Japan Geoscience Union Meeting 2016

Presentation information

Poster

Symbol M (Multidisciplinary and Interdisciplinary) » M-TT Technology & Techniques

[M-TT28] Frontiers in Geochemistry : Prospect for geochemistry and cosmochemistry in future

Sun. May 22, 2016 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall HALL6)

Convener:*Hajime Obata(Marine inorganic chemistry division, Atmosphere and Ocean Research Institute, University of Tokyo), Hirochika Sumino(Department of Basic Science, Graduate School of Arts and Sciences, The University of Tokyo), Tetsuya Yokoyama(Department of Earth and Planetary Sciences, Graduate School of Science and Engineering, Tokyo Institute of Technology), Takafumi Hirata(Graduate School of Science, Kyoto University), Urumu Tsunogai(Graduate School of Environmental Studies, Nagoya University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Shogo Tachibana(Department of Natural History Scieces, Hokkaido University), Katsuhiko Suzuki(Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology), Gen Shimoda(Geological Survey of Japan, AIST), Hiroyuki Kagi(Geochemical Research Center, Graduate School of Science, University of Tokyo), Yusuke Yokoyama(Atmosphere and Ocean Research Institute, University of Tokyo)

5:15 PM - 6:30 PM

[MTT28-P08] Speciation of Cu in seawater by using CLE-CSV with multi-detection windows

*Hajime Obata1, Kuo Hong Wang1, Taejin Kim1, Toshitaka Gamo1 (1.Atmosphere and Ocean Research Institute, University of Tokyo)

Keywords:ocean, Cu, organic ligand

I. Introduction
Copper is an essential micronutrient for all living organisms as it plays an important role in electron transfer in many life-supporting systems, and is present in many enzymes and proteins. On the other hand, at high concentrations in seawater, Cu2+ is known to be toxic for marine phytoplankton. Therefore, many phytoplankton and bacterial species have the ability to release Cu-complexing ligands to decrease the concentration of free Cu2+ and reduce its toxicity. As a result, at the eutrophic surface waters, most of Cu form complexes with organic ligands.
For the Cu speciation study in the ocean, competitive ligand equilibrium/cathodic stripping voltammetry (CLE/CSV) is frequently applied. However, some problems have been proposed on the CLE/CSV methods recently. One problem is concerning on “detection window”, which is defined by the conditional stability constant and concentration of the competitive ligands. To measure the conditional stability constants and concentrations of main ligands (usually two ligands) accurately, we have to apply the CLE/CSV method with multi detection windows for the speciation. In this study, we determined the total dissolved Cu concentrations and estimated Cu speciation in seawater by using the CLE/CSV method with multi detection windows in the East China Sea and its surrounding areas.
II. Sampling and methods
Seawater samples were collected using acid-cleaned, Teflon-coated X-type Niskin samplers mounted on conductivity-temperature-depth carousel multi-sampling system (CTD-CMS) onboard R/V Shinsei Maru during KS-15-6 cruise (2015/06/25 - 2015/07/06). The samples were collected in low-density polyethylene bottles through a 0.2 µm-pore size filter. Samples for total Cu analysis were acidified to a pH of less than 1.8 using ultrapure HCl, and stored. Another set of samples, for CLE/CSV analysis, was frozen at -18oC immediately after sampling. The samples were brought back to the laboratory and analyzed using CLE-CSV with salicylaldoxime (SA) as the competing ligand (Campos and van den Berg, 1994).
Samples used for total dissolved Cu were placed under UV radiation for 60 minutes to destroy all organic ligands prior to analysis. Frozen samples for Cu speciation analysis were allowed to thaw for 24 hours at 4oC, and then placed at room temperature for 4-8 hours. 10mL of sample, borate buffer, and a known concentration of Cu were added into two sets of 10 Teflon vials, left for at least 2 hours to allow the natural ligands to equilibrate with the added Cu, and the competing ligand, SA, was then added into the solution. The vials were then left to equilibrate overnight before analysis. 5 µM SA and 1 µM SA were used as the competing ligand for each of the two titrations, respectively.
III. Results and Discussion
Total dissolved Cu concentrations ranged from 0.47 to 4.65 nM. In surface waters with low salinities, higher concentrations of Cu were observed, which can be attributed to the freshwater discharge with high Cu concentrations from Yangtze River. Two classes of ligands were found in the surface waters in this study. The concentration of the stronger ligand, L1, ranged from 3.6 nM to 11.2 nM, with log K values of 13 – 14.1, whereas for the weaker ligand, L2, the concentrations were in the range of 25.6 nM to 47.6 nM, with log K values of 11.7 – 12.2. The variation of the strong ligands suggests that these ligands were biologically produced in situ by marine microorganisms.