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Snell's Law Refraction Calculator

The current ledger marks this instrument verified clean within the source-bound verification corpus.

Status: VERIFIED_CLEANLifecycle: verified-clean

Inspectable records

Ledger state

The current ledger marks this instrument verified clean within the source-bound verification corpus.

Area
Physics — Kinematics/Projectiles/Orbits, Forces/Energy/Momentum, Rotational Dynamics, Gravitation, Oscillations/Waves, Optics, E&M Fields, Relativity, Quantum, Statistical Thermo
Tranche
tranche-5
Evidence ID
t5-132
Ledger rows
1

No ledger note is attached.

Review findings

The core law is correct, but the specification is incomplete because it does not define angle units, angle reference direction, inverse-solving behavior, physical-domain validation, or total-internal-reflection handling. The verdict is NEEDS_REVIEW until those behaviors are specified.

Formula and scope findings

  • The relation n1 sin(theta1) = n2 sin(theta2) is the standard Snell's law formula for a planar interface, assuming isotropic, non-magnetic media and angles measured from the interface normal.
  • The calculator must explicitly implement the inverse forms theta2 = asin((n1/n2) sin(theta1)) and theta1 = asin((n2/n1) sin(theta2)); the listed equation alone does not specify which angle is solved for.
  • The valid inverse-sine domain must be enforced: if the argument magnitude exceeds 1, no real refracted angle exists because of total internal reflection.
  • The physical branch should normally return angles from 0 to 90 degrees for ordinary refraction; this branch convention is not specified.

Unit assumptions

  • Refractive indices n1 and n2 are dimensionless.
  • Angles in the test vectors are in degrees, and inverse-trigonometric results are converted back to degrees. The specification does not state whether the implementation expects degrees or radians.
  • Angles are measured from the interface normal, not from the interface surface.
  • The media are assumed homogeneous, isotropic, and non-magnetic; refractive index values are wavelength- and condition-dependent.
  • For ordinary transparent media, n1 and n2 are assumed positive and nonzero.

Boundary hardening

Recorded hazards

  • If n2 is zero, the inverse formula divides by zero.
  • If n1 or n2 is negative, the physical interpretation requires handling complex or signed refractive indices; this is not specified.
  • For light going from a higher-index medium to a lower-index medium, an input above the critical angle produces an inverse-sine argument greater than 1 and must be reported as total internal reflection rather than NaN or a fabricated angle.
  • Passing degree values directly to JavaScript Math.sin or Math.asin, which use radians, causes incorrect results; explicit conversion is required.
  • The interface-normal convention is not stated, so complementary angle results are possible if users measure from the surface.
  • A refractive-index table requires wavelength, temperature, pressure, and material-state assumptions; a generic air/water/glass/diamond table can be misleading without those qualifiers.

Errata and corrections

No applied erratum is attached to this unique-name record.

Inspectable example

4 review vectors are recorded. One source-bound sample is shown below.

{
  "inputs": {
    "mode": "solve_theta2",
    "n1": 1,
    "n2": 1.5,
    "theta1_deg": 0
  },
  "expected_outputs": {
    "theta2_deg": 0
  },
  "working": "sin(theta2) = (n1/n2) sin(theta1) = (1.0/1.5) sin(0 degrees) = (2/3)(0) = 0. Therefore theta2 = asin(0) = 0 degrees."
}

Related workflows

No source-defined multi-instrument workflow membership is recorded.

Sources and evidence

These pointers bind the page to evidence. They do not grant authority or collapse verification into deployment.

  • VERIFIED_LEDGER.json · VERIFIED_CLEAN
  • evidence-tranche5/tranche5-results.json