You will find it in most texts on the mechanical behavior of materials. I imagine Astronuc will be able to recommend good ones.
You need to be somewhat familiar with at least the basics of dislocation theory. But simplistically put, at low to moderate temperatures, grain boundaries act as barriers to dislocation movement. For a given material with a specific dislocation density at zero stress, the total number of dislocations that pile up against grain boundaries at a given applied stress is conserved. If the "number of grain boundaries" per unit volume is small (i.e., large grain size), then the number of dislocations built up at the edge of a slip plane is large. The stress build up, at this point on the grain boundary is proportional to the number of dislocations there, and hence, is proportionately large. When this stress exceeds some critical value, the dislocations get to cross the grain boundary and propagate into the neighboring grain. So, if the grain size is large, it takes a relatively small applied stress to make the number of dislocations piled up against the GB sufficient to achieve this critical stress. In other words, a large grain size makes for a low yield strength through easier dislocation movement.
The actual details of what makes the inverse square root behavior is unknown to me, beyond the knowledge that there is some tricky positional dependence on Frank-Reed multiplication - this possibly plays a role.