BAAO 2020, Теория — Задача 1. Apollo 11

British Astronomy and Astrophysics Olympiad 2019-2020 — Astronomy & Astrophysics Competition Paper — Monday 20th January 2020 · 20 януари 2020 г. · 35 т.

Указания

This question paper must not be photographed or taken out of the exam room

Time: 3 hours (approximately 60 minutes per question).

Questions: All three questions should be attempted. The last question is worth slightly fewer marks than the rest.

Solutions: Answers and calculations are to be written on loose paper. Students should ensure their name and school is clearly written on all answer sheets and pages are numbered. EACH QUESTION ANSWERED must be started on a new page. A standard formula booklet with standard physical constants should be supplied.

Instructions: To accommodate students sitting the paper at different times, please do not discuss any aspect of the paper on the internet until 8 am Saturday 25th January.

Clarity: Solutions must be written legibly, in black pen (the papers are photocopied), and working down the page. Scribble will not be marked and overall clarity is an important aspect of this exam.

Eligibility: The International Olympiad will be held during September 2020; all sixth form students are eligible to participate, even if they will be attending university from October.

Calculators: Any standard calculator may be used, but calculators cannot be programmable and must not have symbolic algebra capability.

Training Dates and the IOAA (Bogota, Columbia, 13th to 22nd September 2020)

The best students taking this paper that are eligible to represent the UK at the IOAA will be invited to attend the Training Camp to be held in the Physics Department at the University of Oxford, (Friday 27th March to Tuesday 31st March 2020). Astronomy material will be covered; problem solving skills and observational skills (telescope and naked eye observations) will be developed. At the Training Camp a data analysis exam and a short theory paper will be sat. A team of five students (plus one reserve) will be selected for further training. From April there will be mentoring by email to cover some topics and problems, followed by additional training camps in the summer.

Important Constants
ConstantSymbolValue
Speed of lightcc3.00×108 m s−13.00 \times 10^{8}\ \mathrm{m\,s^{-1}}
Earth’s rotation period1 day24 hours
Earth’s orbital period1 year365.25 days
parsecpc3.09×1016 m3.09 \times 10^{16}\ \mathrm{m}
Astronomical Unitau1.50×1011 m1.50 \times 10^{11}\ \mathrm{m}
Semi-major axis of the Earth’s orbit1 au
Radius of the SunR⊙R_{\odot}6.96×108 m6.96 \times 10^{8}\ \mathrm{m}
Radius of the EarthR⊕R_{\oplus}6.37×106 m6.37 \times 10^{6}\ \mathrm{m}
Mass of the SunM⊙M_{\odot}1.99×1030 kg1.99 \times 10^{30}\ \mathrm{kg}
Mass of the EarthM⊕M_{\oplus}5.97×1024 kg5.97 \times 10^{24}\ \mathrm{kg}
Luminosity of the SunL⊙L_{\odot}3.85×1026 W3.85 \times 10^{26}\ \mathrm{W}
Stephan-Boltzmann constantσ\sigma5.67×10−8 J m−2 K−45.67 \times 10^{-8}\ \mathrm{J\,m^{-2}\,K^{-4}}
Gravitational constantGG6.67×10−11 m3 kg−1 s−26.67 \times 10^{-11}\ \mathrm{m^{3}\,kg^{-1}\,s^{-2}}
Boltzmann constantkBk_{\mathrm{B}}1.38×10−23 J K−11.38 \times 10^{-23}\ \mathrm{J\,K^{-1}}
Permittivity of free spaceε0\varepsilon_08.85×10−12 F m−18.85 \times 10^{-12}\ \mathrm{F\,m^{-1}}
Permeability of free spaceμ0\mu_04π×10−7 H m−14\pi \times 10^{-7}\ \mathrm{H\,m^{-1}}
Planck’s constanthh6.63×10−34 J s6.63 \times 10^{-34}\ \mathrm{J\,s}
Elementary chargeee1.60×10−19 C1.60 \times 10^{-19}\ \mathrm{C}
Proton rest massmpm_{\mathrm{p}}1.67×10−27 kg1.67 \times 10^{-27}\ \mathrm{kg}
Electron rest massmem_{\mathrm{e}}9.11×10−31 kg9.11 \times 10^{-31}\ \mathrm{kg}
Wien’s displacement lawλmax⁡T\lambda_{\max} T2.90×10−3 m K2.90 \times 10^{-3}\ \mathrm{m\,K}

