Skip to main content
PLOS One logoLink to PLOS One
. 2025 Jun 2;20(6):e0323418. doi: 10.1371/journal.pone.0323418

The numerical simulation of droplet impact on surfaces is conducted using the SPH-DEM method

Shilong Bu 1,*, Daming Li 2, Hu Tao 1, Wenjie Hou 1
Editor: Xin Yong3
PMCID: PMC12129337  PMID: 40455828

Abstract

The process of liquid droplet impinging upon the surface of particles entails complex dynamics and significant deformation. In this study, the smoothed particle hydrodynamics (SPH) method coupled with the discrete element method (DEM) is employed to investigate the motion process of liquid droplet impacting the particle surface. A surface tension model is introduced into the SPH motion equation to calculate the motion of the liquid droplet. In the SPH-DEM coupling module, the viscous force and capillary force between the liquid droplet and the particles are taken into account. The surface tension model is verified through two cases: the free deformation process of a stationary square liquid droplet and the impact of a liquid droplet on a hydrophobic wall. The accuracy of the DEM model is validated through experimental verification of dry particle collapse. And the experimental results validate the accuracy of the SPH-DEM model in simulating the liquid droplet impact on the particle surface. The simulation results are in good agreement with the experimental ones. Utilizing the SPH-DEM model, the influences of the droplet impact velocity and the particle diameter on the rebound phenomenon after the water droplet impacts the particle wall of the powder bed are respectively investigated. The results indicate that the higher the droplet impact velocity and the smaller the diameter of the powder bed particles, the faster the rebound rate of the droplet after impacting the powder bed layer.

1. Introduction

The collision between droplets and particles is a common occurrence in nature, daily life, as well as industrial and agricultural production. For instance, raindrop impact on sand [1], high-speed water flow for dust pollution cleaning in industrial processes [2], binder impact on particle surfaces during wet granulation [3], and the formation process of composite materials [4]. The interaction between droplets and particles upon impact is a complex coupled process involving gas, liquid, and solid multiphase conditions. During this process, the behavior of droplets is influenced by various factors such as impact force and surface tension. Researchers are particularly interested in understanding the movement of particles after being impacted by droplets, deformation patterns, and the interaction between moving droplets and particles [5].

The characteristics of droplets (nature, size, initial velocity) as well as particle properties within the bed significantly influence agglomeration resulting from droplet-particle impacts [58]. Although experimental methods have been extensively employed to study the phenomenon of droplet-particle collisions [911], limitations regarding time scale and space scale make it challenging to obtain detailed information about internal velocity fields, force fields, or multiphase media interactions. Consequently, many scholars have turned their attention towards numerical simulations which hold great potential for providing more comprehensive insights.

A droplet impacting the particle surface is a complex coupled action process under multiphase conditions involving gas, liquid, and solid. To gain a deeper understanding of this process, computer simulation can be an effective tool as it has the potential to provide detailed information that is challenging to obtain experimentally [12]. Most macroscopic models [13] primarily focus on obtaining the flow field and flow characteristics. In mesoscale simulation [12], the average volume equation is typically solved using a mesoscale grid model to acquire a representative flow field, where the grid cell size exceeds that of the particle size. Microscale models [14] are capable of capturing fluid effects and individual particles’ behavior. During phase interface determination, the accuracy of volume-of-fluid (VOF) method simulations depends on the scale of the model grid [15]. The mesh method simulates collision processes between different droplets, allowing for reproduction of droplet merging and separation; however, it cannot replicate droplet bouncing due to considering two droplets’ surfaces as merged when they enter the same grid in phase interface treatment methods [16]. This necessitates developing new boundary conditions to address this limitation [17]. The Level Set method describes phase interfaces through zero contours of high-dimensional functions without requiring explicit tracking, making it easily extendable to any dimensional space and efficiently handling complex material interfaces and their changing topological structures [18].

The advantage of these methods lies in the direct calculation of surface tension from the tracked interface shape. It is important to note that these models require intensive mesh recalculation in order for the mesh to conform accurately to the interface shape, resulting in high computational cost and decreased accuracy. The development of meshless methods provides a solution to this problem. The Smoothed Particle Hydrodynamics (SPH) method was initially proposed by Lucy, Gingold, Monaghan, and others in 1977 as a meshless approach with distinct advantages in handling large deformation problems involving free surfaces [19,20]. Due to oscillations before collision with solid surfaces, droplets typically exhibit irregular shapes. The SPH method has extensively investigated droplet vibration and deformation under various external forces and surface tensions [2124]. In recent years, droplet impact simulation methods have achieved remarkable progress in multi-physics field coupling and complex interface handling. For instance, He et al. [25] revealed the aggregation effect of liquid metal droplets on elastic substrates through SPH method, providing novel insights into energy dissipation mechanisms at soft material interfaces; Dong et al. [26] developed a dual-core SPH model that effectively suppresses tensile instability, laying methodological foundations for contact time regulation of macrostructurally structured surfaces; Meanwhile, Huo et al. [27] comparatively demonstrated the robustness of Lagrangian framework-based fluid-solid coupling simulations by contrasting FEM-SPH and SPH-SPH approaches in elastic beam vibration analysis.

While extensive experimental investigations have demonstrated droplet retraction upon contact with particulate surfaces, the factors governing the rate of this phenomenon remain insufficiently investigated. Therefore, this study proposes the SPH-DEM coupled model to investigate droplet retraction, which considers both the viscous force between droplets and particles and the capillary force caused by voids. The coupling model code was implemented in Fortran 95 language using Visual Studio 2010 and Inter Visual Fortran 2010 as the compilation environment. The model adopts a meshless method for interface tracking. The validity of the proposed coupling model in this study is verified through relevant research literature. Based on this, the effects of droplet impact velocity and particle diameters on droplet retraction rate were investigated using the model.

