Unit 2: Structure of Atom Lecture Notes
Historical Theories and the Particle Nature of Matter
- Early Indian and Greek philosophers (circa 400 B.C.) proposed that atoms are the fundamental building blocks of matter. They believed that continuous subdivision of matter would eventually reach a particle that could not be further divided.
- The word 'atom' originates from the Greek word 'a-tomio', meaning 'uncut-able' or 'non-divisible'.
- Early atomic ideas were speculative and lacked experimental verification, remaining dormant until the nineteenth century.
- John Dalton, a British school teacher, provided the first scientific basis for atomic theory in 1808. He regarded the atom as the ultimate particle of matter.
- Dalton's theory successfully explained the law of conservation of mass, the law of constant composition, and the law of multiple proportion.
- Dalton's theory failed to explain certain experimental results, such as why substances like glass or ebonite become electrically charged when rubbed with silk or fur.
- Experiments in the late 19th and early 20th centuries established that atoms are actually composed of sub-atomic particles: electrons, protons, and neutrons.
Discovery of Sub-atomic Particles
- Insights into atomic structure came from experiments involving electrical discharge through gases.
- A fundamental rule of charged particles is that like charges repel each other and unlike charges attract.
- In 1830, Michael Faraday showed that passing electricity through an electrolyte solution caused chemical reactions at electrodes, resulting in the liberation and deposition of matter, suggesting electricity has a particulate nature.
- In the mid-1850s, cathode ray discharge tubes were utilized to study electricity. These tubes are made of glass and contain two metal electrodes (cathode and anode).
- Electrical discharge through gases is only observable at very low pressures and very high voltages. Pressure is adjusted by evacuation.
- When high voltage is applied, current flows as a stream of particles from the negative electrode (cathode) to the positive electrode (anode), known as cathode rays or cathode ray particles.
- The flow is verified by using a perforated anode and coating the tube behind it with a phosphorescent material like zinc sulphide (ZnS). Impact on the coating produces a bright spot.
- Characteristics of Cathode Rays:
- They travel from cathode toward anode.
- The rays themselves are invisible but are detectable via fluorescent or phosphorescent materials (e.g., television picture tubes).
- They travel in straight lines in the absence of electrical or magnetic fields.
- They consist of negatively charged particles (electrons) as they behave like negative charges in electrical or magnetic fields.
- Their characteristics do not depend on the electrode material or the nature of the gas in the tube.
Atomic Properties and Fundamental Constants
- J.J. Thomson (1897) measured the charge to mass ratio (e/me) of the electron using perpendicular electrical and magnetic fields.
- Amount of deviation depends on:
- Magnitude of charge: Higher charge interaction leads to greater deflection.
- Mass: Lighter particles undergo greater deflection.
- Field strength: Deflection increases with increased voltage or magnetic field strength.
- Thomson's calculated value: mee=1.758820×1011C kg−1.
- R.A. Millikan (1906-14) used the oil drop experiment to determine electron charge. He found it to be −1.6×10−19C. The current accepted value is −1.602176×10−19C.
- Mass of the electron (me) was calculated by combining these results: me=9.109382×10−31kg.
- Discovery of Protons: Modified cathode ray tubes revealed canal rays (positively charged gaseous ions). Their mass depends on the gas used. The smallest and lightest was from hydrogen, called a proton (1919).
- Discovery of Neutrons: James Chadwick (1932) bombarded a thin sheet of beryllium with α-particles, emitting neutral particles with mass slightly greater than protons (1.674927×10−27kg, compared to proton's 1.6726216×10−27kg).
Early Atomic Models and Radioactivity
- Wilhalm R\u00f6entgen (1895) discovered X-rays when electrons struck materials in cathode ray tubes. They possess high penetrating power and are not deflected by fields.
- Henri Becqueral (1896) discovered radioactivity. Marie Curie and Rutherford furthered this work, identifying three ray types:
- α-rays: Helium nuclei (He2+), high energy, two units of positive charge, four units of mass.
- β-rays: Negatively charged particles similar to electrons.
