4.9 (574) · $ 10.50 · In stock
The δD vs. δ 18 O values of precipitation in the upper and middle
δD vs δ 18 O values and d-excess vs δ 18 O values for natural water
Global and local meteoric water lines for δ17O/δ18O and the spatiotemporal distribution of Δ′17O in Earth's precipitation
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
Frontiers Underlying Climate Controls in Triple Oxygen (16 O, 17 O, 18 O) and Hydrogen (1 H, 2 H) Isotopes Composition of Rainfall (Central Pyrenees)
Frontiers Underlying Climate Controls in Triple Oxygen (16 O, 17 O, 18 O) and Hydrogen (1 H, 2 H) Isotopes Composition of Rainfall (Central Pyrenees)
Total uncertainty of δD, δ 18 O, and d excess over the range of H 2 O v
Distribution of hydrogen and oxygen stable isotopes and pollution indicators in water during a monsoon transitional period in Min River Basin - ScienceDirect
Isotopic compositions (δD, δ18O) and end-member mixing for the control interface in a complex tidal region - ScienceDirect
Tap water isotope ratios reflect urban water system structure and dynamics across a semiarid metropolitan area - Jameel - 2016 - Water Resources Research - Wiley Online Library
Stable isotope compositions (δ2H, δ18O and δ17O) of rainfall and snowfall in the central United States
Statistical Analysis of the Precipitation Isotope Data with Reference to the Indian Subcontinent
Geosciences, Free Full-Text
Water, Free Full-Text
Correlation between δ18Ow and δ18Οen for estimating human mobility and paleomobility patterns