Basic calculus formulae:

Chain ruleddxf(g(x))=f′(g(x))g′(x)\frac{\mathrm{d}}{\mathrm{d}x} f(g(x)) = f'(g(x))g'(x)
Product ruleddx(uv)=dudxv+udvdx\frac{\mathrm{d}}{\mathrm{d}x}(uv) = \frac{\mathrm{d}u}{\mathrm{d}x}v + u\frac{\mathrm{d}v}{\mathrm{d}x}
Quotient ruleddx(uv)=dudxv−udvdxv2\frac{\mathrm{d}}{\mathrm{d}x}\left(\frac{u}{v}\right) = \frac{\frac{\mathrm{d}u}{\mathrm{d}x}v - u\frac{\mathrm{d}v}{\mathrm{d}x}}{v^2}
Integration by parts∫udvdx dx=uv−∫vdudx dx\int u\frac{\mathrm{d}v}{\mathrm{d}x}\,\mathrm{d}x = uv - \int v\frac{\mathrm{d}u}{\mathrm{d}x}\,\mathrm{d}x
Standard integral∫1x dx=ln⁡∣x∣+C\int \frac{1}{x}\,\mathrm{d}x = \ln\lvert x\rvert + C
Important Formulae

You might find the diagram of an elliptical orbit below useful in solving some of the questions:

Elements of an elliptic orbit:

a=OA (=OP)a = \mathbf{OA}\ (= \mathbf{OP})semi-major axis
b=OB (=OC)b = \mathbf{OB}\ (= \mathbf{OC})semi-minor axis
e=1−b2a2e = \sqrt{1 - \frac{b^2}{a^2}}eccentricity
Ffocus
Pperiapsis (point nearest to F)
Aapoapsis (point furthest from F)

Kepler’s Third Law: For an elliptical orbit, the square of the period, TT, of an object about the focus is proportional to the cube of the semi-major axis, aa (as defined above), such that

T2=4π2GMa3 ,T^2 = \frac{4\pi^2}{GM}a^3\,,

where MM is the total mass of the system (typically dominated by the central object) and GG is the universal gravitational constant.

Vis-Viva Equation: For an elliptical orbit, the speed vv of an object at a distance rr from the focus is related to the semi-major axis, aa, total mass of the system, MM, and universal gravitational constant, GG, (as defined above), such that

v2=GM(2r−1a) .v^2 = GM\left(\frac{2}{r} - \frac{1}{a}\right)\,.

Magnitudes: The apparent magnitudes of two objects, m1m_1 and m0m_0, are related to their apparent brightnesses, b1b_1 and b0b_0, via the formula

b1b0=10−0.4(m1−m0) .\frac{b_1}{b_0} = 10^{-0.4(m_1 - m_0)}\,.

The absolute magnitude of an object, M\mathcal{M}, is the same as its apparent magnitude when viewed from 10 pc, hence the relationship between apparent and absolute magnitude and distance is

m−M=5log⁡(d10),m - \mathcal{M} = 5\log\left(\frac{d}{10}\right),

where dd is measured in parsecs.

Note for markers

BAAO 2019/20 Solutions and Marking Guidelines

Note for markers:

  • Answers to two or three significant figures are generally acceptable. The solution may give more in order to make the calculation clear. Units should be present on final answers when appropriate.
  • There are multiple ways to solve some of the questions; please accept all good solutions that arrive at the correct answer. If a candidate gets the final (numerical) answer then allow them all the marks for that part of the question (as indicated in red), so long as there are no unphysical / nonsensical steps or assumptions made.

Условие

Diagram of an elliptical orbit from the Important Formulae page: ellipse with centre O, focus F (blue dot), periapsis P and apoapsis A at the ends of the major axis, B and C at the ends of the minor axis; dashed semi-axes labelled a and b.

In July 1969 the mission Apollo 11 was the first to successfully allow humans to walk on the Moon. This was an incredible achievement as the engineering necessary to make it a possibility was an order of magnitude more complex than anything that had come before. The Apollo 11 spacecraft was launched atop the Saturn V rocket, which still stands as the most powerful rocket ever made.

