Atomic Structure & Chemical Bonding – Comprehensive Study Notes

Page 1 – Scope, Fundamental Definitions & Daltonian Foundations

1. Latest Syllabus → Key Topics

• Structure of an atom – sub-atomic particles, atomic number ZZ, mass number AA, isotopes, octet rule.
• Types of chemical bonding – electrovalent (ionic) vs covalent with full orbital structures.

2. Atom: Concept & Classical Definitions

• Etymology – from Greek “atomos” (indivisible).
• Democritus: qualitative proposal that matter is made of indivisible units.
• John Dalton (1808) – first quantitative atomic theory.

Postulates of Dalton’s Atomic Theory
  1. Matter consists of small, indivisible, indestructible particles called atoms.

  2. Atoms of the same element are identical; atoms of different elements differ.

  3. Atoms neither created nor destroyed in chemical change.

  4. Atoms combine in simple whole-number ratios to form molecules.

  5. Chemical reactions = rearrangement of atoms.

Modern Corrections to Dalton

Daltonian Statement

Modern View

Atoms are indivisible

Atoms divisible into electrons, protons, neutrons (and further into quarks, etc.).

Atoms indestructible

Nuclear reactions can destroy/create atoms.

All atoms of an element identical

Existence of isotopes: same ZZ, different AA.

Retained idea: atom is smallest entity that participates in chemical reactions; fixed ratio of atoms in a compound.

3. Discovery of the Electron

• 1878 – William Crookes: Electric discharge through low-pressure gas (≈0.010.01 mm Hg) produced “cathode rays.”
• Characteristics of cathode rays (J. J. Thomson, 1897):
– Travel straight from cathode to anode, cast sharp shadows.
– Deflected by magnetic & electric fields toward a positive plate ⇒ negative charge.
– Possess kinetic energy; heat objects they strike.
• Conclusion: cathode rays are streams of identical, negatively charged particles → electrons.
• Quantitative data:
– Mass m<em>e=11837m<em>e = \dfrac{1}{1837} mass of H-atom =9.107×1028g= 9.107\times10^{-28}\,\text{g}. – Charge q</em>e=1.602×1019Cq</em>e = -1.602\times10^{-19}\,\text{C}.
• Electrical neutrality of atoms implied presence of equal positive charge → led to discovery of protons.


Page 2 – Protons, Nucleus, Rutherford & Bohr Models, Neutrons

1. Discovery of the Proton

• Eugen Goldstein: observed “positive rays” (anode rays) when cathode was perforated.
• Rays travelled opposite direction to cathode rays; consisted of positively charged particles → protons.
• Data:
– Mass m<em>p=1.670×1024gm<em>p = 1.670\times10^{-24}\,\text{g} 1837 m</em>e\approx1837\ m</em>e.
– Charge qp=+1.602×1019Cq_p = +1.602\times10^{-19}\,\text{C} (unit positive).

2. Rutherford’s Alpha-Scattering Experiment (1911)

• Alpha particles (He nuclei, 2p+2n2p+2n) fired at gold foil (≈10610^{-6} cm thick).
• Observations:

  1. Majority passed undeflected → atom mostly empty.

  2. Some deflected at small angles → encounter with concentrated positive mass.

  3. Very few rebounded (>9090^{\circ}) → existence of tiny dense nucleus.

Rutherford Atomic Model – Postulates
  1. Nucleus: minute central region containing entire positive charge & almost all mass.

  2. Electrons revolve around nucleus in circular paths; centrifugal force counterbalances electrostatic attraction.

Drawback

• Classical electrodynamics: an accelerating (orbiting) electron should radiate energy → spiral into nucleus → atom unstable. Model failed to explain stability & spectra.

