Engineering Rock Mechanics

(Jacob Rumans) #1

41 4 Appendix A: Stress and strain analysis


For small rotations sin R = R, so that


du=-Rdy
dv = Rdx
or


(b) Normal strain


















                  • Because we use compression
                    I
                    I I
                    I we have


















(and hence contraction) positive,
I
----^__- J I

w+


from which we obtain

du
dx

& x =--

or

(c) Shear strain

This is negative shear strain: P'Q
is longer than PQ, and extension
is negative. For small angles, to a
good approximation we have

du =dysina!+dxcosa-dx

butforsmallanglessina=aandcosa=l,sothatdu= ady+dx-dx=
a dy and similarly dv = adx.
The definition of shear strain is the change in angle between two lines
originally perpendicular to each other, i.e. ywy = (p - V2).

q2 = p+2a =3 -2a= p-x/2 = r,,

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