M09 Computing Ideal Strength: Difference between revisions

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where ''dx'', ''dy'' and ''dz'' are scaled coordinates of the shift vector. Since the [1 1 1] direction is along the <math>\mathbf{c}_2</math> direction, ''dy'' is the relevant parameter that will change the type of (1 1 1) plane exposed at the edge of the simulation cell. Whether or not '''pbcshiftatom''' is required and, if so, the necessary magnitude of ''dy'' can be determined by visually inspect the atomic structure in the X-window. The curves in Fig. 3(a) correspond to the shuffle-set plane<ref name="kangcai2007"/>. The ideal shear strength on the glide-set plane (77.3 GPa for SW model of Si) is much higher than that on the shuffle-set plane.
where ''dx'', ''dy'' and ''dz'' are scaled coordinates of the shift vector. Since the [1 1 1] direction is along the <math>\mathbf{c}_2</math> direction, ''dy'' is the relevant parameter that will change the type of (1 1 1) plane exposed at the edge of the simulation cell. Whether or not '''pbcshiftatom''' is required and, if so, the necessary magnitude of ''dy'' can be determined by visually inspect the atomic structure in the X-window. The curves in Fig. 3(a) correspond to the shuffle-set plane<ref name="kangcai2007"/>. The ideal shear strength on the glide-set plane (77.3 GPa for SW model of Si) is much higher than that on the shuffle-set plane.



⚫
We have also implemented a special command '''calmisfit''' in MD++ that computes the misfit energy <math>\gamma</math> as a function of three parameters (two for the orthogonal slip directions within the plane and one for the opening displacement perpendicular to the plane). The syntax for this command is
== Gamma Surface ==
The above procedure allows us to compute the ideal shear strength on a specified plane along a specific slip direction. However, there are two orthgonal directions within every plane along which slip can occur. The excess energy per unit area as a function of the two-dimensional slip vector can be visualized as a surface, and is usually called the <math>\gamma</math>-surface, or the generalized stacking fault energy.

⚫
We have implemented a command '''calmisfit''' in MD++ that, together with an external Matlab program, computes the <math>\gamma</math>-surface. The command '''calmisfit''' itself computes the misfit energy <math>\gamma</math> as a function of three parameters: two for the 2-dimensional slip vector within the plane and one for the opening displacement <math>\delta</math> perpendicular to the plane. The minimization w.r.t. <math>\delta</math> is performed in the Matlab program. The syntax for this command is


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The input variable needs seven elements, the first of which indicates the surface normal index. If it is 2, the slip plane normal is in <math>y</math>-direction (1 for <math>x</math> and 3 for <math>z</math>-direction) and the periodicity vector <math>\mathbf{c}_2</math> is going to be tilted. The rest six numbers are basically grid points to designate to which
The input variable needs seven elements, the first of which indicates the surface normal index. For example, if ''surfacenormal'' = 2, the slip plane is normal to the <math>\mathbf{c}_2</math> vector. The following nine numbers specifies the range and incremental steps of the offset vector in three directions. In the case study shown in Figs. 1(b) and 2(b), ''x0'', ''dx'', ''x1'' specify the range of <math>d</math>, in units of <math>|\mathbf{c}_1|/N_x</math>. ''y0'', ''dy'', ''y1'' specify the range of <math>\delta</math>, in units of <math>|\mathbf{c}_2|/N_y</math>. Since we are not interested in slip along the <math>\mathbf{c}_3</math> direction, we have set '''z0''' = '''dz''' = '''z1''' = 0.
direction and how much the periodicity vector is tilted (or stretched). The numbers are normalized by the length of one lattice vector in each direction. If '''dx'''=0.001, the increment of tilting the vector in <math>x</math>-direction would be <math>0.001 \times a \times |\mathbf{c}_1|/N_x</math>, where <math>a</math> is the lattice constant. If '''dy'''=0.01, the vector <math>\mathbf{c}_2</math> increases by the amount of <math>0.01 \times a \times |\mathbf{c}_2|/N_y</math> in <math>y</math> direction. In our example, the last
three numbers are all zeros or '''z0''' = '''dz''' = '''z1''' = 0.


Command '''calmisfit''' produces a text output file “Emisfit.out”, which is then analyzed by the Matlab program cal_idealstr.m to perform minimization w.r.t. <math>\delta</math> and to compute the ideal shear strength. The source code for the cal_idealstr.m program is attached at the end of this manual.
After running '''calmisfit''', a text file “Emisfit.out” will be dumped out and it
will be used to calculate the ideal shear strength by the Matlab script attached
at the end.