3. Bohr’s Atomic Model (1913)

  1. Electrons occupy fixed circular orbits (energy levels) with quantised angular momentum.

  2. Principal quantum number n=1,2,3,n = 1,2,3,\ldots labelled K, L, M, N….

  3. Electron neither absorbs nor emits energy while in a given orbit.

  4. Transition between levels involves discrete energy E<em>2E</em>1=hνE<em>2-E</em>1 = h\nu (line spectra).

  5. Provided first explanation of atomic stability & hydrogen spectrum.

4. Discovery of the Neutron (James Chadwick, 1932)

• Mass of He atom (≈4.0034.003 amu) > mass of 2 protons; electrons negligible → existence of neutral massive particles.
• Neutron: charge 00, mass mn=1.676×1024gm_n = 1.676\times10^{-24}\,\text{g} (≈mass of proton).
• Protons + neutrons collectively called nucleons.


Page 3 – Atomic Number, Mass Number & Sub-Atomic Accounting

1. Atom & Element

• Atom: smallest unit of an element participating in chemical reactions (e.g., O,Cl\text{O},\text{Cl}).
• Element: pure substance of identical atoms with same ZZ; cannot be decomposed physico-chemically.

2. Definitions & Symbols

• Atomic number ZZ = number of protons = number of electrons (for neutral atom) = nuclear positive charge.
• Mass number AA = total nucleons =p+n= p+n (whole-number approximation of atomic mass).
• Standard nuclear notation: ZAElement^{A}_{Z}\text{Element}.

Relationships

\begin{aligned}
Z &= p = e,\
A &= p + n,\
n &= A - Z.
\end{aligned}

3. Sub-Atomic Particle Summary (relative to 12C^{12}\text{C} standard)

Particle

Symbol

Charge

Relative mass

Proton

p+p^{+}

+1+1

11

Neutron

n0n^{0}

00

11

Electron

ee^{-}

1-1

negligible (≈11837\tfrac{1}{1837})


Page 4 – Electronic Configuration, 2n2n^2 Rule & First 20 Elements

1. Energy Levels (Shells)

• Electrons revolve in discrete shells K, L, M, N… (n = 1, 2, 3, 4…). Energy increases with distance from nucleus (K < L < M < N).

2. Bohr–Bury Distribution Rules

Rule 1 – Maximum electrons in a shell: 2n22n^{2}.
(K =2=2, L =8=8, M =18=18, N =32=32 …)

Rule 2 – Outermost shell never holds >88 e⁻; penultimate shell never >1818 e⁻. A new shell forms once an octet is completed.

3. Electronic Configurations of Z=1 to 20Z = 1 \text{ to } 20 (representative)

1<em>1H:  1^{1}<em>{1}\text{H}:\;1  • 4</em>2He:  2^{4}</em>{2}\text{He}:\;2  • 7<em>3Li:  2,1^{7}<em>{3}\text{Li}:\;2,120</em>10Ne:  2,8^{20}</em>{10}\text{Ne}:\;2,8 (stable octet)
23<em>11Na:  2,8,1^{23}<em>{11}\text{Na}:\;2,8,140</em>20Ca:  2,8,8,2^{40}</em>{20}\text{Ca}:\;2,8,8,2 (penultimate shell filled to 8, obeying Rule 2).

Diagrams (planetary style) illustrate each shell and valence electrons for all first 20 elements.


Page 5 – Isotopes: Definition, Properties & Examples

1. Definition

Isotopes = atoms of the same element with identical ZZ but different AA (different nn).

2. Chemical vs Physical Behaviour

• Chemical properties depend on electronic configuration (same for isotopes) → essentially identical.
• Physical properties depend on mass → differ among isotopes (density, diffusion rate, melting point, etc.).

3. Common Isotopic Sets

  1. Hydrogen: 1<em>1H^{1}<em>{1}\text{H} (Protium), 2</em>1H^{2}</em>{1}\text{H} (Deuterium), 13H^{3}_{1}\text{H} (Tritium).

  2. Carbon: 12<em>6C,13</em>6C,614C^{12}<em>{6}\text{C},\,^{13}</em>{6}\text{C},\,^{14}_{6}\text{C} (radio-carbon dating).

  3. Oxygen: 16<em>8O,17</em>8O,818O^{16}<em>{8}\text{O},\,^{17}</em>{8}\text{O},\,^{18}_{8}\text{O}.

  4. Chlorine: 35<em>17Cl^{35}<em>{17}\text{Cl} & 37</em>17Cl^{37}</em>{17}\text{Cl} – natural abundance 3 : 1, giving atomic mass 35.535.5 amu.

