Preparation and Analysis of Water 17Oexcess



We employ the water fluorination method using Cobalt (III) fluoride to convert H2O into O2 for subsequent triple oxygen isotope analysis on a Thermo MAT253.

Reference Materials

 We use VSMOW, SLAP, and GISP to calibrate our water flourination system. We have also measured select in-house reference waters for 17Oexcess.

Sample submission

If you would like to submit samples for Δ17O (17Oexcess) of water, please contact us. See the table below for sample analysis pricing. Given the nature of the Δ17O signal, we strongly suggest a minimum of three replicates. You can choose to visit IsoLab and perform analyses yourself, or we can analyze the samples for you.

To calculate costs please visit our rates page.

If you send someone here to learn the method and do the analyses, the cost is calculated using the "Off Campus Funding, Lab Provided Labor" lane for the first three days then the "Off Campus Funding, User Provided Labor" for every day after that. If we run your samples for you, use the "Off Campus Funding, Lab Provided Labor" lane.

These rates are per analysis not per sample and, again, we suggest at least triplicates for a sound interpretation (# of samples x # replicates = total analyses).

Exhaustive description of analysis

Water is fluorinated to produce O2 as previously described (Barkan and Luz 2005, Baker et al. 2002, Barkan and Luz 2007) and the O2 is collected as in Abe (2008). Briefly, 2 mL of water was injected into a 370 °C 15 cm long nickel column containing 7 g CoF3 converting H2O into O2 and creating HF and CoF2 as byproducts. Helium carried O2 at 30 mL min-1 through a trap submerged in liquid nitrogen to collect HF, which is later vented to a fume hood; the NaF trap originally recommended by Baker et al. (2002) is not used. The O2 sample is collected in a trap for 20 min, and then transferred to a 14 cm stainless steel cold finger. Both the trap and cold finger contained approximately 40 mg of 5A (4.2 to 4.4 Å) molecular sieve and were submerged in liquid nitrogen. To minimize memory effects, following Barkan and Luz (2005) we injected and discarded a minimum of four injections when switching between waters with a difference in δ18O value of greater than 5 permil. The cold fingers are sealed using a bellows valve.

The O2 samples are warmed to 60 °C and expanded for 10 min into the sample bellows through a custom multiport on a dual-inlet ThermoFinnigan MAT 253 isotope ratio mass spectrometer (Thermo Electron, Bremen, Germany) with Faraday cup amplifiers for m/z 32, 33, and 34 of 1*109 Ω, 1*1012 Ω, and 1*1011 Ω, respectively. The custom designed multiport used air-actuated bellows valves, air pressure control originally intended
for a stock microvolume, and modified ISL scripts. The O2 sample was analyzed for m/z 32, 33, and 34 abundance ratios to determine d18O and d17O values with reference to O2 gas (δ17O measured s/VSMOW=-4.319 permil, δ18O measured s/VSMOW=-8.255 permil). Each mass spectrometric measurement comprised 90 sample-to-reference comparisons. Each of these comparisons consisted of 26 s of integration and 15 s of idle time. After every 30 comparisons, the m/z 32 signals of the sample and reference gases were balanced to 10 V and the mass spectrometer was peak-centered on m/z 33. The reference bellows was automatically refilled before each sample to a pressure that was equal to that of the sample. Over the course of these measurements the mass spectrometer exhibited an internal reproducibility of 0.002 permil, 0.004 permil, and 0.0037 permil (3.7 per meg) for δ17O, δ18O, and 17Oexcess values, respectively.


see Schoenemann et al. 2013.

Suggested reading

  • O. Abe. Isotope fractionation of molecular oxygen during adsorption/desorption by molecular sieve zeolite. Rapid Commun. Mass Spectrom. 2008, 22, 2510.
  • E. Barkan, B. Luz. High precision measurements of 17O/16O and 18O/16O ratios in H2O. Rapid Commun. Mass Spectrom. 2005, 19, 3737.
  • L. Baker, I. A. Franchi, J. Maynard, I. P. Wright, C. T. Pillinger. A technique for the determination of 18O/16O and 17O/16O isotopic ratios in water from small liquid and solid samples. Anal. Chem. 2002, 74, 1665.
  • E. Barkan, B. Luz. Diffusivity fractionations of H216O/H217O and H216O/H218O in air and their implications for isotope hydrology. Rapid Commun. Mass Spectrom. 2007, 21, 2999.
  • Schoenemann SW, Schauer AJ, Steig EJ. 2013. Measurement of SLAP2 and GISP d17O and proposed VSMOWSLAP normalization for d17O and 17Oexcess. Rapid Commun. Mass Spectrom. 2013, 27, 582–590.

Water 17Oexcess Analysis Pricing

All analysis prices are per sample.

  • UW Budget Number,
    User Provided Labor
  • $54
  • To be eligible for this rate, you must provide a UW budget number for billing as well as have the ability and availability to run the sample analysis yourself from start to finish.
  • Method: Fluorination, dual inlet
  • Request analysis
  • Off Campus Funding, User Provided Labor
  • $62
  • To be eligible for this rate, you must have the ability and availability to run the sample analysis yourself from start to finish. Analysis will be paid for through an off-campus address.
  • Method: Fluorination, dual inlet
  • Request analysis
  • UW Budget Number, Lab Provided Labor
  • $84
  • To be eligible for this rate, you must provide the lab with a UW budget number for billing. An IsoLab lab technician will perform the sample analysis for your sample set.
  • Method: Fluorination, dual inlet
  • Request analysis
  • Off Campus Funding, Lab Provided Labor
  • $97
  • This is the lab's default billing rate. We will apply this rate when no UW budget number is provided and your sample analysis was performed by an IsoLab lab technician.
  • Method: Fluorination, dual inlet
  • Request analysis>

We welcome individuals from all departments and from on or off the University of Washington campus to visit our facility, and to take advantage of our expertise. Please contact us for more information.