<gallery caption="Fig.3" widths="300px" heights="300px" perrow="2">
<gallery caption="Fig.3" widths="300px" heights="300px" perrow="2">
Image:Glideset_e.jpg |(a) A diamond-cubic structure with glide-set (1 1 1) plane exposed at the edge of the simulation cell (normal to <math>\mathbf{c}_2</math>.
Image:Glideset_e.jpg |(a)
Image:Shuffleset.jpg |(b) Two configurations in (a) and (b) are essentially identical before the periodicity vector <math>\mathbf{c}_2</math> is tilted. After <math>\mathbf{c}_2</math> is tilted along <math>\mathbf{c}_1</math> direction, the crystal is shifted on glide-set plane in (a) and shuffle-set plane in (b).
Image:Shuffleset.jpg |(b) A diamond-cubic structure with shuffle-set (1 1 1) plane exposed at the edge of the simulation cell. The structures in (a) and (b) are identical unless slip occurs at the edge of the simulation cell by tilting repeat vector <math>\mathbf{c}_2</math>.
</gallery>
</gallery>


== Ideal Shear Strength in Non-tilting Cell ==
== Computing Ideal Shear Strength without Tilting Simulation Cell ==
For technical reasons, sometimes we cannot tilt the repeat vectors in MD++ when computing the ideal shear strength. For example, the ''meam-baskes'' program requires linking the C-programs of MD++ with a set of Fortran programs (provided by Dr. Mike Baskes) that implements the MEAM potential. Unfortunately, the three repeat vectors are not allowed to tilt arbitrarily in these Fortran programs. In this case, the approach described above will no longer apply. A new algorithm is needed to compute the ideal shear strength and the <math>\gamma</math>-surface. This is implemented in command '''calmisfit2'''.
Sometimes we simply cannot tilt the periodicity vectors. For example, the

original Baskes’ MEAM codes are implemented only for a rectangular cell. In
'''calmisfit2''' litterally moves one block of atoms w.r.t. to the remaining block of atoms, as shown in Fig. 4(a). This creates an interface between the two blocks of atoms. To avoid creating another (unwanted) interface at the periodic boundary, we need to remove several layers of atoms at the edge of the simulation cell before calling '''calmisfit2'''.
⚫
this case, the procedures explained above can not be applied and we have to

⚫
the procedures explained above can not be applied and we have to
move a chunk of atoms literally. Fig. 4(a) shows the initial configuration in
move a chunk of atoms literally. Fig. 4(a) shows the initial configuration in
which a few layers at top and bottom are removed in order to have room for
which a few layers at top and bottom are removed in order to have room for
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to get the ideal shear strength is identical.
to get the ideal shear strength is identical.


To remove top and bottom atoms, two MD++ commands '''fixatoms_by_position'''
In MD++, we can remove a block of atom using commands '''fixatoms_by_position''' and '''removefixedatoms'''. The syntax is
and '''removefixedatoms''' are used. The command '''fixatoms_by_position''' fixes
atoms within a hexahedral volume defined by six numbers ('''x0''', '''x1''', '''y0''', '''y1''', '''z0''' and '''z1''' in scaled coordinate) in input


input = [enable x0 x1 y0 y1 z0 z1 ] fixatoms_by_position
input = [''enable x0 x1 y0 y1 z0 z1'' ] fixatoms_by_position removefixedatoms


''enable'' = 1 is required to activate the command, and the following 6 parameters specifies a parallelepiped volume (in scaled coordinates). All atoms within this volume will be labeled as fixed by the command '''fixatoms_by_positions'''. The following command '''removefixedatoms''' then removes these atoms. To remove two blocks of atoms at the top and bottom of the simulation cell, as shown in Fig. 4(a), the above commands need to be called twice with different input parameters.
when '''enable'''=1. Then the command '''removefixedatoms''' removes those fixed
atoms.


MD++ codes have another command '''calmisfit2''' to calculate the misfit energy
The syntax for calling command '''calmisfit2''' is the following,
in non-tilting cell. The input variable for '''calmisfit2''' has six more numbers
('''xmin''', '''xmax''', '''ymin''', '''ymax''', '''zmin''' and '''zmax''') than '''calmisfit''' to define a hexahedral volume which will be moved by the command. Those six numbers should be given in scaled coordinate. The first 10 numbers in the input variable are explained in the command '''calmisfit'''.


