δD vs δ 18 O values and d-excess vs δ 18 O values for natural
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ACP - Sub-cloud rain evaporation in the North Atlantic winter trade winds derived by pairing isotopic data with a bin-resolved microphysical model
Isotopic study of intraseasonal variations of plant transpiration: an alternative means to characterise the dry phases of monsoon
Solved Examine the graph of δ18O values versus depth below
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
Stable isotope variations of daily precipitation from 2014–2018 in the central United States
SciELO - Brasil - Stable-isotope ratios (δ18O and δD) in a firn core from West Antarctica Stable-isotope ratios (δ18O and δD) in a firn core from West Antarctica
Hydrogen isotope biogeochemistry - Wikipedia
Full article: Plant Water δD and δ18O of Tundra Species from West Greenland
Controls on spatiotemporal variations of stable isotopes in precipitation across Bangladesh - ScienceDirect
