ANNOUNCEMENTS
MTH 437/537 — Spring 2021
- 5/7/21
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The exams have been graded. Answers to questions not asking you to show
something are below.
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(b) $\frac{3m\pm\sqrt{9m^2-8q^2}}{2}$
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(a) all nonzero components are $\pm\frac{1}{a^2}$
(b) $-\frac{3}{a^2}d\rr$
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IF your grade were determined only by your final exam, it would be
(out of 90; extra credit included):
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- $\ge82$: A
- 71–81: A−
- 50–70: B
- 37–49: C
- 20–36: D
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If you have any questions about these answers and/or how your final
was graded, please contact me.
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It may be possible to arrange a time to go over the solutions.
Contact me if you are interested.
- 6/8/21
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In problem 2, you may assume that the cosmological constant vanishes, that
is, that $\Lambda=0$.
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Please remember that there are known errors in some of the results in the
appendix of the textbook; see the
errata page.
- 6/7/21
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The exam will be available on Gradescope starting at 2 PM this afternoon.
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I will hold additional office hours at 4 PM both today and tomorrow, and
at 10 AM both tomorrow and Wednesday.
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Other times should be possible; contact me via email.
- 6/4/21
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The Sage notebook I demonstrated in class can be found
here.
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This notebook uses the definition of the Kerr geometry that is built in
to Sage using a coordinate basis. A version using an orthonormal frame
can be found here, but Sage takes much
longer to compute the Riemann tensor using this method (quite possibly due
to inefficient programming on my part).
- 6/3/21
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I will hold office hours on Monday, 6/7/21, from 10 AM–12 PM.
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There will be roughly an hour of general review followed by roughly an
hour of individual questions and consultation.
(I will record and post the first hour unless there are objections.)
- 5/30/21
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The take-home final will be distributed online on Monday afternoon,
6/7/21.
It will be due on Gradescope at noon on Wednesday, 6/9/21.
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The final covers Chapters 1–9 in the text.
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It is fair to assume that all exam questions can be answered based on
mastery of the material we have covered in class.
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I will be available during the exam. Some times will be scheduled and
posted here, but you can also contact me via email to request an
appointment.
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You may use any non-human resources you wish, except
exam or homework solutions from previous years.
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You may not discuss the exam with anyone other than me during
the exam period, even after you have turned it in.
- 5/29/21
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Additional discussion of the
Standard Models
($\Lambda=0$) can be found in the text.
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Further discussion of
cosmological redshift can also be found in the text.
- 5/28/21
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Several examples have been posted using Sage, including:
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(There is also a partial verification of
Birkhoff's Theorem, which provides a
glimpse of the further capabilities of Sage.)
- 5/26/21
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The deadline for HW 7 has been extended until
Friday, 5/28/21.
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What do you know about the $R^i{}_{jkl}$? What is the relationship between
$R_{ij}$ and $R^i{}_j$?
- 5/24/21
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I have set up an experimental interface to Sage
here that can in principle calculate
the connection 1‑forms $\omega^i{}_j$, the curvature 2‑forms
$\Omega^i{}_j$, and the Ricci and Einstein tensors for any line element in
orthogonal coordinates.
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Further examples will be posted soon. For help using this page, ask.
- 5/20/21
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There are several computer algebra packages available for computing
curvature components:
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A relatively recent option is to use the
SageMath cloud server;
see last term's announcements
dated 2/20/21 and 3/8/21.
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One of the best has been the Maple package
GRTensor,
although I have not used the latest version, GRTensorIII.
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Rough instructions on using the newer DifferentialGeometry
package, available in recent versions of Maple to compute curvature
tensors can be found here
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Another option is the Mathematica code written to accompany Hartle's
textbook, which is available
online.
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Finally, there is a fast but clunky LISP program
called SHEEP (aka CLASSI), which is available on
the ONID shell server, shell.onid.oregonstate.edu.
(See below for instructions.)
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Printouts of (old!) sample computer algebra sessions are available for
GRTensor
and CLASSI.
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Older versions of my instructions, that also include coordinate-based
computations, are available for
Maple and Mathematica packages,
and for SHEEP/CLASSI.
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You may use software to compute curvature on the homework!
