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Last updated: 26 Feb 2006 by nmd
| [1] | Is the gas-particle partitioning in α-pinene secondary organic aerosol reversible? Geophys. Res. Lett. submitted, (A. Grieshop, N. M. Donahue, and A. L. Robinson) 2007. |
| [2] | Insights into the primary-secondary and regional-local contributions to organic aerosol in Pittsburgh, Pennsylvania. Atmos. Environ. submitted, (R. Subramanian, N. M. Donahue, A. Bernardo-Bricker, W. F. Rogge, and A. L. Robinson) 2007. |
| [3] | Evolving mass spectra of the oxidized component of organic aerosol: Results from Aerosol Mass Spectrometer analyses of aged diesel emissions. Atmos. Chem. Phys. Discuss. submitted, (A. M. Sage, E. A. Weitkamp, A. L. Robinson, and N. M. Donahue) 2007. |
| [4] | Ozonolysis of α-pinene: Parameterization of secondary organic aerosol mass fraction. Atmos. Chem. Phys. Discuss. submitted, (R. K. Pathak, A. A. Presto, T. E. Lane, C. O. Stanier, N. M. Donahue, and S. N. Pandis) 2007. |
| [5] | Temperature and ozone dependence of secondary organic aerosol production from β-pinene ozonolysis. Environ. Sci. Technol. submitted, (R. K. Pathak, K. E. Huff Hartz, N. M. Donahue, and S. N. Pandis) 2007. |
| [6] | Organic aerosol formation from photochemical oxidation of diesel exhaust. Environ. Sci. Technol. submitted, (E. Weitkamp, A. M. Sage, J. R. Pierce, N. M. Donahue, and A. L. Robinson) 2007. |
| [7] | Aging of organic aerosol: bridging the gap between laboratory and field studies. Ann. Rev. Phys. Chem. 58, 321-352 (Y. Rudich, N. M. Donahue, and T. F. Mentel) 2007. [ DOI | http ] |
| [8] | Rethinking organic aerosols: Semivolatile emissions and photochemical aging. Science 315, 1259-1263 (A. L. Robinson, N. M. Donahue, M. Shrivastava, A. M. Sage, E. A. Weitkamp, A. Greishop, T. E. Lane, S. N. Pandis, and J. Pierce) 2007. [ http ] |
| [9] | Secondary organic aerosol from limonaketone: Insights into terpene ozonlysis via synthesis of key intermediates. Phys. Chem. Chem. Phys. in press, (N. M. Donahue, J. E. Tischuk, B. Marquis, and K. E. Huff Hartz) 2007. [ DOI ] |
| [10] | Laboratory measurements of the oxidation kinetics of organic aerosol mixtures using a relative rate constants approach. J. Geophys. Res. 112, D04204 (K. E. Huff Hartz, E. A. Weitkamp, A. M. Sage, N. M. Donahue, and A. L. Robinson) 2007. [ DOI | www: ] |
| [11] | Controlled OH radical production via ozone-alkene reactions for use in aerosol aging studies. Environ. Sci. Technol. , 2357 - 2363 (A. T. Lambe, J. Zhang, A. M. Sage, and N. M. Donahue) 2007. [ DOI | http ] |
| [12] | Ozonolysis of α-pinene at atmospherically relevant concentrations: Temperature dependence of aerosol mass fractions (yields). J. Geophys. Res. 112, D03201 (R. K. Pathak, C. O. Stanier, N. M. Donahue, and S. N. Pandis) 2007. [ DOI | http ] |
| [13] | Secondary organic aerosol formation from limonene ozonolysis: Homogeneous and heterogeneous influences as a function of NOx. J. Phys. Chem. A 110, 11053-11063 (J. Zhang, K. E. Huff Hartz, S. N. Pandis, and N. M. Donahue) 2006. [ DOI | http ] |
| [14] | Source apportionment of molecular markers and organic aerosol - 2. Biomass smoke. Environ. Sci. Technol. 40, 7811-7819 (A. L. Robinson, R. Subramanian, N. M. Donahue, A. Bernardo-Bricker, and W. F. Rogge) 2006. [ .pdf ] |
| [15] | Contribution of motor vehicle emissions to organic carbon and fine particle mass in Pittsburgh, Pennsylvania: Effects of varying source profiles and seasonal trends in ambient marker concentrations. Atmos. Environ. 40, 8002-8019 (R. Subramanian, N. M. Donahue, A. Bernardo-Bricker, W. F. Rogge, and A. L. Robinson) 2006. [ DOI | http ] |