2. Methodology

2.1 SPH method

The SPH method is a meshless method for solving the governing equations based on Lagrangian particles. The basic equation of SPH is:

A(ri)=jA(rj)W(rirj,h)mjρj (1)

where A can be any function of the fluid field, j is the particle in the neighborhood of particle i; ri and rj are the positions of particle i and j, respectively; W(ri-rj,h) is called the kernel function or smoothing function; m and ρ are the mass and density, respectively. The size of the neighborhood depends on the smoothing length h of the kernel function W. In the present study, the cubic spline kernel function is applied:

W(r,h)=αd{*20l(2q)34(1q)3,0q<1(2q)3,1q<20,q2 (2)

where q = r/h; r is the distance between particles i and j:h is the smoothing length:αd is the regularization coefficient αd = 5/14πh2 in two-dimensional.

The governing equations of fluid motion are as follows,

dρdt=ρ·v (3)
dvdt=g1ρp+μρ2v (4)

where v is the fluid velocity, p is the fluid pressure, μ is the dynamic viscosity of the fluid, and g denotes the body force acting on the fluid, such as gravitational force. With the SPH kernel summations, the governing equations can be written in the following form,

dρidt=j=1Nmjvij·iWij (5)
dvidt=gijmj(Piρi2+Pjρj2)iWij+j2mjμrij·iWijρiρj(rij2+η)vij (6)

where vij = vi-vj, rij = ri-rj, rij = |rij|. h is the smoothing length. The third term on the right side of the Eq. (6) is the viscous term. The term η = 0.01h2 was added to prevent the singularity of the viscous term when two particles approach each other infinitely.

The artificial viscosity demonstrates notable advantages in complex free-surface scenarios such as wave breaking and splash [2830]. In this study, however, the physical viscous scheme was adopted to prioritize numerical stability and direct alignment with the Navier-Stokes equations.

In the context of mesoscopic and microscopic fluid dynamics, surface tension plays a crucial role that cannot be disregarded. Commonly employed models for surface tension include those based on continuum surface force (CSF) and the inter-particle interaction force (IIF) model proposed by Tartakovsky et al. [31]. In this study, we incorporate the Van der Waals stress term into the equation governing fluid motion to simulate surface tension. This approach avoids direct application of forces between particles and maintains higher consistency with the equation governing fluid motion. After considering the influence of surface tension, the motion equation is modified as follows:

dvidt=gij=1nmj(Piρi2+Pjρj2)iWij+j2mjμrij·iWijρiρj(rij2+η)vijj=1Nmj(p~iρ~i2+p~jρ~j2)iW~ij (7)

where

p~ represents the van der Waals stress;

ρ~ denotes the van der Waals density.

p~=kρ~2 (8)

k represents the van der Waals stress.

In this study, the Van der Waals form of the equation of state is used in the study of surface tension [32]:

P=ρkT1ρbaρ2 (9)

where

k= kb/m (kb is the Boltzmann constant),

a= a/m2, and

b=b/m. Here, a and b are the Van der Waals constants and m is the mass of the particles. mi= ρiVi, ρi represents the density of the particle, and Vi represents the volume of the particle.

In order to avoid the non-physical oscillation caused by the lack of particles near the wall boundary of the support domain, the pressure correction method is adopted, and the pressure field is updated every 30 timesteps [33].

2.2 DEM method

The Discrete Element Method (DEM) was first proposed by Peter Cundall [34] in 1971 as a numerical method for simulating the movement of solid particles in discontinuous media. DEM adopts Newton’s second law of motion to update each particle’s velocity and position, and force-displacement law to calculate each particle’s contact force exerted by surrounding particles or boundaries. The equation of motion of particle α:

mαduαdt=Fα (10)
Iαdωαdt=Mα (11)

where mα, uα and Fα are the solid particle’s mass, translational velocity, and the sum of particle–particle interaction forces, respectively; ωα is the solid particle’s rotational velocity and Mα is the resultant moment, respectively; is the moment of inertia.

According to the force synthesis principle, the final resultant force and moment received by particle i are:

Fα=\nolimitsβ=1k(fnαβ+ftαβ) (12)
Mα=\nolimitsβ=1k(Mαβt+Mαβr) (13)

where k is the number of particles β in contact with particle α in the computational domain; fnαβ is the normal contact force between particles α and β; ftαβ is the tangential contact force between particles α and β;

Mαβt is the tangential torque on particle α due to contact with particle β;

Mαβr is the rolling resistance torque on particle α due to contact with particle β.

The damping effect between particles reflects the dissipation of energy during the collision process. Considering the damping effect, the force on the particles can be expressed as:

{*20cfn=(knλ+cnvij·nn)nnft=(ktδ+ctvij·nt)nt (14)

where kn is the normal spring stiffness of linear spring; kt is the tangential spring stiffness of linear spring; λ and δ are the normal and tangential overlap, respectively; vαβ is the relative velocity between particles α and β at contact point; nn and nt ate the normal and tangential unit vector pointing from particle α to particle β, respectively.

Based on the Hertz-Mindlin contact theory [35], the expression of cn is:

cn=2ξnknmeff (15)

where

meff=mimjmi+mj represents the equivalent mass. ξn is the normal damping ratio, calculated through the recovery coefficient e:

ξn=lneπ2+(lne)2 (16)

The tangential damping coefficient ct is generally proportional to the normal damping.

ct=η·cn (17)

The scaling factor η∈[0.5 ~ 1.0] [36].

According to the Hertz–Mindlin theory [35], the expression of the normal spring stiffness coefficient kn is:

kn=43(1νi2Ei+1νj2Ej)1(ri+rjrirj)1/12\nulldelimiterspace2 (18)

where E,

ν, r are the Young's modulus, Poisson's ratio and radius of the particle, respectively.

The expression of the tangential spring stiffness coefficient kt is:

kt=8λ1/12\nulldelimiterspace2(1νi2Gi+1νj2Gj)1(ri+rjrirj)1/12\nulldelimiterspace2 (19)

where G is the shear modulus of the particle.

If the two particles are not in contact, then both normal and shear contact forces are set to zero according to the criterion of no normal strength in tension. Otherwise, calculating the maximum allowable shear contact force

ftmax according to Coulomb friction law:

ftmax=μfn (20)

where µ is the smaller friction coefficient of the two contact particles.

