We analyze a photochemical smog episode to understand the oxidative capacity and radical chemistry of the polluted atmosphere in Hong Kong and the Pearl River Delta (PRD) region. A photochemical box model based on the Master Chemical Mechanism (MCM v3.2) is constrained by an intensive set of field observations to elucidate the budgets of RO x (RO x = OH+HO 2 +RO 2 ) and NO 3 radicals. Highly abundant radical precursors (i.e. O 3 , HONO and carbonyls), nitrogen oxides (NO x ) and volatile organic compounds (VOCs) facilitate strong production and efficient recycling of RO x radicals. The OH reactivity is dominated by oxygenated VOCs (OVOCs), followed by aromatics, alkenes and alkanes. Photolysis of OVOCs (except for formaldehyde) is the dominant primary source of RO x with average daytime contributions of 34-47 %. HONO photolysis is the largest contributor to OH and the second-most significant source (19-22 %) of RO x . Other considerable RO x sources include O 3 photolysis (11-20 %), formaldehyde photolysis (10-16 %), and ozonolysis reactions of unsaturated VOCs (3.9-6.2 %). In one case when solar irradiation was attenuated, possibly by the high aerosol loadings, NO 3 became an important oxidant and the NO 3 -initiated VOC oxidation presented another significant RO x source (6.2 %) even during daytime. This study suggests the possible impacts of daytime NO 3 chemistry in the polluted atmospheres under con-ditions with the co-existence of abundant O 3 , NO 2 , VOCs and aerosols, and also provides new insights into the radical chemistry that essentially drives the formation of photochemical smog in the high-NO x environment of Hong Kong and the PRD region. recycling (e.g. OH→RO 2 →RO→HO 2 →OH) and produce O 3 and oxygenated VOCs (OVOCs) .