Final published version
Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - Key Role of NO3Radicals in the Production of Isoprene Nitrates and Nitrooxyorganosulfates in Beijing
AU - Hamilton, J.F.
AU - Bryant, D.J.
AU - Edwards, P.M.
AU - Ouyang, B.
AU - Bannan, T.J.
AU - Mehra, A.
AU - Mayhew, A.W.
AU - Hopkins, J.R.
AU - Dunmore, R.E.
AU - Squires, F.A.
AU - Lee, J.D.
AU - Newland, M.J.
AU - Worrall, S.D.
AU - Bacak, A.
AU - Coe, H.
AU - Whalley, L.K.
AU - Heard, D.E.
AU - Slater, E.J.
AU - Jones, R.L.
AU - Cui, T.
AU - Surratt, J.D.
AU - Reeves, C.E.
AU - Mills, G.P.
AU - Grimmond, S.
AU - Sun, Y.
AU - Xu, W.
AU - Shi, Z.
AU - Rickard, A.R.
PY - 2021/1/19
Y1 - 2021/1/19
N2 - The formation of isoprene nitrates (IsN) can lead to significant secondary organic aerosol (SOA) production and they can act as reservoirs of atmospheric nitrogen oxides. In this work, we estimate the rate of production of IsN from the reactions of isoprene with OH and NO3 radicals during the summertime in Beijing. While OH dominates the loss of isoprene during the day, NO3 plays an increasingly important role in the production of IsN from the early afternoon onwards. Unusually low NO concentrations during the afternoon resulted in NO3 mixing ratios of ca. 2 pptv at approximately 15:00, which we estimate to account for around a third of the total IsN production in the gas phase. Heterogeneous uptake of IsN produces nitrooxyorganosulfates (NOS). Two mono-nitrated NOS were correlated with particulate sulfate concentrations and appear to be formed from sequential NO3 and OH oxidation. Di- and tri-nitrated isoprene-related NOS, formed from multiple NO3 oxidation steps, peaked during the night. This work highlights that NO3 chemistry can play a key role in driving biogenic-anthropogenic interactive chemistry in Beijing with respect to the formation of IsN during both the day and night.
AB - The formation of isoprene nitrates (IsN) can lead to significant secondary organic aerosol (SOA) production and they can act as reservoirs of atmospheric nitrogen oxides. In this work, we estimate the rate of production of IsN from the reactions of isoprene with OH and NO3 radicals during the summertime in Beijing. While OH dominates the loss of isoprene during the day, NO3 plays an increasingly important role in the production of IsN from the early afternoon onwards. Unusually low NO concentrations during the afternoon resulted in NO3 mixing ratios of ca. 2 pptv at approximately 15:00, which we estimate to account for around a third of the total IsN production in the gas phase. Heterogeneous uptake of IsN produces nitrooxyorganosulfates (NOS). Two mono-nitrated NOS were correlated with particulate sulfate concentrations and appear to be formed from sequential NO3 and OH oxidation. Di- and tri-nitrated isoprene-related NOS, formed from multiple NO3 oxidation steps, peaked during the night. This work highlights that NO3 chemistry can play a key role in driving biogenic-anthropogenic interactive chemistry in Beijing with respect to the formation of IsN during both the day and night.
KW - Isoprene
KW - Nitrates
KW - Nitrogen oxides
KW - Sulfur compounds
KW - Atmospheric nitrogen
KW - Gasphase
KW - Mixing ratios
KW - NO concentration
KW - Particulate sulfates
KW - Rate of productions
KW - Secondary organic aerosols
KW - Gas industry
U2 - 10.1021/acs.est.0c05689
DO - 10.1021/acs.est.0c05689
M3 - Journal article
VL - 55
SP - 842
EP - 853
JO - Environmental Science and Technology
JF - Environmental Science and Technology
SN - 0013-936X
IS - 2
ER -