Physics Calculators

Mechanics, optics & thermodynamics

Chemistry calculators A-C 🧪

Chemistry calculators C-D 🧪

Chemistry calculators E-F 🧪

Chemistry calculators F-H 🧪

Chemistry calculators I-M 🧪

Chemistry calculators M-P 🧪

Chemistry calculators P-S 🧪

Chemistry calculators S-T 🧪

Chemistry calculators T-Z 🧪

Physics calculators A-E ⚛️

Physics calculators F-N ⚛️

Physics calculators O-S ⚛️

Physics calculators S-W ⚛️

Math and number calculators 🔢

Home and property calculators 🏠

Statistics and probability calculators 📊

Body and wellness calculators ❤️

Tax and income calculators 🧾

Physics Calculators

Physics calculators implement the fundamental laws of nature — Newton's laws of motion, conservation of energy and momentum, thermodynamics, electromagnetism, and relativity — to solve quantitative problems across all branches of classical and modern physics. From calculating the velocity of a projectile to the energy stored in a magnetic field, these tools make physical reasoning accessible and precise.

Physics is the most fundamental of the natural sciences, describing the behavior of matter and energy at all scales from subatomic particles to the structure of the universe. Its quantitative predictions are among the most precisely verified in science: the anomalous magnetic moment of the electron is predicted by quantum electrodynamics to better than 1 part in 10¹⁰ and confirmed experimentally to the same precision.

Classical mechanics — developed by Galileo, Newton, and their successors in the 17th and 18th centuries — describes the motion of macroscopic objects at speeds well below the speed of light. Newton's three laws of motion and the law of universal gravitation unified terrestrial and celestial mechanics, enabling prediction of planetary orbits, artillery trajectories, and ocean tides with a single mathematical framework.

Energy conservation is one of the deepest principles in physics. The total energy of an isolated system is constant, though it transforms between kinetic, potential, thermal, chemical, nuclear, and other forms. Understanding these transformations is essential for engineering efficient machines, analyzing collisions, and designing energy systems. Our physics calculators handle energy conversions, mechanical advantage calculations, and thermodynamic efficiency problems.

Kinematics: Motion Without Forces

Kinematics describes the geometry of motion — position, velocity, acceleration, and time — without reference to the forces causing that motion. The four kinematic equations for constant acceleration provide a complete description of uniformly accelerated motion in one dimension.

Projectile motion — the two-dimensional motion of an object launched at an angle with only gravity acting on it — is the superposition of constant horizontal velocity and vertical free-fall. The range R = (v₀² × sin 2θ) / g, where v₀ is the launch speed, θ is the launch angle, and g = 9.81 m/s² is gravitational acceleration. Maximum range occurs at θ = 45° in the absence of air resistance.

Circular motion involves constant-speed motion along a circular path, requiring centripetal acceleration directed toward the center: a = v²/r, where v is the tangential speed and r is the radius. The centripetal force F = mv²/r must be provided by some agent — gravity for orbital motion, tension for a ball on a string, friction for a car navigating a curve.

Kinematic Equations (Constant Acceleration)

v = v₀ + at | x = v₀t + ½at² | v² = v₀² + 2ax | x = ½(v₀ + v)t

Where:

  • v₀= Initial velocity (m/s)
  • v= Final velocity (m/s)
  • a= Acceleration (m/s²)
  • t= Time (s)
  • x= Displacement (m)

Forces, Energy, and Work

Newton's second law, F = ma, relates the net force on an object to its mass and the resulting acceleration. Forces are vectors — they have both magnitude and direction — and must be added vectorially. When multiple forces act on an object, only the net (resultant) force determines the acceleration.

Work is the transfer of energy by a force: W = F × d × cos θ, where θ is the angle between the force and displacement vectors. Positive work transfers energy to the object; negative work removes energy. The work-energy theorem states that the net work done on an object equals its change in kinetic energy: W_net = ΔKE = ½mv² − ½mv₀².