See me if you would like help getting started.
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You must however document doing so, and it's up to you to ensure that you
are working in an appropriate basis.
- 5/19/21
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A discussion of Birkhoff's Theorem can be found in the
Appendix.
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(There are minor typos in the Schwarzschild curvature 2-forms as given in
§A.3 of the text:
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The coordinate expressions in the middle of Equations (A.52) and
(A.53) are each missing a factor of 1/2.
Also, the initial minus sign should be removed from Equation (A.61).
(The final expressions in terms of an orthonormal frame are correct.)
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The
wiki version has been corrected, and a full list of errata
can be found
here.)
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- 5/18/21
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In question 1b of HW 6, it is not necessary to
integrate your expression for arclength.
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In question 2b, it is not necessary to give an explicit formula for
the individual components $g^{ij}$ in terms of the components $g_{ij}$.
- 5/17/21
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All indices can be raised and lowered with the metric.
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For example, since $\TT=T^i{}_j\sigma^j\ee_i$, we have
$\ee_k\cdot\TT = T^i{}_j\sigma^j\ee_k\cdot\ee_i
= g_{ki}T^i{}_j\sigma^j = T_{kj}\sigma^j$
and similarly for $\RR$ and $\GG$.
- 5/13/21
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WEBSITE RELOCATION:
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OSU is shutting down all ONID user websites
(people.oregonstate.edu)
at the end of May.
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Automatic redirection should take place, but the direct link to the new
course website is
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http://math.oregonstate.edu/~tevian/onid/MTH437
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Both sites are active now, and should be identical.
- 5/12/21
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Notes from today's class can be found
here.
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- 5/10/21
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By popular request, today's class notes are available
here.
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Further details about geodesic deviation can be found in §7 and
§A.2 of the text, both of which can also be found
here.
- 5/8/21
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Further information about charged and rotating black holes and their
Penrose diagrams can be found in the undergraduate
textbook by d'Inverno, which is available in the OSU library.
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A more advanced treatment can be found in the book The Large Scale
Structure of Space-Time by Hawking & Ellis, which is also
available in the OSU library.
- 5/7/21
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Solutions to the midterm questions were discussed in class today; the
answers are below.
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(a) No
(b) $1/\rho$
(c) $\boldsymbol{\hat\alpha}$
(d) $-1$
(e) $1/\rho^2$
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(a) $\rho\,\boldsymbol{\hat\alpha}$
(b) $\rho^2\dot\alpha$
(c) Many answers possible, including $\rho=e^{\pm\alpha}$
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(a) $r=m\pm\sqrt{m^2-q^2}$
(b) $-\sqrt{\frac{2m}{r}-\frac{q^2}{r^2}}$
(c) No
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IF your grade were determined only by your midterm, it would be:
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- $\ge70$: A
- 57–69: AB (too close to call for now)
- 42–56: B
- 30–41: C
- $\lt30$: F
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If you have any questions about these solutions and/or how your midterm
was graded, please contact me.
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- 5/3/21
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Notes from today's review session can be found
here.
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The list of topics suggested via chat can be found
here.
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I will be available most of the day on Wednesday to answer questions about
the midterm.
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Contact me via email either to ask a question or to set up a Zoom session
(using the Office Hours ID).
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I will keep the Office Hours Zoom session open during the normal class time
and subsequent office hour (3–5 PM).
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At other times, I will respond to you as soon as possible.
- 4/28/21
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The midterm will be Wednesday 5/5/21.
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The exam will be available from 8 AM–midnight on Gradescope.
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(You can access Gradescope through Canvas, but the exam will not
show up as a Canvas assignment.)
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The main topics to be covered on the midterm are:
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Line elements;
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Spacetime diagrams;
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Geodesics and their properties;
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Schwarzschild geometry.
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Further information:
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The exam is closed book;
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There will be a review during Monday's class.
Come prepared to ask questions!
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A formula sheet will be provided, and will be discussed at the review.
You can find a draft copy here.
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I will hold extra office hours next week, most likely Tuesday afternoon;
other times will be available by appointment.
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- 4/24/21
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The basis 1-forms $\sigma^T=dT$, $\sigma^R$ in rain coordinates are
defined in
§3.9,
but the rain cooordinate $R$ is not defined until
§A.4.
