z-logo
Premium
High‐precision determination of 18 O/ 16 O ratios of silver phosphate by EA‐pyrolysis‐IRMS continuous flow technique
Author(s) -
Lécuyer Christophe,
Fourel François,
Martineau François,
Amiot Romain,
Bernard Aurélien,
Daux Valérie,
Escarguel Gilles,
Morrison John
Publication year - 2007
Publication title -
journal of mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.475
H-Index - 121
eISSN - 1096-9888
pISSN - 1076-5174
DOI - 10.1002/jms.1130
Subject(s) - chemistry , pyrolysis , analytical chemistry (journal) , phosphate , mass spectrometry , ammonium dihydrogen phosphate , isotope ratio mass spectrometry , calibration curve , nuclear chemistry , chromatography , detection limit , organic chemistry , fertilizer
A high‐precision, and rapid on‐line method for oxygen isotope analysis of silver phosphate is presented. The technique uses high‐temperature elemental analyzer (EA)‐pyrolysis interfaced in continuous flow (CF) mode to an isotopic ratio mass spectrometer (IRMS). Calibration curves were generated by synthesizing silver phosphate with a 13‰ spread in δ 18 O values. Calibration materials were obtained by reacting dissolved potassium dihydrogen phosphate (KH 2 PO 4 ) with water samples of various oxygen isotope compositions at 373 K. Validity of the method was tested by comparing the on‐line results with those obtained by classical off‐line sample preparation and dual inlet isotope measurement. In addition, silver phosphate precipitates were prepared from a collection of biogenic apatites with known δ 18 O values ranging from 12.8 to 29.9‰ (V–SMOW). Reproducibility of ± 0.2‰ was obtained by the EA‐Py‐CF‐IRMS method for sample sizes in the range 400–500 µg. Both natural and synthetic samples are remarkably well correlated with conventional 18 O/ 16 O determinations. Silver phosphate is a very stable material and easy to degas and, thus, could be considered as a good candidate to become a reference material for the determination of 18 O/ 16 O ratios of phosphate by high‐temperature pyrolysis. Copyright © 2006 John Wiley & Sons, Ltd.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here