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The first ten parameters have the same meaning as those for '''calmisfit'''. The last 6 parameters specify the parallelepiped volume (enclosed by the solid lines in Fig. 4(a)) which will be shifted w.r.t. the remaining part of the crystal. The command '''calmisfit2''' also produces a text file, “Emisfit.out”, which has the same format as that produced by '''calmisfit'''. The same Matlab program (cal_idealstr.m) is able to compute the ideal strength using it as the input.
The command '''calmisfit2''' also produces a text file, “Emisfit.out” of the same
format and the same Matlab script will read it to calculate the ideal shear
strength.


<gallery caption="Fig.4" widths="300px" heights="300px" perrow="2">
<gallery caption="Fig.4" widths="300px" heights="300px" perrow="2">

Revision as of 06:55, 25 February 2008

Manual 09 for MD++
Computing Ideal Strength

Keonwook Kang and Wei Cai

Dec. 8, 2007


Ideal strength is the maximum stress that can exist in a perfect crystal. When the applied stress exceeds the ideal strength, the crystal structure will collapse even at zero temperature. The mode of failure depends on the type of applied stress. When the tensile stress exceeds the ideal tensile strength, the crystal is unstable against cleavage fracture. When the shear stress exceeds the ideal shear strength, the crysal is unstable against slip on crystallographic planes. Because a real crystal is not perfect but contains defects (such as surfaces, grain boundaries, dislocations, vacancies), which lowers the mechanical strength of the crystal, the ideal strength provides an upper bound of the strength of a real crystal. When the defect density is made sufficiently small (such as in whiskers), the strength of a real crystal can approach the ideal strength. The ideal strength is also called the theoretical strength.

There are two alternative definitions of the ideal strength depending on the way that the deformation is imposed on the perfect crystal structure. In the first definition, the deformation strain can be applied uniformly to the simulation cell (usually under periodic boundary conditions) resulting in an affine deformation of the entire crystal[1]. In the second definition, the deformation strain can be localized between two crystallographic planes[2]. The ideal strength values obtained from these two approaches are somewhat different but are also expected to co-relate with each other. In this manual, we describe how to compute the ideal strength according to the second definition, using diamond-cubic structure of Si as an example.


Ideal Tensile Strength

Suppose we want to compute the ideal tensile strength of Si along the [1 1 0] direction, i.e., Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \sigma_{[110]}^{\mathrm{th}}} . First, we create a simulation cell under periodic boundary condition (PBC) with the three periodicity vectors Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1 = N_x [1 1 0]} , Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2 = N_y[\bar{1} 1 0]} and . The coordinate system is defined such that , and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_3} are aligned along Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle x} , Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle y} and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle z} directions, respectively. The crystal just created is surrounded by its own images in all three directions.

Next, we change the length of the repeat vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1} while keeping the position of all atoms in the simulation cell fixed. Let Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1^0} be the original value of the repeat vector along the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle x} direction and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle L_x^0 = |\mathbf{c}_1^0|} . Suppose we assign the new repeat vector to be

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1 = \left( 1 + \frac{d}{L_x^0}\right) \mathbf{c}_1^0 } .

This will create a gap of width Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} between the crystal in the simulation cell (primary cell) with its images in the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle x} direction, as shown in Fig. 1(a). For each value of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} , we compute the potential energy of the crystal (without relaxing the positions of the atoms). The excess energy with respect to the case of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d=0} , dividied by the cross section area of the simulation cell perpendicular to the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle x} direction, is defined as function of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d}

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma = \gamma ( d ) } .

and is plotted in Fig. 2(a).

In MD++, the transformation of the simulation cell as described above can be performed conveniently using the command changeH_keepR. Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}} is a 3 by 3 matrix whose three columns correspond to the coordinates of the three repeat vectors, i.e. Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H} = [\mathbf{c}_1 | \mathbf{c}_2 | \mathbf{c}_3]} . The syntax for this command is 

input = [ i j frac ] changeH_keepR

This will lead to the following transformation of the repeat vectors

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_i := \mathbf{c}_i + frac \cdot \mathbf{c}_j } .

Since we want to change the length of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1} without changing its direction, both i and j should be 1 for computing the ideal tensile strength along Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle x} direction. (i and j will be different when computing the ideal shear strength as described in the next section.) A related command changeH_keepS performs identical transformations to the repeat vectors, but the scaled coordinates, instead of the real coordinates of the atoms are kept fixed. This will lead to an affine transformation of the simulation cell and is related to the first definition of the ideal strength as described above.

