The impact of temperature on the water isotope (<sup>2</sup>H/<sup>1</sup>H, <sup>17</sup>O/<sup>16</sup>O, <sup>18</sup>O/<sup>16</sup>O) fractionation upon transport through a low-density polyethylene membrane
Michael E. Böttcher, Iris Schmiedinger
Abstract
In the present study we investigated the isotope effects associated with water loss from closed low-density polyethylene (LDPE) bottles via diffusion at temperatures between 4 and 60 °C. While at low temperatures (4 and 10 °C) no substantial diffusional loss of water was observed within storage time, a pronounced loss was found for the experiments at room temperature and 60 °C. The latter was associated with a substantial increase in δ 18O, δ 17O, and δ 2Η values, and a decrease in the deuterium excess. The magnitude of the isotope effects essentially depended on the extent of water evaporation from the closed bottles through the LDPE membrane.
Topics & Concepts
DeuteriumIsotopeStable isotope ratioChemistryAnalytical Chemistry (journal)Oxygen-18RadiochemistryKinetic isotope effectEvaporationTritiumHeavy waterDiffusionNuclear physicsPhysicsChromatographyThermodynamicsMembrane Separation TechnologiesMembrane Separation and Gas TransportMembrane-based Ion Separation Techniques