Physics 207 – Lecture 19 Review for the third test Physics 207: Lecture 19, Pg 1 Chapter 14, SHM k -A 0(≡Xeq ) T=2π (m/k)½ T=2π (L/g)½ for pendulum m A The general solution is: x(t) = A cos ( ωt + φ) with ω = (k/m)½ and ω = 2π f = 2π /T T = 2π/ω A -A Physics 207: Lecture 19, Pg 2 Page Physics 207 – Lecture 19 Energy of the Spring-Mass System x(t) = A cos( ωt + φ ) v(t) = -ωA sin( ωt + φ ) a(t) = -ω2A cos( ωt + φ ) Potential energy of the spring is U = ½ k x2 = ½ k A2 cos2(ωt + φ) The Kinetic energy is K = ½ mv2= ½ k A2 sin2(ωt+φ) E = ½ kA2 U~cos2 K~sin2 Physics 207: Lecture 19, Pg 3 Damped oscillations lFor small drag (under-damped) one gets: x(t) = A exp(-bt/2m) cos (ωt + φ) x(t) 1.2 1 0.8 0.6 0.4 A 0.2 0 -0.2 -0.4 -0.6 -0.8 -1 ωt t Physics 207: Lecture 19, Pg 4 Page Physics 207 – Lecture 19 Exercise x (m) 0.1 2 1 4 3 t (s) -0.1 l What are the amplitude, frequency, and phase of the oscillation? x(t) = A cos ( ωt + φ) A=0.1 m T=2 sec f=1/T=0.5 Hz ω = 2π f = π rad/s φ=π rad Physics 207: Lecture 19, Pg 5 Chapter 15, fluids Pressure=P0 F=P0A+Mg P0A P=P0+ρgy y Area=A Physics 207: Lecture 19, Pg 6 Page Physics 207 – Lecture 19 Pressure vs. Depth l In a connected liquid, the pressure is the same at all points through a horizontal line. p Physics 207: Lecture 19, Pg 7 Buoyancy y1 F2=P2 Area F1=P1 Area F2-F1=(P2-P1) Area =ρg(y2-y1) Area =ρ g Vobject =weight of the fluid displaced by the object F1 y2 F2 Physics 207: Lecture 19, Pg 8 Page Physics 207 – Lecture 19 Pascal’s Principle Any change in the pressure applied to an enclosed fluid is transmitted to every portion of the fluid and to the walls of the containing vessel. Hydraulics, a force amplifier F1 F2 P1 = P2 F1 / A1 = F2 / A2 d2 d1 A1 A2 / A1 = F2 / F1 A2 Physics 207: Lecture 19, Pg 9 Continuity equation A 2 A 1 v 1 v 2 A1v1 : units of m2 m/s = volume/s A2v2 : units of m2 m/s = volume/s A1v1=A2v2 Physics 207: Lecture 19, Pg 10 Page Physics 207 – Lecture 19 Energy conservation: Bernoulli’s eqn P1+1/2 ρ v12+ρgy1=P2+1/2 ρ v22+ρgy2 P+1/2 ρ v2+ρgy= constant Physics 207: Lecture 19, Pg 11 Chapter 16, Macroscopic description l Ideal gas law PV=nRT P V= N kB T n: # of moles N: # of particles Physics 207: Lecture 19, Pg 12 Page Physics 207 – Lecture 19 PV diagrams: Important processes l Isochoric process: V = const (aka isovolumetric) l Isobaric process: p = const l Isothermal process: T = const Isobaric Isothermal 1 p1V1 = p2V2 1 V1 V2 = T1 T2 Pressure p1 p 2 = T1 T2 Pressure Pressure Isochoric 2 1 2 2 Volume Volume Volume Physics 207: Lecture 19, Pg 13 Work done on a gas Pressure W= - the area under the P-V curve Pi final W = − ∫ PdV initial Vf nRT W =−∫ Pf Vi Vi V dV Vf 1 W = −nRT ∫ dV Vi V Vf W = −nRT ln Vi Vf Volume Physics 207: Lecture 19, Pg 14 Page Physics 207 – Lecture 19 Chapter 17, first law of Thermodynamics ΔU+ΔK+ΔEthermal=ΔEsystem=Wexternal+Q l For systems where there is no change in mechanical energy: ΔEthermal =Wexternal+Q Physics 207: Lecture 19, Pg 15 Pressure Exercise Pi i f Volume Vi 3Vi l What is the final temperature of the gas? l How much work is done on the gas? Physics 207: Lecture 19, Pg 16 Page Physics 207 – Lecture 19 Thermal Properties of Matter Physics 207: Lecture 19, Pg 17 Heat of transformation, specific heat l Latent heat of transformation L is the energy required for 1 kg of substance to undergo a phase change. (J / kg) Q = ±ML l Specific heat c of a substance is the energy required to raise the temperature of 1 kg by 1 K. (Units: J / K kg ) Q = M c ΔT Physics 207: Lecture 19, Pg 18 Page Physics 207 – Lecture 19 Specific heat for gases l For gases we typically use molar specific heat (Units: J / K mol ) Q = n C ΔT l For gases there is an additional complication. Since we can also change the temperature by doing work, the specific heat depends on the path. Q = n CV ΔT (temperature change at constant V) Q = n CP ΔT (temperature change at constant P) CP=CV+R Physics 207: Lecture 19, Pg 19 Page
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