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Scientific Reports logoLink to Scientific Reports
. 2021 Feb 12;11:3711. doi: 10.1038/s41598-021-83227-8

Faceted-rough surface with disassembling of macrosteps in nucleation-limited crystal growth

Noriko Akutsu 1,
PMCID: PMC7881209  PMID: 33580162

Abstract

To clarify whether a surface can be rough with faceted macrosteps that maintain their shape on the surface, crystal surface roughness is studied by a Monte Carlo method for a nucleation-limited crystal-growth process. As a surface model, the restricted solid-on-solid (RSOS) model with point-contact-type step–step attraction (p-RSOS model) is adopted. At equilibrium and at sufficiently low temperatures, the vicinal surface of the p-RSOS model consists of faceted macrosteps with (111) side surfaces and smooth terraces with (001) surfaces (the step-faceting zone). We found that a surface with faceted macrosteps has an approximately self-affine-rough structure on a ‘faceted-rough surface’; the surface width is strongly divergent at the step-disassembling point, which is a characteristic driving force for crystal growth. A ‘faceted-rough surface’ is realized in the region between the step-disassembling point and a crossover point where the single nucleation growth changes to poly-nucleation growth.

Subject terms: Theory and computation, Scaling laws, Nonlinear phenomena, Phase transitions and critical phenomena

Introduction

Determining surface roughness is crucial for understanding many phenomena associated with crystal surfaces113. However, developing methods to measure surface roughness has proven to be not as straightforward as had been expected14,15. The roughness of a surface is defined by the variance of the surface height associated with the roughening transition on low Miller-index surfaces such as the (001) surface at equilibrium14,15. The roughening transition belongs to the Berezinskii–Kosterlitz–Thouless (BKT)1622 universality class. Denoting the roughening transition temperature of the (001) surface as TR(001), the (001) surface is rough for temperatures TTR(001), where the square of the surface width W2(L) is logarithmically divergent with respect to the linear system-size L. For T<TR(001), the (001) surface is smooth and the surface width is constant and does not depend on the system size.

It has been believed that a faceted surface is necessarily smooth. The roughening transition is connected to the faceting transition at equilibrium2328. For a small crystal droplet, the shape of the droplet with the least surface free energy is the equilibrium crystal shape (ECS), which is obtained by the Wulff construction29,30 or by the Andreev method3133. On the ECS, the faceting transition occurs at the roughening transition temperature. The Gaussian curvature on the ECS is proportional to W2(L)/lnL and the inverse of the determinant of the surface stiffness tensor25. Hence, for T<TR(001), the Gaussian curvature of the (001) surface is zero, and the (001) surface then appears on the ECS as a facet. The ECS consists of facets of smooth surfaces and curved rough vicinal surfaces.

For “sharp” but rough surfaces at non-equilibrium, the self-affinity on a surface obtained by a symmetry principle argument can explain a wide range of surfaces or interface phenomena3439. Here, a “sharp” surface means an atomically smooth surface locally. Hence, the surface height is well defined as h(xy) at a site (xy) on a 2D square lattice. Self-affinity is invariance under anisotropic scale transformations, in contrast to self-similarity, which is invariance under isotropic scale transformations. Using the surface height h(xy), the surface width W(Lt) is defined by

W(L,t)=[h(x,y)-h(x,y)]2, 1

where t is time and · is an ensemble average. The surface width W(Lt) for a kinetically roughened surface is known to satisfy a Family–Vicsek scaling relation35,36:

W(L,t)Lαf(L-zt),z=α/β, 2

where the α, β, and z exponents are referred to as the roughness, growth, and dynamic exponents, respectively. In the non-equilibrium steady-state (in the limit t), the surface width W becomes W(L)Lα. The theoretical values of α for a 2D surface in 3D are 0 and 0.386 for the BKT-rough and the Kardar–Parisi–Zhang (KPZ)-rough40,41 surfaces, respectively.

Although the Family–Vicsek scaling relation can explain many cases of algebraic divergence of surface or interface width, the KPZ exponent is rarely observed in crystal growth36,41,42. For example, a recent experiment on thin film growth of CdS43 showed a roughness exponent α of 0.78±0.07.

Faceted-like rocky and “rough” crystal shapes such as SiC7, Si35, or faceted-like dendritic shapes such as snowflakes1, are commonly observed crystal formations. The branching dendrites seen in snowflakes are caused by the Mullins–Sekerka (MS) instability44 in the thermodynamic scale. The tip velocity of a dendrite obeys a universal behaviour based on MS-instability1,45. Interestingly, the branching of the tip of a dendrite for a faceted surface also seems to obey a universal behaviour. However, the reason for the similarity between tip branching for a faceted shape and a rough surface has not been studied sufficiently.

