where X is the element, h is the high mass number, R is the high mass-to-low mass isotope ratio, and Rstandard is Vienna Pee Dee belemnite (VPDB) for carbon and AIR for nitrogen. Units are parts per thousand (per mil, ‰). We used peach leaves (Standard Reference Material [SRM] No. 1547, n = 105, mean ± standard deviation: δ13C = -25.9 ± 0.1 ‰ and δ15N = 2.1 ± 0.1 ‰) and bovine liver (SRM No. 1577, n = 38, δ13C = -21.54 ± 0.1 ‰ and δ15N = 7.9 ± 0.1 ‰) as references to correct the stable isotope ratios for drift and linearity of the mass spectrometer.
Chnos elemental analyzer vario isotope cube
The CHNOS Elemental Analyzer (vario ISOTOPE cube) is a versatile laboratory instrument designed for the determination of carbon, hydrogen, nitrogen, oxygen, and sulfur content in a wide range of solid and liquid samples. The analyzer utilizes state-of-the-art technology to provide accurate and reliable results.
Lab products found in correlation
2 protocols using chnos elemental analyzer vario isotope cube
Stable Isotope Analysis of Biological Samples
where X is the element, h is the high mass number, R is the high mass-to-low mass isotope ratio, and Rstandard is Vienna Pee Dee belemnite (VPDB) for carbon and AIR for nitrogen. Units are parts per thousand (per mil, ‰). We used peach leaves (Standard Reference Material [SRM] No. 1547, n = 105, mean ± standard deviation: δ13C = -25.9 ± 0.1 ‰ and δ15N = 2.1 ± 0.1 ‰) and bovine liver (SRM No. 1577, n = 38, δ13C = -21.54 ± 0.1 ‰ and δ15N = 7.9 ± 0.1 ‰) as references to correct the stable isotope ratios for drift and linearity of the mass spectrometer.
Leaf and Wood Traits Measurement
Dry and ground samples were analyzed for C and N content (% dry weight), and stable isotope ratios (δ 13 C and δ 15 N values, respectively) were extracted with an elemental analyzer/continuous ow isotope ratio mass spectrometry using a CHNOS Elemental Analyzer (vario ISOTOPE cube, Elementar, Hanau, Germany) coupled with an IsoPrime 100 mass spectrometer (Isoprime Ltd, Cheadle, UK). The long-term analytical precision was 0.08‰ for C and 0.14‰ for N. For C-isotope analyses the standard used was V-PDB, and for N-isotope analyses we used N 2 -gas. All isotope analyses were conducted at the Center for Stable Isotope Biogeochemistry at the University of California, Berkeley, CA, USA.
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