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 use the nitrate USGS35 as well as a suite of in-house designer sulfate standards to calibrate.
If you are interested in submitting samples for this type of analysis, please contact us. See the table below for sample analysis pricing.
Exhaustive description of 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 45C, 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 He as the carrier gas. The TC/EA autosampler drops samples into a crimped quartz pyrolysis tube at 585C 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 D17O is calculated. Our measurements of the international standard USGS-35 reference material (NaNO3) result in Δ17O(NO3) = 21.5 ± 0.4%(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%) [Bohlke et al., 2003; Michalski et al., 2003].
Δ17O = δ17O − 0.528 × δ18O
- Savarino et al., 2001
- Michalski et al., 2002
- Bohlke et al., 2003
- Michalski et al., 2003
- Kunasek JGR 2008
- Schauer RCM 2012