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- W84480686 abstract "We used stable isotopes of water in rainfall and streams in the Jonkershoek Valley to determine the relative contribution of new water (i.e. rain) during stormflow conditions. We found significant differences between rain and stream isotopic signatures which facilitated the use of a mass balance equation to calculate the components of stormflow. Analyses indicated that < 5 % of the stormflow comprised direct runoff. This suggests that the rapid response of these streams to rainfall is mainly due to displaced groundwater" @default.
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- W84480686 title "Use of stable isotopes of water (d and o-18) in hydrological studies in the Jonkershoek valley" @default.
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