To reproduce a faceted-like shape of a crystal for “diffuse” and rough surfaces, many phase-field models have been applied4649. The most recent phase-field model and calculations on ice49 reproduced the 3D faceted shapes, including snowflakes. Here, a “diffuse” surface means an “atomically rough” surface, originating from a liquid–gas interface21,50,51. An example of a diffuse (atomically rough) but smooth surface is the (0001) surface of 4He crystals in superfluid helium52. The (110) surfaces of Ag2Se and Ag2S53,54 and the (100) and (111) surfaces of tetrabrommethane55 are considered to be examples of diffuse but globally smooth surfaces at lower temperatures than the roughening transition temperatures. Since the phase-field model applies for the mesoscopic scale, it reproduces the MS instability automatically under appropriate boundary conditions.

However, the problem with phase-field modelling is the connection between the phenomenological parameters in the basic equations of the phase-field model and the physical quantities based on the atomic surface structure4649.

The aim of this article is to clarify whether a vicinal surface with faceted macrosteps can have a self-affine-rough structure in nucleation-limited crystal growth. We will show how sharp and faceted surfaces at equilibrium can roughen while keeping a faceted structure. The squared surface width is calculated using the Monte Carlo method on the vicinal surface tilted from the (001) surface to the (111) surface. To set up faceted macrosteps at equilibrium, the restricted solid-on-solid model with point-contact-type step–step attraction (p-RSOS model)33,5664 is adopted (refer to the section “Methods”). The temperature is set in the step-faceting zone59, where the surface tension is discontinuous, and only the (001) surface and (111) surface are thermodynamically stable at equilibrium.

Results

Faceted-rough surface

Figure 1a shows the Δμ dependence of gW2 (Eq. (15)). gW2 has a maximum at Δμ=ΔμR(L) (Table 1)63. The maximum value increases as the system size increases. gW2 increases as L increases for Δμco(poly)(L)<Δμ<ΔμR(L), contrary to the expectation that gW2 is independent of system size for Δμ<ΔμR(L). Here, ΔμR(L) is the crossover point from a vicinal surface with (111) faceted macrosteps to a tilted surface with locally merged steps, and Δμco(poly)(L) is the crossover point from single nucleation growth to poly-nucleation growth at the lower edge of a faceted macrostep63. In the region Δμco(poly)(L)<Δμ<ΔμR(L), the vicinal surface of the p-RSOS model grows in a step-detachment process in the manner of 2D poly-nucleation at the lower edge of a faceted macrostep63,64.

Figure 1.

Figure 1

Δμ dependence of the square of the surface width gW2, where Δμ is the driving force for crystal growth. g is 1+p¯2, where p¯=32/80.530 is the mean surface slope. ϵint/ϵ=-0.9. kBT/ϵ=0.4. a=1. (a) gW2, with a maximum value at ΔμR(L). The lines represent different sizes and are generated from Eqs. (6)–(12). (b) gW2 scaled by Lα with α=0.385, which is the 2D KPZ roughness exponent in 3D. (c) Y(x, L) (Eq. (6)) scaled by Lα with α=0.25.

Table 1.

Characteristic driving forces. ϵint/ϵ=-0.9.

Value/ϵ Description
Δμy(L) 0.016 Yielding point of the self-detachment of steps from a macrostep63
Δμco(poly)(L) 0.049 Crossover point from single 2D nucleation mode to 2D poly-nucleation mode63
ΔμR(L) 0.124 Transition point between the step-assembled phase and the step-disassembled phase62,63
Δμco(B-K) 0.3 Crossover point between BKT-rough surface and KPZ-rough surface (ϵint=0, RSOS)65
Δμkr(001) 1.15 Kinetic roughening point for the (001) surface65

Surface slope p¯=32/80.530. L=4002a (a=1) for Δμy(L), Δμco(poly)(L), and ΔμR(L).

Figure 2 shows a typical morphology of a vicinal surface in the region Δμco(poly)(L)<Δμ<ΔμR(L) (see also Figs. S1b, and S2a,b). From the side view of the surface, we can see that the surface is covered with (111) side-surfaces and (001) terrace-surfaces. From the top view of the surface, islands with rounded triangle shapes are seen at the lower edge of the faceted macrosteps. Though the vicinal surface seems to be covered with smooth (001) and (111) surfaces, we can confirm that the surface grows continuously under the non-equilibrium steady state63,64. Hence, we call this surface structure for Δμco(poly)(L)<Δμ<ΔμR(L) the faceted-rough surface.

