casey Davis-Van Atta
AileenHui
1st yr.Caltech
GradStudent(not shown)
PomonaChem Majors