Left: photograph of the Saturn V rocket lifting off beside its launch tower. Right: labelled drawing 'Apollo Saturn V' with a height bar '110.6 metres (363 feet)'; stages labelled S-IC first stage, S-II second stage, S-IVB third stage, then adapter containing Lunar Module, Service Module, Command Module and launch escape system; an enlarged inset 'Apollo spacecraft configuration at launch' labels Command Module, Service Module and Lunar Module; a tiny person stands at the base.
Figure 1: Left: The launch of Apollo 11 upon the Saturn V rocket. Credit: NASA. Right: Showing the three stages of the Saturn V rocket (each detached once its fuel was expended), plus the Apollo spacecraft on top (containing three astronauts) which was delivered into a translunar orbit. At the base of the rocket is a person to scale, emphasising the enormous size of the rocket. Credit: Encyclopaedia Britannica.
StageInitial Mass (t)Final mass (t)IspI_{\mathrm{sp}} (s)Burn duration (s)
S-IC2283.9135.6263168
S-II483.739.9421384
S-IV (Burn 1)121.0−421147
S-IV (Burn 2)−13.2421347
Apollo Spacecraft49.7−−−

Table 1: Data about each stage of the rocket used to launch the Apollo 11 spacecraft into a translunar orbit. Masses are given in tonnes (1 t = 1000 kg) and for convenience include the interstage parts of the rocket too. The specific impulse, IspI_{\mathrm{sp}}, of the stage is given at sea level atmospheric pressure for S-IC and for a vacuum for S-II and S-IVB.

The Saturn V rocket consisted of three stages (see Fig 1), since this was the only practical way to get the Apollo spacecraft up to the speed necessary to make the transfer to the Moon. When fully fueled the mass of the total rocket was immense, and lots of that fuel was necessary to simply lift the fuel of the later stages into high altitude - in total about 3000 t (1 tonne, t = 1000 kg) of rocket on the launchpad was required to send about 50 t on a mission to the Moon. The first stage (called S-IC) was the heaviest, the second (called S-II) was considerably lighter, and the third stage (called S-IVB) was fired twice - the first to get the spacecraft into a circular ‘parking’ orbit around the Earth where various safety checks were made, whilst the second burn was to get the spacecraft on its way to the Moon. Once each rocket stage was fully spent it was detached from the rest of the rocket before the next stage ignited. Data about each stage is given in Table 1.

The thrust of the rocket is given as

F=−Ispg0m˙F = -I_{\mathrm{sp}} g_0 \dot{m}

where the specific impulse, IspI_{\mathrm{sp}}, of each stage is a constant related to the type of fuel used and the shape of the rocket nozzle, g0g_0 is the gravitational field strength of the Earth at sea level (i.e. g0=9.81 m s−2g_0 = 9.81\ \mathrm{m\,s^{-2}}) and m˙≡dm/dt\dot{m} \equiv \mathrm{d}m/\mathrm{d}t is the rate of change of mass of the rocket with time.

The thrust generated by the first two stages (S-IC and S-II) can be taken to be constant. However, the thrust generated by the third stage (S-IVB) varied in order to give a constant acceleration (taken to be the same throughout both burns of the rocket).

a. (i) Ignoring the effects of air resistance, the weight of the rocket, and assuming 1-D motion only:

(i) Show that the thrust generated by the S-IC is about 3.3×1073.3 \times 10^{7} N and hence calculate the acceleration experienced by the astronauts firstly at lift-off and secondly when the S-IC finishes its burn (ignore that the S-IC ignites a few seconds before lift off). Give your answer in units of g0g_0. [3 т.]

a. (ii) Determine the constant acceleration produced by the third stage (S-IVB) of the Saturn V rocket and hence calculate the total mass carried into the parking orbit at the end of the first burn. [3 т.]

a. (iii) Sketch an acceleration-time graph of the journey from lift-off to reaching the parking orbit. Give accelerations in units of g0g_0. Assume the time between one stage finishing, detaching, and ignition of the next stage is negligible (i.e. you will have discontinuities in the graph at the end of each stage). [5 т.]

a. (iv) By using your graph or otherwise, work out the speed of the rocket when reaching the parking orbit. [3 т.]

b. (i) In reality, the effects of air resistance and the weight of the rocket are substantial. Once in the parking orbit it is travelling at 7.79 km s−17.79\ \mathrm{km\,s^{-1}}.