Figure 2.

Figure 2

Typical morphology of a faceted-rough surface: snapshot generated by the Monte Carlo method at 4×108 MCS/site. kBT/ϵ=0.4. Δμ/ϵ=0.08. ϵint/ϵ=-0.9. Size: 4002a×4002a. Nstep=300. p¯=Nstepa/L=32/80.530. ld (mean equal distance between 2D nuclei 63), lc, and td are 28a, 13a, and 1.44×103MCS/site (Eq. (4)). Inset: Illustration of a step-detachment mode in a poly-nucleation process at the edge of a faceted macrostep.

Nucleation-limited continuous growth

Figure 3 shows the driving force dependences of the surface velocity V and kinetic coefficient k, where k=Vτϵ/(Δμa), τ=1 is the time for an MCS/site, and a=1. In contrast to the surface width, V and k do not depend on the system size except at the region near equilibrium. V and k are similar to the original RSOS model for Δμ/ϵ>1 in the previous work65. This means that for Δμ/ϵ>1, steps are well separated in most cases (Figs. S1 and S2e,f). It should be noted that the critical nucleus sizes with a square shape are 2 and 1 for Δμ/ϵ of 1 and 2, respectively. For 0.3<Δμ/ϵ<1.0, k increases approximately linearly with respect to Δμ, which gives VΔμ2. For ΔμR(L)<Δμ/ϵ<0.3 where the surface is rough with locally faceted macrosteps (Figs. S1 and S2c,d), k decreases rapidly as Δμ decreases.

Figure 3.

Figure 3

(a,b) Driving force dependence of the surface growth velocity. (c,d) Driving force dependence of the kinetic coefficient. kBT/ϵ=0.4. ϵint/ϵ=-0.9. p=Nstepa/L=32/80.530. θ=27.9 °.

In the region with a faceted-rough surface and for a rough surface with locally faceted macrosteps (Δμ/ϵ<0.3), the vicinal surface grows in the 2D nucleation process at the lower edge of a faceted macrostep63,64. The mean height of a faceted macrostep n obeys the equation

n/t=n+-n-, 3

where n+=vnp/a is the attachment rate of elementary steps to the faceted macrostep, vn is the growth velocity of an elementary step, p is the surface slope on a “terrace”, a is the lattice constant, and n- is the detachment rate of an elementary step from the faceted macrostep. n- is determined by the 2D poly-nucleation rate at the lower edge of the faceted macrostep63,64. At steady state, n/t=0, and n+=n-. The surface slope on a “terrace” is determined by n-, so that the step-attachment rate balances the step-detachment rate.

To understand the poly nucleation rate near equilibrium, a characteristic length ld is introduced, representing the mean equal distance at which critical nuclei arise at the edge of a macrostep (inset in Fig. 2). The nuclei grow to merge with neighbouring nuclei after a time td, at which point a step detaches from the macrostep. The mean step-detachment time td, which is a characteristic time, is then expressed as63,66 td=ld/(2vt)=1/(Inld), where vtΔμ is the step zipping velocity and In is the 2D nucleation rate at the step edge. Then, we obtain for 0.05<Δμ/ϵ<0.1563

td=C2vtZexp{(g/2)/[Δμ-Δμy(L)]},2ZC=ck2kstep(Δμ),ck=0.604,kstep(Δμ)=vtϵ/Δμ=0.094+exp[-5.8+0.18ϵ/Δμ],V=a/td,ld=2vttd, 4

where g/Δμ=G(lc)/kBT, G(lc) is the total step free energy of a critical nucleus at the macrostep-edge with critical size lc, Z is the Zeldovich factor, C is a coefficient, kstep(Δμ) is the kinetic coefficient for an elementary step, V is the surface growth velocity, and a (=1) is the height of an elementary step. Here, Δμy(L) is a correction term introduced in our previous work63 to ensure that the surface velocity agrees with that obtained by the classical 2D nucleation theory. The Monte Carlo results are well reproduced by Eq. (4) for 0.05<Δμ/ϵ<0.1563. When Δμ decreases and approaches Δμy(L), the surface growth velocity V decreases, whereas td and ld increase, based on Eq. (4).