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- 4/23/21
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There are two competing usages of "rain coordinates", due to the confusion
between the two radial coordinates.
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The Painlevé–Gullstrand coordinate system uses
coordinates $(T,r,\theta,\phi)$.
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The rain frame uses basis 1-forms
$\sigma^T=dT= dt + \frac{\sqrt{\frac{2m}{r}}}{1-\frac{2m}{r}} \>dr$,
$\sigma^R = \sqrt{\frac{2m}{r}} \>dR
= \frac{dr}{1-\frac{2m}{r}} + \sqrt{\frac{2m}{r}} \>dt$.
So "rain coordinates" should really refer to $(T,R,\theta,\phi)$, but is
usually used as a synonym for Painlevé–Gullstrand coordinates.
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Only the latter alternative corresponds to an orthogonal coordinate
system, with line element
$$ds^2
= -dT^2 + \frac{2m}{r}\,dR^2 + r^2 (d\theta^2+\sin^2\theta\,d\phi^2)$$
where $r$ is now an implicit function of $T$ and $R$.
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Another way to see that surfaces with $\{T=\hbox{const}\}$ are flat is to
note that $\sigma^R-\sqrt{\frac{2m}{r}}\,\sigma^T=dr$, so that
$\sigma^R=dr$ if $dT=0$.
However, as pointed out in class, the $T$ and $R$ directions are
orthogonal, but not the $T$ and $r$ directions.
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Thus, the operator "$\frac{\partial}{\partial T}$" is ambiguous! Holding
$R$ fixed, the resulting "$T$ direction" is not a symmetry, since the line
element above depends on $T$ (through $r$). Holding $r$ fixed instead
does lead to a symmetry; the Painlevé–Gullstrand line element
has no $T$ dependence. However, the resulting "$T$ direction" is
orthogonal to $r$, not $R$ — and is hence the same as the
Schwarzschild $t$ direction, which we already know is a symmetry.
- 4/19/21
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There will be an extra office hour tonight at 7 PM.
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The due date for the assignment due today is postponed until 2 PM
tomorrow.
You may resubmit your assignment on Gradescope until then without penalty.
- 4/14/21
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The figures shown at the end of class today can be found in
§3.5
of the text.
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Here are some hints for this week's assignment that we didn't quite get to
in class today:
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For timelike trajectories, the 4-velocity $\vv=\frac{d\rr}{d\lambda}$
always satisfies $\vv\cdot\vv=-1$; its magnitude is not the
speed.
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Speed is distance over time. How far did you go? How long did it
take?
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All measurements use the metric (line element).
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The far-away observers introduced in the second problem
are not aware they live in a curved spacetime, so they (incorrectly)
use the Minkowski line element.
- 4/12/21
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Further information about the difference between the geometric radius and
the physical radius can be found in my
recent paper
on embedding diagrams, which was published
here.
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A construction of the Schwarzschild embedding diagram is included, which
should be accessible to students in this class.
- 4/8/21
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One important theme in yesterday's derivation of the geodesic equation is
that differentials are the numerators of derivatives. Thus, an equation
involving 1-forms can be converted to one involving derivatives by
dividing by a differential.
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A more subtle message is that this doesn't work for second derivatives.
In particular, the geodesic equation is a second order system of ODEs, but
there is no way to take two derivatives with respect to the same parameter
using differential forms...
- 4/7/21
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Solutions of the geodesic equation in polar and spherical coordinates can
be found in
§19.5 and
§19.6.
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The latter section also discusses using vector analysis to describe
arbitrary geodesics on the sphere.
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You should check for yourself that $r\phat$ is indeed a Killing
vector, that is, that $d(r\phat)\cdot d\rr=0$.
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Details can be found in
§2.2.
- 4/6/21
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The software I used to draw lines is
GeoGebra,
which can be run online in a browser, or downloaded to most computers,
tablets and smartphones.
(You do not need to create an account in order to save files locally.)