If |ft|>ftmax, that is, when the magnitude of the tangential contact force exceeds the maximum allowable tangential contact force, the tangential contact force is reduced to the limit value while retaining its sign:

ft=ftμfn|ft| (21)

2.3 SPH-DEM coupling module

The interaction between particles in the SPH method is typically achieved by interpolating the physical eigenvalues using a kernel function. In contrast, the DEM method relies on direct contact deformation processes between particles combined with Newton's laws of motion to facilitate particle interactions.

On the mesoscopic scale, there exist distinct gaps between solid particles. Due to capillary action, water infiltrates these boundaries and is drawn into the interstices of the particles, resulting in an indirect adsorption force

fm between the solid particles and water. By calculating the repulsive force, it becomes possible to interpolate the pressure on solid particles and subsequently substitute it into the fluid motion equation for solving forces and accelerations. In practical applications, particle profiles are intricate, particle motions are uncertain, and particle materials are non-uniform. In this study, we simplify the adsorption force caused by capillary action as a direct force acting between fluid particles and solid particles. Assuming that voids within a small range near solid particles are interconnected, these voids can be treated as a whole during calculations. Similar to fluid particles in SPH (Smoothed Particle Hydrodynamics), support domains can be assigned to solid particles in DEM (Discrete Element Method), enabling determination of saturation

Sa [37] by interpolating both the number of solid particles and fluid particles within each particle's support domain. The adsorption force induced by capillary action is influenced by both wetting coefficient

ς [38]and pore pressure P in proximity to each particle.

fim=ςiβ=1NLmimβpβρiρββW (22)

where NL represents the number of fluid particles in the support domain of solid particle β;

ς is the wetting coefficient of the particles, which reflects the infiltration ability of the fluid to the granular particles. Here,

ς is related to the particle material property coefficient

ς and the degree of saturation Sa in the vicinity of the particle.

ς=(1Sa0.5)ς (23)
Sa=β=1NLmβρβWiβ (24)

To sum up, the force

fic of the fluid particle i on the surrounding solid particle β in the analytical coupling model should include three parts, viscous shear force

ften, adsorption force

fm, and repulsion force

frep:

fic=β=1NS(fβrepςβmimβpiρiρβiWiβ+mimβ(4υxiβiWiβ(ρi+ρβ)riβ2)viβ) (25)

where

υ is the kinematic viscosity coefficient of the fluid.

Similarly, the force j is subjected to the surrounding solid particle i can be expressed as:

fβc=i=1NL(firep+ςimimβpiρiρβiWiβ+mimβ(4υxiβiWiβ(ρi+ρβ)riβ2)vβi) (26)

The coupled motion equations can be obtained by bringing the interaction force between solid particles and fluid particles into the respective motion equations of the SPH and DEM models.

2.4 Time Step

The selection of the time step significantly impacts both the stability and efficiency of the model. The critical time step in the DEM model should be associated with the propagation speed of Rayleigh Waves along the surface of solid particles [39]. It is assumed that when two circular particles with a radius R collide, only a Rayleigh Wave propagates between them without affecting other particles (this assumption is similar to that in the DEM soft sphere model). Furthermore, it is assumed that particle interactions are limited to those occurring between contacting particles. Therefore, for this model, the critical time step should be less than or equal to the time required for Rayleigh waves to propagate along a hemisphere [40],

Δtcrit=πRp0.1631ν+0.877ρG (27)

where

tcrit is the critical time step; Rp is radius;

ν is Poisson’s ratio;

G is the shear modulus of the solid particulate material.

The SPH method uses an explicit calculation mode and estimates the time step with the CFL condition. According to the Courant-Friedrichs-Lewy (CFL)condition, the maximum value of the numerical transfer velocity should be larger than the maximum value of the material transfer, so the size of the critical time step in the SPH model should be proportional to the distance between particles. Morris [41] proposed the expression of critical time steps considering viscous diffusion.

tcritλminhi|fi| (28)
tcrit0.125hmin2υ (29)

Where λ is the safety factor, λ = 0.25 [7]; f is the acceleration of the particle;

υ is the kinematic viscosity coefficient of the fluid.

According to the critical time steps

tcritL and

tcritS of the SPH and DEM models, the relationship between the two-time steps can be obtained:

rt=int(max(tcritL)min(tcritS)+1) (30)

where rt is the time step control parameter of the coupled model.

3 The results of numerical simulation

3.1 The test of square drop oscillation

The present example simulates the free deformation process of a stationary square droplet under vacuum conditions, serving as validation for the surface tension model. In this simulation, 2500 droplets with an initial particle spacing of Δx = 0.04mm are placed in a vacuum environment, and their size is set to be 2mm × 2mm. These droplets are allowed to deform freely under the influence of surface tension until they form circular shapes. The surface tension value used in this simulation is 0.02361 N/m. A time step of dt = 1.0 × 10-4ms is employed, along with a dynamic viscosity coefficient η = 1.0 × 10-3Pa·s and an initial density of fluid particles ρ = 1000 kg/m3. Additionally, the smooth length h is defined as 1.3 times Δx (h = 1.3∆x). Fig 1 illustrates the different methods used to capture the shape evolution of these droplets at various time points [42,43]. It can be observed that all methods yield circular shapes for the final droplet configuration; however, this study proposed method achieves greater symmetry compared to others, which aligns more closely with actual physical phenomena occurring in gravity-free environments.

Fig 1. Simulation of the deformation process of a square droplet under the action of surface tension.

Fig 1

3.2 Droplet impact on the hydrophobic wall

In this section, a numerical simulation is conducted to investigate the motion of a droplet impacting a superhydrophobic surface at a velocity of v = 0.54 m/s, taking into account the combined effects of gravity, viscosity, and surface tension. The simulation results are then compared with experimental data from Li et al. [44] for validation purposes. For this specific case study, the droplet has a radius of R = 1.088 mm, and the calculation utilizes a time step of dt = 1.0 × 10-4 ms. The dynamic viscosity coefficient is η = 1.0 × 10-3 Pa·s, while the initial density of fluid particles is ρ = 1.0 × 103 kg/m³. Additionally, the acceleration due to gravity is g = 9.8 m/s² and the van der Waals attractive coefficient is k = 9.66 × 10-3. The simulated results are presented in Fig 2a for comparison with an experiment conducted by Li where they observed an impact between a droplet traveling at v = 0.54 m/s and a solid superhydrophobic material surface as shown in Fig 2b.