For L>ld and t>td, the vicinal surface grows continuously. While for L<ld, the surface grows intermittently in the manner of a 2D single nucleation process at the macrostep edges due to the finite size effect (Fig. S1a). Δμco(poly) is approximately estimated by

ld(Δμco(poly))L. 5

Roughness exponents

Figure 1b shows the ratio of gW to L0.385. The obtained results do not depend on the initial configuration. This is in contrast to the mean-height of a faceted macrostep n, which is known to be sensitive to the history of the surface configuration63,64. As seen from Fig. 1b, the lines for Δμ/ϵ>1.8 for different system sizes coincide. The power 0.385 is a universal value for the roughness exponent α for 2D KPZ-rough surfaces in 3D. Therefore, a vicinal surface for Δμ/ϵ>1.8 is KPZ-rough.

In our previous work on the original RSOS model65, where ϵint=0, the vicinal surface for Δμ/ϵ>1.8 is shown to be KPZ-rough. Around Δμ/ϵ1, a broad peak is observed corresponding to the kinetic roughening point Δμkr(001)/ϵ for the (001) surface. However, such a peak is not observed for p-RSOS. Instead, there is a sharp peak at ΔμR(L), which is less than (1/5)Δμkr(001) of the RSOS model.

For ΔμR(L)<|Δμ|<0.4ϵ, gW2 shows algebraic growth for lengths less than 200a. A typical case is shown in Fig. 4 for Δμ/ϵ=0.2. At a small scale, gW2 increases as L0.95. The value of the exponent agrees with that for a zigzag structure of a 1D single step on a surface. Since relatively large locally merged steps remain, the value of the exponent indicates that the merged steps shift location in a “wiggly” manner, as if they were single steps.

Figure 4.

Figure 4

Size dependence of gW2. kBT/ϵ=0.4. ϵint/ϵ=-0.9. p¯=32/80.530. a=1.

At a scale larger than 200a, the slope changes. We will return to this point in the following subsection.

For the faceted-rough region Δμco(poly)<Δμ<ΔμR(L), gW2 shows an approximate algebraic increase as the system size L increases for large L (Fig. 4). For large lengths 5.5<lnL<7, the Monte Carlo results were fitted to lngW2=2lnw0+2αplnL by the least square method. The obtained values are listed in Table 2. Irrespective of temperature, αp has values between 0.58 and 0.79. These values are about twice the KPZ-universal value of 0.386. Hence, the roughness of a faceted-rough surface is larger than the roughness of the original RSOS model. For large L, the vicinal surface is approximately self-affine. It is interesting that many observed values on the vicinal surface at nanometer scale are similar to those of the roughness exponent36,41. In a real system, a length 4002a with a4Å corresponds to about 230 nm.

Table 2.

Roughness exponent α and provisional roughness exponent αp.

kBT/ϵ=0.4 kBT/ϵ=0.2
Δμ/ϵ αp w0/a Δμ/ϵ αp w0/a
0.06 0.58 0.016 0.2 0.71 0.022
0.08 0.78 0.010 0.25 0.72 0.041
0.1 0.77 0.017 0.275 0.68 0.059
0.12 0.67 0.036 0.3 0.59 0.11
ΔμR/ϵ α ΔμR/ϵ α
0.090 0.60 0.27 0.59

2402aL4002a. ϵint/ϵ=-0.9. p¯=32/80.530.

As shown in Fig.  4, the roughness depends on the length scale (refer to the following subsection). For relatively small Δμ, this change of roughness can be seen clearly. For Δμ/ϵ=0.06, where ld=125a and td=6.7×103 [MCS/site], the vicinal surface is smooth for lengths less than ld/2 (Fig. S1a). While L increases to over ld, gW2 increases algebraically. The slope of the lines becomes slightly steeper as L increases. Therefore, we conclude that faceted-rough surfaces consist of faceted structures at lengths less than ld/2, whereas faceted-rough surfaces have approximately self-affine structures larger than ld.

Scaling function for step-disassembly

To explain why the provisional roughness exponent αp gradually changes, we further analyse the driving force dependence of the surface width.

We assume that gW2 is expressed by the following equation:

gW2=gW2(p1)+Y2(x,L), 6

where gW2(p1) represents the contribution from the “terrace” between the faceted macrosteps with slope p1, Y2(x,L) represents the contribution from step-disassembling/assembling of the macrosteps, and x is an inverse-driving-force distance derived from the maximum value of gW2 as x=ϵ/Δμ-ϵ/ΔμR(L).