  5. Potassium (39<em>19K,41</em>19K^{39}<em>{19}\text{K},^{41}</em>{19}\text{K}), Uranium (235<em>92U,238</em>92U^{235}<em>{92}\text{U},^{238}</em>{92}\text{U}), etc.

4. Fractional Atomic Mass

Average atomic mass =(isotopic mass×abundance)100= \dfrac{\sum (\text{isotopic mass} \times \text{abundance})}{100}.
Chlorine example:
(3×35)+(1×37)4=35.5amu.\dfrac{(3\times35) + (1\times37)}{4} = 35.5\,\text{amu}.


Page 6 – Chemical Activity, Octet/Duplet Rule & Bond Formation

1. Noble Gases: Paradigm of Stability

Noble Gas

ZZ

Shell Configuration

He

22

22 (duplet)

Ne

1010

2,82,8

Ar

1818

2,8,82,8,8

Kr

3636

2,8,18,82,8,18,8

Xe

5454

2,8,18,18,82,8,18,18,8

Rn

8686

2,8,18,32,18,82,8,18,32,18,8

Stable octet/duplet ⇒ chemically inert.

2. Octet Rule

Atoms of other elements are unstable; they undergo chemical change to achieve:
• Duplet (2 e⁻) in K-shell (Helium analogue)
• Octet (8 e⁻) in outer shell (Ne, Ar … analogue)

3. Routes to Stability

  1. Electron Transfer (Ionic/Electrovalent Bond)
    – Metal loses e⁻ → cation; non-metal gains e⁻ → anion; electrostatic attraction forms ionic lattice.
    – Examples:
    23<em>11NaNa++e^{23}<em>{11}\text{Na} \rightarrow \text{Na}^{+} + e^{-} (2,8,12,82,8,1 \Rightarrow 2,8) • 35</em>17Cl+eCl^{35}</em>{17}\text{Cl} + e^{-} \rightarrow \text{Cl}^{-} (2,8,72,8,82,8,7 \Rightarrow 2,8,8)
    Na++ClNaCl\text{Na}^{+} + \text{Cl}^{-} \rightarrow \text{NaCl}.
    Ca2++O2CaO\text{Ca}^{2+} + \text{O}^{2-} \rightarrow \text{CaO}.

  2. Electron Sharing (Covalent Bond)
    – Two atoms share one or more pairs of electrons to complete octet/duplet.
    – Examples (orbital/Lewis structures):
    H<em>2\text{H}<em>2: H+HH:HH\cdot + \cdot H \Rightarrow H:H. • O</em>2\text{O}</em>2: O::O\cdot\cdot O::O \cdot\cdot (double bond).
    N<em>2\text{N}<em>2: triple bond NNN\equiv N. • H</em>2O\text{H}</em>2\text{O}: HOHH-O-H (2 lone pairs on O).
    NH<em>3\text{NH}<em>3: HNHH-N-H with one lone pair. • CH</em>4\text{CH}</em>4, CCl4\text{CCl}_4 illustrate tetra-covalency of carbon.

4. Electronic Theory of Redox (Linkage)

• Oxidation = loss of electrons (e.g., Fe2+eFe3+\text{Fe}^{2+} - e^{-} \rightarrow \text{Fe}^{3+}).
• Reduction = gain of electrons (e.g., Fe3++eFe2+\text{Fe}^{3+} + e^{-} \rightarrow \text{Fe}^{2+}).


Ethical, Philosophical & Real-World Notes

• Evolution of atomic models shows scientific method: hypotheses → experimental evidence → model refinement.
• Isotopes underpin radiometric dating, medical tracers ((^{131}\text{I}), (^{99m}\text{Tc})), and nuclear power ((^{235}\text{U})).
• Octet concept rationalises periodicity: valence e⁻ configuration governs group chemistry.
• Stability considerations of nuclei (balance of protons and neutrons) inform nuclear medicine and environmental safety.