Conservation of energy: in an isolated system, total mechanical energy (KE + PE) is conserved when only conservative forces act. When an object falls a height h: the loss in gravitational PE equals the gain in KE: mgh = ½mv² (ignoring air resistance), giving v = √(2gh). This is valid regardless of the path taken — energy conservation is path-independent for conservative forces.

Momentum and Collisions

Linear momentum p = mv is the product of mass and velocity. Newton's second law in its most general form is: F_net = dp/dt (the net force equals the rate of change of momentum). The impulse-momentum theorem states that the impulse (force × time) equals the change in momentum: J = FΔt = Δp = mΔv.

Conservation of momentum applies when the net external force on a system is zero: the total momentum before a collision equals the total momentum after. In elastic collisions, both momentum and kinetic energy are conserved. In perfectly inelastic collisions, the objects stick together (maximum kinetic energy lost while momentum is conserved). In partially inelastic collisions, some energy is lost to deformation, heat, and sound.

Electricity and Electromagnetism

Electric charge is the source of electric and magnetic fields. Coulomb's law describes the force between two point charges: F = k × q₁q₂/r², where k = 8.99 × 10⁹ N·m²/C² is Coulomb's constant. Like charges repel; unlike charges attract. The force falls off as the square of the distance.

Electric potential energy and voltage (electric potential) describe the energy landscape for charges. A charge q in an electric field experiences force F = qE, and potential energy U = qV. Electric current I = charge/time (amperes), voltage V = energy/charge (volts), and resistance R = V/I (ohms, Ohm's Law). Power P = IV = I²R = V²/R (watts).

Magnetic fields are produced by moving charges (current) and affect moving charges. The force on a charge q moving at velocity v in a magnetic field B is F = qv × B (the cross product gives force perpendicular to both velocity and field). Faraday's law of induction states that a changing magnetic flux through a loop induces an EMF (voltage) proportional to the rate of change.

Worked Examples

Projectile Range Calculation

Solution Steps:

  1. 1A ball is launched at 25 m/s at 35° above horizontal. Find the range (horizontal distance traveled).
  2. 2Horizontal velocity: vₓ = 25 × cos(35°) = 25 × 0.8192 = 20.48 m/s.
  3. 3Vertical initial velocity: vy₀ = 25 × sin(35°) = 25 × 0.5736 = 14.34 m/s.
  4. 4Time in air: 2 × vy₀/g = 2 × 14.34/9.81 = 2.924 s. Range = vₓ × t = 20.48 × 2.924 = 59.9 m. Using the range formula: R = (25² × sin(70°)) / 9.81 = (625 × 0.9397) / 9.81 = 59.9 m ✓.

Conservation of Momentum in a Collision

Solution Steps:

  1. 1Cart A (2 kg) moves at 4 m/s east. Cart B (3 kg) is stationary. They undergo a perfectly inelastic collision (stick together). Find the final velocity.
  2. 2Initial momentum = m_A × v_A + m_B × v_B = 2 × 4 + 3 × 0 = 8 kg·m/s.
  3. 3After collision, combined mass = 2 + 3 = 5 kg. By conservation of momentum: 5 × v_final = 8.
  4. 4v_final = 8/5 = 1.6 m/s east. Initial KE = ½ × 2 × 4² = 16 J. Final KE = ½ × 5 × 1.6² = 6.4 J. Energy lost = 9.6 J (converted to heat, sound, deformation).

Energy Stored in a Compressed Spring

Solution Steps:

  1. 1A spring with k = 500 N/m is compressed 0.15 m (15 cm). Find the potential energy stored and the speed of a 0.2 kg mass when released.
  2. 2Elastic PE = ½ × k × x² = ½ × 500 × (0.15)² = ½ × 500 × 0.0225 = 5.625 J.
  3. 3By conservation of energy, all PE converts to KE: ½mv² = 5.625 J.
  4. 4v² = 2 × 5.625 / 0.2 = 56.25. v = √56.25 = 7.5 m/s. (Friction and air resistance neglected.)

