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Structure and mechanical properties of a Σ= 51 [011] tilt boundary in germanium

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HAL Id: jpa-00245830

https://hal.archives-ouvertes.fr/jpa-00245830

Submitted on 1 Jan 1988

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Structure and mechanical properties of a Σ= 51 [011] tilt boundary in germanium

W. Skrotzki, H. Wendt, C.B. Carter, D.L. Kohlstedt

To cite this version:

W. Skrotzki, H. Wendt, C.B. Carter, D.L. Kohlstedt. Structure and mechanical properties of a Σ=

51 [011] tilt boundary in germanium. Revue de Physique Appliquée, Société française de physique / EDP, 1988, 23 (4), pp.681-681. �10.1051/rphysap:01988002304068100�. �jpa-00245830�

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681

STRUCTURE AND MECHANICAL PROPERTIES OF A 03A3= 51 [011] TILT BOUNDARY IN GERMANIUM

W. Skrotzki*, H. Wendt**, C.B. Carter and D.L. Kohlstedt

Department of Material Science and Engineering,

Cornell University, Ithaca, NY 14853 - 1501, USA

Revue Phys. Appl. 23 (1988) 681 AVRIL 1988,

Interest in understanding the correlation between structure and properties of grain

boundaries has recently been stimulated by

both the technological importance of poly- crystalline Si in the production of solar

cells and electronic devices, and the in- creasing use of ceramic materials for

high-temperature energy conversion. For the first class of materials, the electri-

cal activity of grain boundaries is a pri-

mary problem; for the second class, grain boundary diffusion and mechanical strength

of grain boundaries determine the sinte-

ring behaviour and the service lifetime, respectively. In the present work Ge bicrystals have been chosen as a model ma-

terial to study the relation between structure and mechanical properties of grain boundaries.

The grain boundary discribed here is close

to aL = 51 boundary with 16.1° tilt about [011]. Analysis by conventional and

high resolution transmission electron

microscopy shows that the structure of this boundary consists of a linear array of Lomer dislocations spaced 1.43 nm apart. The secondary dislocations accommo-

dating the small deviation (~ 0,3°) from the £ = 51 coincidence structure repre- sent irregularities in the spacing of the primary dislocations and are found to have

non-primitive DSC-Burgers vectors.

Bicrystals with this grain boundary at an angle of 450 with respect to the specimen

axis have been subjected to creep deforma- tion at 0,95 T. and a stress of 20 MPa. To detect any macroscopic sliding effects along the boundary, marker lines almost perpendicular to the boundary were scribed

on the specimen surface. In addition, a

carbon grid was evaporated onto the sur-

face to help protect the marker lines from thermal etching and to record the inhomo-

geneity of the bicrystal deformation.

Investigations of the microstructure after creep deformation show a subgrain struc-

ture which has knit together with the in- itial large angle grain boundary. With in- creasing distance from the grain boundary

the subgrain size decreases. This result correlates with the higher strains obser-

ved in a region near the grain boundary

compared to the rest of the matrix. The

knitting of a subgrain boundary with the initial grain boundary leads to the addi- tion of the misorientation of the subgrain boundary to the misorientation of the

large angle boundary. Since the misorien- tation of the subgrain boundaries differ,

the density and arrangement of the secon- dary dislocations has to change along the boundary from one grain to another.

Upon entering the grain boundary matrix dislocations décompose into secondary grain boundary dislocations. The decompo- sition product dépends on the type of Bur-

gers vector. Direct crossover of lattice dislocations through the boundary has only

be observed for screw dislocations with a/2 [011] Burgers vector. The passing pro-

cess involves a reaction with the grain boundary structure.

Bowing out of grain boundary dislocations indicates their motion in the interface.

Since secondary dislocations may produce ledges in the boundary, this dislocation movement can result in a shift of the

grain boundary plane, i.e. grain boundary migration. The driving force for grain boundary migration is proceded by the in- terfacial tension which tries to achieve mechanical equilibrium at the triple junc-

tions between the large angle boundary and subgrain boundaries. The dislocation mo-

tion is by glide or climb depending on the Burgers vector. If the Burgers vector has

a component normal to the interface dislo- cation motion involves climb. Motion of

components parallel to the interface pro- duces grain boundary sliding. No offsets

of the marker lines are detected at magni-

fications up to thousand times. Thus pos- sible sliding effects along the grain boundary plane are much smaller than usually observed in métal bicrystals under

similar conditions.

Présent address:

*) Institut für Géologie und Dynamik der Lithosphâre, Universitât Gôttingen, Gold-

schmidtstr. 3, D-3400 Gôttingen, FRG

**) Siemens AG, Otto-Hahn-Ring 6,

D- 8000 München, FRG

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/rphysap:01988002304068100

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