欢迎登录材料期刊网

材料期刊网

高级检索

Due to the non-uniform nature of crack advance, when a cleavage front encounters a high-angle grain boundary,instead of simultaneous break-through along the whole boundary, the front transmission mode can be irregular, which results in a higher fracture resistance and a tortuous percolation behavior. In this paper, this phenomenon is studied quantitatively through the analysis on the work of separation and the change in strain energy for an Fe-3 wt pct Si alloy. The influences of the crystallographic misorientations, the break-through mode, the cleavage front profile, and the grain boundary properties are discussed in detail.

参考文献

[1] R O Ritchie;J F Knott;J R Rice .[J].Journal of the Mechanics and Physics of Solids,1973,21:395.
[2] J F Knott;K S Chan.In Cleavage Fracture-George R. Irwin Symposium Proceedings[M].TMS,Warrendale,PA,1997:171.
[3] Y. Qiao;A.S. Argon .Cleavage crack-growth-resistance of grain boundaries in polycrystalline Fe-2%Si alloy: experiments and modeling[J].Mechanics of materials,2003(1/2):129-154.
[4] Y Qiao .[J].Materials Science and Engineering,2003,A361:350.
[5] G T Hahn;B T Averbach;W.S.Owen;M.Cohen B.L.Averbach, D.K.Felbeck, D.K.Hahn D.A.Thomas.In Fracture[M].MIT Press, Cambridge, MA,1959:91.
[6] R W Armstrong .[J].Materials Science and Engineering,1966,1:251.
[7] A.Kelly;W.R.Tyson;A.H.Cottrell .[J].Philosophical Magazine,1967,15:567.
[8] J.R.Rice;R.Thomson .[J].Philosophical Magazine,1974,29:73.
[9] M.Gell;E.Smith .[J].Acta Materialia,1967,15:253.
[10] F A McClintock;K S Chan.In Cleavage Fracture-George R.Irwin Symposium Proceedings[M].TMS,Warrendale,PA,1997:81.
[11] Y. Qiao;A.S. Argon .Cleavage cracking resistance of high angle grain boundaries in Fe―3%Si alloy[J].Mechanics of materials,2003(3/6):313-331.
[12] B.Gross;J.E.Srawley.[M].NASA Technical Note,D-2395,1964
[13] K Hellan.Introduction to Fracture Mechanics[M].McGrawHill, New York,1984:74-109.
[14] Y Qiao .[D].MIT Cambrige MA,2002.
上一张 下一张
上一张 下一张
计量
  • 下载量()
  • 访问量()
文章评分
  • 您的评分:
  • 1
    0%
  • 2
    0%
  • 3
    0%
  • 4
    0%
  • 5
    0%