AP Physics

Unit 4 - Energy

Beginner

Conceptual

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Step Derivation/Formula Reasoning
1 \[v_{\text{esc,E}} = \sqrt{\frac{2 G M_E}{R_E}}\] To leave Earth, a spacecraft must at least reach the Earth escape velocity, given by the standard gravitational formula with mass \(M_E\) and radius \(R_E\).
2 \[E_{\text{esc,E}} = \frac{1}{2} v_{\text{esc,E}}^{2} = \frac{G M_E}{R_E}\] Escape energy per unit mass from Earth equals the gravitational potential energy that must be overcome, \(G M_E / R_E\).
3 \[v_{\text{esc,M}} = \sqrt{\frac{2 G M_M}{R_M}}\] Analogous expression for escaping the Moon’s weaker gravitational field with mass \(M_M\) and radius \(R_M\).
4 \[E_{\text{esc,M}} = \frac{1}{2} v_{\text{esc,M}}^{2} = \frac{G M_M}{R_M}\] Escape energy per unit mass from the Moon.
5 \[\frac{E_{\text{esc,E}}}{E_{\text{esc,M}}} = \frac{M_E / R_E}{M_M / R_M} \approx 22\] Substituting numerical values \(M_E = 5.97\times10^{24}\,\text{kg},\, R_E = 6.37\times10^{6}\,\text{m},\, M_M = 7.35\times10^{22}\,\text{kg},\, R_M = 1.74\times10^{6}\,\text{m}\) shows Earth’s gravity well is about \(22\) times deeper than the Moon’s.
6 \[\Delta v_{\text{out}} \gg \Delta v_{\text{return}}\] The outbound leg (Earth \(\to\) Moon) needs a much larger total \(\Delta v\) to climb out of Earth’s gravity well than the return leg needs to leave the Moon’s weaker gravity.
7 \[F_{\text{atm}} \text{ assists on return}\] On the way back, Earth’s atmosphere provides free braking (aerodynamic drag and heating), so less propellant is required for deceleration; launch from Earth, however, must fight this same atmosphere, costing extra fuel.
8 \[m_{\text{fuel,out}} > m_{\text{fuel,ret}}\] Because the larger \(\Delta v\) and atmospheric losses occur on departure from Earth, the mass of propellant needed going to the Moon is substantially greater than that needed to come home.

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\(\text{More fuel is required because a spacecraft must overcome Earth’s far deeper gravitational potential and atmospheric drag, whereas leaving the Moon needs far less }\Delta v\text{ and Earth’s atmosphere assists braking on return.}\)

