Transition Elements: Groups 6, 7, and 8 — The Most Competitive Chemistry for JEE, NEET, GATE & CSIR-NET
Complete Chapter Coverage
Welcome to one of the most scoring and most feared chapters in inorganic chemistry. Groups 6, 7, and 8 — the Chromium, Manganese, and Iron groups — are not just textbook elements. They are the building blocks of civilization itself. Stainless steel, blood, batteries, catalysts, pigments, and even the nitrogen cycle all owe their existence to these remarkable metals. This article is your complete, exam-focused guide — written clearly, explained deeply, and packed with the kind of insight that helps you score in competitive exams.
Group 6 — The Chromium Group (Cr, Mo, W)
1. Electronic Configuration and Oxidation States
The first thing every examiner tests: why does chromium have an anomalous electronic configuration? Chromium (Cr) and molybdenum (Mo) both adopt a d5s1 configuration instead of the expected d4s2, because a half-filled d subshell provides exceptional stability due to symmetric electron distribution and exchange energy. Tungsten (W), however, adopts d4s2 — one of the rare cases where the heavier element does not follow the same trend.
| Element | Symbol | Configuration | Most Stable Oxidation States |
|---|---|---|---|
| Chromium | Cr | [Ar] 3d5 4s1 | +III, +II, +VI (strongly oxidizing) |
| Molybdenum | Mo | [Kr] 4d5 5s1 | +VI, +V, +IV, +III |
| Tungsten | W | [Xe] 4f14 5d4 6s2 | +VI, +V, +IV |
2. Occurrence and Extraction — Real World Chemistry
Chromium is the 21st most abundant element in the Earth's crust (~122 ppm). Its only commercially important ore is chromite, FeCr2O4 — a spinel mineral where O2− ions are arranged in a cubic close-packed lattice, Fe2+ sits in tetrahedral holes, and Cr3+ in octahedral holes.
Step-by-Step: Extraction of Pure Chromium
- Step 1 — Roasting with NaOH: Chromite is fused with NaOH in air to oxidize Cr(+III) to Cr(+VI):
4 FeCr2O4 + 8 NaOH + 3½ O2 → 4 Na2[CrO4] + 2 Fe2O3 + 4 H2O (at ~1100 °C)
- Step 2 — Dissolution & Acidification: Soluble sodium chromate Na2CrO4 is leached out; the insoluble Fe2O3 remains. On acidification, orange sodium dichromate Na2Cr2O7 precipitates (less soluble):
2 CrO42− + 2 H+ → Cr2O72− + H2O
- Step 3 — Reduction to Cr2O3:
Na2[Cr2O7] + 2C → Cr2O3 + Na2CO3 + CO
- Step 4 — Thermite Reduction:
Cr2O3 + 2 Al → 2 Cr + Al2O3 (Goldschmidt / thermite reaction)
For industrial use, ferrochrome (Fe + Cr alloy) is made directly by reducing chromite with carbon in an electric furnace:
FeCr2O4 + 4C → Fe + 2Cr + 4CO
3. Oxidation States in Detail — The Most Tested Part
(a) Cr(+VI) State — Chromates and Dichromates
Cr(+VI) compounds are among the most powerful oxidizing agents known in analytical chemistry. They include chromate ion [CrO4]2−, dichromate ion [Cr2O7]2−, chromium trioxide CrO3, and oxohalides like CrO2Cl2.
The Chromate–Dichromate Equilibrium
This is one of the most important equilibria in inorganic chemistry:
2 CrO42−(yellow) + 2 H+ ⇌ Cr2O72−(orange) + H2O
CrO42− (tetrahedral) — in basic medium
Cr2O72− (two tetrahedra sharing one corner O) — in acidic medium
Potassium Dichromate K2Cr2O7 — The Volumetric Star
K2Cr2O7 is preferred over Na2Cr2O7 as a primary standard because the sodium salt is hygroscopic while the potassium salt is not. In acidic solution, it acts as a strong oxidizer with E° = +1.33 V:
½ Cr2O72− + 7H+ + 3e− ⇌ Cr3+ + 3½ H2O E° = +1.33 V
(b) Chromium Trioxide CrO3 — Chromic Acid
CrO3 is a bright orange solid, commonly called "chromic acid." It is prepared by:
Na2Cr2O7 + H2SO4 → 2 CrO3 + Na2SO4 + H2O
CrO3 has a chain structure of fused tetrahedra. It is strongly acidic and dissolves in NaOH forming CrO42−. Above 250 °C it decomposes in stages:
2 CrO3 → 2 CrO2 + O2
2 CrO2 → Cr2O3 + ½ O2
(c) Peroxo Compounds of Chromium — Deep Blue CrO(O2)2
When H2O2 is added to an acidified dichromate solution, a deep-blue peroxo compound forms:
Cr2O72− + 2H+ + 4H2O2 → 2 CrO(O2)2 + 5H2O
This deep blue CrO(O2)2 decomposes quickly in aqueous solution to Cr3+ but can be stabilized by extraction into ether and reaction with pyridine (py) to form py·CrO(O2)2, which has a pentagonal pyramidal structure. This is a classic qualitative test for chromium!
