Reagents having a high redox power (cobalt(III) and chromium(II) ions) were applied to on-line pretreatments in flow analyses. A flow-through electrolysis cell for continuous reagent generation was assembled and put in a system of FIA or HPLC. The cobalt (III) ion was strong enough to oxidatively decompose diverse organic compounds within a short time ( <
ca. 10 min, depending on the chemical structure of the compounds), even at ordinary temperature. Thus, the cobalt(III) pretreatment was successfully applied to the FIA determination of total mercury and organic phosphorus; organomercury and organic phosphorus compounds were digested to mercury(II) and phosphate ions, respectively, which are detectable species by subsequent cold-vapor (CV) - atomic fluorescence (AF) and Molybdenum Blue spectrophotometric detections. Further, the author has proposed a novel method for a chemical oxygen-demand determination based on cobalt (III) oxidation, because it can be done rapidly using a simple FIA manifold with no requirement for a heating process. Chromium(II) ion, on the other hand, has a very strong reducing power. This ion can completely reduce the stable mercury-iodide complex, HgI
42-, to elemental mercury, thus enabling AF detection. In the present method, the addition of iodide ion ( >10 mg dm
-3) to a sample solution gave good results with respect to the accuracy and precision, because iodide ions act as a stabilizer against the coexisting interfering substances and/or mercury deposition at the inner wall of the manifolds. A reversed-phase HPLC system coupled with CV generation based on chromium(II) reduction and AF detection was developed for organomercury speciation. An on-line reagent-generation method was concluded to afford great advantages to flow analyses. It enables the application of highly reactive (thus unstable) or poisonous reagents, which are impracticable under normal analytical condition, because the process from reagent generation to its use can be done within a short time in semi-closed flow system isolated from the atmosphere.
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