Hydrological Processes · 2016 · 122 citations · 60 references
Natural ResourcesEcologyHydrologyCatchment HydrologyEcohydrologySoil-water RelationsCatchment EcohydrologyCatchment Water BalanceForest Catchment HydrologyForest EcohydrologyHydrological ConnectivityPlant Water UseCatchment-scale Soil Water IsotopesForest Catchment Water BalanceForest-stream InteractionsHeadwater HydrologyHeadwater StreamsTree Water UseVegetation Water RelationsXylem Water Transport
Abstract Recent studies using water‐stable isotopes ( δ 18 O and δ 2 H) have suggested an ecohydrological separation of water flowing to streams or recharging groundwater and water used by trees, known as the ‘two water worlds’ (TWW) hypothesis. In this study, we measured water isotopic composition in precipitation [open field and throughfall, i.e. local meteoric water line (LMWL)] and the mobile water compartment (i.e. stream and soil solution), bulk soil water and xylem water over a period of 1.5 years in two headwater catchments: NF, covered with old growth native evergreen forest ( Aetoxicon punctatum , Laureliopsis philippiana and Eucriphya cordifolia ), and EP, covered with 4 and 16‐year‐old Eucalyptus nitens stands. Our results show that precipitation, stream and soil solution plot approximately along the LMWL, while xylem waters from all studied tree species plot below the LMWL, supporting the TWW hypothesis. However, we also found evidence of ecohydrological connectivity during the wet season, likely controlled by the amount of antecedent precipitation. These observations hold for all investigated tree species. On both sites, a different precipitation source for stream and xylem water was observed. However, in EP, bulk soil showed a similar precipitation source as xylem water from both E . nitens stands. This suggests that E . nitens may use water that is recharging the bulk soil compartment. We conclude that under a rainy temperate climate, the TWW hypothesis is temporal and does not apply during wet seasons. Copyright © 2016 John Wiley & Sons, Ltd.
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