On the pile-up model of the grain size-yield stress relation for nanocrystals
On the pile-up model of the grain size-yield stress relation for nanocrystals
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DOI:
10.1016/1359-6462(95)00572-2
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发表时间:
1996-03-01
影响因子:
6
通讯作者:
Nazarov, AA
中科院分区:
文献类型:
--
作者:
Nazarov, AA
The dependences of the yield stress oY or hardness FZ, of conventional polycrystals on the grain size obey the well known Hall-Petch (HP) relations oY= u0+ VI” or H,= Hyo+ k& ‘”[l-3]. Meanwhile, recent hardness tests ofnanocrystals have shown that these relations are violated at grain sizes less than approximately 100 nm. A positive relation with decreased slope kH [4, 5] as well as a transition from positive to negative relation [6, 7] have been obtained in experiments. A series of models have been proposed to account for this phenomenon. The most effort has been made to descrilbe the transition from a normal HP behaviour to an abnormal one [S-12]. However, an analysis of experimental data has shown that the softening with decreasing grain size is not an intrinsic behaviour of nanocrystalline materials but may be due to residual porosity or internal stresses [13]. Though, there is no doubt that the slope of HP relation in nanocrystalline region is less than for coarse grained polycrystals [4, 5, 13].Quite recently, Armstrong and co-workers [141 have clearly demonstrated that the decrease of ky at small grain sizes can be explained in the framework of traditional dislocation pile-up model. The point is that the soluti’on of the pile-up problem for small numbers of dislocations (n< 20) considerably differs from the usually cited solution [151 valid for large n. Due to this, at small grain sizes the dependence cr,,(d”) becomeis a staircase fimction which reaches a plateau equal to aTy””= I%, at n= 1, where M is the Taylor factor and t, the critical shear stress required for the dislocation passing through grain boundaries (for more details, see the next section).