Fig 2. Illustrates the dynamic process of a droplet impacting a hydrophobic wall surface at a velocity of v = 0.54m/s, presenting a comparison between simulation results and experimental data.

Fig 2

The droplet descends due to inertia and upon reaching the wall, it spreads along its surface as depicted in Fig 2 from 0–1.8 ms. A portion of the droplet's kinetic energy is converted into potential energy, while the remaining dissipates due to viscosity. As the droplet's surface area increases, the resistance of surface tension to spreading becomes more evident until the droplet's kinetic energy reaches zero. At this point, the contact area between the droplet and solid wall reaches its maximum; owing to surface tension's “pulling back” effect, as shown in Fig 2 at 4.4 ms, the edge thickness exceeds that of the center. Governed by dominant surface tension, the droplet's surface area continues to decrease until its contact with solid wall diminishes completely resulting in rebound and separation from it as depicted in Fig 2 from 9.4–14.8ms. Overall, simulation results in this section are consistent with Li's experimental findings; comparison figures indicate that apart from discrepancies during rebounding stage, simulation outcomes during impact and retraction stages closely align with experimental results.

The Fig 3 depicts the temporal evolution of the wall-wetting diameter (wd) in both experimental data and simulation results. According to the simulation data, the time interval from 0 to 3.3ms corresponds to the droplet's spreading process on the solid wall surface. During this phase, the droplet demonstrates a higher spreading velocity compared to that observed in experimental data, and its maximum wetting diameter (wd) also exceeds the experimental value. The subsequent period from 3.3ms to 3.8ms represents the retraction process of the droplet, during which its retraction speed surpasses that of the experiment, with a greater disparity between them than observed during spreading. From a force analysis perspective, it is suggested that an excessively high movement speed of the droplet may be attributed to insufficient resistance against motion.

Fig 3. The temporal evolution of wall wettability diameter, comparing simulation results with experimental data.

Fig 3

3.3 Validation of the DEM Model

In order to validate the accuracy of the DEM model established in this paper, a simple sand column collapse experiment was conducted and compared with the simulation results of the DEM model. The cross-section of the two-dimensional sand column model is rectangular, with a length (L) of 12 cm and a height (H) of 6 cm. As shown in Fig 4(a), it depicts the initial distribution of particles in the DEM model. The experimental fine sand used had a diameter ranging from 0.1mm to 0.5mm and a density of 2650 kg/m3. In the DEM model, particle diameter was set at 0.4mm, normal stiffness at 3.0 × 107N/m, tangential stiffness at 2.7 × 107N/m, Poisson's ratio at 0.3, damping coefficient at 0.04, recovery coefficient at 0.8, sliding friction coefficient at 0.4, and time step taken as 1.0 × 10-5s. Fig 4(b) shows particle distribution after removing the retaining plate when the sand column collapsed to its final stable state; while Fig 4(c) presents an image capturing the stable state after collapse.

Fig 4. (a) depicts the initial particle distribution, (b) illustrates the stable particle distribution, and (c) presents the experimental observation of the stable state of particles.

Fig 4

Figs 5 and 6 illustrate the instantaneous distribution of particles and their velocities at time intervals t = 0.05s, 0.3s, 0.5s, and 1.0s. Due to experimental constraints and measurement limitations, it was not feasible to accurately capture the instantaneous collapse of the particle column during the experiment; only the stabilized profile contour was obtained, precluding a direct comparison with simulated instantaneous conditions. Immediately after removing the baffle (as depicted in Fig 5), under gravity's influence, the sand column initially collapsed at its toe region forming a triangular sliding area at t = 0.05s while other particles remained relatively stationary. By t = 0.3s, some particles had moved near the wall surface creating a sliding slope with a significant incline angle. At approximately t = 1.0s, particle movement ceased resulting in a profile similar to that shown in Fig 4(c).

Fig 5. The particle distribution at various time intervals.

Fig 5

Fig 6. Particle velocity distribution at different time.

Fig 6

Fig 7 compared profiles formed by dry particle column collapse against those obtained from experiments. The line demarcating sliding particles from non-sliding ones is termed as relative rest line; the angle between this line and horizontal plane is referred to as relative rest angle. Simulated relative rest angle is about 60° while experimental value stands around 62°with less than5%relative error. Maximum runout distance from simulation measures 19.01 cm whereas experimental observation records 21.8 cm, resulting in an approximate 7.73% relative error.

Fig 7. Comparison of DEM simulation and experimental results of dry particle collapse.

Fig 7

3.4 Simulation of droplet impact on particle surface

The SPH-DEM model in this study is validated by the experimental observation of droplet impacting particle surface conducted by Marston et al. [45]. In Marston's experiment, water droplets with a diameter of D0 = 2.1mm were used to impact particles with an average diameter of d = 31μm. The model parameter setting information can be found in Table 1.

Table 1. Model parameters setting information.

SPH parameters Value DEM parameters Value
Fluid particle density (kg/m3) 1000.0 Particle density (kg/m3) 3000.0
Dynamic viscosity coefficient (Pa·s) 1.0 × 10 − 3 Particle radius (μm) 31
Diameter of droplet (mm) 2.1 Particle elastic modulus (Pa) 55 × 109
Surface tension (N/m) 0.04 Particle shear modulus (Pa) 22 × 109
Droplet initial velocity (m/s) 0.15, 2.2 Granular Poisson's ratio 0.25
Smooth kernel function cubic spline Coefficient of kinetic friction 0.4
Particle Wetting Coefficient 0.01 Static friction coefficient 0.8
SPH time step (s) 1.0 × 10-5 DEM time step(s) 3.0 × 10-6
Gravitational acceleration (m/s2) 9.8

The experimental snapshots of the droplet impacting the particle surface are compared with the simulated results obtained from the SPH-DEM model. In Fig 8, the gray background image represents high-speed camera recordings capturing the droplet movement during testing, while the colored image depicts the simulation results of the model. In this representation, blue corresponds to the droplet and red corresponds to the particles.

Fig 8. Comparison of test results of droplet impacting particles surface with simulation results (a) v1.