After the changeH_keepR, the potential energy is computed by the command eval. However, before computing the potential energy, we need to refresh the neighbor list. MD++ uses the Verlet list algorithm, in which the neighbor list is automatically refreshed whenever any atom is displaced by more than half the skin of the Verlet list since the last time the neighbor list is constructed. However, since here the atom positions do not change when we change the repeat vectors, the neighbor list will not be refreshed automatically. We can force the neighbor list to refresh by calling clearR0 right after the changeH_keepR command.

The MD++ script for this calculation is attached at the end of this manual. A few more commands are used there to facilitate the calculation. The saveH command saves the current value of the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}} matrix to Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}_0} . The restoreH command copies Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}_0} back to Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}} . This commands are used to make the matrix Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{H}} is always restored to the original value whenever the changeH_keepR command is called. The RHtoS command is always called before eval which converts the real coordinates Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{r}_i} of the atoms to the scaled coordinates Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{s}_i} , Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{s}_i = \mathbf{H}^{-1} \mathbf{r}_i} . This is needed because the calculation of potential energy in MD++ is based on the scaled coordinates.


  • Fig.1
  • (a) Creating a gap between the primary and image crystals on a (1 1 0) plane by changing the length of repeat vector '"`UNIQ--postMath-00000024-QINU`"'.

    (a) Creating a gap between the primary and image crystals on a (1 1 0) plane by changing the length of repeat vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1} .

  • (b) Sliding the primary and image crystals w.r.t. each other on a (1 1 1) plane by tilting the repeat vector '"`UNIQ--postMath-00000025-QINU`"' along the '"`UNIQ--postMath-00000026-QINU`"' direction.[2]

    (b) Sliding the primary and image crystals w.r.t. each other on a (1 1 1) plane by tilting the repeat vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} along the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1} direction.[2]


Fig. 2(a) plots the excess energy per unit area of the simulation cell, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma} , as a function of separation distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} for the Stillinger-Weber (SW) model of Si. For large enough Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} , Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma(d)} reaches a plateau, whose value is Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 2\gamma_s} , where Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma_s} is the (unrelaxed) surface energy of (1 1 0) plane of Si. The plateau is reached when Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} becomes greater than the cut-off distance of the interatomic potential. The slope of the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma(d)} has the unit of stress. The maximum slope of this curve can be interpreted as the maximum stress required to separate two rigid blocks of Si along the [1 1 0] direction, i.e. the ideal tensile strength. For the SW model of Si, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \sigma_{[110]}^{\mathrm{th}}} = 41.7 GPa.

  • Fig.2
  • (a) The excess energy per unit area as a function of the opening distance for the SW model of Si.

    (a) The excess energy per unit area as a function of the opening distance for the SW model of Si.

  • (b) The excess energy per unit area as a function of the slip distance for the SW model of Si.

    (b) The excess energy per unit area as a function of the slip distance for the SW model of Si.

Ideal Shear Strength

The procedure of calculating ideal shear strength is similar to that of ideal tensile strength except that we usually need to deal with two degrees of freedom. One is the amount of slip Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} in the plane of interest, and the other is the amount of openining Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} in the direction normal to the plane. The reason is that we usually need to allow Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} to relax when computing the ideal shear strength.

In this example, we will compute the ideal shear strength on a (1 1 1) plane of Si along the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle [1 0 \bar{1}]} direction, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \sigma^{\mathrm{th}}_{(111)[10\bar{1}]}} . We start by creating a perfect crystal with repeat vectors Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_1 = N_x[1 0 \bar{1}]} , Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2 = N_y[1 1 1]} and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_3 = N_z[1 \bar{2} 1]} .

Next, we perform the following change to the repeat vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} while keeping the real coordinates of the atoms fixed,

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \begin{align} \mathbf{c}_2 &= \left(1+ \frac{\delta}{L_z^0}\mathbf{c}_2^0 + \frac{d}{L_x^0}\mathbf{c}_1^0 \right) \\ &= (L_z^0 + \delta)\mathbf{n} + d\mathbf{m} \end{align} }

The excess energy per unit area is now a function of both the slip distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} and the openning distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta}

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma = \gamma ( d, \delta ) } .

For a given Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} , we can let the opening distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} to relax, which leads to a one dimensional function

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \Gamma = \displaystyle\min_{\{\delta\} }\gamma ( d ) } .