K2Cr2O7 + 6 HCl (conc. H2SO4) → 2 CrO2Cl2 + 2 KCl + 3 H2O
CrO2Cl2 + 4 NaOH → Na2CrO4 + 2 NaCl + 2 H2O (solution turns yellow)
(d) Cr(+III) State — The Most Stable and Most Complex
Cr(+III) is the most stable and most important state for chromium. The Cr3+ ion has a d3 configuration with very high crystal field stabilization energy (CFSE), which makes its octahedral complexes extremely stable and kinetically inert.
- Cr2O3 — green solid, corundum (Al2O3) structure, used as a green pigment in paint, rubber, cement; catalyst in the Deacon process and in making polyethylene
- CrCl3 — red-violet flakes (layer lattice), forms hexaaqua ion [Cr(H2O)6]3+ (violet) in solution; multiple halide-aqua complexes exist
- Chrome alum — KCr(SO4)2·12H2O, a double salt: K[Cr(H2O)6][SO4]2
Cr(+III) Complexes: Isomerism Heaven for Exams
- [Cr(NH3)6]3+ — only one form (all equivalent NH3)
- [Cr(NH3)5Cl]2+ — only one form
- [Cr(NH3)4Cl2]+ — cis and trans isomers
- [Cr(NH3)3Cl3] — mer and fac isomers
- [Cr(oxalate)3]3− — d and l optical isomers
Electronic Spectrum of [Cr(H2O)6]3+
Cr(+III) is a d3 ion. In an octahedral crystal field, the ground state is 4A2g(F). The three spin-allowed transitions are:
- 4A2g(F) → 4T2g(F) at ~17,400 cm−1
- 4A2g(F) → 4T1g(F) at ~24,700 cm−1
- 4A2g(F) → 4T1g(P) — charge transfer at ~37,800 cm−1
(e) Cr(+II) State — The Quadruple Bond Marvel
Chromium(II) acetate dihydrate Cr2(CH3COO)4·2H2O is one of the most famous compounds in all of inorganic chemistry. Cr2+ has a d4 configuration with 4 unpaired electrons, but this compound is diamagnetic. Why? Because all four unpaired electrons participate in metal-metal bonding through a quadruple bond: one σ, two π, and one δ bond — giving a Cr–Cr distance of only 2.36 Å. Quadruple bonds are also found in Mo2(CH3COO)4, Re2Cl82−, and others.
4. MoO3, WO3 versus CrO3 — Key Differences
| Property | CrO3 | MoO3 | WO3 |
|---|---|---|---|
| Colour | Orange | White (d0) | Lemon yellow |
| Solubility in H2O | Very soluble | Insoluble | Insoluble |
| Oxidizing power | Strong | Almost none | Almost none |
| Melting point | 197 °C | 795 °C | 1473 °C |
| Structure | Chain of tetrahedra | Layer lattice | Distorted ReO3 |
5. Polyacids of Mo and W — Isopolyacids & Heteropolyacids
When molybdate [MoO4]2− or tungstate [WO4]2− solutions are acidified, the coordination number of Mo or W increases from 4 to 6 (by adding water molecules). This leads to a series of condensed anions — isopolyacids:
[MoO4]4− —pH 6—> [Mo7O24]6− (paramolybdate) —pH 1-2—> [Mo8O26]4− (octamolybdate) —pH<1—> MoO3·2H2O
6. Tungsten Bronzes — A Special Mention
Tungsten bronzes are nonstoichiometric compounds of formula MxWO3 (where M = Na, K, or a lanthanide; x < 1). They are semi-metallic solids with a lustre and conduct electricity. Colour depends on x: x ≈ 0.9 (yellow/gold), x ≈ 0.5 (red), x ≈ 0.3 (blue-black). They are inert to strong acids and alkalis and used in "bronze" and "metallic" paints.
