2 Force and Translational Dynamics
- Syllabus
- 2024
- Section
- 2
- Level
- —
A system is the object or collection of objects chosen for analysis. Draw an imaginary boundary around it: objects inside are the system's constituent parts; everything outside is the environment. The system's properties depend on how its parts interact.
| Ask about the model | Inside the boundary | Across the boundary |
|---|---|---|
| What is tracked? | Parts and their internal interactions | Transfers between system and environment |
| What may change? | Parts may move or behave differently from one another | Energy or mass may enter or leave |
| Can details be ignored? | Yes, if internal structure does not affect the macroscopic behavior | No, if an external change alters the system's substructure or behavior |
Example: choose a cart plus the blocks fixed on it as one system. If the blocks remain fixed and their arrangement does not matter for the motion being studied, model the whole system as one object. If the blocks slide relative to the cart, the internal structure matters and the parts must be analyzed.
A system is not automatically isolated, rigid, or uniform. The boundary is a modeling choice. State what is inside it, identify relevant interactions, and reconsider the single-object model when external conditions change the system's substructure.
The center of mass is the position at which a system can be represented as one object for translational analysis. It is a mass-weighted location: larger masses pull the center of mass closer to themselves. In the formula below, mi is each particle's mass, xi is its signed position from the chosen origin, and ∑imi is the total mass.
xcm=∑imi∑imixi
Hypothetical example: a 2.0kg particle is at x=0m and a 3.0kg particle is at x=4.0m.
xcm=2.0kg+3.0kg(2.0kg)(0m)+(3.0kg)(4.0m)=2.4m.
The result lies between the particles and closer to the heavier 3.0kg particle, as expected.
For a symmetrical mass distribution, the center of mass lies on every applicable line of symmetry; it need not coincide with material. It is not generally the geometric midpoint. AP Physics 1 calculations are limited to five or fewer particles in a two-dimensional arrangement or to highly symmetrical systems.
A force is a vector that describes an interaction: one object or system exerts the force on another. Write FAonB to name both the source A and the target B; its direction tells how A pushes or pulls B.
| Interaction | Objects involved | What the force means |
|---|---|---|
| Contact | Book and table touching | The table exerts an upward contact force on the book |
| Noncontact | Earth and book | Earth exerts a downward gravitational force on the book |
| Internal to a chosen system | Two parts inside the boundary | Parts exert forces on each other, but the system does not exert a net force on itself |
At the macroscopic scale, normal force, friction and tension are contact interactions. Their microscopic origin is electromagnetic interaction between atoms, even when surfaces appear rigid.
A force is not something an isolated object 'has,' and motion does not require a force in the direction of motion. To validate a claimed force, identify the second interacting object and state who exerts what force on whom.
A free-body diagram (FBD) isolates one object or system and shows every external force exerted on it. Replace the chosen system by a dot at its center of mass; the completed diagram is the bridge from the physical situation to force equations.
| Step | AP-compliant action |
|---|---|
| 1. Isolate | Name exactly one object or system |
| 2. Inventory | For each interaction crossing its boundary, identify the force on the system |
| 3. Draw | Use one labeled straight arrow per force, starting at the center-of-mass dot |
| 4. Separate | Draw same-direction forces side by side, never overlapping |
| 5. Choose axes | Align an axis with acceleration when useful; on an incline, choose an axis parallel to the surface |
Example: for a block sliding on a rough incline, the FBD contains the gravitational force by Earth, the normal force by the surface, and—when applicable—the friction force by the surface. Choose axes parallel and perpendicular to the incline, then resolve forces algebraically after the FBD is drawn.
Do not draw velocity, acceleration, the path, or a force exerted by the chosen system on something else. AP Physics 1 expects individual forces—not their components—on the FBD. Components belong in the later algebra, not as extra arrows on the diagram.
When objects A and B interact, each exerts a force on the other at the same time. The forces have equal magnitude and opposite direction: FAonB=−FBonA. They are a pair because they come from the same interaction.
| Pair test | Must be true |
|---|---|
| Interaction | Both forces describe the same interaction |
| Objects | One force acts on A; the other acts on B |
| Magnitude | ∣FAonB∣=∣FBonA∣ |
| Direction | The force vectors point oppositely |
| Timing | Both forces exist simultaneously |
Example: a book rests on a table. The table's upward force on the book pairs with the book's downward force on the table. The book's weight is not that partner; it pairs with the book's gravitational force on Earth. Third-law partners do not cancel on the book because each pair member acts on a different object. If both objects are inside one chosen system, the internal pair cancels in the system force sum and does not change the system's center-of-mass motion.
| Model | Consequence for tension |
|---|---|
| Ideal string | Negligible mass, does not stretch, and has the same tension at all points |
| String or chain with mass | Tension may vary along its length; for a hanging chain it is greater nearer the top |
| Ideal pulley | Negligible mass and negligible axle friction; it rotates about an axle through its center of mass |
Equal-and-opposite arrows on the same object are not a third-law pair. They may instead be balanced forces from different interactions. AP Physics 1 treats tension in a massive string qualitatively, and its noncontact interactions at a distance are limited here to gravity.
