Published September 30, 1999 | Version v1
Journal article

Pathways and mean residence times of dissolved pollutants in the ocean derived from transient tracers and stable isotopes

  • 1. Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York, NY (United States)
  • 2. Institut fuer Umweltphysik, University of Heidelberg, Im Neuenheimer Feld 366, D-69120 Heidelberg (Germany)
  • 3. Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN (United States)
  • 4. Woods Hole Oceanographic Institution, Woods Hole, MA (United States)

Description

During the past decades, a variety of transient tracers have been used to derive information on pathways and mean residence times of oceanic water masses. Here, we discuss how information obtained in such studies can be applied to studying the spreading of dissolved pollutants in the ocean. The discussion focuses on the transient tracers tritium/3He and the H218O/H216O ratio of water. These tracers are used in combination with CFCs and 14C in a case study of Arctic Ocean contaminant transport to: (1) separate the freshwater components contained in the near-surface waters; (2) infer mean pathways of freshwater and associated contaminants from the H218O/H216O distribution in the surface waters; and (3) determine mean residence times of the surface, intermediate, deep and bottom waters

Additional details

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
237-238
Journal Issue
0
Journal Page Range
p. 15-30
ISSN
0048-9697