At equilibrium, p1=0; whereas p1 increases as Δμ increases when Δμ exceeds a characteristic value Δμy(L). This is because an elementary step detaches from the lower edge of a faceted macrostep periodically on average (Eq. (4)). The slope dependence of gW2(p1) at kBT/ϵ=0.4 is expressed by65:

gW2(p1)=[ln(L/a)](A+Blnp1)2,A=0.319,B=0.0650. 7

It should be noted that A and B for kBT/ϵ=0.2, 0.4, and 1.7 at equilibrium are the same within errors, as stated in Ref.65.

The Δμ dependence of the surface slope p1 is obtained by the following equation63:

p1=cp|Δμ/ϵ|exp-gp/2|Δμ/ϵ|-Δμyp(L)/ϵ, 8

where cp, gp, and Δμyp(L) are fitting parameters. It should be noted that the set of values {g,Δμy(L)} in Eq. (4) and Table 1 were obtained by fitting Monte Carlo data to Eq. (8) in the fitting region 0.05<Δμ/ϵ<ΔμR(L)/ϵ0.1463. To describe the Δμ dependence of p1 in the range 0.055Δμ/ϵ0.4, the Monte Carlo data is re-fitted to Eq. (8), giving cp=0.357, gp=0.294, and Δμyp(4002)=0.026ϵ.

We found that Y2(x,L) has a maximum at ΔμR(L), and Y(xL) is approximated by a Gaussian function for Δμco(poly)<Δμ/ϵ<0.4 (Fig. 5), as follows:

Y(x,L)=Ymax(L)exp[-Bx2]. 9

Figure 5.

Figure 5

kBT/ϵ=0.4. ϵint/ϵ=-0.9. p¯=32/80.530. a=1. (a) Scaling function for step-disassembly. Y(xL) follows Eq. (6) with Eqs. (7) and (8). The line follows Eq. (10). (b) Log–log plot of the linear system size L and the difference between ΔμR and ΔμR, where ΔμR is ΔμR in the limit L. Inset: log–log plot of Ymax and L, where Ymax is the value Y(0, L) (Eqs. (11) and (12)). Blue triangles and pink line: kBT/ϵ=0.2. Red squares and light blue line: kBT/ϵ=0.4.

We introduce a scaling function Y(x) such that:

Y(x)=Aexp(-Bx2), 10
Ymax(L)=A(L/a)ζ, 11
ΔμR(L)/ϵ=(ΔμR+A(L/a)-χ)/ϵ. 12

The values of A, A, B, ΔμR, ζ, and χ are listed in Table 3.

Table 3.

Scaling parameters.

kBT/ϵ=0.4 kBT/ϵ=0.2
ζ (=α) 0.60 0.59
χ 0.69 0.67
A 2.7 2.0
A 0.051 0.065
B 0.025 1.26

ϵint/ϵ=-0.9. p¯=32/80.530. Eqs. (9)–(12).

The shape of Y(x) is shown in Fig. 5a by a black line. The Monte Carlo data and Y(x) agree well around |x|=ϵ|1/Δμ-1/ΔμR(L)|<5. For x>5, the surface grows in the single nucleation mode. Hence, the data strays from the line of Y(x). Since the change to the single nucleation mode is a finite size effect, the data for the smaller size begins to deviate for smaller x from the scaling function. For x<-5, faceted macrosteps disassemble to become locally merged steps.

The power law behaviours of ΔμR(L) (Eq. (12)) and Ymax (Eq. (11)) are shown in Fig. 5b. The data agree well with the lines. From the slope of the lines, we obtained ζ and χ. The powers ζ and χ at different temperatures agree well.

The lines calculated using Eq. (6) for Δμ and L with Eqs. (9)–(12) are shown in Fig. 1. The lines reproduce the Monte Carlo results well for Δμco(poly)<Δμ/ϵ<0.4. For kBT/ϵ=0.2, gW2 is similar to the case for kBT/ϵ=0.4. It is interesting that the values of χ and ζ are similar for the cases of kBT/ϵ=0.4 and 0.2. This suggests that the step-disassembling phenomenon around ΔμR is a universal phenomenon. In addition, the point ΔμR is a candidate for the non-equilibrium phase transition point.