7. Biological Importance of Group 6
- Cr(+III) and insulin work together to maintain correct blood glucose levels. In Cr deficiency, glucose removal from blood is halved. Some cases of diabetes reflect faulty Cr metabolism.
- Mo is present in the enzyme nitrogenase — which fixes atmospheric N2 biologically (175 million tonnes/year). The enzyme contains two proteins: molybdoferredoxin and azoferredoxin. It is thought that N2 bonds to Mo through antibonding orbitals, and after reduction gives NH3.
Group 7 — The Manganese Group (Mn, Tc, Re)
1. Electronic Configuration and Oxidation States
All three elements have d5s2 configurations, giving a maximum possible oxidation state of +VII. Manganese is unique in the entire periodic table for showing the widest range of oxidation states — from −III to +VII! The (+II) state is the most stable and most common for Mn because Mn2+ has a half-filled d5 configuration, giving maximum exchange energy stabilization.
| Element | Symbol | Configuration | Most Stable States |
|---|---|---|---|
| Manganese | Mn | [Ar] 3d5 4s2 | +II, +IV, +VII |
| Technetium | Tc | [Kr] 4d5 5s2 | +VII, +IV |
| Rhenium | Re | [Xe] 4f14 5d5 6s2 | +VII, +IV, +III |
2. Technetium — The First Man-Made Element
Technetium does not occur in nature. All its isotopes are radioactive. 99Tc is a β-emitter with half-life 2.1 × 105 years. It is obtained in kilogram quantities from spent nuclear fuel rods as a fission product of uranium. Small amounts of 99mTc compounds are injected into patients for radiographic scanning of organs (particularly the liver and thyroid). 97Tc and 98Tc can be made by neutron bombardment of Mo.
3. Extraction and Uses of Manganese
Manganese is the 12th most abundant element in Earth's crust (~1060 ppm). The chief ore is pyrolusite MnO2. Pure Mn is obtained by electrolysis of aqueous MnSO4 solutions. About 95% of all Mn mined is used in the steel industry:
- Ferromanganese (80% Mn) — made by reducing Fe2O3 + MnO2 with C in a blast furnace. Used as a scavenger (removes O and S, preventing bubbles and brittleness) and for making Hadfield steel (~13% Mn, 1.25% C — extremely hard and shock-resistant, used in rock-crushing machinery)
- Silicomanganese (~65% Mn, 20% Si, 15% Fe)
- Spiegeleisen (5–25% Mn, similar to cast iron)
- Manganin (84% Cu, 12% Mn, 4% Ni) — electrical resistance almost unaffected by temperature; used in precision electrical instruments
4. Oxidation States in Detail
(a) Mn(+II) — The Pale Pink d5 King
Mn(+II) salts are the most common. The [Mn(H2O)6]2+ ion is pale pink. The d5 configuration gives zero CFSE in an octahedral field (all five d orbitals are singly occupied, symmetrically) — so complexes like [Mn(NH3)6]2+ and [MnCl6]4− are not stable in isolation. Chelate ligands like EDTA form more stable complexes.
Mn(+II) in alkaline solution is easily oxidized. Addition of NaOH to Mn2+ solution gives pale pink gelatinous Mn(OH)2 precipitate, which rapidly turns brown-black as it oxidizes to MnO2:
Mn(OH)2 + ½ O2 → MnO2 + H2O (in alkaline solution, easily)
(In acid solution: Mn2+ is stable, E°(Mn3+/Mn2+) = +1.51 V — hard to oxidize in acid)
(b) Mn(+III) — The Unusual Disproportionator
Mn3+ has d4 configuration. Only a small number of Mn(+III) salts are known — MnF3, Mn2(SO4)3, and Mn2O3. The hydrated [Mn(H2O)6]3+ ion cannot be obtained in concentrated solutions because it disproportionates in acid:
2 Mn3+ + 2 H2O → Mn2+ + MnO2 + 4 H+ (acid)
The Jahn-Teller theorem predicts distortion of Mn(+III) octahedral complexes (electronic structure (t2g)3(eg)1 — eg not symmetrically filled), similar to Cu2+. Manganese acetate [Mn3O(CH3COO)6L3]+ (basic acetate, same structure as Cr and Fe basic acetates) is used industrially to oxidize toluene to benzaldehyde.
