Photochemical smog characterized by high concentrations of ozone (O 3 ) is a serious air pollution issue in the North China Plain (NCP) region, especially in summer and autumn. For this study, measurements of O 3 , nitrogen oxides (NO x ), volatile organic compounds (VOCs), carbon monoxide (CO), nitrous acid (HONO), and a number of key physical parameters were taken at a suburban site, Xianghe, in the NCP region during the summer of 2018 in order to better understand the photochemical processes leading to O 3 formation and find an optimal way to control O 3 pollution. Here, the radical chemistry and O 3 photochemical budget based on measurement data from 1−23 July using a chemical box model is investigated. The daytime (0600−1800 LST) average production rate of the primary radicals referred to as RO x (OH + HO 2 + RO 2 ) is 3.9 ppbv h −1 . HONO photolysis is the largest primary RO x source (41%). Reaction of NO 2 + OH is the largest contributor to radical termination (41%), followed by reactions of RO 2 + NO 2 (26%). The average diurnal maximum O 3 production and loss rates are 32.9 ppbv h −1 and 4.3 ppbv h −1 , respectively. Sensitivity tests without the HONO constraint lead to decreases in daytime average primary RO x production by 55% and O 3 photochemical production by 42%, highlighting the importance of accurate HONO measurements when quantifying the RO x budget and O 3 photochemical production. Considering heterogeneous reactions of trace gases and radicals on aerosols, aerosol uptake of HO 2 contributes 11% to RO x sink, and the daytime average O 3 photochemical production decreases by 14%. The O 3 -NO x -VOCs sensitivity shows that the O 3 production at Xianghe during the investigation period is mainly controlled by VOCs.