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Halogen

The halogens constitute Group 17 of the periodic table—fluorine, chlorine, bromine, iodine, astatine, and tennessine—characterized by an ns2np5 valence configuration, high electronegativity, and the formation of diatomic X2 molecules and halide salts.

The halogens constitute Group 17 (formerly Group VIIA) of the periodic table, comprising five chemically related nonmetallic elements—fluorine (F, Z = 9), chlorine (Cl, Z = 17), bromine (Br, Z = 35), iodine (I, Z = 53), and radioactive astatine (At, Z = 85)—together with the synthetic superheavy Period 7 element tennessine (Ts, Z = 117). Coined in 1842 by the Swedish chemist Jöns Jacob Berzelius from the Greek roots háls (ἅλς, "salt" or "sea") and gen- (γεν-, "to produce"), the name reflects the universal propensity of these elements to react directly with alkali and alkaline earth metals to form crystalline ionic halide salts such as sodium chloride (NaCl).

All neutral halogen atoms share the outer valence electron configuration ns2np5, lying exactly one electron short of the closed-shell octet of the adjacent Group 18 noble gas. Consequently, halogens exhibit the most exothermic electron affinities (EA = 295 to 349 kJ mol−1) and highest Pauling electronegativities (χP = 2.66 to 3.98) in their respective periods, existing in the elemental state as covalent diatomic molecules (X2: F2, Cl2, Br2, I2) and acting as powerful oxidizing agents, hypervalent interhalogen formers (ClF3, BrF5, IF7), stratospheric ozone catalysts, and essential trace ions across vertebrate physiology.

🧪 Interactive Simulation: Explore the T-shaped (ClF3), square pyramidal (BrF5, IF5), and linear (I3−) geometries of polyhalogen compounds in VSEPR Lab.

Periodic Trends: Physical States, Bond Energies, and Oxidizing Power

Phase Progression at 298 K Driven by London Dispersion Forces

Group 17 is the only group in the periodic table that spans all three classical states of matter (gas, liquid, and solid) at standard ambient temperature and pressure (298.15 K, 1 atm):

  • Fluorine (F2) and Chlorine (Cl2) are pale-yellow and yellow-green gases (Tb = −188.1 °C and −34.0 °C).
  • Bromine (Br2) is a dense, volatile reddish-brown liquid (Tm = −7.2 °C, Tb = 58.8 °C)—one of only two liquid elements at 298 K alongside mercury (Hg).
  • Iodine (I2) is a lustrous violet-black orthorhombic crystalline solid (Tm = 113.7 °C, Tb = 184.3 °C) that sublimes readily into a violet vapor at room temperature.

Because all homonuclear diatomic X2 molecules are nonpolar (electric dipole moment μ = 0 D), their intermolecular attractions consist solely of London dispersion forces (Vdisp ∝ −*α*2/r6). Moving down Group 17 from F2 (18 total electrons, molecular polarizability α = 1.24 Å3) to I2 (106 total electrons, α = 10.2 Å3), the radial expansion and high polarizability of the diffuse 4*p* and 5*p* electron clouds increase London dispersion energy enough to condense Br2 into a liquid and lock I2 into a molecular solid. The colors of the halogens also deepen progressively down the group (pale yellow F2 → yellow-green Cl2 → red-brown Br2 → violet I2) because the energy gap Δ*E* between the filled antibonding 1*π*g\* HOMO and the vacant antibonding 3*σ*u\* LUMO narrows down the column, shifting the πg\* → σu\* optical absorption band from the ultraviolet (285 nm in F2) across the visible spectrum (330 nm in Cl2, 420 nm in Br2, and 520 nm green absorption in I2).