(c) Mn(+IV) — The Battery Mineral MnO2
MnO2 is the most important Mn(+IV) compound. It occurs naturally as pyrolusite (the main Mn ore) and has the rutile (TiO2) structure. Key uses:
- Dry batteries (Leclanché cells) — over half a million tonnes used annually for 'dry batteries'. Must be very pure and is made electrolytically.
- Brick industry — colours bricks red or brown.
- Glass industry — makes red or purple glass.
- Organic chemistry — oxidizes activated alcohols and alkenes to aldehydes/ketones.
- Catalyst — decomposes KClO3 at 150 °C (instead of 400–500 °C without catalyst):
2 KClO3 —MnO₂, 150°C→ 2 KCl + 3 O2
MnO2 in concentrated HCl is reduced and Cl2 is liberated (Scheele's method — the original industrial method for Cl2 before electrolysis):
MnO2 + 4 HCl → MnCl2 + Cl2 + 2 H2O
(d) Mn(+VII) — Permanganate: The Oxidizing Legend
KMnO4 is intensely purple-black and is one of the most important oxidizing agents in chemistry. The Mn is in a d0 configuration, so the intense colour comes from charge transfer spectra (O2− → Mn7+), not d–d transitions.
Step 1: MnO2 + KNO3 —fuse with NaOH—> K2MnO4 + NO (dark green manganate)
Step 2: K2MnO4 + H2O —electrolytic oxidation—> KMnO4 + KOH + ½ H2
Important Reactions of KMnO4
- Oxidizes H2S → S (in acid)
- Oxidizes Fe2+ → Fe3+ (in acid) — used in volumetric analysis
- Oxidizes oxalate (C2O42−) → CO2 (in hot acid) — Mohr's salt titration
- Oxidizes toluene → benzoic acid; benzaldehyde; oxidizes alkenes to diols
- Disinfects drinking water (oxidizes & kills bacteria without Cl2 taste)
- Manufacture of saccharin, ascorbic acid (Vitamin C), nicotinic acid (niacin)
(e) Mn(+VI) — Dark Green Manganate
Only one Mn(+VI) compound: the manganate ion MnO42−. These dark green compounds are formed by fusing MnO2 in KOH with air or KNO3. They are unstable in dilute alkali and disproportionate (as shown above). They are stable only in concentrated alkali.
5. Tc and Re — The Upper Row Peculiarities
Technetium and rhenium strongly resemble each other (due to the lanthanide contraction). They differ from Mn in:
- Almost no aqueous ionic chemistry except TcO4− and ReO4− (the only stable ions in water)
- Strong tendency to form metal–metal bonds in lower oxidation states (+II, +III, +IV)
- Tc(+VII) and Re(+VII) are only slightly oxidizing (unlike Mn(+VII))
- Re has the second highest melting point of all metals (3180 °C; W is highest at 3380 °C)
The Quadruple Bond in [Re2Cl8]2−
When perrhenates are reduced by H2 or NaH2PO2 in HCl, the remarkable ion [Re2Cl8]2− forms. The Re–Re bond length is only 2.24 Å — interpreted as a quadruple bond: 1σ + 2π + 1δ. The two ReX4 planes are eclipsed (0°), which is a direct consequence of the δ bond (dxy–dxy overlap). If the δ bond were absent, the planes would be staggered.
6. Biological Role of Manganese
- MnII is essential in plant and animal enzymes. In mammals, the enzyme arginase (produced in the liver) converts nitrogenous waste to urea via the ornithine–arginine–citrulline cycle (discovered by Hans Krebs).
- Mn is an essential trace element for plant growth — added to fertilizers in deficient soils.
- Mn(+III) and Mn(+IV) complexes are involved in the release of O2 during photosynthesis (the oxygen-evolving complex in photosystem II contains a Mn4Ca cluster).
Group 8 — The Iron Group (Fe, Ru, Os)
1. Introduction: Iron — The Most Important Metal
Iron is used in larger quantities than any other metal. It is the fourth most abundant element in Earth's crust (~62,000 ppm, or 6.2% by weight). Biologically, it is the most important transition element — involved in oxygen transport (haemoglobin), oxygen storage (myoglobin), electron transfer (cytochromes, ferredoxins), and nitrogen fixation (nitrogenase). Fe forms unusual organometallic compounds, the most famous being ferrocene.