| [16] | Source apportionment of molecular markers and organic aerosol - 3. Food cooking emissions. Environ. Sci. Technol. 40, 7820-7827 (A. L. Robinson, R. Subramanian, N. M. Donahue, A. Bernardo-Bricker, and W. F. Rogge) 2006 (1). [ http ] |
| [17] | Investigation of α-pinene + ozone secondary organic aerosol formation at low total aerosol mass. Environ. Sci. Technol. 40, 3536-3543 (A. A. Presto and N. M. Donahue) 2006 (2). [ DOI | http ] |
| [18] | Constraining the mechanism and kinetics of OH + NO2 and HO2 + NO using the multiple-well master equation. J. Phys. Chem. A 110, 6898-6911 (J. Zhang and N. M. Donahue) 2006 (1). [ DOI | http ] |
| [19] | Coupled partitioning, dilution, and chemical aging of semivolatile organics. Environ. Sci. Technol. 40, 2635 - 2643 (N. M. Donahue, A. L. Robinson, C. O. Stanier, and S. N. Pandis) 2006 (3). [ DOI | http ] |
| [20] | Source apportionment of molecular markers and organic aerosol - 1. Methodology for visually comparing source profiles and ambient data. Environ. Sci. Technol. 40, 7803-7810 (A. L. Robinson, R. Subramanian, N. M. Donahue, A. Bernardo-Bricker, and W. F. Rogge) 2006 (1). [ .pdf ] |
| [21] | Photochemical oxidation and changes in molecular composition of organic aerosol in the regional context. J. Geophys. Res. 111, D03302 (A. L. Robinson, N. M. Donahue, and W. F. Rogge) 2006 (4), doi:10.1029/2005JD006265. [ http ] |
| [22] | Cloud condensation nuclei activation of limited solubility organic aerosol. Atmos. Environ. 40, 605-617 (K. E. Huff Hartz, J. E. Tischuk, M. N. Chan, C. K. Chan, N. M. Donahue, and S. N. Pandis) 2006 (2). [ DOI | http ] |
| [23] | Deconstructing experimental rate constant measurements: Obtaining intrinsic reaction parameters, kinetic isotope effects, and tunneling coefficients from kinetic data for OH + methane, ethane and cyclohexane. J. Photochem. Photobio. 176, 238-249 (A. M. Sage and N. M. Donahue) 2005. [ http ] |
| [24] | Critical factors determining the variation in SOA yields from terpene ozonolysis: A combined experimental and computational study. Faraday Disc. 130, 295-309 (N. M. Donahue, K. E. Huff Hartz, B. Chuong, A. A. Presto, C. O. Stanier, T. Rosenørn, A. L. Robinson, and S. N. Pandis) 2005 (7). [ http ] |
| [25] | Competitive oxidation in atmospheric aerosols: The case for relative kinetics. Geophys. Res. Lett. 32, L16805 (N. M. Donahue, A. L. Robinson, K. E. Huff Hartz, A. M. Sage, and E. Weitkamp) 2005 (3). [ http ] |
| [26] | Cloud condensation nuclei activation of monoterpene and sesquiterpene secondary organic aerosol. J. Geophys. Res. 110, D14208 (K. E. Huff Hartz, T. Rosenørn, S. R. Ferchak, T. M. Raymond, M. Bilde, N. M. Donahue, and S. N. Pandis) 2005 (5). [ http ] |
| [27] | Atmospheric volatile organic compound measurements during the Pittsburgh Air Quality Study: Results, interpretation, and quantification of primary and secondary contributions. J. Geophys. Res. 110, D07S07 (D. B. Millet, N. M. Donahue, S. N. Pandis, A. Polidori, C. O. Stanier, B. J. Turpin, and A. H. Goldstein) 2005 (10). [ http ] |
| [28] | Secondary organic aerosol production from terpene ozonolysis: 1. Effect of UV radiation. Environ. Sci. Technol. 39, 7036-7045 (A. A. Presto, K. E. Huff Hartz, and N. M. Donahue) 2005 (10). [ http ] |
| [29] | Secondary organic aerosol production from terpene ozonolysis: 2. Effect of NOx concentration. Environ. Sci. Technol. 36, 7046-7054 (A. A. Presto, K. E. Huff Hartz, and N. M. Donahue) 2005 (9). [ http ] |
| [30] | Hydrogen and helium pressure broadening of water transitions in the 380-600 cm-1 region. J. Spect. Quant. Rad. Trans. 83, 183-191 (D. W. Steyert, W. F. Wang, J. M. Sirota, N. M. Donahue, and D. C. Reuter) 2004 (2). [ http ] |