Halogen (Z, Symbol)Diatomic State (298 K)Pauling χPElectron Affinity (EA, kJ mol−1)X–X Length (r0) & Bond Energy (*D*°)H–X Bond Energy (*D*°) & Aqueous p*K*aStandard Reduction Potential *E*°(X2/2X−)
Fluorine (9, F)Pale-yellow gas (F2)3.98328.2141.2 pm / 158.8 kJ mol−1568 kJ mol−1 / p*K*a = +3.17 (weak acid)+2.87 V (oxidizes H2O to O2)
Chlorine (17, Cl)Yellow-green gas (Cl2)3.16348.6 (max)198.8 pm / 242.6 kJ mol−1431 kJ mol−1 / p*K*a ≈ −6.3 (strong acid)+1.36 V
Bromine (35, Br)Red-brown liquid (Br2)2.96324.6228.1 pm / 192.8 kJ mol−1366 kJ mol−1 / p*K*a ≈ −8.7 (strong acid)+1.07 V
Iodine (53, I)Violet-black solid (I2)2.66295.2266.6 pm / 151.1 kJ mol−1298 kJ mol−1 / p*K*a ≈ −9.5 (strongest HX)+0.54 V
Astatine (85, At)Dark metalloid solid2.20~233~296 pm (calc.) / ~110 kJ mol−1~240 kJ mol−1~+0.2 to +0.3 V

Two Classic Period-2 Anomalies: The Weak F–F Bond and Weak Hydrofluoric Acid (HF)

Inspecting the quantitative table above reveals two striking non-monotonic trends between Period 2 fluorine and Period 3 chlorine:

  1. Why *D*°(F–F) = 158.8 kJ mol−1 Is Much Weaker Than *D*°(Cl–Cl) = 242.6 kJ mol−1: Based on covalent radii alone, the short F–F bond (141.2 pm) might be expected to be stronger than the Cl–Cl bond (198.8 pm). However, each fluorine atom carries three compact 2*p* lone pairs; bringing two fluorine nuclei within 141.2 pm forces those six non-bonding electron pairs into severe inter-atomic lone-pair–lone-pair Pauli repulsion (manifested as fully occupied πg\* antibonding orbitals in Molecular Orbital theory), destabilizing F2 by ~100 kJ mol−1. Combined with the exceptional hydration enthalpy of the small F− ion (Δ*H*hyd° = −515 kJ mol−1) and high strength of E–F bonds, this weak F–F bond makes F2 the strongest elemental oxidizing agent known (Standard Electrode Potential *E*° = +2.87 V).
  2. Why Hydrofluoric Acid (HF, p*K*a = +3.17) Is a Weak Acid in Water While HCl, HBr, and HI Are Strong Acids (p*K*a −6 to −10): Across the hydrogen halide series (HX(aq) + H2O(l) ⇌ H3O+(aq) + X−(aq)), acidity increases by more than 12 orders of magnitude down the column (HF ≪ HCl < HBr < HI). Although the H–F bond is the most polar, its covalent bond dissociation enthalpy (*D*°(H–F) = 568 kJ mol−1) is 137 to 270 kJ mol−1 stronger than H–Cl (431), H–Br (366), and H–I (298), and the tiny, high-charge-density F− ion (r = 133 pm) binds tightly to H3O+ in an [H3O+···F−] ion pair while ordering surrounding water molecules into a low-entropy hydration cage (unfavorable negative Δ*S*°ioniz = −102 J mol−1 K−1), resulting in Δ*G*°ioniz = +18.1 kJ mol−1 (p*K*a = 3.17).

Interhalogens, Oxyacids, and Halogen Bonding (σ-Holes)

VSEPR Geometries of Interhalogen Compounds (XX′n) and Oxyacids

Because halogens differ substantially in electronegativity and atomic radius down Group 17, a heavier, less electronegative halogen (Cl, Br, or I) can act as the central atom X oxidized by n = 1, 3, 5, or 7 lighter, more electronegative halogen ligands X′ (F or Cl) via three-center four-electron bonds:

  • XX′ (Linear, oxidation state +1): ICl, IBr, BrF, ClF.
  • XX′3 (AX3E2, SN = 5, T-shaped C2v, oxidation state +3): ClF3, BrF3, and I2Cl6 (planar dimer).
  • XX′5 (AX5E1, SN = 6, Square Pyramidal C4v, oxidation state +5): BrF5 (Fax–Br–Feq = 84.8°), IF5 (81.9°), ClF5.
  • XX′7 (AX7E0, SN = 7, Pentagonal Bipyramidal D5h, oxidation state +7): Iodine heptafluoride (IF7)—only large Period 5 iodine (rcov = 139 pm) has enough surface area to pack seven fluorine ligands around a single main-group center (five equatorial fluorines at 72° and two axial fluorines at 90°/180°).