Fig 8

 = 0.15 m/s, time t = 0, 0.5, 1.5, 2.5, 4.5, and 6.5ms; (b) v2 = 2.2 m/s, the times are t = 0, 0.2, 0.4, 0.6, 1.0, and 1.4ms, respectively.

The droplet falls freely under the influence of gravity, and the initial moment of contact between the droplet and the particle surface is defined as t = 0ms. At t = 1.5ms, when the initial velocity of the droplet is 0.15m/s, it impacts the particle surface and spreads along both ends due to boundary resistance. The period from t = 2ms to 4.5ms represents the spreading process of droplets on the particle surface, where inertia force causes gradual spread of liquid in the middle part around. From t = 4.5ms to 6.5ms, retraction occurs due to surface tension acting on the droplet while certain particles are adsorbed on its contact surface through capillary action during spreading process. When the initial velocity of the droplet is 2.2 m/s, experimental and simulation results show a gradual decrease in thickness at its middle part with an increase at its edge due to pullback effect caused by surface tension on spreading fluid [46]. Fig 9 illustrates a plot depicting relationship between spread diameter of droplets on particle surface and impact time for two different velocities (v1 = 0.15m/s and v2 = 2.2m/s), which is compared with theoretical prediction model results [47]. The variation process observed in current model's spread diameters over time aligns well with experimental findings, indicating that SPH-DEM model established in this study successfully simulates droplets impacting particle surfaces.

Fig 9. The droplet velocity v1.

Fig 9

 = 0.15m/s and v2 = 2.2m/s, the relationship between the droplet spread diameter on the particles surface.

4. Discussion

4.1 The impact velocity of droplets and its influence on droplet retraction

The SPH-DEM coupled model is employed in this section to simulate the process of droplets impacting the surface of particles at different velocities. The model parameter settings are presented in Table 2. The droplet impact velocities used were 0.38 m/s, 0.88 m/s, 1.0 m/s, and 1.48 m/s respectively. The movement process of droplets on the particle surface is illustrated in Fig 10, while Fig 11 demonstrates the variation of spread diameter with different impact times for droplets at various velocities.

Table 2. Model parameters of droplet impacting particles surface with different velocities.

SPH parameters Value DEM parameters Value
Fluid particle density(kg/m3) 1000.0 Particle density (kg/m3) 3000.0
Dynamic viscosity coefficient (Pa·s) 1.0 × 10 − 3 Particle radius(μm) 20
Diameter of droplet (mm) 2.1 Particle Elastic Modulus/MPa 22 × 109
Surface tension (N/m) 0.04 Particle shear modulus/MPa 22 × 109
Droplet initial velocity (m/s) 0.38, 0.88, 1.0, 1.48 Granular Poisson's ratio 0.25
Smooth kernel function cubic spline Coefficient of kinetic friction 0.4
Particle Wetting Coefficient 0.05 Static friction coefficient 0.8
SPH time step (s) 1.0 × 10-5 DEM time step (s) 3.0 × 10-6
Gravitational acceleration (m/s2) 9.8

Fig 10. Droplet spread process with different impact velocities.

Fig 10

, (a) Droplet velocity v1 = 0.38m/s, t; (b) Droplet velocity v2 = 0.88m/s; (c) Droplet velocity v3 = 1.0m/s; (d) Droplet velocity v4 = 1.48m/s; t= 0, 0.5, 1.0, 2.0, 4.0, 6.0, 8, 10.0, 12.0ms, respectively.

Fig 11. Variation of the spread diameter of droplets on the surface with time at different impact velocities, and droplet retraction rate.

Fig 11

The movement of droplets impacting the particle surface with different velocities is illustrated in Fig 10, showcasing various time intervals. The droplet velocities depicted in Fig 10(a)~(d) are 0.38m/s, 0.88m/s, 1.0m/s, and 1.48m/s respectively. This study categorizes the motion process of a droplet impacting particles into three stages: impact, spread, and retraction. During the initial stage (t  = 0ms ~ 1ms), referred to as impact stage, droplets descend with distinct initial velocities and make contact with the particle surface resulting in an impact on the particles themselves. The droplets impact the powder surface with a specific initial velocity. During this stage, the primary form of energy possessed by the droplet is kinetic energy. Upon impact, the conversion of kinetic energy into other forms of energy commences, including deformation energy of the powder surface and internal energy within the droplet itself [48]. Compression occurs at the bottom of these droplets leading to a decrease in flow velocity while rapidly increasing pressure levels are observed simultaneously. Particle velocity increases at both ends causing them to move towards opposite directions during this collision process without any noticeable deformation characteristics on either the droplet or particle surfaces being detected so far.

The second stage is droplet spreading. It can be observed from Fig 11 that the maximum diffusion diameter of the droplet increases with an increase in the droplet impact velocity, and the time taken for the droplet to spread to its maximum diameter also increases. Fig 10 shows that the droplets move towards both ends along the surface of the particle body, where fluid particles and solid particles interpenetrate due to gravity and capillary action. As the droplet spreads, it moves together with the particles, resulting in deformation of their surfaces. The entrainment effect reduces kinetic energy of fluid particles on the contact surface, leading to a lower velocity at the lower part of spreading compared to that at upper part. Consequently, a crown-shaped formation occurs for each droplet [47].

The third stage is droplet retraction, during which the droplet begins to retract due to surface tension after spreading to its maximum diameter. Capillary action causes the particles on the contact surface of the droplet to retract along with it. Momentum exchange occurs between the fluid and solid particles wrapped around them during this process. Consequently, under identical conditions, the retraction speed of particles on the upper surface of the droplet becomes significantly more pronounced than that on its lower surface. The particles on the droplet's surface move from underneath towards the top, indicating a tendency for wrapping and accumulation. Moreover, particle thickness gradually increases as retraction progresses.

The influence of droplet impact velocity on droplet retraction time can be observed from Fig 11. A larger absolute value of k in Fig 11 indicates a faster retraction rate for the droplet. The properties of particles entrained on the under surface of the droplet have a specific impact on its retraction rate during the process. Therefore, the next section analyzes the movement of droplets on particle surfaces with different particle diameters.

