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How can the stable isotopes of oxygen 18 and hydrogen 2 be interpreted? 

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The stable isotopes of oxygen 18 and hydrogen 2 can be interpreted to determine the sources, fluxes, and mechanisms of material transfer in various environmental systems. The measurement and analysis of these isotopes provide valuable insight into environmental conditions and processes. For example, in the central Nile delta, the isotopic data of oxygen 18 and hydrogen 2 in water samples were used to determine the sources of groundwater recharge . In forensic cases, the isotopic signals in human hair and drinking water were analyzed to identify potential places of residence . In soil water evaporation studies, the variation of oxygen 18 and hydrogen 2 isotopes with soil depth and time provided insights into soil water movement processes . Additionally, stable water isotopes like oxygen 18 and hydrogen 2 have been used to investigate plant water relations and understand water uptake by grasslands under changing water availability .

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The paper does not provide information on how the stable isotopes of oxygen 18 and hydrogen 2 can be interpreted.
The paper does not provide information on how the stable isotopes of oxygen 18 and hydrogen 2 can be interpreted.
The paper does not provide information on how the stable isotopes of oxygen 18 and hydrogen 2 can be interpreted. The paper is about the isoreader package, which enables the reading and processing of stable isotope data files for reproducible research.
The stable isotopes of oxygen 18 and hydrogen 2 can be used as tracers to determine the sources of groundwater recharge in the central Nile delta.

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