The minimization is performed numerically outside MD++, usually within Matlab, based on the 2-dimensional array output from MD++. Fig. 2(b) plots the function Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \Gamma(d)} for SW model of Si. Due to the periodicity of the lattice, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \Gamma(d)} is a periodic function, with the periodicity being the length of the Burgers vector. Again, the slope of the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \Gamma(d)} curve also has the unit of stress. The maximum slope is defined as the ideal shear strength, which is 9.5 GPa for the SW model of Si.

There are two different sets of (1 1 1) planes in a diamond-cubic crystal: the shuffle-set and the glide-set[2]. Since the sliding is localized between the atomic planes at the edge of the simulation cell, whether or not the ideal shear strength is computed on the shuffle-set or the glide-set plane depends on which plane is exposed at the edge of the simulation cell. This can be changed by periodically shifting the atomic structure within the simulation cell (through command pbcshiftatom) before calling changeH_keepR. The syntax for command pbcshfiftatom is 

input = [ dx dy dz ] pbcshiftatom

where dx, dy and dz are scaled coordinates of the shift vector. Since the [1 1 1] direction is along the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} direction, dy is the relevant parameter that will change the type of (1 1 1) plane exposed at the edge of the simulation cell. Whether or not pbcshiftatom is required and, if so, the necessary magnitude of dy can be determined by visually inspect the atomic structure in the X-window. The curves in Fig. 3(a) correspond to the shuffle-set plane[2]. The ideal shear strength on the glide-set plane (77.3 GPa for SW model of Si) is much higher than that on the shuffle-set plane.


Gamma Surface

The above procedure allows us to compute the ideal shear strength on a specified plane along a specific slip direction. However, there are two orthgonal directions within every plane along which slip can occur. The excess energy per unit area as a function of the two-dimensional slip vector can be visualized as a surface, and is usually called the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma} -surface, or the generalized stacking fault energy.

We have implemented a command calmisfit in MD++ that, together with an external Matlab program, computes the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma} -surface. The command calmisfit itself computes the misfit energy Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma} as a function of three parameters: two for the 2-dimensional slip vector within the plane and one for the opening displacement Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} perpendicular to the plane. The minimization w.r.t. Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} is performed in the Matlab program. The syntax for this command is 

 input = [ surfacenormal
           x0 dx x1
           y0 dy y1
           z0 dz z1 ]
 calmisfit

The input variable needs seven elements, the first of which indicates the surface normal index. For example, if surfacenormal = 2, the slip plane is normal to the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} vector. The following nine numbers specifies the range and incremental steps of the offset vector in three directions. In the case study shown in Figs. 1(b) and 2(b), x0, dx, x1 specify the range of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} , in units of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle |\mathbf{c}_1|/N_x} . y0, dy, y1 specify the range of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} , in units of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle |\mathbf{c}_2|/N_y} . Since we are not interested in slip along the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_3} direction, we have set z0 = dz = z1 = 0.

Command calmisfit produces a text output file “Emisfit.out”, which is then analyzed by the Matlab program cal_idealstr.m to perform minimization w.r.t. Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \delta} and to compute the ideal shear strength. The source code for the cal_idealstr.m program is attached at the end of this manual.

  • Fig.3
  • (a) A diamond-cubic structure with glide-set (1 1 1) plane exposed at the edge of the simulation cell (normal to '"`UNIQ--postMath-00000050-QINU`"'.

    (a) A diamond-cubic structure with glide-set (1 1 1) plane exposed at the edge of the simulation cell (normal to Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} .

  • (b) A diamond-cubic structure with shuffle-set (1 1 1) plane exposed at the edge of the simulation cell. The structures in (a) and (b) are identical unless slip occurs at the edge of the simulation cell by tilting repeat vector '"`UNIQ--postMath-00000051-QINU`"'.

    (b) A diamond-cubic structure with shuffle-set (1 1 1) plane exposed at the edge of the simulation cell. The structures in (a) and (b) are identical unless slip occurs at the edge of the simulation cell by tilting repeat vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} .