4.2 The influence of bed particle size on droplet retraction

In order to investigate the influence of surface particle properties on droplet impact spread, the SPH-DEM coupled model is employed in this section to simulate droplet impacts on surfaces with varying particle diameters. The model parameter settings are presented in Table 3. Fig 12 illustrates the movement of droplets at different time intervals on surfaces with distinct particle diameters, while maintaining a constant droplet impact velocity of 1.0 m/s. Specifically, Fig 12(a)~(c) correspond to particle diameters of 70 μm, 40 μm, and 20 μm respectively. Additionally, Fig 13 demonstrates the variation process of droplet spread diameter over time on surfaces with different particle diameters.

Table 3. Droplet impact particles surface model parameter settings with different particle diameters.

SPH parameters Value DEM parameters Value
Fluid particle density/(kg/m3) 1000.0 Particle density (kg/m3) 3000.0
Dynamic viscosity coefficient (Pa·s) 1.0 × 10 − 3 Particle radius(μm) 10, 20, 35
Diameter of droplet (mm) 2.1 Particle elastic modulus (MPa) 22 × 109
Surface tension (N/m) 0.04 Particle shear modulus (MPa) 22 × 109
Droplet initial velocity (m/s) 1 Granular Poisson's ratio 0.25
Smooth kernel function cubic spline Coefficient of kinetic friction 0.4
Particle Wetting Coefficient 0.05 Static friction coefficient 0.8
SPH time step (s) 1.0 × 10-5 DEM time step (s) 3.0 × 10-6
Gravitational acceleration (m/s2) 9.8

Fig 12.

Fig 12

Movement process of droplets on the particle surface, (a) particle diameter d1  = 20μm; (b) particle diameter d2 = 40μm; (c) particle diameter d3 = 70μm; t = 0, 0.5, 1.0, 2.0, 4.0, 6.0, 8,.0 10.0, 12.0, and 15.0ms, respectively.

Fig 13. The time-dependent process of the droplet spread diameter on the particles surface with different particle diameters, and the droplet retraction rate.

Fig 13

It can be seen from Fig 12 that the droplets impact the particles surfaces of three different particle diameters at the same speed, and the movement process of the droplets can also be divided into three stages. The first stage, the droplet contacts and impact the surfaces. No obvious deformation of the surfaces occurred during the impact stage. In the second stage, the droplet began to spread on the surfaces, and the droplet reached maximum spreading diameter between 3.5ms-4.0ms. It can be seen that when the droplet spreads to the maximum diameter, the particles are already entrained at the bottom of the droplet. At this time, the surfaces were deformed, and erosion pits were formed under the impact of droplets. In the third stage, the droplet starts to retract under the action of surface tension. During the retraction, momentum exchange occurs between the drop and the particles. The retraction speed of the particles on the upper surface of the droplet is significantly greater than that of the lower surface, and the particles on the upper surface of the droplet retract to form bulges. The particles on the droplet's surface undergo migration from the lower to the upper surface, leading to the formation of a particle coating on its surface. The simulation results can clearly describe the nucleation process of droplets being wrapped by particles in this study. It can be seen from Fig 13 that under the same droplet impact velocity, the maximum spread diameter of the droplets on the particle diameter d2 = 40μm and d3 = 70μm particles bed is basically the same, while the maximum diffusion diameter of the droplet on the d1= 20μm particles bed slightly smaller than the previous two. The simulation results (Fig 13) show that the droplet retraction rate is the largest on the d1 = 20μm particles bed, followed by the d2 = 40μm particles bed, and finally 70μm. Therefore, it can be concluded that the particle diameter has a particular influence on the droplet retraction. The rate of retraction of the droplets slows down as the particle diameter increases.

5. Conclusion

This study presents an SPH-DEM coupling model, which considers the viscous force between droplets and particles as well as the capillary force generated by the voids among particles. It is employed to investigate the interaction between droplets and powder particles. The following conclusions have been drawn:

  • (1)

    The correctness of the SPH method for simulating the movement process of droplets in this paper is verified through the square droplet oscillation test and the simulation of droplet impact on hydrophobic surfaces.

  • (2)

    The accuracy of the established DEM model in this paper for studying the movement process of particles is validated by the particle collapse experiment.

  • (3)

    The SPH-DEM coupling model is utilized to simulate the experiment of droplet impact on powder surfaces. The spreading process of the droplet is in good agreement with the experimental results, demonstrating that the established model in this paper can be applied to the research of droplet impact on powder surfaces.

  • (4)

    Furthermore, the influence of the impact velocity of droplets and the diameter difference of powder bed particles on the rebound rate of droplets after impacting the powder bed surface is studied through the SPH-DEM model. The results indicate that the greater the impact velocity of droplets, the faster the rebound rate. The smaller the particle diameter, the faster the rebound rate.

The numerical simulation approach in this paper will offer new possibilities for in-depth exploration of the micro-mechanical mechanism of the interaction between droplets and powder particles.

Data Availability

We have uploaded the data into an online database, which can be found at the link below. https://doi.org/10.6084/m9.figshare.28659227

Funding Statement

The work was supported by the National Natural Science Foundation of China (No. 52360031), Gansu Province higher education industry support plan project (No. 2022CYZC-32), and The Young Scholars Science Foundation of Lanzhou Jiaotong University (No. 1200061253). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