Unexpectedly, as seen from Fig. 1c, Y(xL) calculated by Eq. (6) from the Monte Carlo data shows algebraic divergence with respect to L with a roughness exponent α=0.25. The Y(x,L)/(L/a)0.25 line for each size agrees well with the others for 0.4<Δμ/ϵ<1.6. If gW is simply divided by (L/a)0.25, the gW2Δμ lines do not coincide with each other. The value α=0.25 is the same as that for the tracer diffusion on a 1D lattice67. However, the physical connection between the tracer diffusion and the present case is unclear. This is left as a problem for a future study.

ζ agrees with the roughness exponent α in the limit L. The maximum of Y2(x,L) diverges with exponent L2ζ in the limit L (Eq. (11), Table 2). For L around ΔμR(L), gW2 increases asymptotically as gW2L2ζ. This also means that αpζ for L. Therefore, ζ is the roughness exponent α in the limit L.

For the L dependence of αp around ΔμR(L), since dY(x,L)/Y(x,L)[ζ+2ABxχ(L/a)-χ(ΔμR(L)/ϵ)-2]dL/L from Eqs. (9)–(12), we obtain

αpα+x[2ABχ(L/a)-χ](ΔμR/ϵ)-2+O((L/a)-2χ). 13

The second term in the right-hand side of Eq. (13) indicates the contribution from the shift of ΔμR(L). For Δμ<ΔμR(L) with x>0, αp becomes larger than α. However, for ΔμR(L)<Δμ with x<0, αp becomes smaller than α.

Discussion

The results for faceted-rough surfaces can explain why the giant Naica gypsum (CaSO4· 2H20)911 has a euhedral shape with a large size and high transparency. From laser confocal differential interference contrast microscopy (LCM-DIM) and atomic force microscopy (AFM) observations10, the gypsum surface was found to grow by a 2D nucleation process at the microscopic scale. The giant planar {010} surfaces of the crystal faces were found to consist of a hillock structure at the mesoscopic scale. The side surface of a hillock is a (100) surface, which grows very slowly. Such a slow growth is realised close to equilibrium. The surface is near equilibrium and the size of the critical nucleus is large, and therefore the time between formation of individual nuclei is long. Hence, inhomogeneity of inclusions should occur, which would cloud the crystal.

The continuous growth for the faceted-rough region in this work is possible for Δμ(poly)(L)<Δμ, where Δμ(poly)(L) is given by Eq. (5). Physically, Δμ(poly)(L) can be interpreted as a smaller limit of the driving force for poly-nucleation at the lower edge of a faceted macrostep. When the size is larger, Δμ(poly)(L) decreases. As pointed out by Alexander et al.10, 2D nucleation at the “valley” of the hillock, which is a concave line on the surface and corresponds to the lower edge of a faceted macrostep, has a lower activation energy than 2D nucleation on the {010} terrace surface. A similar 2D nucleation from the lower edge of a macrostep is observed experimentally for diamond68. These observed 2D nucleations at the lower edge of a macrostep are consistent with the present Monte Carlo results for a faceted-rough surface. Since the activation energy for 2D nucleation is significantly smaller than that on a terrace, continuous growth is possible. This contributes to keeping the inclusions homogeneous.

In addition, since the roughness exponent is α=0.6<1, W/L converges to zero in the limit L. This means that the hillocks have an approximate self-affine structure, while the hillocks’ area converges to zero in a large length limit. Therefore, the giant gypsum has a euhedral shape and high transparency.

The faceted-rough surface in the present study may provide a connection between the strong anisotropic parameters in the phase-field modellings and the parameters for the atomic scale. The p-RSOS model has sharp surfaces and the height h(xy) is well defined. However, when a surface is rough, the location of the surface becomes ambiguous. Hence, we consider the mean height of the surface and the variance of the height of the surface, which is divergent with respect to the system size L.

At equilibrium, W2/lnL asymptotically equals the inverse of the determinant of the surface stiffness tensor25 of the BKT rough-surface in the limit L. For a smooth surface, since W2/lnL converges to zero in the large L limit, the determinant of the stiffness tensor is divergent, and the Gaussian curvature on the ECS should be zero.

At non-equilibrium in the faceted-rough region, if we regard the amplitude w0=(W/Lαp) as a local degree of roughness, we can explain the anisotropy of the local roughness of the faceted-rough surface. In the faceted-rough region, w0 is 0.01–0.03, as seen from Table 2, whereas w0 for a non-faceted vicinal surface is 0.0865,69. This anisotropy in w0 is consistent with the anisotropies which were phenomenologically assumed4749.

