Notes for PHYS 7B: Basic Physics II, covering topics such as gravitation, oscillations, and wave motion.
Tue, Mar 31, 2026 11 min read
PHYS 7B: Basic Physics II
Gravitation
Universal Law of Gravitation:
FG=Gr2m1m2
where G≈6.67×10−11N⋅m2/kg2 is the gravitational constant.
Gravitational Field:
g=mFG=Gr2M
Satellite Motion
For a satellite in circular orbit around a planet:
FG=rmv2=Gr2Mm
which leads to the orbital velocity:
v=rGM
aR=rv2=r2GM=g is the centripetal acceleration, which is equal to the gravitational acceleration at that radius.
The period of the satellite is:
T=v2πr=2πGMr3
This is known as Kepler's Third Law.
Escape Velocity
The escape velocity from a planet is the minimum velocity needed for an object to escape the gravitational pull of the planet without further propulsion:
vesc=R2GM
where R is the radius of the planet.
Gravitational Potential Energy
The work against gravity to move a mass m from a distance r1 to r2 is given by:
W=∫r1r2FGdr=∫r1r2Gr2Mmdr=GMm(r21−r11)
The gravitational potential energy at a distance r from a mass M is, where U(∞)=0:
U(r)=−GrMm
The negative sign indicates that the potential energy is lower (more negative) when the masses are closer together, reflecting the attractive nature of gravity. The potential energy approaches zero as r approaches infinity, which means that it takes an infinite amount of energy to separate the masses completely.
Geostationary Orbits
A geostationary orbit is a circular orbit around the Earth where the satellite's orbital period matches the Earth's rotation period (24 hours). The radius of a geostationary orbit can be found using Kepler's Third Law:
T2=GM4π2R3R3=4π2GMT2
Oscillations
Simple Harmonic Oscillator
Hooke's Law: Fs=−kx where k is the spring constant and x is the displacement from equilibrium.
F−kxdt2d2x+mkxω=ma=mdt2d2x=0=mk
The general solution to the equation of motion is:
x(t)=Acos(ωt+ϕ)
where A is the amplitude, ω is the angular frequency, and ϕ is the phase constant determined by initial conditions.
Period: T=ω2π=2πkm.
The total energy of the system is conserved and given by:
E=21mv2+21kx2=21kA2
Thus, x2+(ωv)2=A2.
where L is the length of the pendulum and g is the acceleration due to gravity.
The period is: T=2πgL
Physical Pendulum
For a physical pendulum, the moment of inertia I and the distance d from the pivot to the center of mass are used:
τ−mgdsinθdt2d2θ+Imgdθω=Iα=Idt2d2θ=0=Imgd
The period is: T=2πmgdI
Wave Motion
Mechanical waves: disturbances that propagate through a medium, transferring energy without transferring matter.
Longitudinal waves: particles of the medium oscillate parallel to the direction of wave propagation (e.g., sound waves). Transverse waves: particles of the medium oscillate perpendicular to the direction of wave propagation (e.g., waves on a string).
Sinusoidal Wave
Crest: the highest point of the wave.
Trough: the lowest point of the wave.
Amplitude (A): the maximum displacement of the wave from its equilibrium position. (the height of the crest or trough)
Wavelength (λ): the distance between two consecutive crests or troughs.
Frequency (f): the number of oscillations per unit time.
Period (T): the time it takes for one complete oscillation, T=f1.
Angular frequency (ω): the temporal frequency of the wave, ω=2πf=T2π.
Wave speed (v): the speed at which the wave propagates through the medium, v=λf=Tλ=kω.
Wave number (k): the spatial frequency, k=λ2π=vω.
Snapshot
y(x)=Asin(kx+ϕ)
Traveling wave
y(x,t)=Asin(kx−ωt+ϕ)
Classical Wave Equation
∂x2∂2y=v21∂t2∂2yy is the wave function, x is the spatial coordinate, t is time, and v is the wave speed. The left-hand side represents the spatial curvature of the wave, while the right-hand side represents the temporal curvature.
Transverse Waves on a String
The wave speed on a string is given by:
v=μF
where F is the tension force in the string and μ=dxdm is the linear mass density.
v=λf=Tλ
Coexisting Waves
Principle of superposition: when two or more waves overlap, the resulting wave is the sum of the individual waves.
Constructive interference: when waves are in phase, their amplitudes add up, resulting in a larger amplitude.
Destructive interference: when waves are out of phase, their amplitudes subtract, resulting in a smaller amplitude or complete cancellation.
Wave Boundary
Fixed boundary: the wave is reflected and inverted (phase change of π).
Free boundary: the wave is reflected without inversion (no phase change).
Standing Waves
Incident wave: yi(x,t)=Acos(kx−ωt)
Reflected wave: yr(x,t)=−Acos(kx+ωt)
Resulting wave: y(x,t)=2Asin(kx)sin(ωt)
2Asin(kx) is the amplitude of the standing wave, which varies with position x. The time-dependent part sin(ωt) oscillates between -1 and 1, but the spatial part determines where the nodes and antinodes are located.
Nodes: points where the amplitude is always zero (destructive interference).
Antinodes: points where the amplitude is maximum (constructive interference).
The distance between adjacent nodes or antinodes is 2λ, and the distance between a node and the nearest antinode is 4λ.
Vibrating String
Fundamental Mode: n=1, λ1=2L, f1=2Lv
For a string fixed at both ends, the allowed wavelengths are:
λn=n2L
where L is the length of the string and n is a positive integer (the mode number). The corresponding frequencies are:
fn=λnv=2Lnv
where v is the wave speed on the string. The fundamental frequency (first harmonic) corresponds to n=1, the second harmonic corresponds to n=2, and so on. Each mode of vibration produces a standing wave pattern with n−1 nodes between the fixed ends.
