Measuring actinium-227 by mass spectrometry is feasible, sensitive and reliable!

Science Highlights

5 July 2021

Actinium-227 (227Ac) is a radioelement (half-life = 22 y) produced in marine sediments by the decay of protactinium-231. 227Ac remobilization in the sediment is the main source of actinium to seawater. It makes of the 227Ac a good tracer of the process of remobilization from sediments and of the deep vertical mixing on decadal time scales. However, 227Ac was difficult to study until now because of its very low concentration in the environment, from 0 to 35 ag/kg (1ag = 10-18g) in seawater. Levier and co-authors (2021, see reference below) have developed a new protocol measurement of the dissolved actinium in seawater. This new measurement is by isotope dilution, chromatographic purification, and Multi-Collection Induced Coupled Mass Plasma Mass Spectrometry (ICPMS). The detection limit achieved with this method is around 1 ag/kg measured on samples of 10L of seawater. This new protocol was applied to archived samples from the Bonus GoodHope cruise (GIPY04) collected in 2008 in the Weddell Gyre. The resulting profile (see Figure) is consistent with previous data from the Weddell Gyre obtained by alpha spectrometry on 20-300 L seawater samples (Geibert and Vöge, 2008).

Figure: Seawater 227Ac profiles in Weddell Gyre, at station Super V from the Bonus GoodHope cruise, measured by mass spectrometry (green diamonds) which is in good agreement with 227Ac profiles at station PS2579–2 (Geibert et al., 2002) (black dot) and PS63–121 measured by alpha-spectrometry (Geibert and Vöge, 2008) (grey dots). All uncertainties are expressed at 2σ.

References:

Geibert, W., Vöge, I., 2008. Progress in the determination of 227Ac in sea water. Mar. Chem. 109, 238–249. https://doi.org/10.1016/j.marchem.2007.07.012

Levier, M., Roy-Barman, M., Colin, C., Dapoigny, A., 2021. Determination of low level of actinium 227 in seawater and freshwater by isotope dilution and mass spectrometry. Mar. Chem. 233, 103986. https://doi.org/10.1016/j.marchem.2021.103986

Latest highlights

The tumultuous life of the Antarctic Circumpolar Current over 5,3 million years, including focus on the glacial-interglacial forcing!

To reconstruct the strength of the Antarctic Circumpolar Current, the authors used sediment records from the pelagic central and remote South Pacific.

North-South radium-228 section in the Pacific Ocean

Moore and colleagues present results from radium-228 along the U.S. GEOTRACES Pacific Meridional Transect (GP15).

Strong lithogenic imprints in the Indian Ocean waters

Ueki and co-authors reported the first sectional distributions of zirconium, hafnium and niobium along a north-south track in the Indian Ocean.

The development of the modern Antarctic Circumpolar Current occurred much later than previously thought!

This study is challenging the belief that the onset of the Antarctic Circumpolar Current was solely triggered by the opening and deepening of Southern Ocean Gateways.

Rechercher