References

  • 1.Zhao S-C, de Jong R, van der Meer D. Raindrop impact on sand: a dynamic explanation of crater morphologies. Soft Matter. 2015;11(33):6562–8. doi: 10.1039/c5sm00957j [DOI] [PubMed] [Google Scholar]
  • 2.Kondo T, Ando K. Simulation of high-speed droplet impact against a dry/wet rigid wall for understanding the mechanism of liquid jet cleaning. Phys Fluids. 2019;31(1). doi: 10.1063/1.5079282 [DOI] [Google Scholar]
  • 3.Nguyen T, Shen W, Hapgood K. Drop penetration time in heterogeneous powder beds. Chem Eng Sci. 2009;64(24):5210–21. doi: 10.1016/j.ces.2009.08.038 [DOI] [Google Scholar]
  • 4.Wang P, Li H, Qi L, Zeng X, Zuo H. Synthesis of Al-TiAl3 compound by reactive deposition of molten Al droplets and Ti powders. Prog Nat Sci. 2011;21(2):153–8. doi: 10.1016/s1002-0071(12)60049-5 [DOI] [Google Scholar]
  • 5.Marston JO, Zhu Y, Vakarelski IU, Thoroddsen ST. Deformed liquid marbles: Freezing drop oscillations with powders. Powder Technol. 2012;228:424–8. doi: 10.1016/j.powtec.2012.06.003 [DOI] [Google Scholar]
  • 6.Abberger T, Seo A, Schaefer T. The effect of droplet size and powder particle size on the mechanisms of nucleation and growth in fluid bed melt agglomeration. Int J Pharm. 2002;249(1–2):185–97. doi: 10.1016/s0378-5173(02)00530-6 [DOI] [PubMed] [Google Scholar]
  • 7.Nefzaoui E, Skurtys O. Impact of a liquid drop on a granular medium: Inertia, viscosity and surface tension effects on the drop deformation. Exp Therm Fluid Sci. 2012;41:43–50. doi: 10.1016/j.expthermflusci.2012.03.007 [DOI] [Google Scholar]
  • 8.Miyanaji H, Momenzadeh N, Yang L. Effect of printing speed on quality of printed parts in Binder Jetting Process. Addit Manuf. 2018;20:1–10. doi: 10.1016/j.addma.2017.12.008 [DOI] [Google Scholar]
  • 9.Marston JO, Thoroddsen ST, Ng WK, Tan RBH. Experimental study of liquid drop impact onto a powder surface. Powder Technol. 2010;203(2):223–36. doi: 10.1016/j.powtec.2010.05.012 [DOI] [Google Scholar]
  • 10.Katsuragi H. Morphology scaling of drop impact onto a granular layer. Phys Rev Lett. 2010;104(21):218001. doi: 10.1103/PhysRevLett.104.218001 [DOI] [PubMed] [Google Scholar]
  • 11.Supakar T, Moradiafrapoli M, Christopher GF, Marston JO. Spreading, encapsulation and transition to arrested shapes during drop impact onto hydrophobic powders. J Colloid Interface Sci. 2016;468:10–20. doi: 10.1016/j.jcis.2016.01.028 [DOI] [PubMed] [Google Scholar]
  • 12.Washino K, Tan HS, Hounslow MJ, Salman AD. A new capillary force model implemented in micro-scale CFD–DEM coupling for wet granulation. Chem Eng Sci. 2013;93:197–205. doi: 10.1016/j.ces.2013.02.006 [DOI] [Google Scholar]
  • 13.Sakai M, Koshizuka S. Large-scale discrete element modeling in pneumatic conveying. Chem Eng Sci. 2009;64(3):533–9. doi: 10.1016/j.ces.2008.10.003 [DOI] [Google Scholar]
  • 14.Jain D, Deen NG, Kuipers JAM, Antonyuk S, Heinrich S. Direct numerical simulation of particle impact on thin liquid films using a combined volume of fluid and immersed boundary method. Chem Eng Sci. 2012;69(1):530–40. doi: 10.1016/j.ces.2011.11.018 [DOI] [Google Scholar]
  • 15.Hirt CW, Nichols BD. Volume of fluid (VOF) method for the dynamics of free boundaries. J Comput Phys. 1981;39(1):201–25. doi: 10.1016/0021-9991(81)90145-5 [DOI] [Google Scholar]
  • 16.Gotaas C, Havelka P, Jakobsen HA, Svendsen HF, Hase M, Roth N, et al. Effect of viscosity on droplet-droplet collision outcome: experimental study and numerical comparison. Phys Fluids. 2007;19(10). doi: 10.1063/1.2781603 [DOI] [Google Scholar]
  • 17.Malgarinos I, Nikolopoulos N, Marengo M, Antonini C, Gavaises M. VOF simulations of the contact angle dynamics during the drop spreading: standard models and a new wetting force model. Adv Colloid Interface Sci. 2014;212:1–20. doi: 10.1016/j.cis.2014.07.004 [DOI] [PubMed] [Google Scholar]
  • 18.Osher S, Sethian JA. Fronts propagating with curvature-dependent speed: Algorithms based on Hamilton-Jacobi formulations. J Comput Phys. 1988;79(1):12–49. doi: 10.1016/0021-9991(88)90002-2 [DOI] [Google Scholar]
  • 19.Lucy LB. A numerical approach to the testing of the fission hypothesis. Astronom J. 1977;82:1013. doi: 10.1086/112164 [DOI] [Google Scholar]
  • 20.Gingold RA, Monaghan JJ. Smoothed particle hydrodynamics: theory and application to non-spherical stars. Monthly Notices R Astronom Soc. 1977;181(3):375–89. doi: 10.1093/mnras/181.3.375 [DOI] [Google Scholar]
  • 21.Nishio N, Yamana K, Yamaguchi Y, Inaba T, Kuroda K, Nakajima T, et al. Large‐scale SPH simulations of droplet impact onto a liquid surface up to the consequent formation of Worthington jet. Num Methods Fluids. 2010;63(12):1435–47. doi: 10.1002/fld.2141 [DOI] [Google Scholar]
  • 22.Li D, Li X, Lin Y. Numerical simulation of droplet impacting liquid surface by SPH. Sci China Technol Sci. 2011;54(7):1873–80. doi: 10.1007/s11431-011-4422-0 [DOI] [Google Scholar]
  • 23.Meng S, Yang R, Wu J, Zhang H. Simulation of droplet spreading on porous substrates using smoothed particle hydrodynamics. Int J Heat Mass Tran. 2014;77:828–33. doi: 10.1016/j.ijheatmasstransfer.2014.05.056 [DOI] [Google Scholar]
