Radium isotopes and 228Th in surface water samples collected on POLARSTERN expedition PS94

Radium isotopes are produced by decay of an isotope of thorium, a highly particle reactive element. Radium is relatively soluble in seawater such that once a thorium isotope in suspended or bottom sediments decays, a fraction of the produced radium isotope may be released to solution. 224Ra (3.7-day...

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Bibliographic Details
Main Authors: Rutgers van der Loeff, Michiel M, Stimac, Ingrid, Bauch, Dorothea, Valk, Ole, Geibert, Walter, Vieira, Lucia Helena
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Arctic Ocean
Area/locality
ARK-XXIX/3
Barents Sea
DATE/TIME
DEPTH
water
Event label
Gamma spectroscopy
GEOTRACES
Global marine biogeochemical cycles of trace elements and their isotopes
In situ pump
In-Situ-Pump
ISP
LATITUDE
LONGITUDE
Method comment
Polarstern
PS94
PS94/050-5
PS94/054
PS94/058
PS94/062
PS94/068
PS94/075
PS94/081-9
PS94/087
PS94/091
PS94/096-5
PS94/099
PS94/101-6
PS94/117-7
PS94/119
PS94/121
PS94/123
PS94/125-8
PS94/129
PS94/132
PS94/135
PS94/136
PS94/137
PS94/138
PS94/139
PS94/140
PS94/147
PS94/153-6
PS94/161-5
PS94/169
PS94/173
PUMP
Arctic
Makarov Basin
makarov basin
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.936052
https://doi.org/10.1594/PANGAEA.936052

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