Z. Cochnar et al., Creep of copper single crystals oriented for multiple slip at temperatures873-973 K and applied stresses ranging from 3 to 9 MPa, KOVOVE MAT, 37(1), 1999, pp. 42-57
In the present paper creep of copper single crystals with the crystallograp
hic directions [001] or [111] parallel to the tensile stress axis was inves
tigated. The constant stress creep tests were performed at stresses ranging
from 3 to 9 MPa and temperatures 873, 923, and 973 K. The creep testing ti
mes ranged from 8 to 7000 ks and 7 to 8000 ks and the total creep strains r
anged to 0.055 and 0.02 for the orientation [001] and [111], respectively.
The "minimum" creep strain rates ranged from 10(-10)s(-1) to 3 x 10(-5)s(-1
) depending on testing conditions. The main attention was paid to the chang
es of morphology as observed on the crept specimen surfaces.
The slip pattern on the surface of specimens with [001] orientation has an
appearance of fine waves oriented in parallel with the lines of intersectio
ns of {111} planes with the specimen surface. The generation of these fine
waves is attributed to the local microscopic slip of one slip system with t
he identical shear stress. The creep strain rate attains maximum values at
the creep strains less than 0.01 and with the strain increasing in time abo
ve this value it continuously decreases. In this respect, the creep strain
rate behaviour is similar to that of single crystals oriented for easy glid
e as well as for double slip.
On the surfaces of single crystals of (111) orientation no microscopic chan
ges were observed. The maximum creep strain rate is observed at the beginni
ng of creep tests; with increasing creep strain, the creep strain rate quic
kly decreases. This specific creep strain rate behaviour is due to differen
t geometric condition for development of slip bands in both microscopic and
submicroscopic scale.