Investigation of iron(III) reduction and trace metal interferences in the determination of dissolved iron in seawater using flow injection with luminol chemiluminescence detection

被引:38
|
作者
Ussher, Simon J. [1 ]
Milne, Angela [1 ,2 ]
Landing, William M. [2 ]
Attiq-ur-Rehman, Kakar [4 ]
Seguret, Marie J. M. [1 ]
Holland, Toby [1 ]
Achterberg, Eric P. [3 ]
Nabi, Abdul [4 ]
Worsfold, Paul J. [1 ]
机构
[1] Univ Plymouth, SEOES, Plymouth PL4 8AA, Devon, England
[2] Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA
[3] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England
[4] Univ Balochistan, Dept Chem, Quetta, Pakistan
基金
英国自然环境研究理事会;
关键词
Flow injection; Chemiluminescence; Luminol; Seawater; Iron; PICOMOLAR CONCENTRATIONS; CHEMI-LUMINESCENCE; REDOX SPECIATION; NANOMOLAR LEVELS; SURFACE WATERS; NORTH PACIFIC; MANGANESE; PRECONCENTRATION; COMPLEXATION; OXIDATION;
D O I
10.1016/j.aca.2009.06.011
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
A detailed investigation into the performance of two flow injection-chemiluminescence (FI-CL) manifolds (with and without a preconcentration column) for the determination of sub-nanomolar dissolved iron (Fe(II) + Fe(III)), following the reduction of Fe(III) by sulphite, in seawater is described. Kinetic experiments were conducted to examine the efficiency of reduction of inorganic Fe(III) with sulphite under different conditions and a rigorous study of the potential interference caused by other transition metals present in seawater was conducted. Using 100 mu M concentrations of sulphite a reduction time of 4 h was sufficient to quantitatively reduce Fe(III) in seawater. Under optimal conditions, cobalt(II) and vanadium(IV)/(III) were the major positive interferences and strategies for their removal are reported. Specifically. cobalt(II) was masked by the addition of dimethylglyoxime to the luminol solution and vanadium(IV) was removed by passing the sample through an 8-hydroxyquinoline column in a low pH carrier stream. Manganese(II) also interfered by suppression of the CL response but this was not significant at typical open ocean concentrations. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:259 / 265
页数:7
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