Computing Ideal Shear Strength without Tilting Simulation Cell

For technical reasons, sometimes we cannot tilt the repeat vectors in MD++ when computing the ideal shear strength. For example, the meam-baskes program requires linking the C-programs of MD++ with a set of Fortran programs (provided by Dr. Mike Baskes) that implements the MEAM potential. Unfortunately, the three repeat vectors are not allowed to tilt arbitrarily in these Fortran programs. In this case, the approach described above will no longer apply. A new algorithm is needed to compute the ideal shear strength and the Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \gamma} -surface. This is implemented in command calmisfit2.

calmisfit2 litterally moves one block of atoms w.r.t. to the remaining block of atoms, as shown in Fig. 4(a). This creates an interface between the two blocks of atoms. To avoid creating another (unwanted) interface at the periodic boundary, we need to remove several layers of atoms at the edge of the simulation cell before calling calmisfit2.

the procedures explained above can not be applied and we have to move a chunk of atoms literally. Fig. 4(a) shows the initial configuration in which a few layers at top and bottom are removed in order to have room for atoms to be shifted as shown in Fig. 4(b). Other than that, the rest of process to get the ideal shear strength is identical.

In MD++, we can remove a block of atom using commands fixatoms_by_position and removefixedatoms. The syntax is 

input = [enable x0 x1 y0 y1 z0 z1 ] fixatoms_by_position removefixedatoms

enable = 1 is required to activate the command, and the following 6 parameters specifies a parallelepiped volume (in scaled coordinates). All atoms within this volume will be labeled as fixed by the command fixatoms_by_positions. The following command removefixedatoms then removes these atoms. To remove two blocks of atoms at the top and bottom of the simulation cell, as shown in Fig. 4(a), the above commands need to be called twice with different input parameters.

The syntax for calling command calmisfit2 is the following, 

 input = [ surfacenormal
           x0 dx x1
           y0 dy y1
           z0 dz z1
           xmin xmax ymin ymax zmin zmax]
 calmisfit2

The first ten parameters have the same meaning as those for calmisfit. The last 6 parameters specify the parallelepiped volume (enclosed by the solid lines in Fig. 4(a)) which will be shifted w.r.t. the remaining part of the crystal. The command calmisfit2 also produces a text file, “Emisfit.out”, which has the same format as that produced by calmisfit. The same Matlab program (cal_idealstr.m) is able to compute the ideal strength using it as the input.

  • Fig.4
  • (a) Configuration to calculate the ideal shear strength in non-tilting simulation cell: (a) the initial configuration and (b) the shifted configuration

    (a) Configuration to calculate the ideal shear strength in non-tilting simulation cell: (a) the initial configuration and (b) the shifted configuration

  • (b)

    (b)

Script

The MD++ script and the Matlab script are given below for those who want to reproduce the results or try to calculate the ideal strength of other crystal materials. Let’s say MD++ script file name is “idealstr.tcl”. If you type 

$ bin/sw_gpp scripts/work/idealstr.tcl 0

it calculates the surface energy of (1 1 0) plane in terms of the opening distance Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle d} . If you type 

$ bin/sw_gpp scripts/work/idealstr.tcl 1

it calculates the misfit energy of (1 1 1) plane along Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle [1\, 0\, \bar{1}]} direction by tilting the periodicity vector Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \mathbf{c}_2} . If you type 

$ bin/sw_gpp scripts/work/idealstr.tcl 2

it will calculate the same misfit energy in different method explained in Sec. 3.


MD++ Script

# -*-shell-script-*-
source "scripts/Examples/Tcl/startup.tcl"
#*******************************************
# Definition of procedures
#*******************************************
proc initmd { } {
  MD++ setnolog
  MD++ setoverwrite
  MD++ dirname = runs/si_idealstr
  MD++ NIC = 200 NNM = 200
}

proc openwindow { } { MD++ {
# Plot Configuration
  atomradius = 0.67 bondradius = 0.3 bondlength = 0
  atomcolor = orange bondcolor = red backgroundcolor = gray70
  win_width = 300 win_height = 300
  plotfreq = 10 rotateangles = [ 0 0 0 1.25 ]
  plot_atom_info = 1 # reduced coordinates of atoms
#  plot_atom_info = 2 # real coordinates of atoms
#  plot_atom_info = 3 # energy of atoms
openwin alloccolors rotate saverot eval plot
} }

