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The calculations of the interaction energy between walls of double-walled carbon nanotubes showed that the barriers for motion of the short wall relative to the long wall are very sensitive to the length of the long wall [25].
The Lennard-Jones potential is used for calculating the barriers for motion of the fullerenes along the axis and rotation about the axis of the (8,8) nanotube with the Kekule structure and the structure with all equal bonds corresponding to low-temperature and high-temperature phases, respectively.
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"Fullerene-nanotube interaction" section presents the semiempirical calculations of the barriers for motion and rotation of the fullerenes inside the nanotube.
Significant changes of the barriers for motion along the nanotube axis and rotation of these fullerenes inside the (8,8) nanotube are found at the Peierls transition.
Using molecular dynamics (MD) simulations, the strengthening mechanism of silicon carbide (SiC) particle acted as barrier for the motion of edge dislocation in copper (Cu) matrix nanocomposites under shear loading is investigated.
In other words, the temperature T P should be of the same order of magnitude (or a few orders of magnitude less) as energy barriers ΔE for motion and/or rotation of the molecule inside the nanotube at this phase.
For this cut-off distance the errors of calculation of the interaction energy E W between the fullerenes and the (8,8) nanotube and the barriers for relative motion and rotation of the fullerenes inside the nanotube are less than 0.1%.
Particle dispersions strengthen metals by acting as barriers to the motion of dislocations.
Changes of the energy barrier for cation motion and of the metal oxide and oxide oxygen work functions are related to the transformation of the amorphous, non-stoichiometric oxide film into crystalline ZrO2.
The ferrite refinement process is greatly facilitated by the presence of dispersed cementite particles, as the cementite/ferrite interfaces are effective nucleation sites for dislocations and also barriers for dislocation motions.
This implies that the absence of seismic activity at depths ≳700 km should not be interpreted as direct evidence for the hypothesis that the 650-km discontinuity in the mantle acts as a barrier to vertical motion of subducted slabs.
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