1 − 2σ F sin θ,
2(1 − σ)

where θ is the angle between the radius vector r and the line of action of F. The line marked T in fig. 30 shows the direction of the tangential traction on the spherical surface.

Fig. 30.
Fig. 31.

Thus the lines of stress are in and perpendicular to the meridian plane, and the direction of one of those in the meridian plane is inclined to the radius vector r at an angle

½ tan−1 ( 2 − 4σtan θ ).
5 − 4σ

The corresponding displacement at any point is compounded of a radial displacement of amount

1 + σ F cos θ
2(1 − σ) 4πEr

and a displacement parallel to the line of action of F of amount

(3 − 4σ) (1 + σ) F 1.
2(1 − σ) 4πEr

The effects of forces applied at different points and in different directions can be obtained by summation, and the effect of continuously distributed forces can be obtained by integration.