This is a problem from the problem book by IE Irodov (Problem 1.106). We have a rough inclined plane with coefficient of friction $\mu = \tan\alpha$. A particle is kept on the incline and projected with an initial velocity $v_0$ 'sideways' to the incline, that is into the the plane of the figure shown below.
A coordinate system is set up in the problem with the x-axis pointing down the incline and the y-axis along the initial velocity vector (the origin is at the initial position of the particle). We need to figure out the magnitude of the velocity as a function of the angle $\phi$ its vector makes with the x-axis.
I did the problem in the following manner:
We may fix the velocity vector at the origin and resolve components of the forces acting on the particle as shown:
$v$ is the velocity at an arbitrary time, $F_2$ is the frictional force ($\mu mg\cos\alpha=mg\sin\alpha$), and $F_1$ is the component of gravity along the incline ($mg\sin\alpha$). Note that $\angle DAB$ is $\phi$. Now, we can figure out the tangential acceleration,
$$-\frac{dv}{dt} = g\sin\alpha(1-\cos\phi)\tag1$$
and the radial acceleration
$$v\frac{d\phi}{dt}=-g\sin\alpha\sin\phi\tag2$$
We can introduce a change of variables in $(1)$
$$\frac{dv}{dt} = \frac{dv}{d\phi}\cdot\frac{d\phi}{dt} = \frac{-g\sin\alpha\sin\phi}{v}\cdot\frac{dv}{d\phi}$$
we can substitute this into $(1)$ to get,
$$\frac{dv}{v} = (\csc\phi-\cot\phi)d\phi$$
Integrating yields a solution of the form,
$$\boxed{v=v_0e^{f(\phi)}}$$
where $f$ is a function of $\phi$
But, when I saw the solution, the problem was solved quite simply: we can see that the acceleration along x-axis is $g\sin\alpha(1-\cos\phi)$, which is equal in magnitude to the tangential acceleration. Thus, $v$ and $v_x$ will at any point differ by the same constant value $C$
$$v-v_x = C$$
This $C$ can be easily determined from the initial conditions. This yields,
$$v = \frac{v_0}{1+\cos\phi}$$
Where did I go wrong?
EDIT: This is another figure I'm including just to clarify the situation presented in the problem. Here are different views of the incline for an arbitrary $\phi$.
perpendicular
to the incline, i.e., at an angle of $\alpha$ counterclockwise from vertical. Are you sure? $\endgroup$into the page
. The new figures help quite a bit. $\endgroup$