Tension on the spring points inward from the circle to its center, while the gravity always points downward.
If the weight is moving counter-clockwise:
then on the left side of the circle, $$\frac {v^2}r=\frac{mg+T}m,$$so$$T=m\frac{v^2}r−mg,$$ and on the right side of the circle, $$\frac{v^2}r=−\frac{mg+T}m,$$so$$T=\frac{mv^2}r+mg.$$The spring alternates between storing the acceleration of gravity on the downward part of the circular path, and restoring it compensatorily on the upward part of the circular path.
ehild said:
let be ##\vec r## the position vector of the particle. A the spring has zero relaxed length, the spring force is ##-k \vec r##. the total force also includes gryvity. WE set the coordinate system with horizontal x-axis and vertical down y axis.
The vertical axis would not be restricted to 'down' only, but the gravity is always downward.
The equation of motion in coordinates is
##m\ddot x=−kx##
##m\ddot y=−ky+mg##
Given that ##k## is always directed along ##\vec r## toward the center, while ##mg## is always directed down, the ##\ddot y## acceleration of ##mg## alternates between
##m\ddot y=−ky+mg##
and
##m\ddot y=−ky−mg##.
This is a linear , constant coeffient, inhomogeneous DE. the solution of the homogeneous part is a two-dimensional vibration with angular frequancy
##ω=k/m## A particular solution of the inhomogeneous equation is ##h=mg/k## that corresponds to the steady state.
For the new variables ##X=x## and ##Y= y-h##, the differential equation becomes ##m\ddot X=−kX## and ##m\ddot Y=−kY##. The solution can be a circular motion with angular frequeny ##ω=\frac k m##, and arbitrary radius ##R##. Then the speed is constant, ##ωR##.
The problem maker might have took that straightforward, when assuming constant speed.
No basis is shown for assuming constant speed.
Given only the spring force, gravity, and from an initial static state at the equilibrium point an external initial tangential impetus sufficient to incipiate rotation, I think that the speed component of the angular velocity ##\omega##, although it would be of a constant frequency and period, would vary within the cycle, increasing in the left semicircle, and decreasing in the right, with ##v_{max}## at the lowest point, ##v_{min}## at the highest, and ##v_{mean}## at the two exactly vertical exorbital tangent points, downward and upward, at the leftmost and rightmost points, respectively.
The rightmost of these is the one that the problem recipient is in the solution asked to consider, and it is in my view sufficient for purposes of the argument that this point has the mean vertical velocity; the velocity is not, and need not be, constant throughout the cycle.
If there's something that I'm missing it wouldn't be the first time.
@berkeman: A minor edit produced ##LaTeX## rendering failure -- post-edit preview was fine, but upon save, no rendering . . . the only change made was from ##vec r## to ##\vec r## . . . (now fixed, thanks) (oops . . . editing to acknowledge the fix and say thanks broke it again)