δD vs δ 18 O values and d-excess vs δ 18 O values for natural water
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![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://www.researchgate.net/publication/337285053/figure/fig3/AS:824950151733248@1573694851015/The-dD-and-d-18-O-values-from-the-cities-Here-dD-or-d-18-Orepresents-the.png)
The △δD and △δ 18 O values from the cities. Here, △δD (or △δ 18
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://media.springernature.com/lw685/springer-static/image/prt%3A978-1-4020-4411-3%2F14/MediaObjects/978-1-4020-4411-3_14_Part_Fig36-163_HTML.jpg)
Oxygen Isotopes
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://media.springernature.com/full/springer-static/image/art%3A10.1038%2Fs41597-022-01151-6/MediaObjects/41597_2022_1151_Fig1_HTML.png)
Stable isotope variations of dew under three different climates
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://ars.els-cdn.com/content/image/1-s2.0-S2214581816303561-gr3.jpg)
Tracing isotopic signatures (δD and δ18O) in precipitation and glacier melt over Chorabari Glacier–Hydroclimatic inferences for the Upper Ganga Basin (UGB), Garhwal Himalaya - ScienceDirect
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://media.springernature.com/m685/springer-static/image/art%3A10.1007%2Fs10040-022-02526-0/MediaObjects/10040_2022_2526_Fig4_HTML.png)
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://www.frontiersin.org/files/MyHome%20Article%20Library/640292/640292_Thumb_400.jpg)
Frontiers Continuous-Flow Analysis of δ17O, δ18O, and δD of H2O on an Ice Core from the South Pole
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://www.frontiersin.org/files/Articles/987685/fmars-09-987685-HTML/image_m/fmars-09-987685-g001.jpg)
Frontiers Using dual water isotopes to quantify the mixing of water masses in the Pearl River Estuary and the adjacent northern South China Sea
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://pastglobalchanges.org/sites/default/files/2023-10/pic2_p102-103.png)
Advances in triple oxygen isotope analysis and applications for ice-core paleoclimate science
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://d3i71xaburhd42.cloudfront.net/018e0bbcf0e3fd7260c265e603ef10cdfc800ff4/13-Table1-1.png)
Table 1 from Measurement of δ18O, δ17O, and 17O-excess in water by off-axis integrated cavity output spectroscopy and isotope ratio mass spectrometry.
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://ars.els-cdn.com/content/image/1-s2.0-S2214581816303561-gr4.jpg)
Tracing isotopic signatures (δD and δ18O) in precipitation and glacier melt over Chorabari Glacier–Hydroclimatic inferences for the Upper Ganga Basin (UGB), Garhwal Himalaya - ScienceDirect
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://media.springernature.com/m685/springer-static/image/art%3A10.1007%2Fs10040-022-02526-0/MediaObjects/10040_2022_2526_Fig2_HTML.png)
Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area
![δD vs δ 18 O values and d-excess vs δ 18 O values for natural water](https://media.springernature.com/m685/springer-static/image/art%3A10.1007%2Fs10040-023-02654-1/MediaObjects/10040_2023_2654_Fig4_HTML.png)
Hydrological processes and water quality in arid regions of Central Asia: insights from stable isotopes and hydrochemistry of precipitation, river water, and groundwater
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