Friction is the force that opposes relative motion between surfaces in contact. It arises from the interlocking of microscopic irregularities and acts parallel to the surface, opposite to the direction of motion (or attempted motion). Without it we could not walk, drive or even hold a pencil.
- Static friction ($f_s$) acts when the body is still. It is self-adjusting — it grows to match the applied force up to a maximum (limiting) value: $f_s \le \mu_s N$, where $\mu_s$ is the coefficient of static friction and $N$ the normal reaction.
- Kinetic friction ($f_k$) acts once the body slides, and is nearly constant: $f_k=\mu_k N$. In general $\mu_k < \mu_s$, which is why it is harder to start an object moving than to keep it moving.
- Friction depends on the nature of the surfaces and the normal reaction, but (to a good approximation) not on the area of contact.
Motion on an inclined plane. For a block on a plane inclined at angle $\theta$, the weight resolves into $mg\sin\theta$ down the slope and $mg\cos\theta$ perpendicular to it, so $N=mg\cos\theta$. The block is on the verge of sliding when $mg\sin\theta=\mu_s mg\cos\theta$, giving the angle of repose $\theta=\tan^{-1}\mu_s$. Once sliding, its acceleration is $a=g(\sin\theta-\mu_k\cos\theta)$.
Dynamics of circular motion. A body moving in a circle of radius $r$ at speed $v$ is always accelerating toward the centre — the centripetal acceleration $a_c=\frac{v^2}{r}$. A real force must supply this; the required centripetal force is $F=\frac{mv^2}{r}$. For a car on a level road this is provided by friction; the maximum safe speed is $v_{max}=\sqrt{\mu_s rg}$.
Banking of roads. To turn at higher speed safely, roads are banked (tilted inward at angle $\theta$) so the horizontal component of the normal reaction supplies the centripetal force, reducing reliance on friction. For the ideal (frictionless) banking speed, $\tan\theta=\frac{v^2}{rg}$. A conical pendulum (a bob whirled in a horizontal circle on a string making angle $\theta$ with the vertical) obeys the same relation: the tension's horizontal component gives the centripetal force while its vertical component balances gravity, so again $\tan\theta=\frac{v^2}{rg}$.