davidge said:
I should have said that I was using the same symbol ##r## in two different cases.
You're still missing the point. You wrote this in the OP:
$$
ds^2 = \frac{dr^2}{1 - k r^2}
$$
Here ##dr## is a coordinate differential of the coordinate ##r##. You don't have a choice about that, because you obtained this expression from the standard FRW metric by setting ##dt = d\theta = d\phi = 0##. That means you have to give ##dr## and ##r## the meanings they have in that metric, which are what I said. And that is all that is needed to justify the criticism that I made: that this metric, by itself, cannot describe a circle of radius ##r##, because you can't use the radius of a circle as the coordinate along the circle, and ##r## is the coordinate in the 1-dimensional manifold defined by the above metric.
davidge said:
I still don't see how we can derive
$$
ds^2 = \frac{dr^2}{1 - k r^2} + r^2 d\theta^2
$$
Um, by taking the standard FRW metric, and just setting ##dt = d\phi = 0##? (I.e., by leaving one angular coordinate free.)
Let's step back even further, since it still seems like you don't understand how to properly use the tools you are trying to use. Let's just set ##dt = 0## in the standard FRW metric:
$$
ds^2 = \frac{dr^2}{1 - k r^2} + r^2 \left( d\theta^2 + \sin^2 \theta d\phi^2 \right)
$$
What is this the metric of? It's the metric of a 3-dimensional manifold that corresponds to "space" in the FRW spacetime at some constant value of coordinate time ##t##. Depending on the value of ##k##, this "space" is either a 3-sphere, flat Euclidean 3-space, or hyperbolic 3-space.
Visualizing these (at least the curved versions) is difficult, so let's drop one dimension by setting ##d\phi = 0##; i.e., we are now considering a 2-dimensional surface in this 3-dimensional space defined by picking out a particular value of ##\phi## (for concreteness, let's say it's ##\phi = 0##). That gives us the metric I wrote that appears to be confusing you:
$$
ds^2 = \frac{dr^2}{1 - k r^2} + r^2 d\theta^2
$$
Now, to make it perfectly clear what this is describing, let's first consider the easiest case to visualize: the case ##k = 0##, where this metric is just describing a flat Euclidean plane. Suppose I want to pick out a circle in this plane centered on the origin. How will that circle be described? Obviously we set ##r## to some constant value (the radius of the circle), and leave ##\theta## free. In other words, the metric on this circle will be:
$$
ds^2 = r^2 d\theta^2
$$
Now for the key question: what if we take ##k = + 1## or ##k = - 1##? What will the metric on a circle centered on the origin look like in those cases? The answer is,
exactly the same as what I just wrote down. The fact that there is an extra factor in the ##dr^2## term in the metric of the 2-dimensional surface
makes no difference when we pick out a circle centered on the origin and write its metric.
So what difference does the value of ##k## make? It tells us the relationship between the
coordinate radius of the circle, namely ##r##, and the
physical radius of the circle, which will be given by the integral
$$
R = \int_0^r \frac{dr'}{\sqrt{1 - k r'^2}}
$$
where the integration variable is now ##r'## to make it clear that it is distinct from the coordinate value ##r## that is the upper limit of integration. For the case ##k = 0##, the Euclidean plane, we have ##R = r##; but for the other cases, we don't. If you work it out, you will see that ##k = +1## gives ##R > r##, and the case ##k = -1## gives ##R < r##. If you work things out further, you will see that ##k = +1## describes the intrinsic geometry of a 2-sphere, while the case ##k = -1## describes the intrinsic geometry of hyperbolic 2-space.
Note, however, that this physical radius ##R##
makes no difference to the metric on the circle itself--that metric has ##r## in it, not ##R##, which means that a unit increment of ##\theta## (i.e., one radian) gives a physical arc length along the circle of ##r##. This is true regardless of the value of ##k##.
So what 1-dimensional manifold do we get if we set ##d\theta = 0##, so we just have the metric you wrote down in your OP? That metric, once again, is
$$
ds^2 = \frac{dr^2}{1 - k r^2}
$$
Let's first consider the case of the Euclidean plane, ##k = 0##. The above metric then just describes a straight line through the origin (which line depends on which constant value of ##\theta## we pick when we set ##d\theta = 0##--for concreteness, again, let's assume that we pick ##\theta = 0##).
The case ##k = -1## is similar, except that the "line" now does not have a constant increment of physical distance for a constant increment of the coordinate ##r##--each increment of ##r## gives a smaller increment of physical distance. If we look at an embedding of this manifold in a higher-dimensional Euclidean space, we will see that the manifold looks like a hyperbola (in fact it is just one hyperbolic "grid line" on the hyperbolic 2-space we obtained earlier), and the coordinate distance ##r## is arc length along the hyperbola, while the physical distance ##R## (which will be given by the same integral I wrote above) is the length along a straight line which is perpendicular to the axis of the hyperbola.
The case ##k = +1## has an extra complication, which is that the integral is undefined for ##r \ge 1##. Within that limitation, we see that each constant increment of ##r## gives a larger increment of physical distance; and if we take the limit as ##r \rightarrow 1##, we see that the physical distance comes out to ##\pi##. If we look at an embedding of this manifold in a higher-dimensional Euclidean space, we see that it is an arc of a great circle on the 2-sphere we obtained earlier. But the radius of this great circle is
not ##r## (it can't be, because ##r## is a coordinate and the radius of the great circle is a constant). Nor is it ##R## (which also varies with ##r##). Nor is it even ##1##, the limiting value of ##r##, or ##\pi##, the physical distance in the limit ##r \rightarrow 1##. The actual radius of the great circle turns out to be ##1/2##.
If we look at an embedding of this manifold in a higher-dimensional Euclidean space, we see that it is half of a "meridian" of a 2-sphere, starting at the North Pole, which corresponds to ##r = 0##, and where the limit ##r \rightarrow 1## corresponds to the South Pole. (The actual South Pole is technically not part of the manifold since the metric is singular there.) The physical distance ##R## corresponds to arc length along this meridian. The coordinate distance ##r## corresponds to distance along the diameter of the 2-sphere that passes through the North and South Poles; but a constant increment of ##r## does
not correspond to a constant increment of distance along this diameter. So it is not even true, for example, that the coordinate value ##r = 1/2## corresponds to the center of the 2-sphere (which you might erroneously think should be the case since the radius of the sphere is ##1/2##, as above).