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Stable Isotope Analysis – Measuring δ17O in Water by CRDS

recommended sample size Sample size recommended
  • 5 mL – Please do not add acids or any chemicals to the sample.
carbon dating services Turnaround time
  • 14 business days
recommended container Recommended container
  • Use a small plastic vial with no prior use and fill to the top with no headspace. Please use a box with sufficient packing to prevent breakage during shipment.
lab recommendation
  • Please let us know if your water samples contain salt or have been in the proximity of any location using labeled 14C (artificial 14C).
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vial water analysisThe lab only accepts samples that are ready for δ17O measurement (filtered, no chemicals added, do not require pretreatment).

Stable Isotope Analysis Cost

Beta Analytic provides δ17O water analysis on a standalone basis or in conjunction with δ18O and δD measurements for a fee using a cavity ring-down spectrometer (CRDS).

To request for a formal quotation, please let us know the number of water samples for analysis and the billing information of the paying institution.

Submittal – Please use this online form. For details on how to collect and submit water samples, please see our Radiocarbon Dating Groundwater page.

printed sampleIf you have any questions about your sample, please contact the lab.

Why Measure δ17O in Water?

Triple isotopic variability reveals more information about environmental conditions than dual isotopic tools alone. For example, deuterium excess in water – interpreting the variability of protium to deuterium isotopes in relation to δ18O from meteoric waters has been used to enhance the interpretation of humidity and its effects on the fractionation of water isotopes. Since many geological materials (evaporite minerals) do not incorporate H into their structural components, the use of deuterium excess has its limits as an environmental proxy, few materials can produce meaningful results (Li et al., 2015).

Oxygen has the potential to be a triple isotopic tool that can reveal additional information about evaporation and condensation oxygen systematics among many oxygen-bearing materials. Δ17O (δ18O v. δ17O) or the variability of 17O and 18O to 16O has only recently been recognized to have the potential as an additional proxy as the precision of isotopic analysis has increased. Current research has been focused on understanding Δ17O variability in modern meteoric waters as baseline investigations to relate results of Δ17O to other materials.

Disclaimer: This video is hosted in a third-party site and may contain advertising.

This video excerpt is part of Beta Analytic’s webinar: Isotopes in Hydrology

Beta Analytic’s Capabilities

The lab’s current CRDS is capable of determining the δ17O ((17O/16OUNKN/17O/16OSTD-1)*1000) values of water vapor at a precision of +/- 0.8 ‰ or better as well as determine a 17O-excess value (also referred to as Δ17O).

The 17O-excess value is defined as the deviation from an expected relationship in 17O/16O and 18O/16O ratios (Li et al., 2015). The CRDS measures both the δ17O and δ18O and the software calculates the 17O-excess.

The data are used to suggest information regarding the conditions in which the phase change occurred. Did water evaporate in a climate that was arid or humid or at a high elevation or low elevation? Δ17O data can refine conditions further by the addition of condensation and evaporation effects on fractionation.

Evaporation has been found to vary both δ18O and Δ17O values whereas condensation has been found to only significantly shift δ18O values. Suggesting that δ17O and δ18O values covary at different rates with evaporation and condensation.


Li, S., Levin, N. E., & Chesson, L. A. (2015). Continental scale variation in 17O-excess of meteoric waters in the United States. Geochimica et Cosmochimica Acta, 164, 110-126.

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Page last updated: October 2022

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