The results in the present study are consistent with the phenomena observed for Si melt–solid interfaces. In the case of Si melt growth, faceted dendrites5 similar to a rough surface or a faceted saw-like shape larger than 10 μm in length are known to appear on a vicinal interface during fast crystal growth, whereas the vicinal interface is planar for slow crystal growth3. Studies on Si melt growth have shown that the faceted plane is close to the (111) surface. Hence, the faceted surface was considered to be smooth and the surface grows in the 2D nucleation process. Nevertheless, the faceted saw-like shape was shown to be formed by MS instability44,45 by the observation of a negative temperature gradient before the solid–liquid interface4. The MS instability should be applicable to a rough surface45. This observed conflict may be solved by the present study. In the present work, we showed that the interface can be rough while maintaining a self-affine faceted macrostep structure near equilibrium with a 2D poly-nucleation process at the macrostep edges. Further experimental studies are expected.

Conclusions

  • In the faceted-rough region, a surface is smooth and faceted on the small scale, whereas at large scales, surfaces are rough and statistically self-affine with a roughness exponent of α=0.60.

  • The surface width W has a maximum at ΔμR(L), where ΔμR(L) is the step disassembling point and L is the linear size of the system. The maximum value of W diverges as Lζ with ζ=0.60±0.02. ζ agrees with α in the limit L. ΔμR(L) is much closer to the equilibrium than the kinetic roughening point of the terraces.

  • ΔμR(L) converges to ΔμR in the limit L. ΔμR is a candidate for the non-equilibrium phase transition point.

  • A faceted-rough vicinal surface is realized for Δμco(poly)(L)<Δμ<ΔμR(L), where Δμco(poly)(L) is the crossover point between the 2D single nucleation mode and the successive poly-nucleation mode at the lower edge of a faceted macrostep. In this region, the provisional roughness exponent is 0.58<αp<0.79.

Methods

p-RSOS model

The surface energy of a vicinal surface around the (001) surface is expressed by the following discrete Hamiltonian:

Hp-RSOS=Nϵsurf+n,mϵ[|h(n+1,m)-h(n,m)|+|h(n,m+1)-h(n,m)|]+n,mϵint[δ(|h(n+1,m+1)-h(n,m)|,2)+δ(|h(n+1,m-1)-h(n,m)|,2)]-n,mΔμh(n,m), 14

where h(nm) is the surface height at site (nm), N is the total number of lattice points, ϵsurf is the surface energy per unit cell on the planar (001) surface, and ϵ is the microscopic ledge energy. The summation with respect to (nm) is taken over all sites on the square lattice. The RSOS condition, in which the height difference between the nearest neighbouring sites is restricted to {0,±1}, is required implicitly.

The third and fourth terms in the right-hand side of Eq. (14) represent the point-contact-type step–step attraction. Here, δ(a,b) is the Kronecker delta and ϵint is the microscopic point-contact-type step–step interaction energy. ϵint contributes to the surface energy only at the collision point of neighbouring steps where the height difference can be ±2. When ϵint is negative, the step–step interaction becomes attractive (sticky steps). Quantum mechanically, ϵint is regarded as the energy gain by forming a bonding state between the dangling bonds at step edges at the collision point of neighbouring steps.

The fifth term in the right-hand side of Eq. (14) represents the driving force for crystal growth. Here, Δμ is μambient-μcrystal, where μambient and μcrystal are the bulk chemical potentials in the ambient phase and the crystal, respectively. At equilibrium, Δμ=0; for Δμ>0, the crystal grows, while for Δμ<0, the crystal shrinks. Explicitly, Δμ is expressed by kBTlnP/Peq for an ideal gas and by kBTlnC/Ceq for an ideal solution, where kB is the Boltzmann constant, T is temperature, P is vapour pressure, Peq is the vapour pressure at equilibrium, C is the solute-concentration, and Ceq is the solute-concentration at equilibrium. If P/Peq or C/Ceq is expressed by 1+σsat, where σsat is the super saturation, ΔμkBTσsat for σsat<<1.

The p-RSOS model is a coarse-grained model relative to the model for first-principle quantum mechanical calculations, but it is a microscopic model relative to the phase-field model. In the p-RSOS model (Eq. (14)), the step–step attraction ϵint is the origin of the discontinuous surface tension. The surface energy Esurf corresponds to the surface free-energy, which includes entropy originating from lattice vibrations and distortions70. ϵ and ϵint may soften due to lattice vibrations as the temperature increases. Hence, Esurf, ϵ, or ϵint may slightly decrease as the temperature increases. However, Esurf, ϵ, and ϵint are assumed to be constant throughout the work because we concentrate on studying the size and driving force dependence of the surface roughness.

