2928 J. Phys. Chem. A, Vol. 111, No. 15, 2007
Park et al.
that may coalesce within or on aerosol droplets and segregate
to the surface to form mixed monolayers of widely varying
porosity and reactivity.27 We hope to extend the alcohol
measurements here to soluble organic molecules with different
functional groups to determine their surface activity in sulfuric
acid and their ability to impede or enhance gas-liquid transport
and interfacial reactions.
HNO3 desorption was also measured for a much shorter
observation time of 0.27 s using a continuously rotating wheel.
In this case, fremain rises from 0.18 to 0.52. Despite this large
correction, the final value for γ(N2O5) was determined to be
the same in the bare acid, 0.15 ( 0.02, suggesting that the stop-
start technique may not be necessary to determine hydrolysis
probabilities even when the HNO3 product dissolves for long
times.
No corrections are necessary for HCl dissolution in 72 wt %
H2SO4 at 216 K because τ is so short (τ ) 2 × 10-4 and fremain
) 0.03). HBr dissolves for longer times in the bare acid (τ )
0.002 s and fremain ) 0.09), but again drops to 2 × 10-4 s in the
alkyl-coated acids because R ≈ fexch is larger. The value for
HBr entering the bare acid in Table 1 has been corrected for a
10% increase due to HBr molecules accumulating in solution
over the 0.27 s exposure and observation time.
Acknowledgment. We are grateful to the Air Force Office
of Scientific Research for supporting this work, to the Camille
and Henry Dreyfus Foundation for providing a postdoctoral
fellowship in environmental chemistry to S.-C.P., and to the
Vilas Foundation of the University of Wisconsin. We also thank
John Morris for performing early studies of N2O5 on bare
sulfuric acid, James Krier and Casey Harris for surface tension
measurements, and Steven Brown for advice on N2O5 synthesis.
We also thank the reviewers for their valuable comments.
References and Notes
(1) Finlayson-Pitts, B. J.; Pitts, J. N. Chemistry of the Upper and Lower
Atmosphere; Academic Press: New York, 2000; Chapters 9.C and 12.C.
(2) Solomon, S. ReV. Geophys. 1999, 37, 275.
Appendix: Determining the Fraction of HNO3 Remaining
in Solution
(3) Hanson, D. R.; Lovejoy, E. R. J. Phys. Chem. 1996, 100, 6397.
(4) Jacob, D. Atmos. EnViron. 2000, 34, 2131.
We determine the fraction of N2O5 molecules that are
converted into HNO3 by measuring the relative flux of HNO3
molecules that desorb from solution. Because some of the HNO3
molecules created by hydrolysis remain behind in solution over
(5) Rodriguez, J. M.; Ko, M. K. W.; Sze, N. D. Nature 1991, 352,
134.
(6) Hanson, D. R.; Ravishankara, A. R.; Solomon, S. J. Geophys. Res.
Atmos. 1994, 99, 3615.
the measurement time texp, the measured flux IHNO in eq 2 is
3
(7) Wennberg, P. O.; Cohen, R. C.; Stimpfle, R. M.; Koplow, J. P.;
Anderson, J. G.; Salawitch, R. J.; Fahey, D. W.; Woodbridge, E. L.; Keim,
E. R.; Gao, R. S.; Webster, C. R.; May, R. D.; Toohey, D. W.; Avallone,
L. M.; Proffitt, M. H.; Loewenstein, M.; Podolske, J. R.; Chan, K. R.; Wofsy,
S. C. Science 1994, 266, 398.
(8) Fahey, D. W.; Kawa, S. R.; Woodbridge, E. L.; Tin, P.; Wilson, J.
C.; Jonsson, H. H.; Dye, J. E.; Baumgardner, D.; Borrmann, S.; Toohey,
D. W.; Avallone, L. M.; Proffitt, M. H.; Margitan, J.; Loewenstein, M.;
Podolske, J. R.; Salawitch, R. J.; Wofsy, S. C.; Ko, M. K. W.; Anderson,
D. E.; Schoeberl, M. R.; Chan, K. R. Nature 1993, 363, 509.
(9) Hendricks, J.; Lippert, E.; Petry, H.; Ebel, A. J. Geophys. Res.
Atmos. 1999, 104, 5531.
(10) See, for example, Badger, C. L.; Griffiths, P. T.; George, I.; Abbatt,
J. P. D.; Cox, R. A. J. Phys. Chem. A 2006, 110, 6986 and ref 19.
(11) Dentener, F. J.; Crutzen, P. J. J. Geophys. Res. Atmos. 1993, 98,
7149.
(12) Tie, X.; Emmons, L.; Horowitz, L.; Brasseur, G.; Ridley, B.; Atlas,
E.; Stround, C.; Hess, P.; Klonecki, A.; Madronich, S.; Talbot, R.; Dibb, J.
