Vectors have magnitude and direction, while scalars have magnitude only.
Distance is the length of the path taken between initial and final positions (scalar).
Displacement is the straight-line distance between initial and final positions (vector).
\Delta x=x_{f}-x_{i} , indicating the change in position along the x-axis.
Distance an object travels is greater than or equal to the magnitude of its displacement.
Average velocity equals displacement over change in time (vector).
\vec{v}_{avg} = \frac{\Delta \vec{x}}{\Delta t}
Average acceleration equals change in velocity over change in time (vector).
\vec{a}_{avg} = \frac{\Delta \vec{v}}{\Delta t}
Instantaneous velocity or acceleration is the value at a specific time.
Uniformly Accelerated Motion (UAM) equations (kinematics equations) apply when acceleration is constant.
There are 5 variables and 4 equations, knowing 3 variables allows solving for the other 2.
Slope of a position vs. time graph is velocity.
Slope of a velocity vs. time graph is acceleration.
Area between the curve and the time axis on a velocity vs. time graph is change in position.
Area between the curve and the horizontal time axis on an acceleration vs. time graph is change in velocity.
Area above the horizontal axis is positive, below is negative.
Vectors are broken into component vectors using sine and cosine trigonometric functions.
The angle theta isn't always measured from the horizontal, so x-component doesn't always use cosine.
Projectile motion occurs when the only force is gravity near the Earth's surface.
Acceleration in the y-direction: \vec{a}_y = -9.81 \frac{m}{s^2} (Use -10 \frac{m}{s^2} on AP exams).
UAM equations apply in the y-direction.
Acceleration in the x-direction is zero, so constant velocity applies in the x-direction.
Relative motion: Description of motion depends on the observer's frame of reference; often involves vector addition.
Center of mass equation:
Xcm=\frac{\sum\operatorname{mi}\cdot ri}{\sum mi}
Can replace position with velocity or acceleration.
Forces are vectors resulting from interactions between two objects.
Free Body Diagrams (FBDs) show all forces acting on an object.
Only force vectors are included in FBDs.
Forces start at the center of mass (offset slightly if multiple forces act in the same direction).
Never break forces into components in a free body diagram answer on an AP Physics exam.
The force normal (caused by a surface) is perpendicular to the surface, pushing away.
Tension in a rope is parallel to the rope, a pull.
Newton’s First Law (Law of Inertia): An object at rest stays at rest, and an object in motion stays in motion with a constant velocity, unless acted upon by a net, external force.
Inertia is the tendency to resist acceleration.
Newton’s Second Law: \vec{a} = \frac{\sum \vec{F}}{m} , relates net force, mass, and acceleration.
Translational equilibrium occurs when the net force on an object is zero, meaning the object is at rest or moving at a constant velocity.
Newton’s Third Law: For every force object one exerts on object two, object two exerts a force on object one that is equal in magnitude and opposite in direction, and these forces act simultaneously.
Gravitational force: F_g = mg , where g is the gravitational field strength.
The direction of the force of gravity on an object is always towards the center of mass of the planet; down.
Friction is parallel to the surface and opposes sliding motion, independent of the force applied.
Kinetic friction: F_{fk}=\mu_{k}F_{n} , occurs when surfaces are sliding relative to one another.
\mu_k (coefficient of kinetic friction) is dimensionless, non-negative, and experimentally determined.
Static friction: F_{fs}=\mu_{s}F_{n} , occurs when surfaces are not sliding relative to one another.
Static friction adjusts to prevent sliding.
Friction does not depend on the contact surface area.
Newton’s Law of Universal Gravitation: F_{g}=\frac{Gm1m2}{r^2} where G is the gravitational constant.
Gravitational force is directed along a line connecting the centers of mass, directed towards the other mass.
Local gravitational field (little g) is nearly constant on a planet's surface.
Ideal spring force (Hooke’s Law): F_{spring} = -kx, where k is the spring constant and x is the displacement from equilibrium.
The direction of the spring force is always toward equilibrium position.
The negative sign indicates that the spring force and displacement are opposite in direction.
The magnitude of the slope of a graph of spring force vs. displacement from equilibrium position is the spring constant k.
Tangential velocity: Linear velocity of an object moving along a circular path, directed perpendicularly to the radius and parallel to the path.