Mean surface slope and discontinuous surface tension

The mean surface slope tilted towards the 111 direction p¯ is determined to be p¯=Nstepa/L, where Nstep is the number of elementary steps and a is the lattice constant. The partition function of the vicinal surface with slope p¯ is obtained from Z=h(x,t)exp[-H/kBT] with fixed Nstep. The surface free energy f(p¯) is obtained from f(p¯)=-kBTlnZ, and the surface tension γ(p¯) is obtained from γ(p¯)=f(p¯)/1+p¯2.

Our previous studies at equilibrium showed that the p-RSOS model has a discontinuous surface tension33,5659,61 at low temperatures with respect to the surface slope. The faceting diagram corresponding to the connectivity of the surface tension is obtained by calculating the partition function using the density-matrix renormalization group (DMRG) method. For T<Tf,1, the surface tension near the (111) surface becomes discontinuous. For T<Tf,2, which we refer to as the step-faceting zone59, only the surfaces with (001) and (111) are thermodynamically stable at equilibrium57. Hence, the vicinal surface with mean slope p¯ becomes covered in hillocks with (001) terrace-surfaces and (111) side surfaces.

Monte Carlo method

The vicinal surface between the (001) surface and the (111) surface is considered using the Monte Carlo method with the Metropolis algorithm. The external parameters are temperature T, Δμ, number of steps Nstep, and the linear size of the system L. Atoms are captured from the ambient phase to the crystal surface, and escape from the crystal surface to the ambient phase. The number of atoms in a crystal is not conserved. Details of the Monte Carlo calculations are given in Ref.69. Figure 2 shows a snapshot of the vicinal surface.

Mean surface height and surface width

The square of the surface width W for a tilted surface in the non-equilibrium steady state is defined by69

gW2=(a/L)x~[h(x~,y~,t)-(a/L)y~h(x~,y~,t)]2,g=(1+px2+py2)=1/cos2θ,px=py=Nstepa2/L, 15

where x~ and y~ represent a site on the surface along the 110 and 1¯10 directions, respectively, · is the time average, g is the determinant of the first fundamental quantity of a curved surface25, and θ is the tilt angle inclined towards the 111 direction from the 001 direction. The time average is taken over 2×108 Monte Carlo steps per site (MCS/site), discarding the first 2×108 MCS/site69.

In our previous study on the surface width for the original RSOS model65, we found that the kinetic roughening point of the (001) surface Δμkr(001) is different from the crossover point between the BKT-rough surface and the KPZ-rough surface ΔμcoB-K (Table 1) with respect to the driving force for crystal growth Δμ. For high Δμ, the vicinal surface of the RSOS model near the (111) surface is KPZ-rough; whereas the vicinal surface of the RSOS model near the (001) surface is BKT-rough.

Surface velocity and “terrace slope”

Using the Monte Carlo method, the surface velocity is calculated by V=[h¯(t0+τ)-h¯(t0)]/τ~, where h¯(t) is the mean surface height averaged over the surface area at time t, and t0 and τ~ are 2×108 MCS/site6264.

At equilibrium, the terrace surface is exactly the (001) surface. However, at non-equilibrium, due to step-detachments the “terrace” surface is slightly tilted. The “terrace slope” is obtained from the mean-macrostep-height n, which is calculated by the Monte Carlo method, as follows6264:

p1=2/2-p¯p¯z+1,z=1n-NmNstep, 16

where p¯ is Nstepa/L, Nstep is the number of elementary steps, and Nm is the number of macrosteps in the simulated system.

Supplementary Information

Acknowledgements

The author wishes to acknowledge Prof. T. Ohachi, Prof. G. Sazaki, Prof. Fujiwara, Dr. Maeda, and Prof. Y. Kangawa for their valuable advice. The author also wishes to acknowledge Prof. K. Tsukamoto, Prof. T. Koshikawa, Dr. A. Pavlovska, and Prof. E. Bauer for their continual encouragement. This work was supported by KAKENHI Grants-in-Aid (nos. JP25400413 and JP17K05503) from the Japan Society for the Promotion of Science (JSPS). This work was supported in part by the Collaborative Research Program of Research Institute for Applied Mechanics, Kyushu University.

Author contributions

N.A. conceived and conducted the calculations, and analyzed the results.

Competing interests

The author declares no competing interests.

Footnotes

Publisher's note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Supplementary Information

The online version contains supplementary material available at 10.1038/s41598-021-83227-8.

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