Author/Authors :
P. Schlosser، نويسنده , , b، نويسنده , , U، نويسنده , , R. Bayer ، نويسنده , , G. B¨onischa، نويسنده , , L.W. Cooperd، نويسنده , , B. Ekwurzela، نويسنده , ,
W.J. Jenkinse، نويسنده , , S. Khatiwalaa، نويسنده , , b، نويسنده , , S. Pfirmana، نويسنده , , f، نويسنده , , W.M. Smethiea، نويسنده ,
Abstract :
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
tritiumr 3He and the H128OrH126O 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 H128OrH126O
distribution in the surface waters; and 3. determine mean residence times of the surface, intermediate, deep and
bottom waters.
Keywords :
Tracers , Oceanic waters , Pathways , Residence times , pollutants