Ferroin

Complex of Fe<sup>2+</sup> by ortho-phenanthroline
title: "Ferroin" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["iron-complexes", "phenanthrolines"] description: "Complex of Fe2+ by ortho-phenanthroline" topic_path: "general/iron-complexes" source: "https://en.wikipedia.org/wiki/Ferroin" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0
::summary Complex of Fe2+ by ortho-phenanthroline ::
| verifiedrevid = 446896598 | ImageFile = Ferroin-cation-3D-balls.pngclass=bg-transparent | ImageSize = 240px | ImageName = The structure of the [Fe(o-phen)3]2+ complex cation in ferroin |Section1={{Chembox Identifiers | InChI = 1/3C12H8N2.Fe.H2O4S/c31-3-9-5-6-10-4-2-8-14-12(10)11(9)13-7-1;;1-5(2,3)4/h31-8H;;(H2,1,2,3,4)/q;;;+2;/p-2 | InChIKey = CIWXFRVOSDNDJZ-NUQVWONBAU | StdInChI_Ref = | StdInChI = 1S/3C12H8N2.Fe.H2O4S/c31-3-9-5-6-10-4-2-8-14-12(10)11(9)13-7-1;;1-5(2,3)4/h31-8H;;(H2,1,2,3,4)/q;;;+2;/p-2 | StdInChIKey_Ref = | StdInChIKey = CIWXFRVOSDNDJZ-UHFFFAOYSA-L | CASNo = 14634-91-4 | CASNo_Ref = | UNII_Ref = | UNII = YP88WTW2E4 | PubChem = 84567 | ChemSpiderID_Ref = | ChemSpiderID = 76289 | SMILES = c12c3[n+]4cccc3ccc2ccc[n+]1[Ru-4]456(c7cccc(c78)ccc(c78)ccc[n+]67)[n+]1cccc2ccc3ccc[n+1]5c3c12 |Section2={{Chembox Properties | Formula = C36H24FeN62+ | MolarMass = 596.27 g/mol
Ferroin, also known as tris(o-phenanthroline)iron(II), is the chemical compound with the formula [Fe(o-phen)3]SO4, where o-phen is the abbreviation of ortho-phenanthroline for 1,10-phenanthroline, a bidentate ligand. The term "ferroin" is used loosely and includes salts of other anions such as chloride. Ferroin is one of many transition metal complexes of 1,10-phenanthroline.
Structure
Many salts of [Fe(o-phen)3]2+ have been characterized by X-ray crystallography. The structures of [Fe(o-phen)3]2+ and [Fe(o-phen)3]3+ are almost identical, consistent with both being low-spin. These cations are octahedral with D3 symmetry group. The Fe-N distances are 197.3 pm.
Preparation and reactions
Ferroin sulfate can be prepared by combining phenanthroline to ferrous sulfate dissolved in water: : 3 phen + Fe2+ → [Fe(phen)3]2+
The oxidation of this complex from Fe(II) to Fe(III), involving the fast and reversible transfer of only one electron, makes it a useful redox indicator in aqueous solution:
: [Fe(phen)3]2+ → [Fe(phen)3]3+ + 1 e−
Addition of sulfuric acid to an aqueous solution of [Fe(phen)3]2+ causes its hydrolysis and the formation of a neutral ion pair [phenH]HSO4: : [Fe(phen)3]2+ + 3 H2SO4 + 6 H2O → [Fe(OH2)6]2+ + 3 [phenH]+HSO4−
Addition of cyanide to an aqueous solution of precipitates .
Redox indicator
This complex is used as an indicator in analytical chemistry. The active ingredient is the [Fe(o-phen)3]2+ ion, which is a chromophore that can be oxidized to the ferric derivative [Fe(o-phen)3]3+. The potential for this redox change is +1.06 volts in 1 M H2SO4. It is a popular redox indicator for visualizing oscillatory Belousov–Zhabotinsky reactions.
Ferroin is suitable as a redox indicator, as the color change is reversible, very pronounced and rapid, and the ferroin solution is stable up to 60 °C. It is the main indicator used in cerimetry.
Nitroferroin, the complex of iron(II) with 5-nitro-1,10-phenanthroline, has a transition potential of +1.25 volt. It is more stable than ferroin, but in sulfuric acid with Ce4+ ion, it requires a significant excess of titrant. It is, however, useful for titration in perchloric acid or nitric acid solution, where the cerium redox potential is higher.
The redox potential of the iron-phenanthroline complex can be varied between +0.84 V and +1.10 V by adjusting the position and number of methyl groups on the phenanthroline core.
Fe2+ direct UV-visible spectrophotometric determination
In analytical chemistry, the red color specific for the reduced form of ferroin was once used for the direct UV-visible spectrophotometric determination of . The maximum absorbance of the Fe(II) o-phenanthroline complex is at 511 nm. However, another related N-ligand called ferrozin (3-(2-pyridyl)-5,6-diphenyl-1,2,4-triazine-p,p′-disulfonic acid monosodium salt hydrate) is also used and must not be confused with ferroin. Ferrozin was specifically synthesised in the 1970s to obtain a less expensive reagent for automated chemical analysis. Ferrozine reacts with to form a relatively stable magenta-colored complex with a maximum absorbance at 562 nm. The ferrozin method allows the determination of Fe(II)/Fe(III) speciation in natural fresh or marine waters at the submicromolar level.
In 2021, Smith et al. reexamined the formation kinetics and stability of ferroin and ferrozine Fe(II) complexes. They have found that while the kinetics of binding by o-phenanthroline are very fast, the kinetics of complexation by ferrozine depend on ligand concentration. An excess ligand concentration provides a more stable absorbance, while the formation of Fe(II) complexes is pH-independent.
Related complexes
References
References
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- (1975). "Crystal structure, electron spin resonance, and magnetism of tris(o-phenanthroline)iron(III) perchlorate hydrate". Journal of the Chemical Society, Dalton Transactions.
- (2014). "Boron Cluster Anions [B''n''H''n'']2– ( ''n'' = 10, 12) in Reactions of Iron(II) and Iron(III) Complexation with 2,2′-Bipyridyl and 1,10-Phenanthroline". Zeitschrift für Anorganische und Allgemeine Chemie.
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- Harris, D. C.. (1995). "Quantitative Chemical Analysis". W. H. Freeman.
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- (1938-02-01). "Determination of iron with o-phenanthroline: A spectrophotometric study". Industrial & Engineering Chemistry Analytical Edition.
- (1944-05-19). "Determination of iron. A study of the o-phenanthroline method". Industrial & Engineering Chemistry Analytical Edition.
- (2019). "Iron determination by colorimetric method using o-phenanthroline". Bulletin of Pure & Applied Sciences – Chemistry.
- "Ferrozine".
- Stookey, Lawrence L.. (1970-06-01). "Ferrozine—a new spectrophotometric reagent for iron". Analytical Chemistry.
- (2017). "Optimized high-throughput methods for quantifying iron biogeochemical dynamics in soil". Geoderma.
- (2000). "The ferrozine method revisited: Fe(II)/Fe(III) determination in natural waters". Applied Geochemistry.
- (2021). "Complexation of ferrous ions by ferrozine, 2,2′-bipyridine and 1,10-phenanthroline: Implication for the quantification of iron in biological systems". Journal of Inorganic Biochemistry.
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