| [31] | Cycloalkene ozonolysis: Collisionally mediated mechanistic branching. J. Am. Chem. Soc. 126, 12363-12373 (B. Chuong, J. Zhang, and N. M. Donahue) 2004 (3). [ http ] |
| [32] | On the mechanism for nitrate formation via the peroxy radical + NO reaction. J. Phys. Chem. A 108, 9082-9095 (J. Zhang, T. Dransfield, and N. M. Donahue) 2004 (11). [ http ] |
| [33] | Fitting multiple datasets in kinetics: n-butane + OH -> products. Int. J. Chem. Kin. 36, 259-272 (N. M. Donahue and J. S. Clarke) 2004 (2). [ http ] |
| [34] | Ozonolysis fragment quenching by nitrate formation: The pressure dependence of prompt OH radical formation. J. Phys. Chem. A 108, 9096-9104 (A. A. Presto and N. M. Donahue) 2004 (3). [ http ] |
| [35] | Reaction barriers: Origin and evolution. Chem. Rev. 103, 4593-4604 (N. M. Donahue) 2003 (13). [ http ] |
| [36] | Pressure broadening coefficients of rotational transitions of water in the 380-600 cm-1 range. J. Spect. Quant. Rad. Trans. 72, 775-782 (D. W. Steyert, W. F. Wang, D. C. Reuter, M. Sirota, and N. M. Donahue) 2002 (7). [ http ] |
| [37] | Gas-phase ozonolysis of alkenes: formation of OH from anti carbonyl oxides. J. Am. Chem. Soc. 124, 8518-8519 (J. H. Kroll, V. J. Cee, N. M. Donahue, K. L. Demerjian, and J. G. Anderson) 2002 (16). [ http ] |
| [38] | Product analysis of the OH oxidation of isoprene and 1,3-butadiene in the presence of NO. J. Geophys. Res. A 107, 4268 (M. Sprengnether, K. L. Demerjian, N. M. Donahue, and J. G. Anderson) 2002 (4). [ http ] |
| [39] | Revisiting the Hammond postulate: The role of reactant and product ionic states in regulating barrier heights, locations, and frequencies. J. Phys. Chem. A 105, 1489-1497 (N. M. Donahue) 2001 (24). [ http ] |
| [40] | Constraining the mechanism of OH + NO2 using isotopically labeled reactants: Experimental evidence for HOONO formation. J. Phys. Chem. A 105, 1515-1520 (N. M. Donahue, M. K. Dubey, R. Mohrschladt, T. J. Dransfield, and J. G. Anderson) 2001 (34). [ http ] |
| [41] | High pressure flow reactor product study of the reactions of HOx + NO2: The role of vibrationally excited intermediates. J. Phys. Chem. A 105, 1507-1514 (T. J. Dransfield, N. M. Donahue, and J. G. Anderson) 2001 (22). [ DOI | http ] |
| [42] | Mechanism of HOx formation in the gas-phase ozone-alkene reaction: 1. Direct, pressure-dependent measurements of OH yields. J. Phys. Chem. A 105, 1554-1560 (J. H. Kroll, J. S. Clarke, N. M. Donahue, J. G. Anderson, and K. L. Demerjian) 2001 (46). [ http ] |
| [43] | Mechanism of HOx formation in the gas-phase ozone-alkene reaction: 2. Prompt versus thermal dissociation of carbonyl oxides to form OH. J. Phys. Chem. A 105, 4446-4457 (J. H. Kroll, S. Shahai, J. Anderson, K. L. Demerjian, and N. Donahue) 2001 (43). [ http ] |
| [44] | Accurate, direct measurements of OH yields from ozone-alkene reactions using the Harvard HOx instrument. Geophys. Res. Lett. 28, 3863-3866 (J. H. Kroll, T. F. Hanisco, N. M. Donahue, J. G. Anderson, and K. L. Demerjian) 2001 (11). [ http ] |
| [45] | Near-field influence on barrier evolution in symmetric atom transfer reactions: A new model for two-state mixing. J. Phys. Chem. A 105, 1498-1506 (H. A. Rypkema, N. M. Donahue, and J. G. Anderson) 2001 (6). [ http ] |
| [46] | Multiple excited states in a two-state crossing model: Predicting barrier height evolution for H + alkene addition reactions. J. Phys. Chem. A 104, 4458 - 4468 (J. S. Clarke, H. A. Rypkema, J. H. Kroll, N. M. Donahue, and J. G. Anderson) 2000 (11). [ http ] |
| [47] | An experimental method for testing reactivity models: A high-pressure discharge-flow study of H + alkene and haloalkene reactions. J. Phys. Chem. A 104, 5254 - 5264 (J. S. Clarke, J. H. Kroll, H. A. Rypkema, N. M. Donahue, and J. G. Anderson) 2000 (6). [ http ] |