The electric field E at a point in space is defined as the force F experienced by a positive test charge q placed at that point, divided by the magnitude of the test charge:
E=qF
The electric field due to a point charge Q at a distance r is given by:
E=kr2Qr^
Continuous charge distribution
E=k∫r2dqr^
Line charge distribution: dq=λdx, E=r2kλr^ where r is the distance from the line charge to the point.
Ring charge distribution: dq=λdl, E=(x2+R2)3/2kxQx^ where R is the radius of the ring and x is the distance from the center of the ring along the axis perpendicular to the plane of the ring.
Disk charge distribution: dq=σdA=σ2πrdr, E=2ϵ0σ(1−x2+R2x)x^ where R is the radius of the disk.
For R≫x, E≈2ϵ0σx^ (infinite plane approximation).
Surface charge distribution: dq=σdA, E=2ϵ0σn^
E=∫r2kdqr^=kσ∫r2dAn^=kσ4πn^=2ϵ0σn^ where n^ is the unit normal vector to the surface.
Volume charge distribution: dq=ρdV, E=3ϵ0ρr^
Field Lines
The direction of the electric field at any point is tangent to the field line at that point.
The magnitude of the electric field is proportional to the density of the field lines: the closer the field lines are to each other, the stronger the electric field at that point.
Field lines begin on positive charges and end on negative charges.
Field lines never cross each other.
Electric Dipole
An electric dipole consists of two equal and opposite charges separated by a distance d. The dipole moment p is defined as:
p=qd
Direction: from the negative charge to the positive charge.
Torque
τ=p×E
Potential energy
U=−p⋅E
Electric Flux
The electric flux ΦE through a surface is defined as the total electric field passing through that surface:
ΦE=E⊥A=EAcosϕ=E⋅AΦE=∫E⋅dA
where E⊥ is the component of the electric field perpendicular to the surface, A is the area of the surface, and ϕ is the angle between the electric field and the normal to the surface.
Gauss's Law
ΦE=∮E⋅dA=ϵ0Qenc
where Qenc is the total charge enclosed within the Gaussian surface.
For a point charge Q at the center of a spherical Gaussian surface of radius r:
ΦE=E⋅4πr2=ϵ0Q⟹E=kr2Q
For a charged insulating sphere with total charge Q and radius R:
For r<R: Qenc=R3Qr3, E=kR3Qr=4πϵ01R3Qr
For r≥R: Qenc=Q, E=kr2Q=4πϵ01r2Q
For a charged conducting sphere with total charge Q and radius R:
Multiple point charge sources: V=k∑riqi.
Continuous charge distribution: V=k∫rdq.
For a charged conducting sphere
outside the sphere, the potential is the same as if all the charge were concentrated at the center
inside the sphere, the potential is constant and equal to the potential at the surface.
For a charged insulating sphere
outside the sphere, the potential is the same as if all the charge were concentrated at the center
inside the sphere, the potential is given by V=k2R3Q(3R2−r2).
Electric field lines point from higher potential to lower potential.
Capacitance
Capacitor: two conductors separated by an insulating material (air).
Capacitance is the ability to store electrical charge.
C=VQ=EdQ=dϵ0A
units: 1F (farad)=1C/V.
Spherical capacitor: C=4πϵ0rb−rararb where ra and rb are the radii of the inner and outer spheres, respectively.
Capacitors in series: Ceq1=∑Ci1 (same charge)
Capacitors in parallel: Ceq=∑Ci (same voltage)
Energy stored in a capacitor:
U=∫0QVdQ=21CV2=21QV=21CQ2
Energy density in an electric field:
u=AdU=21ϵ0E2
Dielectrics
When the capacitor is filled with a dielectric material, the capacitance increases by a factor of the dielectric constant κ:
C′=κCE′=κEV′=κV
Electric Circuits
Electric Current
Electric current I is the rate of flow of electric charge:
I=dtdQ=nqAvd
where n is the number of charge carriers per unit volume, q is the charge of each carrier, A is the cross-sectional area of the conductor, and vd is the drift velocity of the charge carriers.
units: 1A (ampere)=1C/s.
Conventional current: positive charges would move, which is opposite to the actual flow of electrons.
Real current: the actual flow of electrons, from the negative terminal to the positive terminal.
Resistance
Ohm's Law:
R=IV=AρL
where ρ is the resistivity of the material, L is the length of the conductor, and A is the cross-sectional area.
units: 1Ω(ohm)=1V/A.
Resistivity of metals:
ρ=JE
where E is the electric field and J is the current density.
Resistors in series: Req=∑Ri (same current)
Resistors in parallel: Req1=∑Ri1 (same voltage)
Battery
Battery: a device that converts chemical energy into electrical energy, providing a potential difference (voltage) to drive current through a circuit.
Electromotive force (emf)E: the maximum potential difference provided by the battery when no current is flowing. Internal resistancer: the resistance within the battery that causes a voltage drop when current flows. Terminal voltageV: the actual voltage across the battery terminals when current is flowing, given by
V=E−Ir
Power
Power delivered by the battery:
P=IV=I(E−Ir)=IE−I2r
Power delivered to the resistor:
PR=IV=I2R=RV2
The first term IE represents the power supplied by the battery, while the second term I2r represents the power lost due to the internal resistance of the battery. The efficiency of the battery can be calculated as
Efficiency=PtotalPuseful=IEIE−I2r=1−EIr
Kirchhoff's Laws
Kirchhoff's Current Law (KCL): The total current entering a junction equals the total current leaving the junction.
Kirchhoff's Voltage Law (KVL): The sum of the potential differences around any closed loop in a circuit must equal zero.