Table 2. Experimental Conditions^a.

expt #	date	BVOC	[BVOC]I (ppb)	[N2O5]I (ppb)	kNO3+BVOC @298 K (cm3 molec-1 s–-1)	[N2O5]i/[BVOC]i
1	9/15/11	α-pinene (seeded)	48	54	6.16 × 10–12	1.1
2	9/28/11	β-pinene “high”	41	60	2.51 × 10–12	1.5
3	10/18/11	β-pinene “low”	10	10	2.51 × 10–12	1.0
4	9/19/11	Δ-3-carene “high”	16	42	9.1 × 10–12	2.6
5	10/21/11	Δ-3-carene “low”	10	9	9.1 × 10–12	0.9
6	10/3/11	limonene “high”	40	60	1.22 × 10–11	1.5
7	10/11/11	limonene “low”	10	10	1.22 × 10–11	1.0
8	10/15/11	limonene (+ O3 + NO2)	10	[O3]i = 12 ppb; [NO2]i= 6.3 ppb	1.22 × 10–11	1.2
9	9/22/11	β-caryophyllene “high”	109	40	1.9 × 10–11	0.4
10	10/26/11	β-caryophyllene “low”	3	10	1.9 × 10–11	3.0
11	11/11/11	sabinene	9	10	1 × 10–11	1.1

^aExcept α-pinene, all experiments were conducted without seed aerosol. Rate constants at 298 K are taken from Calvert et al. (2000).²¹ For the “low” experiments, the ratio of N₂O₅ to BVOC in the inlet line was approximately 1:1; for the “high” experiments, the oxidant was generally in slight excess (with the exception of Expt # 9). The highest purity sabinene source available was 80%, and contained 20% β-pinene. No correction was applied for this, so sabinene SOA reflects this mixture.