2. Electronic Configuration and Oxidation States
| Element | Symbol | Configuration | Most Stable States |
|---|---|---|---|
| Iron | Fe | [Ar] 3d6 4s2 | +II, +III |
| Ruthenium | Ru | [Kr] 4d7 5s1 | +III, +IV, +VIII |
| Osmium | Os | [Xe] 4f14 5d6 6s2 | +IV, +VIII |
3. Extraction of Iron — Blast Furnace Chemistry
The blast furnace is one of the most tested topics in competitive exams. Let's do it step by step:
Raw Materials Charged from the Top:
- Iron ore (Fe2O3 — haematite, Fe3O4 — magnetite, FeO(OH) — limonite)
- Coke (reducing agent + fuel)
- Limestone CaCO3 (slag-forming agent)
Temperature-Dependent Reactions in the Blast Furnace:
200–400 °C: 3Fe2O3 + CO → 2Fe3O4 + CO2
400–700 °C: Fe3O4 + CO → 3FeO + CO2
500–600 °C: 2CO → C + CO2 (C deposits as soot, reduces FeO)
700 °C: FeO + C → Fe + CO (also FeO + CO → Fe + CO2)
900 °C: CaCO3 → CaO + CO2
1000 °C: FeO + CO → Fe + CO2 | CO2 + C → 2CO
1800 °C: CaO + SiO2 → CaSiO3 (slag) | MnO + C → Mn(in Fe) + CO
Molten iron (pig iron) collects at the bottom. It contains 3–4% C, 1–2% Si, 0.05–2% P, 0.05–1% S, 0.5–2% Mn. This brittleness from excess C is removed in steel making.
Steel Making — Know all Four Processes:
- Puddling (obsolete): Mixing pig iron with Fe3O4 and burning off C → wrought iron
- Bessemer process: Silica-lined converter; compressed air blown through molten pig iron burns Si, Mn, then C. Cannot remove P.
- Thomas–Gilchrist process: Basic-lined (dolomite/limestone) converter for P-rich ores; basic slag (Ca3(PO4)2) is a valuable phosphate fertilizer
- Basic Oxygen Process (BOP) — Modern standard: pure O2 blown at high speed onto molten pig iron through retractable water-cooled lances. Converts 300 tonnes in 40 minutes. No nitrogen uptake. Cleaner product.
4. Fe(+II) State — Ferrous Chemistry
Fe(+II) salts are called ferrous salts. The [Fe(H2O)6]2+ ion is pale green. Fe2+ has a d6 configuration.
- FeSO4·7H2O (green vitriol) — pale green crystals, used as a mordant in dyeing and ink-making
- Mohr's salt — FeSO4·(NH4)2SO4·6H2O — more stable than FeSO4 alone (less easily oxidized), primary standard in volumetric analysis with dichromate and permanganate
- Fenton's reagent — FeSO4 + H2O2 → generates hydroxyl radicals (OH•), used to oxidize alcohols to aldehydes
- FeO — nonstoichiometric, formula Fe0.95O; NaCl structure; formed by heating Fe(II) oxalate in vacuum
High-Spin vs Low-Spin Fe2+ Complexes:
Fe2+ (d6) complexes can be either high-spin or low-spin depending on the ligand field strength:
Prussian Blue and Turnbull's Blue
The hexacyanoferrate(II) ion [Fe(CN)6]4− (yellow, ferrocyanide) and hexacyanoferrate(III) [Fe(CN)6]3− (orange-red, ferricyanide) form the most famous pigment pair:
- Prussian blue: KFeIII[FeII(CN)6] — deep blue; formed when Fe3+ is added to ferrocyanide K4[Fe(CN)6]
- Turnbull's blue: KFeII[FeIII(CN)6] — identical to Prussian blue by X-ray; formed when Fe2+ is added to ferricyanide K3[Fe(CN)6]
- White precipitate K2FeII[FeII(CN)6] forms when Fe2+ + ferrocyanide → test for Fe2+
Brown Ring Test for Nitrates
FeSO4 (fresh) + NO3− + H2SO4(conc.) → [Fe(H2O)5NO]2+ (brown ring at interface)
The complex formally contains Fe(+I) and NO+; magnetic moment ≈ 3.9 BM (3 unpaired e−)
5. Fe(+III) State — Ferric Chemistry
Fe3+ has a d5 configuration — similar to Mn2+. Fe(+III) solutions are frequently yellow-brown due to colloidal iron oxide or FeO·OH. Fe(+III) forms complexes preferring O-donor ligands over N-donor ligands.
