Published

Dissolved Fe (DFe) and Fe-binding dissolved organic ligands were analysed during two GEOTRACES cruises in the Mediterranean Sea in May and August 2013 - data Version 5

Loes Gerringa (Royal Netherlands Institute for Sea Research) Royal Netherlands Institute for Sea Research https://doi.org/10.25850/nioz/7b.b.fj

Method: Competing ligand exchange adsorptive cathodic stripping voltammetry (CLE-aCSV) was performed using two systems consisting of a μAutolab potentionstat (Metrohm Autolab B.V.), a 663 VA stand with a Hg drop electrode (Metrohm) and a 778 sample processor with ancillary pumps and dosimats (Metrohm), all controlled using a consumer laptop running Nova 1.9 (Metrohm Autolab B.V.). The characteristics of Fe-binding dissolved organic ligands, that is both the ligand concentration [Lt] (in nano-equivalents of molar Fe, nEq of M Fe) and the conditional binding constant K′ (M−1) with respect to [Fe3+], commonly expressed as log K′ are determined using 2- (2-Thiazolylazo)-p-cresol (TAC) as an added measuring ligand (Croot and Johansson, 2000). TAC was used with a final concentration of 10 μM, and the complex (TAC)2-Fe was measured after equilibration (> 6 h). The increments of Fe concentrations used in the titration were 0 (2×), 0.2, 0.4, 0.6, 0.8, 1.0, 1.2, 1.5, 2, 2.5, 3, 4, 6, and 8 (2×) nM. Using a non-linear regression of the Langmuir isotherm, the electrical signal recorded in nA (nano-Ampere) was converted into a concentration in nM, and the ligand concentration [Lt] and the binding strength K were estimated (Gerringa et al., 2014). Using [Lt] and K, the concentration of Fe bound to a natural Febinding ligand [FeL], the concentration of inorganic Fe [Fe′] and the concentration of natural unbound ligand [L′] were calculated under the assumption of chemical equilibrium. Since K is log transformed, the standard error (SE) is asymmetric to lower and upper values; therefore two SE values are obtained, one to lower (down) and to upper (up) values.

Data and Resources

Additional Info

Field Value
Subject Earth and Environmental Sciences
DAS Code 7b.b.fj
Source https://doi.org/10.25850/nioz/7b.b.fj
Version 5
Creator(s)
Gerringa, Loes (Royal Netherlands Institute for Sea Research)
ORCID
Contact the corresponding author

Slagter, Hans (Royal Netherlands Institute for Sea Research)
ORCID

Rijkenberg, Micha (Royal Netherlands Institute for Sea Research)
ORCID
Depositor loes gerringa (loes.gerringa@nioz.nl)
Publication Date 2025-03-11T10:08:06.8962839
Deposit Date 2025-03-11
Dataset Persistent Identifier DOI:10.25850/nioz/7b.b.fj
Alternate identifier
Related identifier http://dx.doi.org/10.1016/j.marchem.2017.05.012
Contributor Royal Netherlands Institute for Sea Research (NIOZ)
Distributor Research Data Management(NIOZ Royal Netherlands Institute for Sea Research)
Distribution Date 2025-03-11
Production Date 2025-03-11
Dates
Collected
2013-05-14 until 2013-06-05

Collected
2013-07-25 until 2013-08-11
Funding References
NWO (822.01.015)
Geotraces

NWO (822.01.018)
PhD - HS
Geographic Coverage
North Bound: 40.96124
South Bound: 33.8426
West Bound: -14.1665
East Bound: 31.94044