Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

In the context of this paper, stable isotopic proxies are those preserving directly, or via
known or calculable fractionation factors, a record of 18O/16O and/or 2H/1H in the water …

There remains a lack of understanding of environmental isotopes and their use; students
and practitioners typically find the concepts of isotope concentrations and partitioning to be …

Groundwater recharged by meteoric water supports human life by providing two billion
people with drinking water and by supplying 40% of cropland irrigation. While annual …

In detrital coastal aquifers, seawater and surface water may interact with groundwater in
multiple ways. Understanding the interference of water fluxes in this type of environment is …

The isotopic composition of precipitation has been measured in samples simultaneously
collected during individual precipitation events at two neighbouring high-altitude stations …

The deuterium excess is a function of the isotopic composition of oxygen and hydrogen in
water. Traditionally, the d-excess is used worldwide to constrain the moisture sources of …

The hydrodynamic of the multi-aquifer system (the Continental Intercalaire “CI” and the
Complex Terminal “CT”) of the North Gafsa basin is largely determined by tectonics …

A negative stable isotope-altitude gradient is commonly observed on the windward side of a
mountain. However, after the precipitation passes over a mountain range to the leeward …

This paper reviews all available stable isotopic data concerning precipitation and spring
water in Greece, from the 1960s until today. Spatial variability is investigated in order to …