- Fe2O3 — haematite structure; red-brown; used as a pigment
- Fe3O4 — magnetite, a mixed oxide FeIIFe2IIIO4 (inverse spinel), ferromagnetic; black solid formed at 1400 °C from Fe2O3
- FeCl3 — black solid in gas phase (FeCl3 dimer), layer lattice in solid; yellow-brown in water; used in manufacture of CCl4, as mordant in dyeing
SCN− Test for Fe(+III):
Fe3+ + SCN− → [Fe(SCN)(H2O)5]2+ (blood-red colour)
→ further SCN−: [Fe(SCN)2]+, Fe(SCN)3, [Fe(SCN)4]−, [Fe(SCN)6]3−
Colour destroyed by F− ions (forms [FeF6]3−)
6. Fe(+VI) — Ferrate Ions
Ferrate(VI) ions FeO42− are prepared by passing Cl2 into alkaline hydrated iron(III) oxide, or by oxidizing Fe(+III) with NaOCl in alkali. They are purple and are stronger oxidizers than KMnO4. Stability of +VI state across the period: CrO42− > MnO42− > FeO42− >> CoO42−.
7. Ru and Os — The Noble Platinum Group
Ru and Os are very rare, noble, and resistant to attack. They are found in the metallic state with platinum metals. The most important compounds are:
- RuO4 and OsO4 — yellow volatile solids (tetrahedral, d0). OsO4 is a biological stain (reduces to OsO2 in tissue), used in organic chemistry to add to double bonds giving cis-diols. Both are toxic. OsO4 is more stable than RuO4.
- Ru(+II) NO complexes — an interesting series [RuIINO·L4]n, where the NO ligand is strongly bonded through σ and π; the Ru–N–O angle can be linear or bent.
- Both Ru and Os form carbonyls: Os(CO)5, Ru(CO)5, and trinuclear Ru3(CO)12, Os3(CO)12. The dinitrogen complex [Ru(NH3)5N2]Cl2 was the first reported dinitrogen complex (1965).
8. Bioinorganic Chemistry of Iron — The Most Important Section
Haemoglobin — Nature's Oxygen Transporter
The human body contains about 4 g of iron. About 70% is in haemoglobin (red blood cells). Haemoglobin (Hb) has molecular weight ~65,000 and consists of four subunits, each containing a haem b group — a porphyrin ring with Fe2+ bonded to four N atoms and a fifth N from histidine in the globin protein. The sixth coordination position is either a water molecule (deoxy) or dioxygen (oxy).
- In oxyhaemoglobin: Fe2+ is low-spin (diamagnetic) — it fits in the porphyrin plane. O2 occupies the sixth position.
- In deoxyhaemoglobin: Fe2+ is high-spin (paramagnetic, 4 unpaired e−) and larger (radius increases by 28%) — it sits 0.7–0.8 Å above the porphyrin ring, distorting the complex.
- Cooperative effect: When one subunit picks up O2, Fe2+ contracts and moves into the plane → pulls histidine → causes conformational changes in other subunits → enhances their ability to attract O2.
- CO poisoning: CO binds irreversibly to the same site as O2, preventing oxygen transport → lethal.
Myoglobin
Similar to one haemoglobin subunit; only one Fe atom; MW ~17,000. Stores O2 in muscle tissue and binds O2 more strongly than haemoglobin.
Cytochromes
Electron carriers in the mitochondria. They contain Fe in both +II and +III states and cycle reversibly between them. There are three classes: cytochrome a (E° = +0.28 V), cytochrome b (E° = +0.04 V), cytochrome c (E° = +0.26 V). The sequence of electron transfer is b → c → a, gradually releasing energy stored as ATP.
Ferredoxins
Non-haem iron proteins responsible for electron transfer in plants and bacteria. They contain Fe–S clusters (Fe2S2 or Fe4S4 cubane-type). Rubredoxin (simplest) contains one Fe atom surrounded by 4 S atoms from cysteine residues.