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KinematicsForces
\(\Delta x = v_i t + \frac{1}{2} at^2\)\(F = ma\)
\(v = v_i + at\)\(F_g = \frac{G m_1 m_2}{r^2}\)
\(v^2 = v_i^2 + 2a \Delta x\)\(f = \mu N\)
\(\Delta x = \frac{v_i + v}{2} t\)\(F_s =-kx\)
\(v^2 = v_f^2 \,-\, 2a \Delta x\) 
Circular MotionEnergy
\(F_c = \frac{mv^2}{r}\)\(KE = \frac{1}{2} mv^2\)
\(a_c = \frac{v^2}{r}\)\(PE = mgh\)
\(T = 2\pi \sqrt{\frac{r}{g}}\)\(KE_i + PE_i = KE_f + PE_f\)
 \(W = Fd \cos\theta\)
MomentumTorque and Rotations
\(p = mv\)\(\tau = r \cdot F \cdot \sin(\theta)\)
\(J = \Delta p\)\(I = \sum mr^2\)
\(p_i = p_f\)\(L = I \cdot \omega\)
Simple Harmonic MotionFluids
\(F = -kx\)\(P = \frac{F}{A}\)
\(T = 2\pi \sqrt{\frac{l}{g}}\)\(P_{\text{total}} = P_{\text{atm}} + \rho gh\)
\(T = 2\pi \sqrt{\frac{m}{k}}\)\(Q = Av\)
\(x(t) = A \cos(\omega t + \phi)\)\(F_b = \rho V g\)
\(a = -\omega^2 x\)\(A_1v_1 = A_2v_2\)
ConstantDescription
[katex]g[/katex]Acceleration due to gravity, typically [katex]9.8 , \text{m/s}^2[/katex] on Earth’s surface
[katex]G[/katex]Universal Gravitational Constant, [katex]6.674 \times 10^{-11} , \text{N} \cdot \text{m}^2/\text{kg}^2[/katex]
[katex]\mu_k[/katex] and [katex]\mu_s[/katex]Coefficients of kinetic ([katex]\mu_k[/katex]) and static ([katex]\mu_s[/katex]) friction, dimensionless. Static friction ([katex]\mu_s[/katex]) is usually greater than kinetic friction ([katex]\mu_k[/katex]) as it resists the start of motion.
[katex]k[/katex]Spring constant, in [katex]\text{N/m}[/katex]
[katex] M_E = 5.972 \times 10^{24} , \text{kg} [/katex]Mass of the Earth
[katex] M_M = 7.348 \times 10^{22} , \text{kg} [/katex]Mass of the Moon
[katex] M_M = 1.989 \times 10^{30} , \text{kg} [/katex]Mass of the Sun
VariableSI Unit
[katex]s[/katex] (Displacement)[katex]\text{meters (m)}[/katex]
[katex]v[/katex] (Velocity)[katex]\text{meters per second (m/s)}[/katex]
[katex]a[/katex] (Acceleration)[katex]\text{meters per second squared (m/s}^2\text{)}[/katex]
[katex]t[/katex] (Time)[katex]\text{seconds (s)}[/katex]
[katex]m[/katex] (Mass)[katex]\text{kilograms (kg)}[/katex]
VariableDerived SI Unit
[katex]F[/katex] (Force)[katex]\text{newtons (N)}[/katex]
[katex]E[/katex], [katex]PE[/katex], [katex]KE[/katex] (Energy, Potential Energy, Kinetic Energy)[katex]\text{joules (J)}[/katex]
[katex]P[/katex] (Power)[katex]\text{watts (W)}[/katex]
[katex]p[/katex] (Momentum)[katex]\text{kilogram meters per second (kgm/s)}[/katex]
[katex]\omega[/katex] (Angular Velocity)[katex]\text{radians per second (rad/s)}[/katex]
[katex]\tau[/katex] (Torque)[katex]\text{newton meters (Nm)}[/katex]
[katex]I[/katex] (Moment of Inertia)[katex]\text{kilogram meter squared (kgm}^2\text{)}[/katex]
[katex]f[/katex] (Frequency)[katex]\text{hertz (Hz)}[/katex]

General Metric Conversion Chart

Example of using unit analysis: Convert 5 kilometers to millimeters. 

  1. Start with the given measurement: [katex]\text{5 km}[/katex]

  2. Use the conversion factors for kilometers to meters and meters to millimeters: [katex]\text{5 km} \times \frac{10^3 \, \text{m}}{1 \, \text{km}} \times \frac{10^3 \, \text{mm}}{1 \, \text{m}}[/katex]

  3. Perform the multiplication: [katex]\text{5 km} \times \frac{10^3 \, \text{m}}{1 \, \text{km}} \times \frac{10^3 \, \text{mm}}{1 \, \text{m}} = 5 \times 10^3 \times 10^3 \, \text{mm}[/katex]

  4. Simplify to get the final answer: [katex]\boxed{5 \times 10^6 \, \text{mm}}[/katex]

Prefix

Symbol

Power of Ten

Equivalent

Pico-

p

[katex]10^{-12}[/katex]

Nano-

n

[katex]10^{-9}[/katex]

Micro-

µ

[katex]10^{-6}[/katex]

Milli-

m

[katex]10^{-3}[/katex]

Centi-

c

[katex]10^{-2}[/katex]

Deci-

d

[katex]10^{-1}[/katex]

(Base unit)

[katex]10^{0}[/katex]

Deca- or Deka-

da

[katex]10^{1}[/katex]

Hecto-

h

[katex]10^{2}[/katex]

Kilo-

k

[katex]10^{3}[/katex]

Mega-

M

[katex]10^{6}[/katex]

Giga-

G

[katex]10^{9}[/katex]

Tera-

T

[katex]10^{12}[/katex]

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