- γ-rays: High energy neutral radiations, most penetrating.
- J.J. Thomson's Model (1898): 'Plum pudding' or 'watermelon' model. Atom is a sphere of positive charge (radius ∼10−10m) with electrons embedded. It assumed uniform mass distribution.
- Rutherford's Scattering Experiment (1909): Bombarded a gold foil (∼100nm thick) with α-particles.
- Observations: Most particles passed undeflected; a small fraction was deflected by small angles; a very few (1 in 20,000) bounced back (180∘).
- Conclusions: Atom is mostly empty space. Positive charge and mass are concentrated in a tiny volume (nucleus). Radius of nucleus is ∼10−15m. Analogy: If nucleus is a cricket ball, atom radius is 5km.
- Rutherford's Model Postulates:
- Positive charge/mass concentrated in the nucleus.
- Electrons move around nucleus in circular paths (orbits), resembling the solar system.
- Electrons and nucleus are held by electrostatic forces.
Nuclear Composition: Atomic and Mass Numbers
- Atomic number (Z) = Number of protons in the nucleus = number of electrons in a neutral atom.
- Mass number (A) = Number of protons (Z) + Number of neutrons (n). Collectively called nucleons.
- Notation: ZAX.
- Isobars: Atoms with the same mass number but different atomic numbers (e.g., 614C and 714N).
- Isotopes: Atoms with the same atomic number but different mass numbers due to different neutron counts.
- Hydrogen isotopes: Protium (11H, 99.985%), Deuterium (12D, 0.015%), Tritium (13T, trace amounts).
- Chemical properties are determined by electron count (protons), so isotopes show identical chemical behavior.
Failures of Rutherford's Model
- Stability Problem: According to Maxwell's electromagnetic theory, an accelerated charged particle (electron in orbit) should emit radiation. This energy loss should cause the electron to spiral into the nucleus in 10−8s.
- Distribution Problem: It says nothing about how electrons are distributed or their energies.
- Stationary Electrons: If electrons were stationary, electrostatic attraction would pull them into the nucleus.
Developments Leading to the Bohr Model
- Neils Bohr improved early models by incorporating the dual character of electromagnetic (EM) radiation (wave-like and particle-like properties) and experimental atomic spectra results.
- Wave Nature of EM Radiation: Maxwell (1870) proposed that oscillating charged particles produce alternating electrical and magnetic fields transmitted as waves.
- Waves do not require a medium and travel at the speed of light (c=2.997925×108m s−1, approx 3.0×108m s−1).
- Frequency (ν) and wavelength (λ) relationship: c=νλ.
- Wavenumber (νˉ): Number of wavelengths per unit length: νˉ=λ1.
- EM Spectrum Regions:
- Radio: ∼106Hz.
- Microwave: ∼1010Hz.
- Infrared: ∼1013Hz.
- Visible light: ∼1015Hz.
- Ultraviolet: ∼1016Hz.
- Black-body Radiation: Ideal bodies that absorb and emit all frequencies uniformly. Max Planck (1900) proposed energy is emitted/absorbed in discrete units called quanta. Equation: E=hν, where Planck's constant h=6.626×10−34J s.
- Photoelectric Effect: Electrons are ejected from metals (like K,Rb,Cs) upon exposure to light. Einstein (1905) applied Planck's theory: hν=hν0+21mev2. hν0 is the work function (W0).
Atomic Spectra and Bohr's Model of Hydrogen
- Emission Spectrum: Spectrum of radiation from a substance that has absorbed and then emitted energy.
- Absorption Spectrum: Like a photographic negative of emission, showing dark spaces where specific wavelengths were absorbed.
- Line Spectra (Atomic Spectra): Discrete bright lines emitted by gas-phase atoms. Elements have unique line spectra ('fingerprints').
- Hydrogen Line Series:
- Balmer formula (1885): νˉ=109,677(221−n21)cm−1, where n≥3.
- Rydberg expression: νˉ=109,677(n121−n221)cm−1.
