Dw. Yang et al., ASSAY OF LOW DEUTERIUM ENRICHMENT OF WATER BY ISOTOPIC EXCHANGE WITH [U-C-13(3)]ACETONE AND GAS-CHROMATOGRAPHY MASS-SPECTROMETRY, Analytical biochemistry, 258(2), 1998, pp. 315-321
Citations number
26
Categorie Soggetti
Biology,"Biochemical Research Methods","Chemistry Analytical
A sensitive assay of the H-2-enrichment of water based on the isotopic
exchange between the hydrogens of water and of acetone in alkaline me
dium is described and validated. For low H-2-enrichments (0.008 to 0.5
%), the sample is spiked with [U-C-13(3)]acetone and NaOH. After excha
nge, H-2-enriched [U-C-13(3)]acetone is extracted with chloroform and
assayed by gas chromatography-mass spectrometry. With some instruments
, ion-molecule reactions, resulting in increased baseline enrichment,
are minimized by lowering the electron ionization energy from the usua
l 70 to 10 eV. The H-2-enrichment of water is amplified nearly sixfold
in the M4/M3 ratio of [U-C-13(3)]acetone. For high H-2-enrichments (0
.25 to 100%), the use of unlabeled acetone suffices. After exchange, t
he mass isotopomer distribution of acetone is analyzed, yielding the H
-2 enrichment of water. The assay with [U-C-13(3)]acetone allows measu
ring the H-2-enrichment of water even in biological samples containing
acetone. This technique is more rapid and economical than the classic
al isotope ratio mass spectrometric assay of the enrichment of hydroge
n gas derived from the reduction of water. (C) 1998 Academic Press.