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Estimate of European 129I Releases Supported by 129I Analysis in an Alpine Ice Core
journal contribution
posted on 2006-10-01, 00:00 authored by Herbert Reithmeier, Vitali Lazarev, Werner Rühm, Margit Schwikowski, Heinz W. Gäggeler, Eckehart Nolte129I in the European environment originates predominantly
from the industrial nuclear fuel reprocessing plants
Sellafield (Great Britain), Marcoule, and La Hague (both
France). While reliable data on 129I releases from La Hague
exist for the whole period of operation, less is known
about the contributions from Sellafield and Marcoule. For
those periods where no data are available, i.e., for the
first 16 years of the Sellafield operation and for the first 3
decades of the Marcoule operation, we estimated
releases into the atmosphere of 118 GBq and 825 GBq,
respectively. Hence, Marcoule was the major European
source of airborne 129I, contributing about 45% to the total
airborne 129I releases from all the European reprocessing
facilities, until it was decommissioned in 1997. The estimated
total emissions were compared with 129I deposition
fluxes for the time period 1970−2002, obtained from the
analysis of an ice core from Fiescherhorn glacier, Swiss Alps
(46°33'N, 08°04'E; 3900 m asl). The temporal evolution of
the 129I deposition agrees well with the total 129I releases into
the atmosphere from the European reprocessing facilities
and from atmospheric nuclear weapons tests, supporting
our estimated release rates. However, the 129I concentrations
and deposition fluxes at Fiescherhorn glacier were a
factor of 6 lower than values obtained from the analysis
of rainwater collected near Zurich (408 m asl) in Switzerland
in the years 1994−97. This suggests a strong vertical
concentration gradient of 129I, typical for water-soluble
atmospheric trace species which are removed from the
atmosphere in the course of days by precipitation scavenging,
and must be taken into account if glaciers are used as
an archive for a retrospective quantification of 129I deposition
fluxes. In addition, the temporal evolution of the contribution
of 129I re-emitted from the ocean's surface for the 129I
inventory in the atmosphere was quantified for the first
time. Although the annual amount of 129I released this way
was very low until the early 1990s, it is similar to the
airborne 129I releases from Sellafield and La Hague in the
present time.