| [48] | Fourier transform ultraviolet spectroscopy of the A2Π3/2 <- X2Π3/2 transition of BrO. J. Phys. Chem. A 103, 8935-8945 (D. M. Wilmouth, T. F. Hanisco, N. M. Donahue, and J. G. Anderson) 1999 (36). [ http ] |
| [49] | Temperature and pressure dependent kinetics of the gas-phase reaction of the hydroxyl radical with nitrogen dioxide. Geophys. Res. Lett. 26, 687-690 (T. J. Dransfield, K. K. Perkins, N. M. Donahue, J. G. Anderson, M. M. Sprengenther, and K. L. Demerjian) 1999 (52). [ http ] |
| [50] | Testing frontier orbital control: OH + ethane, propane, and cyclopropane from 180 K to 360 K. J. Phys. Chem. A 102, 9847-9857 (J. S. Clarke, J. H. Kroll, N. M. Donahue, and J. G. Anderson) 1998 (40). [ http ] |
| [51] | New rate constants for ten OH alkane reactions from 300 to 400 K: An assessment of accuracy. J. Phys. Chem. A 102, 3121-3126 (N. M. Donahue, K. L. Demerjian, and J. G. Anderson) 1998 (39). [ http ] |
| [52] | Direct observation of OH production from the ozonolysis of olefins. Geophys. Res. Lett. 25, 59-62 (N. M. Donahue, J. H. Kroll, J. G. Anderson, and K. L. Demerjian) 1998 (75). [ http ] |
| [53] | Predicting radical-molecule barrier heights: The role of the ionic surface. J. Phys. Chem. A 102, 3923-3933 (N. M. Donahue, J. S. Clarke, and J. G. Anderson) 1998 (44). [ http ] |
| [54] | Comment on: “The measurement of tropospheric OH radicals by laser-induced fluorescence spectroscopy during the POPCORN field campaign,” by Hofzumahaus et al., and “Intercomparison of tropospheric OH radical measurements by multiple folded long path laser absorption and laser induced fluorescence,” by Brauers et al. Geophys. Res. Lett. 24, 3039-3038 (E. J. Lanzendorf, T. R. Hanisco, N. M. Donahue, and P. O. Wennberg) 1997 (20). [ http ] |
| [55] | High pressure flow study of the reactions OH + NOx -> HONOx: Errors in the falloff region. J. Geophys. Res. 102, 6159-6168 (N. M. Donahue, M. K. Dubey, R. Mohrschladt, K. L. Demerjian, and J. G. Anderson) 1997 (69). [ http ] |
| [56] | Isotope specific kinetics of hydroxyl radical (OH) with water (H2O): Testing models of reactivity and atmospheric fractionation. J. Phys. Chem. A 101, 1494-1500 (M. K. Dubey, R. Mohrschladt, N. M. Donahue, and J. G. Anderson) 1997 (45). [ http ] |
| [57] | Free radical kinetics at high pressure: A mathematical analysis of the flow reactor. J. Phys. Chem. 100, 5821-5838 (N. M. Donahue, J. S. Clarke, K. L. Demerjian, and J. G. Anderson) 1996 (36). [ http ] |
| [58] | Reaction modulation spectroscopy: A new approach to quantifying reaction mechanisms. J. Phys. Chem. 100, 17855-17861 (N. M. Donahue, K. L. Demerjian, and J. G. Anderson) 1996 (12). [ http ] |
| [59] | In situ nonmethane hydrocarbon measurements on SAGA 3. J. Geophys. Res. 97, 16915-16932 (N. M. Donahue and R. G. Prinn) 1993 (52). [ http ] |
| [60] | Ozone observations and a model of marine boundary layer photochemistry during SAGA 3. J. Geophys. Res. 97, 16955-16968 (A. M. Thompson, J. E. Johnson, A. L. Torres, T. S. Bates, K. C. Kelly, E. Atlas, J. P. Greenberg, N. M. Donahue, S. A. Yvon, E. S. Saltzman, B. G. Heikes, B. W. Mosher, A. A. Shashkov, and V. I. Yegorov) 1993 (92). [ http ] |
| [61] | Nonmethane hydrocarbon chemistry in the remote marine boundary layer. J. Geophys. Res. 95, 18387-18411 (N. M. Donahue and R. G. Prinn) 1991 (63). [ http ] |
| [62] | Relationship between peroxyacetyl nitrate (PAN) and nitrogen oxides in the clean troposphere. Nature 318, 347-349 (H. L. Singh, B. Ridley, J. Shetter, N. M. Donahue, F. Fehsenfeld, D. Fahey, D. Parish, E. Williams, S. Liu, G. Hebler, and P. Murphy) 1985 (72). [ .html ] |
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