#*******************************************
# Main program starts here
#*******************************************
if { $argc == 0 } {
  set status 0
} elseif { $argc > 0 } {
  set status [lindex $argv 0]
}

puts "status = $status"

if { $status == 0 } {
# calculate surface opening energy on (1 1 0).
  initmd
  MD++ {
    element0 = Si latticeconst = 5.43095
    crystalstructure = diamond-cubic
    latticesize = [ 1 1 0 5
                   -1 1 0 5
                    0 0 1 7 ]
    makecrystal }
  MD++ saveH eval
  set Lx0 [MD++_Get H_11]
  set Ly0 [MD++_Get H_22]
  set Lz0 [MD++_Get H_33]
  set EPOT0 [MD++_Get EPOT]
  set Area [expr $Ly0 * $Lz0]
  set fileID [open "Esurf.dat" w]
  for {set i -10} {$i <= 100} {incr i} {
    set strain [expr $i/1000.0]
    MD++ restoreH RHtoS
    MD++ input = \[ 1 1 $strain \] changeH_keepR
    MD++ clearR0 # enforce refresh neighbor list
    MD++ eval
    set Lx [MD++_Get H_11]
    set dist [expr $Lx - $Lx0]
    set EPOT [MD++_Get EPOT]
    # Esurf2 : excessive energy per area to create 2 free surfaces.
    set Esurf2 [expr ($EPOT - $EPOT0)/$Area]
    puts $fileID "[format %18.14e $dist]\t \
                  [format %18.14e $Esurf2]"
  }
  close $fileID
  MD++ quit

} elseif { $status == 1 } {
# calculate generalized stacking fault energy on (1 1 1) along [1 0 -1]
  initmd
# surface normal direction 1/x 2/y 3/z
  set surfacenormal 2
  set lattconst 5.43095
  set c1 "1 0 -1"; set c2 "1 1 1"; set c3 "1 -2 1"
  set Nx 5; set Ny 4; set Nz 3

  set gridx " 0.000 0.005 0.500"
  set gridy "-0.050 0.010 0.150"
  set gridz " 0.000 0.050 0.000"

# write the matlab script
  set fileID [open "parameter.m" w]
  puts $fileID "normaldir = $surfacenormal"
  puts $fileID "latticeconst = $lattconst"
  puts $fileID "latticesize = \[ $c1 $Nx "
  puts $fileID "                 $c2 $Ny "
  puts $fileID "                 $c3 $Nz \]"
  puts $fileID "dxyz = \[ $gridx "
  puts $fileID "          $gridy "
  puts $fileID "          $gridz \]"
  close $fileID

  MD++ {
    element0 = Si
    crystalstructure = diamond-cubic
  }
  MD++ latticeconst = $lattconst
  MD++ latticesize = \[$c1 $Nx $c2 $Ny $c3 $Nz\]
  MD++ makecrystal

# To make shuffle set of (111) plane exposed
  MD++ { input = [0 0.05 0 ] pbcshiftatom }
  MD++ input = \[ $surfacenormal $gridx $gridy $gridz \]
  MD++ calmisfit
  MD++ quit

} elseif { $status == 2 } {
# calculate generalized stacking fault energy on (1 1 1) along [1 0 -1]
  initmd
# surface normal direction 1/x 2/y 3/z
  set surfacenormal 2
  set lattconst 5.431
  set c1 "1 0 -1"; set c2 "1 1 1"; set c3 "1 -2 1"
  set Nx 5; set Ny 6; set Nz 3
  set gridx " 0.000 0.005 0.500"
  set gridy "-0.050 0.010 0.150"
  set gridz " 0.000 0.050 0.000"
  set xmin -1.00; set xmax 1.00
  set ymin  0.01; set ymax 1.00
  set zmin -1.00; set zmax 1.00

# write the matlab script
  set fileID [open "parameter.m" w]
  puts $fileID "normaldir = $surfacenormal"
  puts $fileID "latticeconst = $lattconst"
  puts $fileID "latticesize = \[ $c1 $Nx "
  puts $fileID "                 $c2 $Ny "
  puts $fileID "                 $c3 $Nz \]"
  puts $fileID "dxyz = \[ $gridx "
  puts $fileID "          $gridy "
  puts $fileID "          $gridz \]"
  close $fileID

  MD++ {
    element0 = Si
    crystalstructure = diamond-cubic
  }
  MD++ latticeconst = $lattconst
  MD++ latticesize = \[$c1 $Nx $c2 $Ny $c3 $Nz\]
  MD++ makecrystal

  MD++ input = \[1 -1 1 0.4 1 -1 1 \] fixatoms_by_position removefixedatoms
  MD++ input = \[1 -1 1 -1 -0.42 -1 1 \] fixatoms_by_position removefixedatoms
  MD++ input = \[ $surfacenormal $gridx $gridy $gridz $xmin $xmax $ymin $ymax $zmin $zmax \]
  MD++ calmisfit2

  openwindow
  MD++ sleep quit
  MD++ quit

} else {
puts "unknown status = $status"
MD++ quit
}

Matlab Script

After running MD++, you just run the following matlab script in the directory where the output files exist. Then the matlab script will plot the energy curve and calculate ideal strengths. 

