Fracture experiments to evaluate the cleavage energy of the (110) [110] and (111) [112] cleavage systems in silicon at room temperature and humidity give 2.7 +/- 0.3 and 2.2 +/- 0.2 J/m(2), respectively, lower than any previous measurement and inconsistent with density functional theory ( DFT) surface energy calculations of 3.46 and 2.88 J=m(2). However, in an inert gas environment, we measure values of 3.5 +/- 0.2 and 2.9 +/- 0.2 J=m(2), consistent with DFT, that suggest a previously undetected stress corrosion cracking scenario for Si crack initiation in room conditions. This is fully confirmed by hybrid quantum-mechanics molecular-mechanics calculations.
Dissociative chemisorption of O2 inducing stress corrosion cracking in silicon crystals / Gleizer, Anna; Peralta, Giovanni; Kermode, James R.; DE VITA, Alessandro; Sherman, Dov. - In: PHYSICAL REVIEW LETTERS. - ISSN 0031-9007. - 112:11(2014), pp. 115501.115501-115501.115505. [10.1103/PhysRevLett.112.115501]
Dissociative chemisorption of O2 inducing stress corrosion cracking in silicon crystals
DE VITA, ALESSANDRO;
2014-01-01
Abstract
Fracture experiments to evaluate the cleavage energy of the (110) [110] and (111) [112] cleavage systems in silicon at room temperature and humidity give 2.7 +/- 0.3 and 2.2 +/- 0.2 J/m(2), respectively, lower than any previous measurement and inconsistent with density functional theory ( DFT) surface energy calculations of 3.46 and 2.88 J=m(2). However, in an inert gas environment, we measure values of 3.5 +/- 0.2 and 2.9 +/- 0.2 J=m(2), consistent with DFT, that suggest a previously undetected stress corrosion cracking scenario for Si crack initiation in room conditions. This is fully confirmed by hybrid quantum-mechanics molecular-mechanics calculations.Pubblicazioni consigliate
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