BAAO 2019, Теория — Задача 2. 360 Days in a Year

British Astronomy and Astrophysics Olympiad 2018-2019 — Astronomy & Astrophysics Competition Paper — Monday 21st January 2019 · 21 януари 2019 г. · 25 т.

Указания

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

Time: 3 hours plus 15 minutes reading time (no writing permitted). Approx 45 minutes per question.

Questions: All four questions should be attempted.

Marks: The questions carry similar marks.

Solutions: Answers and calculations are to be written on loose paper or in examination booklets. Students should ensure their name and school is clearly written on all answer sheets and pages are numbered. 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 26th 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 paper.

Eligibility: The International Olympiad will be held during August 2019; all sixth form students are eligible to participate, even if they will be attending university from October.

Training Dates and the International Astronomy and Astrophysics Olympiad (IOAA)

The IOAA this year will be held in Zanka, Hungary, from 2nd to 11th August 2019.

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, (Saturday 13th April to Wednesday 17th April 2019). 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 May 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}
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.

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 2018/19 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

A day on Earth can be defined in two ways: relative to the Sun (called solar or synodic time) or relative to the background stars (called sidereal time). The mean solar day is 24 hours (within a few milliseconds), whilst the mean sidereal day is shorter at 23 hours 56 minutes 4 seconds (to the nearest second). The solar day is longer as over the course of a sidereal day the Earth has moved slightly in its orbit around the Sun and so has to rotate slightly further for the Sun to be back in the same direction (see Figure 4).

The Sun with a distant star straight above it, and the Earth shown at three positions along its orbit (dashed arc), each with a meridian marker m and S; an orange angle marks the extra rotation. Below, sky views at 12:00:00, 11:56:04 and 12:00:00 and time bars labelled 23h 56′ 04″ a sidereal day, 3′ 56″ and 24h a mean solar day.
Figure 4: A solar day is defined as the time between two consecutive passages of the Sun through the meridian, corresponding to local midday (which in the Northern hemisphere is in the South), whilst a sidereal day is the time for a distant star to do the same. The difference between the two is due to the Earth having moved slightly in its orbit around the Sun. Credit: Wikipedia.

The length of a year on Earth is 365.25 solar days (to 2 d.p.), however some ancient civilizations used to believe that there were once exactly 360 solar days in a year, with various myths explaining where the extra days came from. In this question you will look at how to return the Earth to this time.

[Note that this question is very sensitive to the precision of the fundamental constants used, so throughout please take G=6.674×10−11 m3 kg−1 s−2G = 6.674 \times 10^{-11}\ \mathrm{m^{3}\,kg^{-1}\,s^{-2}}, R⊕=6371R_{\oplus} = 6371 km, M⊕=5.972×1024M_{\oplus} = 5.972 \times 10^{24} kg, M⊙=1.989×1030M_{\odot} = 1.989 \times 10^{30} kg and 1 au = 1.496×10111.496 \times 10^{11} m.]

a. How many sidereal days elapse during a year? Give your answer to 2 d.p. [2 т.]

b. Without further calculation, suggest how many sidereal days there would be if a year was in fact only 360 solar days. [1 т.]

c. What reduction in the Earth’s semi-major axis would be required for the year to be shortened down to 360 solar days? [3 т.]

d. (i) Imagine creating an incredibly powerful rocket, positioned on the Earth’s equator, that when fired once can apply a huge force to the Earth in a very short time period, delivering a total impulse of Δp\Delta p. Assuming the Earth’s orbit is initially circular, calculate:

(i) The total impulse required to slow the Earth’s rotation to give a year of 360 solar days, but with no change in the orbit. [6 т.]

d. (ii) The total impulse required to change the orbit to give a year of 360 solar days, but with no change in the length of a solar day, also explaining how the rocket needs to be fired. [7 т.]

e. Tidal interactions between the Moon and the Earth mean that the Earth’s rotation rate is slowing down, such that a solar day has lengthened over the last 2800 years by an average of 2.3 ms per century. Similar interactions between the Earth and the Sun, as well as mass loss by the Sun due to nuclear fusion and the solar wind, mean that the distance between them is increasing by about 1.5 cm per year. Assuming these rates have stayed constant over time and that the Earth’s orbit has remained circular throughout, is there any time in either the Earth’s past or future when it had or when it will have a year with 360 solar days? Give your answer in Myr (where 1 Myr = 10610^{6} years). [For reference, the age of the Earth is 4543 Myr.] [6 т.]

Helpful equations:

The moment of inertia, II, of a sphere of mass MM and radius RR is I=25MR2I = \frac{2}{5}MR^2.

The angular momentum, LL, of a spinning object with an angular velocity of ω\omega is L=Iω=r×pL = I\omega = r \times p, where pp is the linear momentum of a point particle a distance rr from the axis of rotation.

The speed, vv, of an object in an elliptical orbit of semi-major axis aa around an object of mass MM when a distance rr away can be calculated as

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

Отговори

Решение

Questions proposed by

END OF PAPER

Questions proposed by:

Dr Alex Calverley (Royal Grammar School, Guildford)

John Hayton (University of Cambridge)

Josh Brown (University of Cambridge)


Оригинал в Архива: BAAO_2019.pdf · официални решения: BAAO_2019_solutions.pdf