TY - JOUR
T1 - Anthropogenic 236U and 129I in the Mediterranean Sea
T2 - First comprehensive distribution and constrain of their sources
AU - Castrillejo, M.
AU - Casacuberta, N.
AU - Christl, M.
AU - Garcia-Orellana, Jordi
AU - Vockenhuber, C.
AU - Synal, H.A.
AU - Masque Barri, Pere
PY - 2017/9/1
Y1 - 2017/9/1
N2 - The first basin-wide distribution of 236U/238U atom ratios and 129I concentrations is presented for the Mediterranean Sea. During the GEOTRACES GA04S-MedSeA expedition in 2013 seawater was collected from 10 vertical profiles covering the principal sub–basins of the Mediterranean Sea. The main objective was to understand the distributions of 236U and 129I in relation to the water masses, and to constrain their sources in this region. The 236U/238U atom ratios and the 129I concentrations ranged from (710 ± 40) × 10− 12 to (2220 ± 60) × 10− 12 and from (4.0 ± 0.1) × 107 to (13.8 ± 0.3) × 107 at·kg− 1, respectively. The results show that radionuclide–poor Atlantic Water is entering at the surface through the Strait of Gibraltar whereas comparably radionuclide-enriched Levantine Intermediate Water is sinking in the Eastern Basin and flowing westward at intermediate depths. Low radionuclide levels were found in the oldest water masses at about 1000–2000 m depth in the Eastern Basin. At greater depths, waters were relatively enriched in 236U and 129I due to dense water formation occurring in both, the Eastern and Western Basins. The inventories of 236U and 129I cannot be explained only by global fallout from atmospheric nuclear bomb testings carried out in the 1950s and 1960s. We estimate that the liquid input of 236U from the nuclear reprocessing facility of Marcoule (France), via the Rhône river, was of the same order of magnitude than the contribution from global fallout, whereas liquid and gaseous releases of 129I from Marcoule were up to two orders of magnitude higher than global fallout. For both radionuclides, the contribution from the Chernobyl accident is found to be minor.
AB - The first basin-wide distribution of 236U/238U atom ratios and 129I concentrations is presented for the Mediterranean Sea. During the GEOTRACES GA04S-MedSeA expedition in 2013 seawater was collected from 10 vertical profiles covering the principal sub–basins of the Mediterranean Sea. The main objective was to understand the distributions of 236U and 129I in relation to the water masses, and to constrain their sources in this region. The 236U/238U atom ratios and the 129I concentrations ranged from (710 ± 40) × 10− 12 to (2220 ± 60) × 10− 12 and from (4.0 ± 0.1) × 107 to (13.8 ± 0.3) × 107 at·kg− 1, respectively. The results show that radionuclide–poor Atlantic Water is entering at the surface through the Strait of Gibraltar whereas comparably radionuclide-enriched Levantine Intermediate Water is sinking in the Eastern Basin and flowing westward at intermediate depths. Low radionuclide levels were found in the oldest water masses at about 1000–2000 m depth in the Eastern Basin. At greater depths, waters were relatively enriched in 236U and 129I due to dense water formation occurring in both, the Eastern and Western Basins. The inventories of 236U and 129I cannot be explained only by global fallout from atmospheric nuclear bomb testings carried out in the 1950s and 1960s. We estimate that the liquid input of 236U from the nuclear reprocessing facility of Marcoule (France), via the Rhône river, was of the same order of magnitude than the contribution from global fallout, whereas liquid and gaseous releases of 129I from Marcoule were up to two orders of magnitude higher than global fallout. For both radionuclides, the contribution from the Chernobyl accident is found to be minor.
KW - I
KW - U
KW - Artificial radionuclides
KW - GEOTRACES
KW - Mediterranean Sea
UR - http://www.scopus.com/inward/record.url?scp=85016424062&partnerID=8YFLogxK
U2 - 10.1016/j.scitotenv.2017.03.201
DO - 10.1016/j.scitotenv.2017.03.201
M3 - Article
C2 - 28364609
AN - SCOPUS:85016424062
SN - 0048-9697
VL - 593-594
SP - 745
EP - 759
JO - Science of the Total Environment
JF - Science of the Total Environment
ER -