- Series: Lyman (n1=1, UV), Balmer (n1=2, Visible), Paschen (n1=3, IR), Brackett (n1=4, IR), Pfund (n1=5, IR).
- Bohr's Postulates for Hydrogen (1913):
- Electrons move in circular 'stationary' orbits with fixed radius and energy.
- Energy change occurs only during jumps between orbits: ΔE=E2−E1=hν.
- Angular momentum is quantized: mevr=n2πh, where n=1,2,3....
- Bohr's Mathematical Results:
- Radii: rn=n2a0 where a0=52.9pm.
- Energy: En=−RH(n21) where RH=2.18×10−18J.
- For hydrogen-like ions (He+,Li2+,Be3+): En=−2.18×10−18(n2Z2)J; rn=Z52.9(n2)pm.
- Limitations of Bohr Model: Fails to explain multi-electron atoms, finer 'doublet' details of spectra, Zeeman effect (magnetic splitting), Stark effect (electric splitting), and chemical bonding.
Mechanics of the Microscopic World
- de Broglie Relation (1924): Matter has dual behavior. λ=mvh=ph. This was confirmed by electron diffraction.
- Heisenberg Uncertainty Principle (1927): Impossible to determine exactly both position and momentum of an electron simultaneously: ΔxΔpx≥4πh.
- Implications: Rules out definite electron trajectories. Significant only for microscopic objects.
- Quantum Mechanics: Theoretical science developed by Heisenberg and Erwin Schr\u00f6dinger (1926) dealing with dual nature of matter. Schr\u00f6dinger Equation: H^ψ=Eψ where H^ is the Hamiltonian operator.
- Atomic Orbital: The wave function ψ for an electron. Probability density is ∣ψ∣2. Regions where ∣ψ∣2 is zero are called nodes.
Quantum Numbers and Orbital Shapes
- Principal Quantum Number (n): Positive integer (1,2,3...). Defines shell size and energy. Number of orbitals in a shell = n2.
- Azimuthal Quantum Number (l): Range 0 to n−1. Defines three-dimensional shape (sub-shells).
- l=0 (s), l=1 (p), l=2 (d), l=3 (f).
- Magnetic Orbital Quantum Number (ml): Range −l to +l. Defines spatial orientation. Total orientations = 2l+1.
- Electron Spin Quantum Number (ms): Two orientations (+1/2,−1/2), represented by ↑ and ↓.
- Shapes:
- s-orbitals: Spherical. Size increases with n. Number of radial nodes = n−1.
- p-orbitals: Two lobes (dumb-bell). Designated px,py,pz. Nodal plane passes through nucleus. Radial nodes = n−2.
- d-orbitals: Designated dxy,dyz,dxz,dx2−y2,dz2. First four have four lobes.
- Total nodes = (n−1) [sum of angular nodes (l) and radial nodes (n−l−1)].
Rules for Filling Orbitals and Configuration
- Energies of Orbitals:
- For hydrogen, energy depends only on n. Orbitals with same energy are 'degenerate'.
- For multi-electron atoms, energy depends on n and l. Determined by (n+l) rule: Lower (n+l) means lower energy. If (n+l) is equal, the orbital with lower n has lower energy.
- Aufbau Principle: Orbitals are filled in order of increasing energies: 1s,2s,2p,3s,3p,4s,3d,4p...
- Pauli Exclusion Principle: No two electrons in an atom can have the same four quantum numbers. An orbital can hold only two electrons with opposite spins.
- Hund's Rule of Maximum Multiplicity: Electron pairing in degenerate orbitals (p, d, f) doesn't start until each orbital is singly occupied.
- Electronic Configuration: Distribution of electrons into orbitals (e.g., Hydrogen is 1s1, Helium is 1s2).
- Exceptional Configurations: Chromium (Z=24) is [Ar]3d54s1 and Copper (Z=29) is [Ar]3d104s1. Extra stability arises from:
- Symmetrical distribution of electrons.
- High exchange energy: Energy released when electrons with same spin in degenerate orbitals swap positions.