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Water transit times vary over several orders of magnitude in between and within each of the main compartments of the hydrological cycle (Sprenger et al., 2019). This distribution has fundamental consequences for the water availability, renewal (Gleeson et al., 2016;Jasechko et al., 2017) and quality (Appelo & Postma, 1994;Wachniew et al., 2016). This is especially the case for shallow aquifers in direct connection to anthropogenic activities. Water ages broadly range from some weeks to several decades. This has immediate consequences on the transmission or buffering of recharge deficits and contamination loads (Cuthbert et al., 2019). Being intermediary between the surface and the deeper subsurface, shallow subsurface flows are potentially controlled by both geology and geomorphology (

Gas exchanges between streams and atmosphere strongly impact biogeochemical cycles, yet their quantification in space and time remains challenging. We propose a new method to measure gas exchange rate coefficients in headwater streams. The method is based on simultaneous slug injections of a conservative tracer and a volatile tracer, coupled to in situ semicontinuous measurements. Its originality lies in the mathematical exploitation of the tracers' breakthrough curves. Taking advantage of the entire breakthrough curves, we infer the gas exchange rate coefficient from a comparative analysis of the shape of the volatile and the conservative breakthrough curves. Tests on synthetic datasets confirmed the validity of the mathematical framework for the whole range of gas exchange rate coefficients found in headwater streams. Field experiments further attested to the real-world applicability of the method. Salt and helium injections were performed in a first-order stream and the helium breakthrough curves were obtained using in situ membrane inlet mass spectrometry. This new method allows to determine the gas exchange rates directly in the field, without any external calibration of the data. Its fast implementation enables a wider spatial coverage of the measurements of gas exchange rates, and thus offers an opportunity to improve the large-scale estimates of CO 2 emissions from headwater streams. More generally, our study highlights the informative potential of semicontinuous datasets and encourages further investigation of possible use of temporal signals.