scholarly journals Assessment of the amount of body water in the Red Knot (Calidris canutus): an evaluation of the principle of isotope dilution with2H,17O, and18O as measured with laser spectrometry and isotope ratio mass spectrometry

2006 ◽  
Vol 42 (1) ◽  
pp. 1-7 ◽  
Author(s):  
Erik R. T. Kerstel ◽  
Theunis A. J. Piersma ◽  
G. Jim Gessaman ◽  
Anne Dekinga ◽  
Harro A. J. Meijer ◽  
...  
Data in Brief ◽  
2020 ◽  
Vol 29 ◽  
pp. 105349
Author(s):  
Simon Damien Carrière ◽  
Nicolas K. Martin-StPaul ◽  
Coffi Belmys Cakpo ◽  
Nicolas Patris ◽  
Marina Gillon ◽  
...  

2002 ◽  
Vol 35 ◽  
pp. 125-130 ◽  
Author(s):  
Radboud van Trigt ◽  
Harro A. J. Meijer ◽  
Arny E. Sveinbjörnsdóttir ◽  
Sigfús J. Johnsen ◽  
Erik R.Th. Kerstel

AbstractWe report on the first application of a new technique in ice-core research, based on direct absorption infrared laser spectrometry (LS), for measuring 2H, 17Oand 18O isotope ratios. the data are used to calculate the deuterium excess d (defined as δ2H– 8δ18O) for a section of the Dye-3 (south Greenland) deep ice core around the Bølling transition (14 500 BP). the precision of LS is slightly better than that of most traditional methods for deuterium, but not for the oxygen isotopes. the ability to measure δ17O is new and is used here to improve the precision of the δ18O determination. Still, the final precision for δ18O remains inferior to traditional isotope ratio mass spectrometry (IRMS). Therefore, deuterium excess was calculated from a combination of the LS and IRMS isotope determinations.


2002 ◽  
Vol 93 (6) ◽  
pp. 2147-2154 ◽  
Author(s):  
R. Van Trigt ◽  
E. R. T. Kerstel ◽  
R. E. M. Neubert ◽  
H. A. J. Meijer ◽  
M. McLean ◽  
...  

In Japanese quail ( Coturnix c. japonica; n = 9), the doubly labeled water (DLW) method (2H, 18O) for estimation of CO2 production (l/day) was validated. To evaluate its sensitivity to water efflux levels ( r H2 Oe ; g/day) and to assumptions of fractional evaporative water loss ( x; dimensionless), animals were repeatedly fed a dry pellet diet (average r H2 Oe of 34.8 g/day) or a wet mash diet (95.8 g/day). We simultaneously compared the novel infrared laser spectrometry (LS) with isotope ratio mass spectrometry. At low r H2 Oe , calculated CO2 production rate exhibited little sensitivity to assumptions concerning x, with the best fit being found at 0.51, and only little error was made employing an x value of 0.25. In contrast, at high r H2 Oe , sensitivities were much higher with the best fit at x = 0.32. Conclusions derived from isotope ratio mass spectrometry and LS were similar, proving the usefulness of LS. Within a threefold range of r H2 Oe , little error in the DLW method is made when assuming one single x value of 0.25 (recommended by Speakman JR, Doubly Labelled Water. Theory and Practice. London: Chapman & Hall, 1997), indicating its robustness in comparative studies.


The Analyst ◽  
2000 ◽  
Vol 125 (12) ◽  
pp. 2189-2195 ◽  
Author(s):  
Céline S. J. Wolff Briche ◽  
Gavin O’Connor ◽  
Ken S. Webb ◽  
Tim Catterick ◽  
Helena Hernández

Author(s):  
Xing Wang ◽  
Henk G. Jansen ◽  
Haico Duin ◽  
Harro A. J. Meijer

AbstractThere are two officially approved methods for stable isotope analysis for wine authentication. One describes δ18O measurements of the wine water using Isotope Ratio Mass Spectrometry (IRMS), and the other one uses Deuterium-Nuclear Magnetic Resonance (2H-NMR) to measure the deuterium of the wine ethanol. Recently, off-axis integrated cavity output (laser) spectroscopy (OA-ICOS) has become an easier alternative to quantify wine water isotopes, thanks to the spectral contaminant identifier (SCI). We utilized an OA-ICOS analyser with SCI to measure the δ18O and δ2H of water in 27 wine samples without any pre-treatment. The OA-ICOS results reveal a wealth of information about the growth conditions of the wines, which shows the advantages to extend the official δ18O wine water method by δ2H that is obtained easily from OA-ICOS. We also performed high-temperature pyrolysis and chromium reduction combined with IRMS measurements to illustrate the “whole wine” isotope ratios. The δ18O results of OA-ICOS and IRMS show non-significant differences, but the δ2H results of both methods differ much more. As the δ2H difference between these two methods is mainly caused by ethanol, we investigated the possibility to deduce deuterium of wine ethanol from this difference. The results present large uncertainties and deviate from the obtained 2H-NMR results. The deviation is caused by the other constituents in the wine, and the uncertainty is due to the limited precision of the SCI-based correction, which need to improve to obtain the 2H values of ethanol as alternative for the 2H-NMR method.


Sign in / Sign up

Export Citation Format

Share Document