Skip to content

🧱 p-Block Elements (Groups 13–18) ​

The p-block exhibits remarkable structural diversity—from electron-deficient multi-center boranes to hypervalent noble gas fluorides. Key competitive exam topics include inert pair effect oxidation state stabilities, oxyacid structural basicities, silicate chain and sheet topology, and Xenon fluoride hydrolysis stoichiometry.


1. 🔒 The Inert Pair Effect ​

As we descend Groups 13, 14, and 15, the intervening filled d and f subshells shield nuclear charge poorly, causing the valence ns2 electrons to be held tightly by the nucleus ("inert"):

Lower oxidation state becomes progressively MORE stable down the group
  • Group 13: +3 stability: B>Al>Ga>In>Tl; +1 stability: Tl>In>Ga>Al>B.
    • Tl3+ is a powerful oxidizing agent (Tl3++2e−→Tl+).
  • Group 14: +4 stability: C>Si>Ge>Sn>Pb; +2 stability: Pb>Sn>Ge>Si.
    • PbO2 is a strong oxidizing agent; Sn2+ is a reducing agent (Sn2+→Sn4++2e−).
  • Group 15: +5 stability: N>P>As>Sb>Bi; +3 stability: Bi>Sb>As>P>N.
    • Bi2O5 is unstable; Bi5+ acts as a strong oxidizing agent.

2. 🧪 Group 13: Boron Compounds & Diborane ​

2.1 Diborane (B2H6) Structure & Reactions ​

  • Each Boron is sp3 hybridized. Contains four terminal B−H bonds (2c−2e, length 1.19 \AA) and two bridging B−H−B bonds (3c−2e banana bonds, length 1.33 \AA).
  • Reaction with Ammonia (NH3):
    • Low temperature (1:2 ratio): Symmetrical cleavage gives [BH2(NH3)2]+[BH4]−.
    • High temperature (1:2 ratio heated to 200∘C): Yields Borazine ("Inorganic Benzene") B3N3H6:3B2H6+6NH3→Δ2B3N3H6+12H2
    • Borazine is isoelectronic and isostructural with Benzene, but more reactive due to Bδ+−Nδ− bond polarity (undergoes electrophilic additions without catalyst).

3. 🌲 Group 14: Silicones & Silicates ​

3.1 Silicate Mineral Classification (Based on Shared [SiO4]4− Tetrahedral Corners) ​

Silicate TypeFundamental Anion FormulaShared Oxygens per TetrahedronExamples
Orthosilicates (Nesosilicates)[SiO4]4−0 (Isolated tetrahedra)Forsterite (Mg2SiO4), Phenacite (Be2SiO4), Zircon (ZrSiO4)
Pyrosilicates (Sorosilicates)[Si2O7]6−1Thortveitite (Sc2Si2O7), Hemimorphite
Cyclic / Ring Silicates[Si3O9]6− or [Si6O18]12−2Beryl (Be3Al2Si6O18), Benitoite (BaTiSi3O9)
Chain Silicates (Pyroxenes)[(SiO3)n]2n−2 (Linear single chain)Diopside (CaMg(SiO3)2), Spodumene (LiAl(SiO3)2)
Double Chain (Amphiboles)[(Si4O11)n]6n−Alternate 2 and 3Asbestos, Tremolite
Sheet Silicates (Phyllosilicates)[(Si2O5)n]2n−3 (2D infinite sheets)Talc (Mg3(Si2O5)2(OH)2), Mica, Kaolinite
3D Framework (Tektosilicates)[(SiO2)n]4 (All four corners shared)Quartz, Feldspar, Zeolites

4. ⚡ Group 15 & 16: Oxyacids of Phosphorus & Sulfur ​

4.1 Oxyacids of Phosphorus ​

OxyacidFormulaOxidation State of PBasicity (P−OH)P−H Bonds (Reducing)P=O Bonds
Hypophosphorous (Phosphinic)H3PO2+11 (Monobasic)2 (Strong reducing agent)1
Phosphorous (Phosphonic)H3PO3+32 (Dibasic)1 (Reducing agent)1
OrthophosphoricH3PO4+53 (Tribasic)0 (Non-reducing)1
PyrophosphoricH4P2O7+54 (Tetrabasic)0 (1×P−O−P bridge)2

4.2 Oxyacids of Sulfur: Marshall's Acid & Caro's Acid ​

  • Caro's Acid (H2SO5, Peroxomonosulfuric acid): Contains one peroxide linkage (−O−O−). O.S. of Sulfur is +6 (NOT +8!).
  • Marshall's Acid (H2S2O8, Peroxodisulfuric acid): Structure HO−SO2−O−O−SO2−OH. O.S. of both Sulfur atoms is +6.

5. 💎 Group 18: Xenon Compounds & Hydrolysis ​

5.1 Preparation & Hydrolysis of Xenon Fluorides ​

  • Xe+F2→673 K,1 barXeF2 (1:1 ratio)
  • Xe+2F2→873 K,7 barXeF4 (1:5 ratio)
  • Xe+3F2→573 K,60−70 barXeF6 (1:20 ratio)

Hydrolysis Stoichiometry: ​

  1. XeF2 (Redox Hydrolysis):2XeF2+2H2O→2Xe↑+4HF+O2↑
  2. XeF4 (Disproportionation Hydrolysis):6XeF4+12H2O→2XeO3+4Xe↑+24HF+3O2↑
  3. XeF6 (Complete Non-Redox Hydrolysis):XeF6+3H2O→XeO3+6HF
    • Partial hydrolysis: XeF6+H2O→XeOF4+2HF; XeF6+2H2O→XeO2F2+4HF.