Sulfate or Nitrate - Δ17O
We use a TC/EA to thermally degrade silver nitrate or silver sulfate to O2 and byproducts. The O2 is then passed to a Finnigan MAT253 for δ18O and δ17O analysis. We have adapted and automated previously developed techniques (Savarino et al., 2001; Michalski et al., 2002). For each sample, isolation of nitrate or sulfate and conversion to silver nitrate or silver sulfate is performed using an automated system including ion chromatographic separation, ion exchange, and a fraction collector. A Dionex Ion Chromatograph with an IonPac AS19 column (4x 250 mm) and a multistep eluent concentration gradient of 7 mM/10 mM/15 mM KOH is used to separate nitrate and sulfate fractions. Fractions then flow directly through an AMMS1 III ion exchange membrane (4 mm) with 2.5 mM Ag2SO4 regenerant for conversion to silver salts (e.g., AgNO3) prior to separate collection by the fraction collector. In multiple successive steps by a miVac Duo centrifuging concentrator at 45°C, silver nitrate fractions are transferred to and dried in silver capsules while silver sulfate samples are transfered to and dried in quartz or gold capsules. Analysis of oxygen isotopes of nitrate is performed using a Finnigan Temperature Conversion Elemental Analyzer (TC/EA) in-line with a continuous flow Finnigan MAT 253 isotope ratio mass spectrometer with helium as the carrier gas. The TC/EA autosampler drops samples into a crimped quartz pyrolysis tube at 585°C for nitrate and 1000 °C for sulfate. In the pyrolysis tube, pyrolysis of AgNO3 samples proceeds via 2AgNO3 --> O2 + 2NO2 + 2Ag(s) + (N2, NO in trace amounts). Ag2SO4 samples proceeds via Ag2SO4 --> O2 + SO2 + 2Ag + SO3 (trace). NO2 or SO2 and other condensible by-products are removed by a liquid N2 trap before the pyrolysis products flow through a molecular sieve 5A gas chromatograph column and into the IRMS.
Evolved O2 is measured for 16O16O, 16O17O, and 16O18O, from which Δ17O is calculated (Δ17O = δ17O − 0.528 × δ18O). Our measurements of the international standard USGS-35 reference material (NaNO3) result in Δ17O(NO3) = 21.5 ± 0.4 permil (1s error) for samples of 2–5 mmol O2 (4–10 mmol nitrate), which shows excellent agreement with accepted standard values (Δ17O(NO3) = 21.6 ± 0.2 permil) [B&oum;hlke et al., 2003; Michalski et al., 2003]. We use the nitrate USGS35 as well as a suite of in-house designer sulfate standards to calibrate.
We accept samples for nitrate / sulfate Δ17O analysis on a collaborative basis. The first step, then, is for you to tell us about the goals and purpose of the measurements. If needed, we will work with you to design an appropriate analysis strategy. This method requires that you visit IsoLab and perform the analyses yourself. We will then work together when interpreting the data. We would discuss the plan at length and make sure the data make sense for you to interpret. These analyses are scheduled 6 months in advance.
To calculate costs, visit our rates page. This analysis requires Silver salt preparation to convert the nitrate or sulfate to a silver salt form and Nitrate and / or Sulfate - Δ17O to analyze the silver salt for oxygen isotopic abundance. The cost is calculated using the "Off Campus Funding, Lab Provided Labor" lane until the visitor is self sufficient, 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 we require at least triplicates for a sound interpretation (# of samples x # replicates = total analyses).
Standard Operating Procedures
- Böhlke JK, Mroczkowski SJ, Coplen TB. (2003) Oxygen isotopes in nitrate: new reference materials for 18O:17O:16O measurements and observations on nitrate-water equilibration. Rapid Communications in Mass Spectrometry 17. doi: 10.1002/rcm.1123
- Kunasek SA, Alexander B, Steig EJ, Hastings MG, Gleason DJ, Jarvis JC. (2008) Measurements and modeling of Δ17O of nitrate in snowpits from Summit, Greenland. Journal of Geophysical Research 113. doi: 10.1029/2008JD010103
- Michalski G, Savarino J, Böhlke JK, Thiemens M. (2002) Determination of the Total Oxygen Isotopic Composition of Nitrate and the Calibration of a Δ17Ο Nitrate Reference Material. Analytical Chemistry 74. doi: 10.1021/ac0256282
- Michalski G, Scott Z, Kabiling M, Thiemens MH. (2003) First measurements and modeling of Δ17O in atmospheric nitrate. Geophysical Research Letters 30. doi: 10.1029/2003GL017015
- Savarino J, Alexander B, Darmohusodo V, Thiemens, MH. (2001) Sulfur and Oxygen Isotope Analysis of Sulfate at Micromole Levels Using a Pyrolysis Technique in a Continuous Flow System. Analytical Chemistry 73. doi: 10.1021/ac010017f
- Schauer AJ, Kunasek SA, Sofen ED, Erbland J, Savarino J, Johnson BW, Amos HM, Shaheen R, Abaunza M, Jackson TL, Thiemens MH, Alexander B. (2012) Oxygen isotope exchange with quartz during pyrolysis of silver sulfate and silver nitrate. Rapid Communications in Mass Spectrometry 26. 10.1002/rcm.6332