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Diffraction and Polarization

Single Slit Diffraction

Diffraction is the bending of light around obstacles and its spreading into geometrical shadow regions, fundamentally explained by Huygens' Principle.
Single Slit DiffractionVisualization of Huygens' principle and the resulting intensity pattern for a single slit.Intensity (I)Slit width (b)Central MaximumIncident Plane WavesDiffraction Pattern
Determines the angular position of the first minimum in a single-slit pattern.
=Angle to the first dark fringe(radians)
=Wavelength of incident light(m)
=Slit width (aperture size)(m)
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Negligible diffraction (light travels in straight lines)
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Significant spreading of the Central Maximum
Huygens' Principle: Every point on the wavefront within the slit acts as a source of secondary wavelets.
Central Maximum: The bright broad peak directly opposite the slit, containing most of the wave energy.
Secondary Maxima: Fainter bright fringes on either side of the center caused by partial constructive interference.
General Minima Condition: Dark fringes occur at where
Proportionality Shortcut: — doubling wavelength doubles the spread; doubling slit width halves it.
Diffraction Prominence: The effect is significant only when . For , light essentially travels in straight lines.

Diffraction Gratings

A Diffraction Grating uses thousands of parallel slits to produce extremely sharp and localized interference maxima through Constructive Interference.
Predicts the angles of principal maxima for multi-slit interference.
=Grating element (spacing between slits)(m)
=Order of diffraction(integer)
=Angular deviation of the nth order(degrees)
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Zero-order maximum (central spot)
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Order not observable (sin θ cannot exceed 1)
Grating Element: The slit spacing is the reciprocal of line density: . Convert units carefully — 5000 lines/cm means m.
Maximum Observable Order: Since , the highest order is (the greatest integer ≤ ).
Angular Dispersion: Higher orders () separate different wavelengths more effectively, producing wider spectra.
White Light: Each wavelength diffracts at a different angle, producing a spectrum at each order. Higher orders show more spread-out spectra.

Bragg's Law — X-ray Diffraction by Crystals

X-rays have wavelengths (~ m) comparable to interplanar spacing in crystals, so crystal lattice planes act as a natural Diffraction Grating for X-rays.
Bragg's Law of X-ray DiffractionDiagram showing X-rays reflecting off two parallel crystal lattice planes, illustrating the path difference and the derivation of Bragg's Law.θθdd sin θd sin θPath Difference ΔL = 2d sin θnλ = 2d sin θ
Bragg's equation: gives the condition for constructive interference of X-rays reflected from parallel crystal planes.
=Interplanar spacing between crystal planes(m)
=Bragg angle (angle of incidence measured from the crystal plane, not the normal)(degrees)
=Order of reflection(integer)
=Wavelength of incident X-rays(m)
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First-order reflection — strongest and most commonly observed
increases
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Higher-order reflections become possible, but intensity decreases
Path Difference: The extra distance traveled by the beam reflecting from the lower plane is , leading to the factor of 2.
Applications: Determining crystal structure (X-ray crystallography), used to find the structure of DNA and haemoglobin.
Grating vs Bragg: The grating equation has no factor of 2 because it involves transmission through slits, not reflection from parallel planes.

Polarization

Polarization proves light is a Transverse Wave by restricting oscillations to a single plane using a Polarizer.
Brewster's Angle and PolarizationVisualizing unpolarized light hitting an interface at Brewster's angle, resulting in a perfectly polarized reflected ray and a 90-degree angle between reflected and refracted rays.θpθpUnpolarized LightLinearly PolarizedPartially PolarizedAir (n1)Glass (n2)n2 / n1 = tan(θp)
Malus's Law: Relates transmitted intensity to the alignment of two polarizers.
=Transmitted intensity(W/m²)
=Intensity of polarized light entering the analyzer(W/m²)
=Angle between polarizer and analyzer axes(degrees)
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Parallel polarizers; full intensity transmitted
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Half intensity transmitted ()
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Crossed polarizers; zero intensity transmitted
Unpolarized Light: Random oscillations in all planes perpendicular to propagation.
Selective Absorption: Polaroid sheets (dichroic materials) absorb E-field components perpendicular to the transmission axis.
Half-Rule: When unpolarized light passes through the first polarizer, transmitted intensity is always , regardless of polarizer orientation.
Crossed Polarizers: Two polaroids at block all light. Inserting a third at between them allows light through — a classic demonstration.
Proof of Transverse Nature: Longitudinal waves cannot be polarized. The fact that light can be polarized proves it is a transverse wave.
Optical Rotation: Certain substances (quartz, sugar solutions) rotate the plane of polarization. This property is used to measure concentration of optically active solutions.

Brewster's Law

Light reflected from a surface is perfectly plane-polarized at Brewster's Angle, where the reflected and refracted rays are perpendicular.
Calculates the specific angle of incidence for complete polarization by reflection.
=Refractive index of the medium(dimensionless)
=Brewster angle of incidence(degrees)
Water ()
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90° Rule: At Brewster's angle, the reflected and refracted rays are exactly perpendicular ().
Glare Reduction: Polaroid sunglasses block horizontally polarized light reflected from roads, water, and glass surfaces.
Partial Polarization: At angles other than Brewster's, the reflected ray is only partially polarized.
Common Values: Glass () → ; Water () → .