High resolution pore water delta2H and delta18O measurements by H2O(liquid)-H2O(vapor) equilibration laser spectroscopy.
A new H2O(liquid)-H2O(vapor) pore water equilibration and laser spectroscopy method provides a fast way to obtain accurate high resolution deltaD and delta18O profiles from single core samples from saturated and unsaturated geologic media. The precision and accuracy of the H2O(liquid)-H2O(vapor) equilibration method was comparable to or better than conventional IRMS-based methods, and it can be conducted on geologic cores that contain volumetric water contents as low as 5%. Significant advantages of the H2O(liquid)-H2O(vapor) pore water equilibration method and laser isotopic analysis method include dual hydrogen- and oxygen-isotope assays on single small core samples, low consumable and instrumentation costs, and the potential for field-based hydrogeologic profiling. A single core is sufficient to obtain detailed vertical isotopic depth profiles in geologic, soil, and lacustrine pore water, dramatically reducing the cost of obtaining pore water by conventional wells or physical water extraction methods. In addition, other inherent problems like contamination of wells by leakage and drilling fluids can be eliminated.
Wassenaar
L I
LI
Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK, Canada. len.wassenaar@ec.gc.ca
Hendry
M J
MJ
Chostner
V L
VL
Lis
G P
GP
D002170:Canada; D003903:Deuterium / Q000032:analysis*; D005618:Fresh Water / Q000737:chemistry; D006813:Humidity; D007834:Lasers; D010100:Oxygen / Q000032:analysis*; D010103:Oxygen Isotopes; D016062:Porosity; D015203:Reproducibility of Results; D013057:Spectrum Analysis / Q000379:methods*; D013227:Steam / Q000032:analysis*; D013696:Temperature; D013997:Time Factors; D014867:Water / Q000737:chemistry*
D010103:Oxygen Isotopes; D013227:Steam; D014867:Water; D003903:Deuterium; D010100:Oxygen