1) This study presents the first measurements of the diurnal cycle of Δ17O in CO2 at a pine forest field site in the Netherlands. Flask samples were collected over 24 hours in summer 2019. 2) Modeling with an MXL model showed reasonable agreement with observations and allowed exploration of sensitivities driving Δ17O variations. A TM5 model simulation indicated biospheric exchange and fossil fuel combustion were the main processes influencing the Δ17O signal. 3) Observations showed the Δ17O signal exceeded measurement uncertainty, though interpretation was difficult. The timing of different processes in the TM5 model reduced the amplitude of the diurnal Δ17O cycle in CO2. The largest diurnal cycles were