200 FLUIDITY AND PLASTICITY which causes any cubical figure of the fluid to assume the form of a rhombohedron, will cause the sphere to rotate, thereby assisting the flow. The stream lines are curved on account of the presence of the sphere, but the sphere itself moves in a linear direction and with the velocity of the stratum of fluid which would, if continuous, pass through the center of the sphere. Spheres in the same stratum do not approach each other since they all have the same velocity. Spheres in different strata move with unequal velocity, hence collisions must take place, depending upon the radii of the spheres, their number per unit volume, and also upon any attraction or repulsion which may exist between them. The FIG. 72.—Two spheres before, during, and after collision. The initial rota- tion of the individual spheres is lost on collision and this results in the dissipation of energy as heat. In the place of this individual rotation there develops a rotation of the system. It should be noted that this latter rotation causes the centers of the spheres to move in a transverse direction, indicated by the dis- tances from the dotted lines. surfaces of two spheres which are approaching each other must be moving in opposite directions, which are at right angles to the line joining their centers, Fig. 72. The viscous resistance to this shearing action which is set up as they approach will rapidly dissipate as heat their energy of rotation. In other words, their energy of rotation is converted into heat by the "collision" of the particles. The contact of two particles, which are large in comparison with molecular dimensions, brings the laws of ordinary friction into play. The spheres cannot rotate unless the torque exceeds a certain definite value, which will become very important when we come to consider plastic flow. This value depends upon the pressure existing at their point of contact normal to the surfaces and this pressure in turn depends not only on the rate of shear but on the attraction or repulsion which may exist