Analysis reveals the impact of temperature on Be+ + H2O reaction kinetics, indicating shifts in rate coefficients for ground and excited states.
We investigate the Be⁺ + H₂O → BeOH⁺ + H reaction using a laser-cooled ion trap coupled with a high-resolution time-of-flight mass spectrometer (TOF-MS) over a range of reaction temperatures (Ecol/kB ≈ 127-416 K). By selectively preparing Be⁺ in either the Be⁺(²P3/2) or Be⁺(²S1/2) electronic states and controlling ion micromotion to tune the reaction temperature, we determine state-specific reaction rate coefficients. The measured rates for ground-state Be⁺(²S1/2) exhibit a pronounced decrease with increasing reaction temperature, in good agreement with quasi-classical trajectory (QCT) calculations. In contrast, the rates for excited-state Be⁺(²P3/2) decrease even more rapidly with increasing reaction temperature, deviating significantly from predictions by the classical capture model. This temperature-dependent behavior underscores the key role of a submerged reaction barrier in shaping the kinetics. Our measurements demonstrate the importance of experimental access to temperature-controlled ion-molecule reactions, revealing limitations of widely used capture theories.
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Peng et al. (2025) studied this question.
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