1 research outputs found
Mineral Oxides Change the Atmospheric Reactivity of Soot: NO<sub>2</sub> Uptake under Dark and UV Irradiation Conditions
The
heterogeneous reactions between trace gases and aerosol surfaces
have been widely studied over the past decades, revealing the crucial
role of these reactions in atmospheric chemistry. However, existing
knowledge on the reactivity of mixed aerosols is limited, even though
they have been observed in field measurements. In the current study,
the heterogeneous interaction of NO<sub>2</sub> with solid surfaces
of Al<sub>2</sub>O<sub>3</sub> covered with kerosene soot was investigated
under dark conditions and in the presence of UV light. Experiments
were performed at 293 K using a low-pressure flow-tube reactor coupled
with a quadrupole mass spectrometer. The steady-state uptake coefficient,
γ<sub>ss</sub>, and the distribution of the gas-phase products
were determined as functions of the Al<sub>2</sub>O<sub>3</sub> mass;
soot mass; NO<sub>2</sub> concentration, varied in the range of (0.2–10)
× 10<sup>12</sup> molecules cm<sup>–3</sup>; photon flux;
and relative humidity, ranging from 0.0032% to 32%. On Al<sub>2</sub>O<sub>3</sub>/soot surfaces, the reaction rate was substantially
increased, and the formation of HONO was favored compared with that
on individual pure soot and pure Al<sub>2</sub>O<sub>3</sub> surfaces.
Uptake of NO<sub>2</sub> was enhanced in the presence of H<sub>2</sub>O under both dark and UV irradiation conditions, and the following
empirical expressions were obtained: γ<sub>ss,BET,dark</sub> = (7.3 ± 0.9) × 10<sup>–7</sup> + (3.2 ± 0.5)
× 10<sup>–8</sup> × RH and γ<sub>ss,BET,UV</sub> = (1.4 ± 0.2) × 10<sup>–6</sup> + (4.0 ± 0.9)
× 10<sup>–8</sup> × RH. Specific experiments, with
solid sample preheating and doping with polycyclic aromatic hydrocarbons
(PAHs), showed that UV-absorbing organic compounds significantly affect
the chemical reactivity of the mixed mineral/soot surfaces. A mechanistic
scheme is proposed, in which Al<sub>2</sub>O<sub>3</sub> can either
collect electrons, initiating a sequence of redox reactions, or prevent
the charge-recombination process, extending the lifetime of the excited
state and enhancing the reactivity of the organics. Finally, the atmospheric
implications of the observed results are briefly discussed