J. Geophys. Res. 2003, 108, 8364.
TD
too small. This flux can be corrected by estimating the fraction
of HNO3 molecules that remain dissolved in the acid. The
predicted thermal-desorption flux from a fresh liquid continu-
ously exposed for a time texp is Itrue ) Ienter(1 - (erfc[(texp/τ)1/2]‚
TD
etexp/τ),66 where Ienter is the equivalent flux of HNO3 entering
the solution generated by the impinging N2O5 molecules. This
flux depends on the characteristic residence time τ of the HNO3
molecules in solution. It is given by τ ) D(4H*RT/Rth V )2,
where H* is the overall solubility of HNO3 in M atm-1, D is
the HNO3 diffusion constant, Rth is the HNO3 entry probability
averaged over a Boltzmann distribution of collision energies at
temperature T, and V is the thermal velocity of HNO3. Over
the time t ) 0 to τ, the desorption flux rises from 0 to 57% of
the flux entering solution. We use the values H* ) 2 × 106 M
atm-1 for HNO3 in 72 wt % H2SO4 at 216 K from ref 43, D )
7 × 10-9 cm2 s-1 from ref 42, and Rth ) 1 from ref 53 to obtain
τ ) 0.2 s.
(13) Evans, M. J.; Jacob, D. J. Geophys. Res. Lett. 2005, 32, L09813.
(14) Hanson, D. R.; Ravishankara, A. R. J. Geophys. Res. Atmos. 1991,
96, 17307.
(15) Zhang, R. Y.; Leu, M. T.; Keyser, L. F. Geophys. Res. Lett. 1995,
22, 1493.
The fraction fremain of HNO3 molecules that accumulate within
the acid over the time texp is given by eq 8c in ref 67, where it
is also graphed:
(16) Fried, A.; Henry, B. E.; Calvert, J. G.; Mozurkewich, M. J. Geophys.
Res. Atmos. 1994, 99, 3517.
(17) Robinson, G. N.; Worsnop, D. R.; Jayne, J. T.; Kolb, C. E.;
Davidovits, P. J. Geophys. Res. Atmos. 1997, 102, 3583.
(18) Williams, L. R.; Manion, J. A.; Golden, D. M.; Tolbert, M. A. J.
Appl. Meteorol. 1994, 33, 785.
(19) Kane, S. M.; Caloz, F.; Leu, M.-T. J. Phys. Chem. A 2001, 105,
6465.
(20) Murphy, D. M.; Thomson, D. S.; Mahoney, T. M. J. Science 1998,
282, 1664.
(21) Singh, H.; Chen, Y.; Tabazadeh, A.; Fukui, Y.; Bey, I.; Yantosca,
R.; Jacob, D.; Arnold, F.; Wohlfrom, K.; Atlas, E.; Flocke, F.; Blake, D.;
Blake, N.; Heikes, B.; Snow, J.; Talbot, R.; Gregory, G.; Sachse, G.; Vay,
S.; Kondo, Y. J. Geophys. Res. Atmos. 2000, 105, 3795.
(22) Singh, H.; Chen, Y.; Staudt, A.; Jacob, D.; Blake, D.; Heikes, B.;
Snow, J. Nature 2001, 410, 1078.
(23) Apel, E. C.; Hills, A. J.; Lueb, R.; Zindel, S.; Eisele, S. J. Geophys.
Res. 2003, 108, 8794.
(24) Tervahattu, H.; Juhanoja, J.; Vaida, V.; Tuck, A. F.; Niemi, J. V.;
Kupiainen, K.; Kulmala, M.; Vehkamaki, H. J. Geophys. Res. Atmos. 2005,
110, D06207.
texp
true
TD
Ientertexp
-
I
dt
∫
0
fremain(texp) )
Ienter exp
t
) (τ/texp){erfc[(texp/τ)1/2] etexp/τ + 2(texp/πτ)1/2 - 1)}
(A.1)
For texp ) 6 s and τ ) 0.2 s, fremain is 0.18, indicating that 18%
of the HNO3 molecules remain in the acid even over times much
longer than τ. In this case, IdTiDff should be divided by 0.82 in eq
2 to obtain the true relative flux. This correction increases
frxn(bare) from 0.12 to 0.15, frxn(hexyl) from 0.05 to 0.06, and
frxn(butyl) from 0.08 to 0.10 in Table 1, where the corrected
(25) Brown, S. S.; Ryerson, T. B.; Wollny, A. G.; Brock, C. A.; Peltier,
R.; Sullivan, A. P.; Weber, R. J.; Dube, W. P.; Trainer, M.; Meagher, J. F.;
Fehsenfeld, F. C.; Ravishankara, A. R. Science 2006, 311, 67.
(26) Barnes, G. T. Colloids Surf. A. 1997, 126, 149.
(27) Gilman, J. B.; Vaida, V. J. Chem. Phys. A 2006, 110, 7581.
quantities are labeled γ and represent our best estimates of the
hydrolysis probabilities. The ratios of frxn before and after
correction remain essentially unchanged, such that γfilm/γbare
rxn(film)/frxn(bare).
≈
f