Centripetal acceleration: Acceleration directed inward toward the center of the circle.
a_c = \frac{v^2}{r}
Period (T): Time for one complete circle.
Frequency (f): Revolutions per second.
T = \frac{1}{f}
Centripetal force: Net force in the in-direction causing centripetal acceleration, not a new force, never in a free body diagram.
Translational kinetic energy: KE = \frac{1}{2}mv^2
Work: W = Fd \cos(\theta), amount of mechanical energy transferred into or out of a system.
Work done by a conservative force is path-independent (e.g., gravity, spring force).
Work done by a nonconservative force is path-dependent (e.g., friction, air resistance).
Mechanical energy types: kinetic, gravitational potential, and elastic potential energy.
Potential Energy: Energy stored in a system due to the positions of objects.
Change in gravitational potential energy: \Delta U_g = mg \Delta h .
General form for gravitational potential energy: U_{g}=-\frac{Gm1m2}{r^{}}
Elastic potential energy: U_{s}=\frac{1}{2}kx^2
Work and Energy are scalars.
A system with only one object can only have kinetic energy.
Energy changes are balanced by equivalent changes or energy transfer.
Total mechanical energy remains constant if zero net work is done and zero work is done by nonconservative forces.
When there is net work done on a system, energy is transferred between the system and its surroundings.
Work done by friction equals the change in mechanical energy of the system.
Work-energy principle: W_{net} = \Delta KE, always valid.
When using energy equations, identify the system, initial point, final point, and horizontal zero line.
Power: Rate at which energy changes with time.
Average power: P_{avg} = \frac{W}{\Delta t}
Instantaneous power: P = Fv \cos(\theta)
Linear momentum (vector): \vec{p} = m\vec{v}
During collisions and explosions, the net external force is negligibly small.
Newton’s Second Law in terms of momentum: \vec{F}_{net} = \frac{\Delta \vec{p}}{\Delta t}
Impulse (vector): \vec{J} = \Delta \vec{p} = \vec{F}_{avg} \Delta t
Impulse equals the area under a force vs. time curve.
\sum F=0\rightarrow J=0\rightarrow\Delta p=0\left(MOMENTUMREMAINSCONSTANT\right)
If the net force on a system is zero, the velocity of the center of mass is constant.
When the net force is nonzero, linear momentum is transferred between the system and the environment.
Types of collisions:
Elastic: Kinetic energy is conserved.
Inelastic: Kinetic energy decreases.
Perfectly inelastic: Objects stick together.
Most real-world collisions are inelastic.
Linear momentum is conserved in all collisions.
Angular displacement: \Delta\theta=\theta_{f}-\theta_{i}
1 \text{ revolution} = 360^\circ = 2\pi \text{ radians}
Average angular velocity: \omega_{avg} = \frac{\Delta \theta}{\Delta t}
Average angular acceleration: \alpha_{avg} = \frac{\Delta \omega}{\Delta t}
Rigid objects maintain shape; all points have the same angular displacement, velocity, and acceleration.
Uniformly Angularly Accelerated Motion (UAM) equations are analogous to UAM equations.
Slope of angular position vs. time is angular velocity.
Slope of angular velocity vs. time is angular acceleration.
Area under angular acceleration vs. time is change in angular velocity.
Area under angular velocity vs. time is change in angular position.
Arc length: s = r\theta
Tangential velocity: v_t = r \omega
Tangential acceleration: a_t = r \alpha
Radians are dimensionless, required for linear-rotational conversions.
Centripetal acceleration: a_{c}=\frac{v^2}{r}=r\omega^2
Accelerations in circular motion: angular, tangential, and centripetal.
Angular acceleration is an angular quantity (\frac{rad}{s^2}).
Tangential and centripetal accelerations are linear (\frac{m}{s^2}).
Tangential acceleration is tangent to the circular path, perpendicular to the radius.
Centripetal acceleration is perpendicular to the circular path, inward along the radius.
Tangential and centripetal acceleration are always perpendicular to one another.
Circular motion requires centripetal acceleration.
Tangential acceleration changes the magnitude of tangential velocity.
Centripetal acceleration changes the direction of tangential velocity.