The net force on a system is the vector sum of every external force exerted on it. Direction matters: forces pointing oppositely contribute opposite vector components.
i∑Fi=0
| Component test | What it tells you |
|---|---|
| ∑Fx=0 and ∑Fy=0 | The net-force vector is zero, so the system is in translational equilibrium |
| ∑Fx=0, ∑Fy=0 | Only the x component of velocity changes |
| ∑Fx=0, ∑Fy=0 | Only the y component of velocity changes |
Example: a crate moves right while the floor's upward normal force balances Earth's downward gravitational force. If a rightward pull is larger than the leftward resistive force, the vertical forces are balanced but the horizontal forces are not. The crate's vertical velocity stays constant while its horizontal velocity changes.
Zero net force does not mean zero velocity or no forces. It means velocity is constant: the system may remain at rest or keep moving at constant speed in a straight line. This statement is verified in an inertial reference frame; a frame that accelerates relative to an inertial frame is not inertial.
Forces are unbalanced when their vector sum is not zero. A system's center-of-mass velocity changes only when a nonzero net external force acts on the system.
asys=msys∑iFi=msysFnet
Worked example: choose right as positive. A 4.0kg cart has a 12N force right and a 4.0N force left.
Fnet=+12−4.0=+8.0N
a=mFnet=4.0kg+8.0N=+2.0m/s2.
The positive result means the cart's velocity changes by 2.0m/s toward the right each second.
| Change | Acceleration consequence |
|---|---|
| Double ∣Fnet∣ at fixed mass | Double ∣a∣ |
| Double msys at fixed net force | Halve ∣a∣ |
| Reverse Fnet | Reverse a |
Acceleration points with the net force, but velocity need not. If the cart is initially moving left while the net force points right, it first slows down. For a multi-object system, sum external forces and use the total system mass to describe the center-of-mass acceleration; internal forces do not enter that external-force sum.
Every pair of masses attracts. Each gravitational force acts along the line joining the systems' centers of mass, toward the other system.
∣Fg∣=Gr2m1m2
| Change | New gravitational-force magnitude |
|---|---|
| Double either mass | 2∣Fg∣ |
| Double both masses | 4∣Fg∣ |
| Double center-to-center distance r | ∣Fg∣/4 |
A gravitational field describes the force effect at each position without requiring a test object to remain there. For source mass M, ∣g∣=m∣Fg∣=Gr2M. Field strength has units N/kg; if gravity is the only force, its numerical value equals free-fall acceleration in m/s2.
The gravitational force from an astronomical body on a relatively small nearby object is its weight: Weight=Fg=mg. Mass is measured in kilograms; weight is a force measured in newtons. Here r is center-to-center distance, not the gap between surfaces.
Gravitational force can be treated as constant over a motion when the change in center-to-center distance is small enough that the resulting change in gravitational force is negligible for the analysis.
g≈10 N/kg≈10 m/s2near Earth’s surface
Example: for an object moving through a classroom-scale height near Earth's surface, its distance from Earth's center changes by a negligible fraction. Use one nearly constant g, so a fixed mass has nearly constant weight Fg=mg throughout that motion.
This is an approximation, not a universal rule. If the change in center-to-center distance is large enough that GM/r2 changes appreciably, calculate the changing field or force instead of using one constant g.
Your apparent weight is the magnitude of the normal force exerted on you by a supporting surface. Your gravitational force is Fg=mg; these are different forces and need not have equal magnitudes.
∑Fy=N−mg=may(upward positive)
| Vertical contact case | Apparent weight N |
|---|---|
| ay>0 | N>mg: you feel heavier |
| ay=0 | N=mg |
| ay<0 while contact remains | 0<N<mg: you feel lighter |
| Free fall | N=0: weightless |
Example: you and a freely falling elevator accelerate together under gravity alone. The floor no longer needs to push on you, so N=0 and your apparent weight is zero—even though gravity still acts and Fg=mg is not zero.
Weightlessness means zero support force, not zero gravity. The equivalence principle says that, using only local observations, an observer in a noninertial frame cannot distinguish apparent-weight effects from those produced by a gravitational field.
Inertial mass measures how strongly an object's motion resists changing during an interaction. For the same net force, a larger inertial mass produces a smaller acceleration.
