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Material Type: Exam; Class: STELLAR STRCTR/EVOL; Subject: Physics; University: University of California - Santa Barbara; Term: Fall 2008;
Typology: Exams
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Department of Physics
2008 FALL STARS Professor Martin
Midterm Exam October 17, 2008
This exam is closed book. No calculators are allowed. Please turn off your cell phone before the exam begins. The last page includes constants and equations which may be useful. Please explain what you are doing with words as well as equations. It makes it much easier for us to follow your logic and give partial credit. The exam ends promptly at 2:50pm.
(a,2pts) Find the average pressure inside the star. (b,4pts) Calculate the central pressure in the star. (c, 2pts) Assume the required pressure is supplied by ionized hydrogen, i.e. by an ideal gas with γ = 5/3. Find the internal energy of the star, Ein, and the total energy of the star, Etot = Ein + EGR. (d, 2pts) Assume the required pressure is supplied by radiation pressure, i.e. by a photon gas. Find the internal energy of the star, Ein, and the total energy of the star, Etot = Ein + EGR.
(a, 1pt) What is the pressure of this gas where the density is ρ and the temperature T? (b, 1pt) Write down the heat transport equation and, presuming that the outward flux, F , is constant and that the gas is ideal, find dT /dz. (c, 4pts) Now find dT/dP, which is the change of temperature with pressure in the atmosphere, and show that the relation between density and temperature in the atmosphere is ρ ∝ T 3. (d, 2pts) At a fixed pressure in this atmosphere or, equivalently, a fixed location, how does the temperature depend on the composition of the atmosphere? Specfically, if the atmosphere were composed of completely ionized Helium instead of ionized Hydrogen, by what factor would the temperature change? (e, 2pts) We assumed pressure support from an ideal gas in this atmosphere. Let’s check whether this assumption is likely to hold at all heights in the atmosphere. Calculate the ratio of the radiation pressure to the gas pressure as a function of height, z. If our assumption is good at the base of the atmosphere, is it likely to hold higher up?