%#! /usr/local/bin/octave -qf
% Matlab script, cal_idealstr.m
% to calculate ideal tensile strength "sigma" and shear strength "tau"
clear

%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
% calculate ideal tensile strength along [110] direction
%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
data = load(’Esurf.dat’);
d = data(:,1);     % openning distance in A
gamma = data(:,2); % excessive energy per area creating 2 free surfaces (eV/A^2)

sigma = max(gamma(2:end)-gamma(1:end-1))/(d(2) - d(1)) * 160.2;
disp(sprintf(’Ideal tensile stregnth = %e(GPa)’,sigma));

figure(1)
set(gca,’fontsize’,14)
plot(d, gamma, ’.-’), grid
xlabel(’Opening Distance \it d \rm(Angstrom)’,’fontsize’,16),
ylabel(’\gamma (eV/Angstrom^2)’,’fontsize’,16)
line([-1 1.1],[gamma(end) gamma(end)],’linewidth’,2,’color’,’k’)
text(-1.3, gamma(end),’2\gamma_s’,’fontsize’,16)

%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
% calculate ideal shear strength on (111) along [110] direction
%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
if (~exist(’parameter.m’,’file’))
    error(’No parameter.m found’)
else
    parameter

    dx = dxyz(1,2); dy = dxyz(2,2); dz = dxyz(3,2);
    vx = latticesize(1,1:3); Lx = latticeconst*norm(vx);
    vy = latticesize(2,1:3); Ly = latticeconst*norm(vy);
    vz = latticesize(3,1:3); Lz = latticeconst*norm(vz);

    data = load(’Emisfit.out’);
    Mx=max(data(:,1)); My=max(data(:,2)); Mz=max(data(:,3));

%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
% convert data to relaxed energy
    MM=-sort(-[Mx+1,My+1,Mz+1]);         % Then MM(1) > MM(2) > MM(3)
    E = reshape(data(:,4),MM(1),MM(2));

    Erlx = zeros(MM(1),1);
    Zrlx = zeros(MM(1),1);

    normalgrid = dxyz(normaldir,1):dxyz(normaldir,2):dxyz(normaldir,3);
    normalfinegrid = dxyz(normaldir,1):dxyz(normaldir,2)/1000:dxyz(normaldir,3);

    for i = 1:MM(1),
        a = E(i,:);
        a_interp = interp1(normalgrid,a,normalfinegrid,’spline’);
        [Erlx(i), ind] = min(a_interp);
        Zrlx(i) = normalfinegrid(ind);
    end

% retrieve unrelaxed energy
    Eunrlx=E(:,find(abs(normalgrid)<1e-8));

% calculate ideal shear strength
    tau = max(Erlx(2:end)-Erlx(1:end-1))/(dx*Lx) * 160.2;
    disp(sprintf(’Ideal shear stregnth = %e(GPa)’,tau));

    figure(2); set(gca,’fontsize’,14)
    plot([0:Mx]/Mx, Erlx-Erlx(1), ’b.-’,...
         [0:Mx]/Mx, Eunrlx-Eunrlx(1),’r-’);
    legend(’relaxed’,’unrelaxed’);
    xlabel(’Sheared Distance, d/|b| where b = [1 0 1]/2’,’fontsize’,16)
    ylabel(’\Gamma (eV/Angstrom^2)’,’fontsize’,16)

    figure(3); set(gca,’fontsize’,14)
    plot([0:Mx]/Mx,Zrlx, ’r.-’, ...
         [0 1],[1 1]*dxyz(normaldir,1),’b-’,...
         [0 1],[1 1]*dxyz(normaldir,3),’b-’);
    xlabel(’Sheared Distance, d/|b| where b = [1 0 1]/2’,’fontsize’,16)
    ylabel({’Lowest energy height,’; ’\delta/|c_2| where c_2 = [1 1 1]’},’fontsize’,16)
end

Notes

  1. ↑ D. Roudy and M. L. Cohen, Phys. Rev. B 64 212103 (2001))
  2. ↑ 2.0 2.1 2.2 2.3 Keonwook Kang and Wei Cai, Philosophical Magazine, 87 2169–2189 (2007)
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