Gravitational mass determines how strongly a system participates in gravitational attraction: it appears in the gravitational-force relationship between masses.
| Role | Revealed by | Relationship |
|---|---|---|
| Inertial mass mi | Response to net force | Fnet=mia |
| Gravitational mass mg | Strength of gravitational interaction | ∣Fg∣∝mg |
Experiments verify that inertial and gravitational mass are equivalent: for a given object, their measured values are equal. The roles remain conceptually distinct—one describes response to force, the other gravitational interaction—so equivalence is an empirical result, not merely a definition.
Kinetic friction acts when two surfaces in contact slide relative to each other. On each surface, it points opposite that surface's motion relative to the other surface.
∣Ff,k∣=μk∣Fn∣
| Quantity | Meaning |
|---|---|
| Fn | Perpendicular contact-force component, directed away from the surface |
| μk | Dimensionless coefficient set by the material pair |
| Ff,k | Friction magnitude; direction is chosen separately from relative sliding |
Worked example: a 5.0kg block slides on a horizontal surface with μk=0.20. With no vertical acceleration, Fn=mg=(5.0kg)(10m/s2)=50N. Therefore Ff,k=μkFn=(0.20)(50N)=10N, opposite the block's motion relative to the surface.
In this friction model, the force does not depend on the apparent contact area. Also, Fn is not automatically mg; determine it from forces perpendicular to the surface and the motion in that direction.
Static friction may act when contacting surfaces are not sliding relative to each other. It points in the direction needed to prevent the impending relative motion.
∣Ff,s∣≤μs∣Fn∣
Static friction self-adjusts from zero up to a maximum: Ff,s,max=μsFn. Below the threshold, solve for the friction actually required to prevent sliding; use the maximum only at impending slip.
Threshold example: a surface has Fn=50N and μs=0.40, so Ff,s,max=(0.40)(50N)=20N. A 12N horizontal push produces 12N of opposing static friction and no slip. A requested 25N exceeds the 20N limit, so static friction cannot prevent sliding.
Static friction is not always μsFn. Once the surfaces slide, switch to kinetic friction. For a given surface pair, μs is typically greater than μk, so the maximum static friction is typically greater than the kinetic-friction magnitude for the same normal force.
An ideal spring has negligible mass. Its force is proportional to the change in length Δx measured from its relaxed length.
Fs=−kΔx
| Spring change | Displacement sign | Spring-force direction |
|---|---|---|
| Stretched to the right | Δx>0 | Fs<0: left, back toward equilibrium |
| Compressed to the left | Δx<0 | Fs>0: right, back toward equilibrium |
| Relaxed | Δx=0 | Fs=0 |
Worked example: take right as positive. A spring with k=200N/m is stretched Δx=+0.030m.
Fs=−kΔx=−(200N/m)(+0.030m)=−6.0N.
The spring exerts a 6.0N force to the left, toward equilibrium.
The minus sign gives direction; force magnitude is ∣Fs∣=k∣Δx∣. The spring constant k has units N/m and measures stiffness. Hooke's law is the ideal linear model: doubling the displacement doubles the force magnitude within that model.
At any point on the circle:
For radius r and tangential speed v, ac=rv2. In uniform circular motion, at=0 even though ac=0. One revolution takes period T and frequency is revolutions per second: T=f1 and T=v2πr.
There is no new force called 'centripetal force.' The inward net component of real forces satisfies ∑Finward=mac. Gravity can supply it alone; normal force and static friction components can supply it on a banked path; a tension component supplies it for a conical pendulum.
Top-of-loop threshold: at the minimum speed that maintains contact, the contact force has just fallen to zero, so gravity alone supplies the inward force: mg=mrv2. Therefore vmin=gr. Below this speed, the required inward force would exceed what gravity provides at that point, so contact cannot be maintained.
Constant speed does not mean zero acceleration in a circle because velocity direction keeps changing. For banked curves, AP Physics 1 expects quantitative analysis only when no friction is required for uniform circular motion; friction-required banked curves are analyzed qualitatively.
For a satellite of mass m in a circular orbit of radius R around a central mass M, gravitational attraction supplies the entire inward force. Orbit radius is measured from the central body's center of mass.
GR2Mm=mRv2 and v=T2πR. Substitution cancels the satellite mass and gives Kepler's third-law form for a circular orbit: T2=GM4π2R3.
| Comparison | Consequence |
|---|---|
| Same M: R increases by factor q | T increases by q3/2 |
| Same R: M increases by factor q | T decreases by q |
| Satellite mass m changes | Circular-orbit period at the same R is unchanged |
Ratio example: around the same central body, if orbit B has RB=4RA, then TATB=(RARB)3/2=43/2=8. The farther circular orbit takes eight times as long. AP Physics 1 does not require Kepler's first or second laws; keep this derivation to circular orbits.