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The curves I drew in class were obtained by successively entering the
following ordered pairs in the algebra panel:
$(2,y)$, $(x,2)$, $(x,x)$, $(3;\theta)$, $(x;\frac\pi3)$,
$(\frac{1}{\cos\theta};\theta)$, $(\frac{1}{\cos\theta},\theta)$
Be sure to distinguish commas from semicolons when entering these
expressions!
- 4/5/21
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We didn't quite finish deriving the geodesic equation on the sphere.
The answer can be found in
§19.3.
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- 4/2/21
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A copy of my paper on the cylindrical twin paradox has been posted on
canvas (as an ungraded reading assignment).
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Today's office hour is replaced by the final exam review from last term.
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The review will use the MTH 437/537 classroom Zoom ID, not the Office
Hours link.
- 3/31/21
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The sets of spacelike, timelike, and lightlike vectors do not close under
addition (even with the zero vector included), and thus do not form a
vector space.
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Can you find counterexamples?
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However, the set of future-pointing (or past-pointing) timelike
vectors do close under addition (with the zero vector included), and
therefore do form a vector space.
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- 3/29/21
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As discussed in class today, I propose an extra, optional meeting to go
over the final exam from last term.
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This session is tentatively scheduled for this Friday, 4/2/21, at 4 PM,
using our regular classroom Zoom ID.
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The session will be recorded, and posted on the Canvas pages for both
courses.
- 3/24/21
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Welcome to another term of remote teaching! Below is some information
about how this course will be run.
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Overview:
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Class meetings will be held via Zoom
at the scheduled time.
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Expect a combination of lecture, discussion, and both individual and
group problem solving.
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All class meetings will be recorded and available afterward to watch
online via Canvas.
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All assignments will be submitted via
Gradescope.
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Details:
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General information about getting started with Zoom is available
here.
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General information about submitting assignments via Gradescope can be
found
here.
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Further information can be found on my own information pages for
Gradescope and
Zoom.
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Each assignment exists in 3 places: on this website, in Gradescope,
and on Canvas:
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The assignment itself can be found (only) on the
homework page.
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Each assignment has a name, such as "Use Gradescope" or "HW 1".
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When you have completed the assignment, export or scan it to PDF.
Please do not take photographs of your work except as a last
resort.
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Upload your PDF to Gradescope, following the instructions
here.
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After grading, your corrected assignment will be available on
Gradescope.
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After grading, your score will be available on Canvas.
- 3/23/21
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The primary text for this course will be my own
book,
which can be read online as an
ebook
through the OSU library.
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There is also a freely accessible
wiki
version available, which is however not quite the same
as the published version.
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We will also refer briefly to my
book on special relativity.
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You may purchase this book if you wish, but it can also be read online
as an
ebook
through the OSU library, and again there is also a
wiki
version.
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You may also wish to purchase a more traditional text, in which case I
recommend any of the first three optional texts listed on
the books page. The level of this course will be
somewhere between that of these books, henceforth referred to as EBH
(Taylor & Wheeler), Relativity (d'Inverno), and Gravity
(Hartle).
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EBH uses only basic calculus to manipulate line elements, and
only discusses black holes, but does so in great detail.
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Relativity discusses the math first, then the physics.
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Gravity begins essentially the same way, starting from a
given line element to discuss applications, including both black
holes and other topics. This is followed by a full treatment of
tensor calculus, including a derivation of Einstein's equation.
This book is the most advanced of the three, and is aimed at
advanced undergraduate physics majors.
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We will cover more material than EBH, but we will stop short of the
full tensor treatment in Relativity or (the back of) Gravity.
We will also cover some of the material on black holes from EBH which
is not in Gravity or Relativity.
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If you are seriously interested in the physics of general relativity,
Gravity is worth having.
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If you are primarily interested in the mathematics, you may find
Relativity easier to read. It covers more topics more quickly
than Gravity.
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However, we will use the language of differential forms wherever we
can, which is not extensively covered in any of these other books.
We will therefore take a somewhat more sophisticated approach
than EBH, while trying to avoid most of the tensor analysis
in Gravity or Relativity.
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In short, none of these books is perfect, but all are valuable resources.
In addition to the above books, OSU owns an electronic copy of
Relativity Demystified,
which summarizes many of the key aspects of relativity, but provides no
derivations. By all means use it for reference, but I would not recommend
using it as a primary text.
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