Angular displacement, velocity, and acceleration describe the entire rotating object, while arc length, tangential velocity, tangential acceleration, and centripetal acceleration describe a specific location.
Torque: \tau = rF \sin(\theta), the ability of a force to cause angular acceleration.
r_{\perp} is the lever arm.
Use clockwise and counterclockwise to indicate torque direction in AP Physics 1.
Force diagrams are used to show where forces act on rigid objects.
Rotational inertia: I = mr^2 for a point particle, resistance to angular acceleration.
Rotational inertia of a system is the sum of individual rotational inertias.
Equations for rotational inertia of rigid objects with shape are provided on the exam.
Parallel Axis Theorem: I = I_{CM} + md^2
Rotational equilibrium means constant angular velocity.
Newton’s First Law in Rotational Form: An object at rest remains at rest, and a rotating object maintains a constant angular velocity, unless acted upon by a net external torque or the distribution of the mass of the object changes.
Newton’s Second Law in rotational form: \tau_{net} = I\alpha
Static equilibrium: Both translational and rotational equilibrium; net torque about any axis is zero.
Translational Kinetic Energy: Objects whose center of mass is changing location have Translational Kinetic Energy.
Rotational Kinetic Energy: KE_{rot} = \frac{1}{2}I\omega^2
Total kinetic energy: KE{total} = KE{rot} + KE_{trans}
Work done by a torque: W = \tau \Delta \theta
Angular Momentum: L = I\omega
Angular Momentum of a Point Particle: L = rmv sin(\theta)
Rotational form of Newton’s Second Law: \tau_{net} = \frac{\Delta L}{\Delta t}
Angular impulse: J_{ang} = \Delta L = \tau \Delta t
Total angular momentum remains constant if the net torque is zero.
Rolling without slipping: Equations for displacement, velocity, and acceleration of the center of mass are related to circular motion equations.
v_{CM} = r\omega
Rolling with slipping invalidates the rolling without slipping equations.
Circular orbits: Total mechanical energy, gravitational potential energy, angular momentum, and kinetic energy are constant.
Elliptical orbits: Total mechanical energy and angular momentum are constant, but gravitational potential and kinetic energy are not.
Linear momentum does not remain constant. Angular momentum remains constant.
Escape velocity: Initial speed needed to reach infinite distance with zero final velocity.
Periodic motion repeats in equal time intervals.
Simple Harmonic Motion (SHM) results from a restoring force proportional to displacement from equilibrium.
Equilibrium position is where the net force is zero.
Restoring force is always directed towards equilibrium.
Period (T) is the time for one full cycle.
Amplitude (A) is the maximum distance from equilibrium.
Mass-spring system positions:
Position 1 (max displacement): displacement = A, velocity = 0, force and acceleration are max and directed left.
Position 2 (equilibrium): displacement = 0, velocity is max, force and acceleration = 0.
Position 3 (max negative displacement): displacement = -A, velocity = 0, force and acceleration are max and directed right.
Period of a mass-spring system: T = 2\pi \sqrt{\frac{m}{k}}
Restoring force is the spring force.
Period of a simple pendulum: T = 2\pi \sqrt{\frac{L}{g}}(for \theta < 15^\circ).
Restoring force is the component of gravity tangent to the motion.
Frequency is the number of cycles per second.
Position in SHM: x = A \cos(2\pi f t)
Cosine and sine are phase-shifted by 90^\circ
Total mechanical energy in SHM is constant: E = KE + PE
Total energy of a mass-spring system: E = \frac{1}{2}kA^2 = \frac{1}{2}mv_{max}^2
Density: \rho = \frac{m}{V}
Pressure: P = \frac{F}{A}
Absolute pressure: P_{abs}=P_0+\varrho gh
Gauge pressure: P_{gauge} = \rho g h, independent of container's cross-sectional area.
Buoyant force: F_{B}=\varrho Vg
Continuity equation:A_1v_1=A_2v_2
Bernoulli’s equation: P_1+\frac12\varrho v_{1^{}}^2+\varrho gy_1=P_2+\frac12\varrho v_2^2+\varrho gy_2
Bernoulli’s Principle: If fluid speed increases, fluid pressure decreases (assuming height is negligible).
Torricelli’s Theorem: v = \sqrt{2gh}