(i) What is its height above the Earth’s surface (measured from sea level)? Give your answer in km. [2 т.]

b. (ii) The Apollo 11 spacecraft was in the parking orbit for 2 hours 32 mins 27 secs. How many revolutions of the Earth did it do? [3 т.]

By the end of the second burn the Apollo spacecraft, apart from a few short burns to give mid-course corrections, coasted all the way to the far side of the Moon where the engines were then fired again to circularise the orbit. All of the early Apollo missions were on a orbit known as a ‘free-return trajectory’, meaning that if there was a problem then they were already on an orbit that would take them back to Earth after passing around the Moon. The real shape of such a trajectory (in a rotating frame of reference) is like a stretched figure of 8 and is shown in the top panel of Fig 2. To calculate this precisely is non-trivial and required substantial computing power in the 1960s. However, we can have two simplified models that can be used to estimate the duration of the translunar coast, and they are shown in the bottom panel of the Fig 2.

The first is a Hohmann transfer orbit (dashed line), which is a single ellipse with the Earth at one focus. In this model the gravitational effect of the Moon is ignored, so the spacecraft travels from A (the perigee) to B (the apogee). The second (solid line) takes advantage of a ‘patched conics’ approach by having two ellipses whose apoapsides coincide at point C where the gravitational force on the spacecraft is equal from both the Earth and the Moon. The first ellipse has a periapsis at A and ignores the gravitational effect of the Moon, whilst the second ellipse has a periapsis at B and ignores the gravitational effect of the Earth. If the spacecraft trajectory and lunar orbit are coplanar and the Moon is in a circular orbit around the Earth then the time to travel from A to B via C is double the value attained if taking into account the gravitational forces of the Earth and Moon together throughout the journey, which is a much better estimate of the time of a real translunar coast.

Top: figure-of-eight trajectory with arrows looping around the Earth (large blue sphere, left) and around the Moon (small grey sphere, right). Bottom: the Earth at left with point A just to its left, the Moon at right with point B just to its right; a dashed outer ellipse from A to B; a long solid ellipse from A to point C and a small solid ellipse from C around the Moon to B; a curved arrow through the Moon shows its orbital motion.
Figure 2: Top: The real shape of a translunar free-return trajectory, with the Earth on the left and the Moon on the right (orbiting around the Earth in an anti-clockwise direction). This diagram (and the one below) is shown in a co-ordinate system co-rotating with the Earth and is not to scale. Credit: NASA. Bottom: Two simplified ways of modelling the translunar trajectory. The simplest is a Hohmann transfer orbit (dashed line, outer ellipse), which is an ellipse that has the Earth at one focus and ignores the gravitational effect of the Moon. A better model (solid line, inner ellipses) of the Apollo trajectory is the use of two ellipses that meet at point C where the gravitational forces of the Earth and Moon on the spacecraft are equal.

For the Apollo 11 journey, the end of the second burn of the S-IVB rocket (point A) was 334 km above the surface of the Earth, and the end of the translunar coast (point B) was 161 km above the surface of the Moon. The distance between the centres of mass of the Earth and the Moon at the end of the translunar coast was 3.94×1083.94 \times 10^{8} m. Take the radius of the Earth to be 6370 km, the radius of the Moon to be 1740 km, and the mass of the Moon to be 7.35×10227.35 \times 10^{22} kg.

c. For the Hohmann transfer orbit (dashed line), find its semi-major axis and hence the duration of a translunar coast from A to B (expressed in hours and minutes). [4 т.]

d. (i) For the patched conics approach (solid lines):

(i) Find the distance from the centre of the Earth to point C, and hence the semi-major axes of both ellipses. [4 т.]

d. (ii) Calculate the speed of the spacecraft at point A and point B. Give your answer in km s−1\mathrm{km\,s^{-1}} and as a percentage of the escape speed of the spacecraft at that distance from the relevant closest gravitational body. Comment on what this implies for the eccentricity of the orbits. [5 т.]

d. (iii) Determine the best estimate of the duration of the real Apollo 11 translunar coast. Give your answer in hours and minutes. [3 т.]

Отговори

Решение

Questions proposed by

END OF PAPER

Questions proposed by:

Dr Alex Calverley (Royal Grammar School, Guildford)

Alan Sun (University of Cambridge)

Navonil Neogi (University of Cambridge)


Оригинал в Архива: BAAO_2020.pdf · официални решения: BAAO_2020_solutions.pdf