Isotope effects accompanying δ2H, δ18O and δ17O analyses of aqueous saline solutions using cavity ring-down laser spectroscopy

被引:0
|
作者
Dulinski, Marek [1 ]
Rozanski, Kazimierz [1 ]
Pierchala, Anna [1 ,2 ]
Gorczyca, Zbigniew [1 ]
机构
[1] AGH Univ Krakow, Fac Phys & Appl Comp Sci, Krakow, Poland
[2] AGH Univ Krakow, Fac Phys & Appl Comp Sci, Al Mickiewicza 30, PL-30059 Krakow, Poland
关键词
LIQUID WATER EQUILIBRATION; STABLE-ISOTOPE; SALT-SOLUTIONS; HYDROGEN ISOTOPES; EVAPORATING BRINES; OXYGEN-ISOTOPE; FRACTIONATION; ORIGIN; BASIN; GEOCHEMISTRY;
D O I
10.1002/rcm.9680
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
Rationale: The presence of substantial amounts of dissolved salts creates serious difficulties in isotope analyses of water samples using conventional isotope ratio mass spectrometry. Although nowadays laser-based instruments are increasingly used for this purpose, a comprehensive assessment of isotope effects associated with direct analyses of aqueous saline solutions using this technology is lacking.Methods: Here we report the results of laboratory experiments aimed at quantifying isotope effects associated with direct, delta H-2, delta O-18 and delta O-17 analyses of single-salt solutions and double-salt mixtures prepared with a water of known isotopic composition. Three single-salt solutions (NaCl, CaCl2 and MgSO4) and two double-salt mixtures (NaCl + CaCl2 and NaCl + MgSO4) were prepared and investigated for a wide range of molalities. The triple-isotope composition of the prepared solutions was analysed with the aid of a Picarro L2140-i Cavity Ring-Down Spectroscopy analyser.Results: The NaCl and CaCl2 solutions revealed small negative salt effects, independent of molality and comparable with measurement uncertainty. The MgCl2 solution showed the highest salt effects, reaching saturated solution ca. +2.7 parts per thousand (H-2), -3.5 parts per thousand (O-18) and -1.7 parts per thousand (O-17). Salt effects for the double-salt mixtures generally mirrored the effects observed for the single-salt solutions. The observed salt effects are discussed in the context of processes occurring during the injection of the salt solutions into the vaporizer unit of the CRDS analyser.Conclusions: The presented study has demonstrated feasibility of direct, triple-isotope analyses of aqueous salt solutions using a Picarro L2140-i CRDS analyser for a broad range of salinities up to saturated conditions. Large uncertainties of O-17-excess determinations for solutions forming hydrated salts preclude the use of this parameter for interpretation purposes.
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页数:13
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