Ferritin — Iron Storage
Animals absorb Fe as Fe(+II) from food. It immediately reacts to form transferrin (a transport protein with MW 76,000–80,000 carrying 2 Fe atoms per molecule). Fe is stored as ferritin — a roughly spherical protein shell (apoferritin, ~120 Å diameter) enclosing a micelle of Fe(+III) hydroxide/oxide/phosphate containing 2,000–5,000 Fe atoms.
9. Ferrocene and Organometallic Chemistry
In 1951, G. Wilkinson and E.O. Fischer independently prepared an astonishing compound — ferrocene (π-C5H5)2Fe — marking the birth of modern organometallic chemistry. For this work they were jointly awarded the Nobel Prize in Chemistry in 1973.
2 C5H5MgBr + FeCl2 → Fe(C5H5)2 + MgBr2 + MgCl2 (orange crystals)
2 C5H5− + FeCl2 → (η5-C5H5)2Fe + 2 Cl−
- Ferrocene has a sandwich structure: Fe atom sandwiched between two parallel, planar cyclopentadienyl rings.
- Stable in air, thermally stable to 500 °C, soluble in organic solvents, insoluble in water and NaOH — orange crystals.
- The two C5H5 rings are in staggered conformation in the crystal (space group constraint), but with only ~4 kJ/mol barrier to rotation.
- Fe–C bond length: 2.06 Å. C–C bond in ring: 1.39 Å (same as benzene! — aromatic character).
- Ferrocene undergoes Friedel-Crafts acylation (electrophilic aromatic substitution) — e.g., acetylation with CH3COCl in presence of AlCl3.
- Rutenocene and osmocene are analogous compounds where the rings adopt the eclipsed conformation.
10. Iron Carbonyls
Fe(CO)5 (iron pentacarbonyl) is a liquid at room temperature, available commercially. In carbonyls, CO acts as a σ donor and strong π acceptor (dπ–pπ* back bonding):
- Fe(CO)5 — mononuclear, D3h (trigonal bipyramidal)
- Fe2(CO)9 — dinuclear with three bridging CO groups, two terminal CO on each Fe
- Fe3(CO)12 — trinuclear; has two CO bridges between one pair of Fe atoms
Fe(CO)5 + 3 NaOH → Na[HFe(CO)4] + Na2CO3 + H2O
Fe(CO)5 + PF3 → (PF3)3Fe(CO)2 + 3 CO (substitution)
Standard Reduction Potentials — Latimer Diagrams Summary
🎯 Consolidated Exam Tips — JEE, NEET, GATE, CSIR-NET, IIT-JAM, BITSAT
Most Frequently Asked Topics (by Exam)
| Topic | JEE Adv. | NEET | GATE/CSIR | IIT-JAM |
|---|---|---|---|---|
| Electronic configurations (Cr, Mo) | ★★★ | ★★★ | ★★ | ★★★ |
| K₂Cr₂O₇ reactions + titrations | ★★★ | ★★★ | ★★★ | ★★★ |
| KMnO₄ reactions (pH dependent) | ★★★ | ★★★ | ★★★ | ★★★ |
| Chromate–dichromate equilibrium | ★★★ | ★★ | ★★★ | ★★★ |
| Chromyl chloride test | ★★ | ★★ | ★★ | ★★ |
| Blast furnace reactions | ★★ | ★★★ | ★★ | ★★ |
| Prussian blue / ferrocyanide | ★★★ | ★★ | ★★★ | ★★★ |
| Haemoglobin / spin state of Fe²⁺ | ★★ | ★★★ | ★★★ | ★★★ |
| Quadruple bonds (Cr₂, Re₂Cl₈²⁻) | ★★ | ★ | ★★★ | ★★★ |
| Ferrocene synthesis & bonding | ★★ | ★ | ★★★ | ★★★ |
| Crystal field theory (Mn²⁺, Fe³⁺) | ★★★ | ★★ | ★★★ | ★★★ |
| Isopolyacids / heteropolyacids (Mo, W) | ★ | ★ | ★★★ | ★★★ |
Quick Revision — 30 Key Facts to Never Forget
- Cr has [Ar] 3d5 4s1 (half-filled d is extra stable) — anomalous configuration.
- Cr(+III) is the most stable state of Cr; Cr(+VI) is strongly oxidizing (E° = +1.33 V vs NHE).
