Table 1. Observed pseudo-first order rate constants for the reaction of Py on the substrates examined in this study with 3 ppmv NO2 (kobs), apparent reaction probabilities of NO2 with the surface-adsorbed Py (γ), percentage of degraded Py (DPy), yields of 1-NP (Y1−NP), and initial surface coverages of Py (θPy,0).
Substrates | kobs × 105 (s−1)* | γ × 108* | DPy (%)† | Y1−NP (%)† | DNP formation‡ | θPy,0 × 102 |
---|---|---|---|---|---|---|
Chinese desert dust (CDD) | 86 ± 4 | 14 ± 1 | 96 | 53 | + | 2.8 |
Arizona test dust (ATD) | 36 ± 1 | 6.1 ± 0.2 | 88 | 58 | + | 7.7 |
Kaolin§ | 110 ± 10 | 18 ± 1 | 98 | 60 | + | 1.5 |
Montmorillonite A | 53 ± 5 | 9.0 ± 0.8 | 95 | 89 | + | 2.0 |
Montmorillonite B | 29 ± 4 | 4.9 ± 0.7 | 84 | 79 | + | 5.8 |
Saponite | 39 ± 3 | 6.6 ± 0.4 | 82 | 73 | − | 0.27 |
Potassium feldspar | 1.1 ± 0.2 | 0.19 ± 0.03 | 14 | 10 | − | 11 |
Sodium feldspar | 0.30 ± 0.06 | 0.05 ± 0.01 | 12 | 6 | − | 58 |
Feldspar | 0.86 ± 0.14 | 0.15 ± 0.02 | 17 | 4 | − | 27 |
Limestone | 1.4 ± 0.1 | 0.24 ± 0.01 | 18 | 5 | − | 21 |
Dolomite | 0.83 ± 0.15 | 0.14 ± 0.03 | 16 | 4 | − | 11 |
Calcium sulfate | 1.5 ± 0.5 | 0.25 ± 0.09 | 6 | 0 | − | 49 |
Quartz | 1.7 ± 0.1 | 0.28 ± 0.01 | 9 | 5 | − | 63 |
Aluminum oxide | 0.25 ± 0.00 | 0.04 ± 0.00 | 2 | 1 | − | 6.7 |
Iron (III) oxide | 9.0 ± 3.3 | 1.5 ± 0.6 | 17 | 0 | − | 6.9 |
Titanium (IV) oxide | 1.4 ± 0.0 | 0.24 ± 0.00 | 14 | 3 | − | 5.2 |
Montmorillonite K10|| | 250 ± 20 | 43 ± 3 | 100 | 6 | + | 0.72 |
ATD w/ NH3 titration¶ | 15 ± 2 | 2.5 ± 0.4 | 62 | 31 | − | 7.7 |
Graphite# | 1.9 ± 0.1 | 0.32 ± 0.01 | 9 | 1 | − | 2.6 |
*Errors represent one standard error derived from nonlinear least-squares fitting for the Py decay plots.
†Obtained from reactions for 2 h.
‡Reaction time, 12 h; +, yes; −, no.
§Note that kaolin consists largely of kaolinite.
||Acid-activated montmorillonite.
¶Acidic surface of ATD was pre-titrated with NH3. See Methods for details.
#As a control.