Tips & Best Practices

  • Always draw a free body diagram before applying Newton's laws — visualizing all forces prevents missing forces and incorrect sign conventions.
  • Choose a coordinate system that aligns with the expected motion — putting the x-axis along the direction of motion simplifies the math significantly.
  • In problems with energy conservation, identify where all mechanical energy is at the start and end — any 'missing' energy was converted to heat or internal energy.
  • Double-check units throughout your calculation — most physics calculation errors are either sign errors or unit errors.
  • When a problem involves gravity near Earth's surface, use g = 9.81 m/s² unless told otherwise; for rough estimates, g ≈ 10 m/s² is often convenient.
  • In momentum problems, treat momentum as a vector — you must conserve momentum in EACH direction independently for 2D and 3D problems.
  • Centripetal acceleration always points toward the center of the circular path — the centripetal force is whatever physical force provides this (gravity, tension, normal force, friction).
  • The work done by static friction is zero (no displacement) — friction only does work when there IS relative motion (kinetic friction) or when a surface moves with the object.

Frequently Asked Questions

Speed is a scalar quantity — it has magnitude only. Velocity is a vector quantity — it has both magnitude and direction. A car moving at 60 mph northward has speed = 60 mph and velocity = 60 mph north. When a car rounds a curve at constant speed, its speed is unchanged but its velocity is changing (direction is changing), so there is acceleration even though the speedometer reading is constant. Net force causes changes in velocity (acceleration), not changes in speed alone.
In an elastic collision, both momentum AND kinetic energy are conserved. Billiard balls, atomic collisions, and elastic rubber balls approximately follow this model. In an inelastic collision, momentum is conserved but some kinetic energy is converted to internal energy (heat, sound, deformation). Perfectly inelastic collisions result in the objects sticking together — maximum possible kinetic energy loss while still conserving momentum. No macroscopic collision is perfectly elastic; atomic collisions between like atoms can be.
Mass is an intrinsic property of an object — a measure of its inertia (resistance to acceleration) and its gravitational interaction. Mass is measured in kilograms and doesn't change with location. Weight is the gravitational force on an object: W = mg, where g is the local gravitational field strength (9.81 m/s² on Earth's surface, 1.62 m/s² on the Moon). An astronaut with a mass of 80 kg has a weight of 785 N on Earth, 130 N on the Moon, and 0 N in deep space — but their mass is 80 kg everywhere.
Gravitational PE is the energy an object has due to its position in a gravitational field: U = mgh, where m is mass, g is gravitational acceleration (9.81 m/s² near Earth's surface), and h is height above the reference level. The choice of reference level (h=0) is arbitrary — only changes in PE (ΔU = mgΔh) are physically meaningful. When an object falls from height h to the ground, it loses PE = mgh, which converts entirely to KE (kinetic energy) in the absence of friction: ½mv² = mgh, so v = √(2gh).
Pressure is force per unit area: P = F/A (in pascals, Pa = N/m²). The same force applied over a smaller area creates greater pressure. This is why a sharp knife cuts better than a dull one (same force, smaller contact area, higher pressure) and why snowshoes distribute weight to avoid sinking. Atmospheric pressure at sea level is approximately 101,325 Pa = 14.7 psi = 1 atm. Gauge pressure measures above atmospheric; absolute pressure includes atmospheric.
In vacuum (without air resistance), all objects fall with the same acceleration regardless of mass — approximately 9.81 m/s² near Earth's surface. This is because the gravitational force is proportional to mass (F = mg), and Newton's second law gives acceleration a = F/m = g. The mass cancels, leaving a constant acceleration for all masses. Galileo demonstrated this experimentally (the Leaning Tower of Pisa legend). Air resistance differs for different objects — a feather and a hammer fall at different rates in air but identically in vacuum (as NASA demonstrated on the Moon).

Sources & References

Last updated: 2026-06-15

💡

Help us improve!

How would you rate the Physics Calculators?