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

Anthropogenic iron impact on the surface productivity in the Pacific Transition Zone

Hawco and colleagues investigated the influence of industrial emissions on oceanic iron supply and its ecological consequences in the North Pacific.

Trace metal effluxes from Peruvian shelf sediments

Liu and co-authors compared four methods to estimate dissolved iron fluxes from Peruvian shelf sediments, revealing large variability.

Coupling copper and neodymium data highlights the importance of the margin sources for the copper oceanic cycle

Lemaitre and co-workers analysed the dissolved concentrations and isotopes along the GEOVIDE (GA01) section in the North Atlantic Ocean.

High levels of anthropogenic lead in the Indian Ocean

Yadav and her colleagues provide comprehensive insights into the distribution and sources of dissolved lead in the Indian Ocean.

Rechercher