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Determining the stable isotope composition of pore water from saturated and unsaturated zone core: improvements to the direct vapour equilibration laser spectrometry method.
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High Resolution Pore Water δ2H and δ18O Measurements by H2O (liquid)−H2O (vapor) Equilibration Laser Spectroscopy. Please note that between September and April inclusive samples must be shipped in insulated containers in order to prevent freezing!! If samples freeze the vial shatters and your sample is gone!ĭirect Vapour Equilibration: Soil Water Methodology Samples must be well packaged to reduce breakage! *Prices include sample transfer and filtering. All samples will be scanned for volatile organic compound contamination with LGR’s Spectral Contamination software. All values are reported as parts per thousand (δ or per mil) according to the Vienna Standard Mean Ocean Water-Standard Light Antarctic Precipitation (VSMOW-SLAP) scales. Our lab maintains an accuracy of ≤ ☑.0 for D/H and ☐.2 for 18O/ 16O and 17O/ 16O.
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