Similarly, chlorine, bromine, and iodine form four series of halogen oxyacids whose aqueous acidity increases steeply with the number of terminal oxo (=O) groups as negative charge delocalizes across the conjugate oxyanion: hypochlorous acid (HOCl, Cl(+1), p*K*a = 7.53) < chlorous acid (HClO2, Cl(+3), p*K*a = 1.96) < chloric acid (HClO3, Cl(+5), p*K*a ≈ −1) < perchloric acid (HClO4, Cl(+7), p*K*a ≈ −10).

The σ-Hole and Directional Halogen Bonding

In organohalogens (R–X, where X = I, Br, or Cl), formation of the covalent C–X σ bond pulls electron density out of the outer lobe of the halogen's npz orbital along the C–X axis while leaving the three non-bonding lone pairs in an equatorial belt of negative electrostatic potential around the waist of the halogen atom. Directly opposite the C–X bond on the distal tip of the halogen atom (at 180°), this depletion of pz electron density exposes the positively charged nuclear core, creating a localized region of positive electrostatic potential called a σ-hole (scales in magnitude as I > Br > Cl ≫ F). In medicinal chemistry and crystal engineering, this electropositive σ-hole interacts attractively and strictly linearly (~175°–180°) with Lewis bases (such as carbonyl oxygens in protein backbones) to form a halogen bond (R–X···:B, 5–40 kJ mol−1), exploited in the binding of thyroid hormones and halogenated pharmaceuticals.

Biological, Physiological, and Atmospheric Roles

  1. Vertebrate Physiology (Cl−, I−, Br−, and F−):
  • Chloride (Cl−): The principal extracellular anion in vertebrates (~100–108 mmol L−1 in human plasma); governs osmotic pressure, inhibitory GABAA/glycine receptor hyperpolarization in neurons, parietal-cell gastric acid (HCl, pH 1.5–2.0) secretion, the red-blood-cell Hamburger chloride shift (Cl−/HCO3− exchange), and neutrophil myeloperoxidase generation of microbicidal hypochlorous acid (HOCl) during the innate immune oxidative burst; defective CFTR chloride channels cause cystic fibrosis.
  • Iodide (I−): Actively concentrated into the thyroid gland via the Na+/I− symporter (NIS) and oxidized by thyroid peroxidase to iodinate tyrosine residues into thyroxine (T4, 3,5,3′,5′-tetraiodothyronine) and triiodothyronine (T3), the master regulators of basal metabolic rate and amphibian/lamprey metamorphosis.
  • Bromide (Br−): Essential cofactor for peroxidasin-catalyzed formation of covalent sulfilimine bonds (–S=N–) cross-linking collagen IV networks in animal basement membranes, and used by eosinophil peroxidase to generate antiparasitic hypobromous acid (HOBr).
  • Fluoride (F−): Substitutes for hydroxide (OH−) in tooth enamel hydroxyapatite (Ca5(PO4)3OH, Ksp ≈ 10−58) to form acid-resistant fluorapatite (Ca5(PO4)3F, Ksp ≈ 10−60).
  1. Stratospheric Ozone Layer Depletion: Photolysis of anthropogenic chlorofluorocarbons (CFCs) and halons by solar UV-C radiation in the stratosphere releases atomic chlorine (Cl•) and bromine (Br•) radicals that destroy ozone via the Molina–Rowland catalytic cycle (Cl• + O3 → ClO• + O2; ClO• + O → Cl• + O2; net O3 + O → 2 O2), where a single Cl• or Br• atom destroys up to 105 O3 molecules before termination.

