Rationale Stable isotope analyses of environmental waters (δ2H, δ18O) are an important
assay in hydrology and environmental research with rising interest in δ17O, which requires …

Measurements of δ2H and δ18O composition of pore waters in saturated and unsaturated
soil samples are routinely performed in hydrological studies. A variety of in‐situ and lab …

For more than two decades, research groups in hydrology, ecology, soil science, and
biogeochemistry have performed cryogenic water extractions (CWEs) for the analysis of δ 2 …

Cryogenic water extraction is the most widely used method to facilitate the laboratory
removal of soil pore water for isotopic analysis. However, recent studies have suggested that …

Stable isotopes are extensively used as tracers for the study of plant‐water sources. Isotope‐
ratio infrared spectroscopy (IRIS) offers a cheaper alternative to isotope‐ratio mass …

Rationale The stable isotope ratios of water (δ2H and δ18O values) have been widely used
to trace water in plants in a variety of physiological, ecohydrological, biogeochemical and …

High-precision analysis of the 17 O/16 O isotope ratio in water and water vapor is of interest
in hydrological, paleoclimate, and atmospheric science applications. Of specific interest is …

Cryogenic vacuum extraction (CVE), the most popular method for obtaining xylem water for
isotopic analysis of ecosystems, is known to cause δ 2 H offset and may lead to biased …

Rationale Water stable isotope ratios (δ 2H and δ 18O values) are widely used tracers in
environmental studies; hence, accurate and precise assays are required for providing sound …

Rationale Although laser absorption spectrometry (LAS) instrumentation is easy to use, its
incorporation into laboratory operations is not easy, owing to extensive offline manipulation …