Vertical Fe GoFlo measurements from R/V Tangaroa cruise 61TG_3052 in the Southern Ocean in 1999 (SOIREE project)

• Main Authors: Andrew R. Bowie, Dr Russell D. Frew, Doug Mackie
• Format: Dataset
• Language: unknown
• Published: Biological and Chemical Oceanography Data Management Office (BCO-DMO) 2009
• Subjects: oceans; Bruland; Southern Ocean
• Online Access: https://search.dataone.org/view/sha256:da958eedfb789098c3d5e6c19f7274557550cd1c880aad2c903c507c18738410

SOIREE Vertical Fe GoFlo Data<br><br> During the cruise we had the following three objectives:<br> (1) Undertake continuous sampling of the infused patch for dissolved/total iron<br> (2) Obtain samples from vertical profiles, using Go-Flo bottles, to examine the<br> partitioning between dissolved and particulate iron within the water column, both<br> inside and outside the patch.<br> (3) Undertake measurements to determine iron speciation within the water column.<br> <br> Go-Flo casts were taken both inside and outside the patch during the course<br> of the experiment. Typically, water samples were obtained from four standard<br> depths (20, 40, 60 and 80 m) throughout the water column at each station. Deeper<br> samples (> 80 m) were obtained at some stations to examine the concentration of<br> iron below the mixed layer. Both filtered (0.2 um) and unfiltered samples were<br> collected. These samples will be analysed for Fe and other trace metals (Zn, Cd, Mn, Cu)<br> back in the clean laboratory at the University of Otago.<br> <br> The speciation of iron was measured using competitive ligand exchange cathodic stripping<br> voltammetry (CLE CSV) on samples from 40 m depth from stations both inside and outside the<br> patch. This technique determines the total concentration of iron binding ligands present<br> in the sample and their relative binding strengths. From the data generated an estimation<br> of the inorganic iron concentration, Fe`, can also be made, this value can be used to<br> approximate the amount of iron that may be available for uptake by the phytoplankton.<br> <br> <i><b>References</b><br> Bowie, A.R., Maldonado, M.T., Frew, R.D., Croot P.L., Achterberg, E.A., Mantoura, R.F.C.,<br> Worsfold, P.J., Law, C.S., Boyd P.W., The Fate of Added Iron during a Mesoscale Fertilisation<br> Experiment in the Southern Ocean, Deep-Sea Research II (2001), SOIREE special issue, in the press.<br> <br> Bruland, K.W., Franks, R.P., Knauer, G.A., Martin, J.H., 1979. Sampling and analytical methods for<br> the determination of copper, cadmium, zinc and nickel at the nanogram per litre level in seawater.<br> Analytica Chimica Acta 105, 233-245.<br> <br> Danielsson, L.G., Magnusson, B., Westerlund, S., Zhang, K., 1982. Trace-metal determinations<br> in estuarine waters by electrothermal atomic-absorption spectrometry after extraction of<br> dithiocarbamate complexes into freon. Analytica Chimica Acta 144, 183-188.<br> </i><br>