Frequently Asked Questions

Why does only iodine form a seven-coordinate interhalogen (IF7), whereas chlorine and bromine stop at ClF5 and BrF5?

Forming a seven-coordinate heptafluoride (XF7, oxidation state +7) requires both promoting all seven ns2np5 valence electrons into bonding combinations and physically packing seven fluorine atoms (rvdW = 147 pm) around the central halogen X without prohibitive steric ligand-ligand repulsion. In chlorine (rcov = 102 pm) and bromine (rcov = 120 pm), the central atom is too small to accommodate more than five or six fluorine atoms in its coordination sphere (and for bromine, the 3*d*-block contraction stabilizes the 4*s*2 pair, making Br(+7) kinetically and thermodynamically difficult to reach with F2). Period 5 iodine has a large enough covalent radius (rcov = 139 pm) and accessible 5*s*/5*p* shell to accommodate five equatorial fluorines and two axial fluorines in pentagonal bipyramidal IF7 (D5h).

How do carbon-fluorine (C–F) bonds make PFAS ("forever chemicals") and fluorinated pharmaceuticals resistant to metabolic degradation?

The carbon–fluorine single bond is the strongest single bond in organic chemistry (*D*° = 485 kJ mol−1 in CH3F, rising to 530–545 kJ mol−1 in perfluoroalkyl –CF2–CF3 chains because multiple geminal fluorines contract the carbon orbitals and add electrostatic Cδ+–Fδ− attraction). Furthermore, fluorine's three 2*p* lone pairs are held tightly around the C–F backbone with minimal polarizability (α = 0.56 Å3), forming a steric and electrostatic shield that prevents oxidative attack by hepatic cytochrome P450 monooxygenases. In medicinal chemistry, strategically replacing a metabolically labile C–H bond with a C–F bond (nearly isosteric in van der Waals radius: H = 120 pm vs. F = 147 pm) extends drug half-life, while in per- and polyfluoroalkyl substances (PFAS) complete perfluorination prevents environmental biodegradation.

Why is astatine (At, Z = 85) the rarest naturally occurring element in Earth's crust?

Every isotope of astatine is radioactive with a short half-life: the longest-lived isotope, synthetic 210At, decays via electron capture and α-emission with a half-life of only 8.1 hours, while the α-emitting medical radionuclide 211At has a half-life of 7.21 hours. In nature, isotopes 215At, 218At, and 219At (with half-lives of milliseconds to 56 seconds) are produced only as rare, low-probability (<0.02%) branched-chain decay daughters within the natural 235U, 238U, and 232Th decay series, leaving less than 1 to 30 grams of astatine present in the entire continental crust of the Earth at any instant.

References

  1. Greenwood, N. N., & Earnshaw, A. (1997). Chemistry of the Elements (2nd ed., Chapter 17: The Halogens). Butterworth-Heinemann. ISBN 978-0750633659
  2. Cavallo, G., Metrangolo, P., Milani, R., Pilati, T., Priimagi, A., Resnati, G., & Terraneo, G. (2016). "The halogen bond." Chemical Reviews, 116(4), 2478–2601. https://doi.org/10.1021/acs.chemrev.5b00484
  3. McCall, A. S., Cummings, C. F., Bhave, G., Vanacore, R., Page-McCaw, A., & Hudson, B. G. (2014). "Bromine is an essential trace element for assembly of collagen IV scaffolds in tissue development and architecture." Cell, 157(6), 1380–1392. https://doi.org/10.1016/j.cell.2014.05.009
  4. Molina, M. J., & Rowland, F. S. (1974). "Stratospheric sink for chlorofluoromethanes: chlorine atom-catalysed destruction of ozone." Nature, 249(5460), 810–812. https://doi.org/10.1038/249810a0
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