%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Tweed, S.
%A Munksgaard, N.
%A Marc, V.
%A Rockett, N.
%A Bass, A.
%A Forsythe, A. J.
%A Bird, M. I.
%A Leblanc, Marc
%T Continuous monitoring of stream delta O-18 and delta H-2 and stormflow hydrograph separation using laser spectrometry in an agricultural catchment
%D 2016
%L fdi:010066159
%G ENG
%J Hydrological Processes
%@ 0885-6087
%K isotopes ; hydrograph separation ; nutrients ; groundwater and surface ; water interactions
%K AUSTRALIE
%M ISI:000369165900011
%N 4
%P 648-660
%R 10.1002/hyp.10689
%U https://www.documentation.ird.fr/hor/fdi:010066159
%> https://www.documentation.ird.fr/intranet/publi/2016/02/010066159.pdf
%V 30
%W Horizon (IRD)
%X A portable Wavelength Scanned-Cavity Ring-Down Spectrometer (Picarro L2120) fitted with a diffusion sampler (DS-CRDS) was used for the first time to continuously measure O-18 and H-2 of stream water. The experiment took place during a storm event in a wet tropical agricultural catchment in north-eastern Australia. At a temporal resolution of one minute, the DS-CRDS measured 2160 O-18 and H-2 values continuously over a period of 36h with a precision of +/- 0.08 and 0.5 parts per thousand for O-18 and H-2, respectively. Four main advantages in using high temporal resolution stream O-18 and H-2 data during a storm event are highlighted from this study. First, they enabled us to separate components of the hydrograph, which was not possible using high temporal resolution electrical conductivity data that represented changes in solute transfers during the storm event rather than physical hydrological processes. The results from the hydrograph separation confirm fast groundwater contribution to the stream, with the first 5h of increases in stream discharge comprising over 70% pre-event water. Second, the high temporal resolution stream O-18 and H-2 data allowed us to detect a short-lived reversal in stream isotopic values (O-18 increase by 0.4 parts per thousand over 9min), which was observed immediately after the heavy rainfall period. Third, O-18 values were used to calculate a time lag of 20min between the physical and chemical stream responses during the storm event. Finally, the hydrograph separation highlights the role of event waters in the runoff transfers of herbicides and nutrients from this heavily cultivated catchment to the Great Barrier Reef.
%$ 062