- Chromate is yellow in basic, dichromate is orange in acidic medium.
- K2Cr2O7 (not Na2Cr2O7) is a primary standard — Na salt is hygroscopic.
- CrO3 is called "chromic acid" — bright orange, chain structure, acidic oxide.
- Deep blue CrO(O2)2 is a qualitative test for Cr (chromate + H2O2 + acid).
- Chromyl chloride test confirms Cl− using K2Cr2O7 + conc. H2SO4 → CrO2Cl2 (deep red vapour).
- Cr(+II) acetate is diamagnetic due to a Cr≡Cr quadruple bond (σ + 2π + δ).
- W has the second-highest melting point of all elements (3380 °C) after carbon.
- MoS2 is an excellent solid lubricant (layer lattice).
- Mn has the widest range of oxidation states: −III to +VII.
- Mn(+II) has d5 configuration — half-filled d → very stable; pale pink colour (spin-forbidden d–d).
- Mn(+III) disproportionates in acid into Mn2+ + MnO2.
- MnO2 (pyrolusite) — rutile structure; used in dry batteries, catalyst in O2 generation.
- KMnO4 in acid gives Mn2+ (Δ = 5e−), in alkaline gives MnO2 (Δ = 3e−).
- KMnO4 colour arises from charge transfer (d0), not d–d spectra.
- Technetium is the first man-made element — all isotopes radioactive.
- 99mTc used in nuclear medicine (liver and organ scanning).
- Fe is the fourth most abundant element in Earth's crust (62,000 ppm).
- Fe oxidation states: +II (ferrous) and +III (ferric) most common; +VIII is for Os, Ru (tetroxides).
- Fe2+ high-spin (weak field): 4 unpaired e−; low-spin (strong field, CN−): 0 unpaired e−.
- Prussian blue = KFeIII[FeII(CN)6] = Turnbull's blue (confirmed identical by X-ray).
- Brown ring test: [Fe(H2O)5NO]2+ — test for nitrates.
- SCN− test gives blood-red colour with Fe3+ (destroyed by F−).
- In haemoglobin, oxygenated Fe2+ is low-spin (diamagnetic); deoxygenated is high-spin (paramagnetic).
- Cooperative effect in Hb: binding one O2 enhances affinity of the other three subunits.
- Cytochromes: electron carriers between +II and +III states; sequence b → c → a releases energy as ATP.
- Ferrocene (Nobel Prize 1973, Fischer & Wilkinson): sandwich structure η5-C5H5 rings; undergoes Friedel-Crafts acylation.
- OsO4 is more stable than RuO4; used in organic chemistry to add to double bonds (cis-diols).
- Fe3O4 is an inverse spinel: FeIIFe2IIIO4 — ferromagnetic, black solid.
- The ore of chromium is _____ (chromite, FeCr2O4)
- _____ is used as a primary standard in redox titrations (K2Cr2O7)
- The colour of KMnO4 is due to _____ (charge transfer, not d–d)
- MnO4− in acid medium accepts _____ electrons (5)
- Ferrocene was first synthesised in _____ (1951)
- The spin-only magnetic moment of [Fe(CN)6]4− is _____ BM (0 — diamagnetic)
- The ore of tungsten used in India is _____ (wolframite / scheelite)
- _____ is called "fool's gold" (FeS2, iron pyrites)
Common Mistakes to Avoid
- Do NOT say Cr has d4s2 configuration — it is d5s1.
- Do NOT confuse chromate (yellow, basic) with dichromate (orange, acidic) — many students swap these.
- Do NOT say Prussian blue and Turnbull's blue are different compounds — they are identical.
- Do NOT say the colour of MnO4− is d–d — it's a d0 ion; colour is from charge transfer.
- Do NOT apply the blast furnace equation as a single step — it proceeds in stages at different temperatures.
- Do NOT forget that KMnO4 titrations in acid give Mn2+ (5e− change), while in alkaline give MnO2 (3e− change) — stoichiometry will be completely different.
References & Further Reading: J.D. Lee, Concise Inorganic Chemistry, 5th Ed., Blackwell Science; Atkins, Shriver & Atkins' Inorganic Chemistry; IUPAC Recommendations for Nomenclature of Inorganic Chemistry (2005). All molecular geometries, bond angles, and oxidation states are consistent with IUPAC guidelines and experimental crystallographic data.
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