Onboard analysis of dissolved zinc everywhere in the open ocean with a Lab on Valve (LOV) system of the size of a bottle of wine is becoming possible

Thanks to the work of Maxime Grand and collaborators (2016, see reference below), it is now possible to analyse dissolved zinc (DZn) on board, from any kind of seawater using a “Lab On Valve (LOV)” method. For the first time, automated matrix removal, extraction of the target element, and fluorescence detection have been performed within a miniaturized flow manifold. The original flow programming is designed to pass sample through a minicolumn where the target analyte and other complexable cations are retained, while the seawater matrix is washed out. Once eluted, Zn is merged with a Zn selective fluorescent probe (FluoZin-3) prior to fluorescence detection in the LOV flow cell. This new shipboard method features a detection limit of 0.02 nM and a reagent consumption of 150 microliters per sample.

Successful comparison with GEOTRACES reference standards and analytical comparison with inductively coupled plasma mass spectrometry (ICPMS) eventually validate this beautiful, tiny and robust method.

16 Grandetal
Figure: A close up of the Lab-On-Valve (LOV) module, where microliter volumes of fluids are manipulated prior to fluorescence detection in the LOV flow cell (red circle). Right: Comparison of DZn profiles from the South Indian Gyre analysed via LOV and ICPMS.

Reference:

Grand, M. M., Chocholouš, P., Růžička, J., Solich, P., & Measures, C. I. (2016). Determination of trace zinc in seawater by coupling solid phase extraction and fluorescence detection in the Lab-On-Valve format. Analytica Chimica Acta, 923, 45–54. doi:10.1016/j.aca.2016.03.056

 

Latest highlights

Continuous record of the Antarctic Circumpolar Current latitude over the last glacial-interglacial cycles

The meridional positions of the oceanic fronts separating subtropical and Antarctic waters are key to constraining the mechanisms that drive the degassing of deeply-stored CO2 at the end of the glacial periods…

23 Million Years of iron sources reconstructed in the Northwest Pacific Ocean using iron isotopes in a ferromanganese crust

Using iron isotopes and elemental records, Chu and co-workers analysed an iron-manganese crust recovered from the Hongyan Seamount, and reconstructed the sources of dissolved Fe to the Northwest Pacific Ocean…

Variability of the past deep-water masses in the Arabian Sea over the last 41ka

Shukla and colleagues propose a high-resolution authigenic ƐNd record measured from a sediment core located in the eastern Arabian Sea…

Arctic outflows to Davis Strait and the Labrador Sea traced by radionuclide distributions

This study demonstrates that Arctic outflows through the Canadian Arctic Archipelago play a much more significant role than previously recognised.

Rechercher