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Moreover, this assay was able to detect As(III) ions with high sensitivity and revealed to have remarkable potential applications.
Consistent experimental measurements for iron and other metals and the use of other techniques suggests that their interpretation of iron(III) being non-bioavailable is incorrect and, rather, the use of CLE-AdSV needs to be modified.
It is possible to determine 1–150 mg of iron(III).
The recoveries obtained for the spiked trace amount of Fe(III) ions were >95%, which confirmed the reliability of the method.
The results obtained are scientifically relevant, pointing out the potential of the new and straightforwardly synthesized ligands as analytical reagents for determination of iron(III).
It has been applied satisfactorily to the determination of iron(III) in tap water samples.

Related Questions

What colour is the iron(II) coordination polymer vs iron(III) coordination polymer?4 answersIron(II) coordination polymers exhibit a yellow color. Iron(III) coordination polymers, on the other hand, have a greenish color that changes to yellow upon the spin crossover phenomenon.
What are the standard methods for determining iron levels in the human body?4 answersStandard methods for determining iron levels in the human body include atomic absorption spectroscopy (AAS), titrimetric analysis, voltammetry, flame atomic absorption spectrometry, chromatography, flow injection analysis, gravimetry, photometry, and spectrophotometric methods. Non-invasive diagnostics using Magnetic Resonance Imaging (MRI) is also an accurate method for assessing iron accumulation in the body. Biochemical and biophysical methods have been developed for the determination of iron and iron-containing compounds in distinct biological samples. A unified-ferene (u-ferene) assay has been developed for the quantification of both labile and total iron from the same preparation of a biological specimen, offering an economic and readily accessible method with the same sensitivity as the gold standard, inductively coupled plasma mass spectrometry (ICP-MS). Systems and methods using a sensor for assessing iron concentration in body fluid samples, such as whole blood, have also been developed.
What is the reasons why lead extraction is higher in higher FeCl3 concentrations?5 answersLead extraction is higher in higher FeCl3 concentrations due to several reasons. FeCl3 promotes the cleavage of heteroatom bonds and accelerates the decomposition of asphaltenes in residual bitumen, leading to an enhanced yield of shale oil in subcritical water extraction. FeCl3 also promotes the secondary cracking of saturated hydrocarbons in residual bitumen, rather than in shale oil, due to its adsorption in the shale matrix. Additionally, FeCl3 inhibits the polycondensation of kerogen and promotes the ring-opening reaction of aromatic structure in the presence of FeCl3. Furthermore, the acidic FeCl3 solution induces the decomposition of carbonate minerals in the oil shale matrix, providing additional mass transfer channels for the migration of bitumen products. These combined effects of FeCl3 contribute to the higher extraction of lead in higher FeCl3 concentrations.
Importance ofe Fe(III) in marine sediments?5 answersFe(III) in marine sediments plays a crucial role in various biogeochemical processes. It is an important source of Fe(II) in illuminated aquatic and sedimentary environments, where Fe(III) can be photoreduced to Fe(II) by wavelengths <500 nm. The coprecipitation of dissolved organic matter (DOM) and phosphate with Fe(III) at the sediment-water interface contributes to the biogeochemical cycle of organic carbon (OC) and phosphorus (P) in aquatic ecosystems. Fe(III)-reducing bacteria are enriched in marine sediments, with dominant bacteria such as Clostridium and Enterobacter sp. being responsible for high Fe(III) reduction rates. Post-depositional chemical reactions involving iron in shallow-marine sediments govern the types of minerals that precipitate, influencing sedimentary environments and mineral-water-bacteria interactions. The activity of nitrate-reducing and phototrophic Fe(II)-oxidizers, as well as microbial Fe-redox cycling, is influenced by the organic carbon content in coastal marine sediments.
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