hdl:10013/epic.32593
227Ac in the marine environment
Contact
wgeibert [ at ] awi-bremerhaven.de
Abstract
Users of the RaDeCC-system routinely measure 227Ac in order to determine 223Ra excess. The obtained 227Ac signal is more than just background. It has the potential to be widely used for water mass dating, calculation of mixing rates, or the determination of deep upwelling. This presentation aims to give an overview about the properties of Actinium and the resulting applications.
Item Type
Conference
(Talk)
Authors
Divisions
Programs
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL2-Southern Ocean climate and ecosystem
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL7-From permafrost to deep sea in the Arctic
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL2-Southern Ocean climate and ecosystem
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL7-From permafrost to deep sea in the Arctic
Publication Status
Published
Event Details
Overview Lecture, 1st workshop on measurements of short-lived Radium isotopes using the RaDeCC delayed coincidence system, Marine Environment Laboratory of the IAEA, 2-6 Oct, Monaco..
Eprint ID
15763
Cite as
Geibert, W.
(2006):
227Ac in the marine environment
,
Overview Lecture, 1st workshop on measurements of short-lived Radium isotopes using the RaDeCC delayed coincidence system, Marine Environment Laboratory of the IAEA, 2-6 Oct, Monaco.
.
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ANT > XV > 2
ANT > XV > 3
ANT > XVI > 3
ANT > XVII > 4
ANT > XX > 2
ANT > XXIII > 1
ANT > XV > 3
ANT > XVI > 3
ANT > XVII > 4
ANT > XX > 2
ANT > XXIII > 1
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