  • 24.Zhang R, Zhang B, Lv Q, Li J, Guo P. Effects of droplet shape on impact force of low-speed droplets colliding with solid surface. Exp Fluids. 2019;60(4). doi: 10.1007/s00348-019-2712-7 [DOI] [Google Scholar]
  • 25.He Z, Xiao R, Qu S. A study on the impact of liquid metal droplets onto metal and elastomer substrates. Acta Mech Sin. 2024;41(4). doi: 10.1007/s10409-024-24165-x [DOI] [Google Scholar]
  • 26.Huo Y, Zhong Y, Xin M, Li S. Modeling and simulation of droplet impact on an elastic beam based on FEM-SPH and SPH-SPH FSI methods. Ocean Eng. 2024;310:118730. doi: 10.1016/j.oceaneng.2024.118730 [DOI] [Google Scholar]
  • 27.Dong X, Feng L, Zhang Q. Droplet asymmetry bouncing on structured surfaces: a simulation based on SPH method. Int J Adhes Adhes. 2024;132:103734. doi: 10.1016/j.ijadhadh.2024.103734 [DOI] [Google Scholar]
  • 28.He F, Jiang H, Lin Y, Pan J, Zhang Y, Huang C. Multi-phase SPH-FDM and experimental investigations on the hydrodynamics of an oscillating water column wave energy device. Coastal Eng. 2024;192:104569. doi: 10.1016/j.coastaleng.2024.104569 [DOI] [Google Scholar]
  • 29.Wang XJ, Huang C, Yan WH, Aly AM, Zhao QL, He GP. Study on hydrodynamic characteristics of multiple fish based on smoothed particle hydrodynamics. Phys Fluids. 2024;36(11). doi: 10.1063/5.0236386 [DOI] [Google Scholar]
  • 30.Huang C, Zhang DH, Shi YX, Si YL, Huang B. Coupled finite particle method with a modified particle shifting technology. Num Meth Eng. 2017;113(2):179–207. doi: 10.1002/nme.5608 [DOI] [Google Scholar]
  • 31.Tartakovsky A, Meakin P. Modeling of surface tension and contact angles with smoothed particle hydrodynamics. Phys Rev E Stat Nonlin Soft Matter Phys. 2005;72(2 Pt 2):026301. doi: 10.1103/PhysRevE.72.026301 [DOI] [PubMed] [Google Scholar]
  • 32.Nugent S, Posch H. Liquid drops and surface tension with smoothed particle applied mechanics. Phys Rev E Stat Phys Plasmas Fluids Relat Interdiscip Topics. 2000;62(4 Pt A):4968–75. doi: 10.1103/physreve.62.4968 [DOI] [PubMed] [Google Scholar]
  • 33.Randles PW, Libersky LD. Smoothed Particle Hydrodynamics: some recent improvements and applications. Comput Methods Appl Mechan Eng. 1996;139(1–4):375–408. doi: 10.1016/s0045-7825(96)01090-0 [DOI] [Google Scholar]
  • 34.Cundall PA. A computer model for simulating progressive large-scale movements in blocky rock systems. Procintsympon Rock Fract. 1971;1(ii-b):11–8. [Google Scholar]
  • 35.Mindlin RD, Deresiewicz H. Elastic spheres in contact under varying oblique forces. Japplmechasme. 1953;20(3):327–44. doi: 10.1007/978-1-4613-8865-4_35 [DOI] [Google Scholar]
  • 36.Cundall PA, Strack ODL. Discussion: a discrete numerical model for granular assemblies. Géotechnique. 1980;30(3):331–6. doi: 10.1680/geot.1980.30.3.331 [DOI] [Google Scholar]
  • 37.Li Y, Li D, Bie S, Wang Z, Zhang H, Tang X, et al. Numerical simulation for fluid droplet impact on discrete particles with coupled SPH-DEM method. HFF. 2018;28(11):2581–605. doi: 10.1108/hff-11-2017-0464 [DOI] [Google Scholar]
  • 38.Zhichao W, Daming LI, Yangyang LI, Jiao N. Numerical studies on droplet impact to wettable solid boundary based on SPH method. Chin Sci Bull. 2017. doi: 10.1360/N972016-01288 [DOI] [Google Scholar]
  • 39.Rayleigh L. On waves propagated along the plane surface of an elastic solid. Proclondmathsoc. 2016;1:4–11. doi: 10.1112/plms/s1-17.1.4 [DOI] [Google Scholar]
  • 40.Campbell CS, Brennen CE. Computer simulation of granular shear flows. J Fluid Mech. 1985;151(1):167. doi: 10.1017/s002211208500091x [DOI] [Google Scholar]
  • 41.Morris JP, Fox PJ, Zhu Y. Modeling low reynolds number incompressible flows using SPH. J Comput Phys. 1997;136(1):214–26. doi: 10.1006/jcph.1997.5776 [DOI] [Google Scholar]
  • 42.Qiang H, Chen F, Gao W. Smoothed particle hydrodynamics method with modified surface tension and its implementation. Chinese. J Comput Phys. 2011;28(3):375–84. doi: 10.1631/jzus.A1000257 [DOI] [Google Scholar]
  • 43.Chen S, Shengyao J, Riqiang D. Accurate continuum surface force model applicable to particle methods. J Tsinghua Univ (Sci Technol). 2018. doi: 10.16511/j.cnki.qhdxxb.2018.25.002 [DOI] [Google Scholar]
  • 44.Li X, Ma X, Lan Z. Dynamic behavior of the water droplet impact on a textured hydrophobic/superhydrophobic surface: the effect of the remaining liquid film arising on the pillars’ tops on the contact time. Langmuir. 2010;26(7):4831–8. doi: 10.1021/la903603z [DOI] [PubMed] [Google Scholar]
  • 45.Marston JO, Sprittles JE, Zhu Y, Li EQ, Vakarelski IU, Thoroddsen ST. Drop spreading and penetration into pre-wetted powders. Powder Technol. 2013;239:128–36. doi: 10.1016/j.powtec.2013.01.062 [DOI] [Google Scholar]
  • 46.Clarke A, Blake TD, Carruthers K, Woodward A. Spreading and imbibition of liquid droplets on porous surfaces. Langmuir. 2002;18(8):2980–4. doi: 10.1021/la0117810 [DOI] [Google Scholar]
  • 47.Ma T, Feng L, Wang H, Liu H, Yao M. A numerical study of spray/wall impingement based on droplet impact phenomenon. Int J Heat Mass Transfer. 2017;112:401–12. doi: 10.1016/j.ijheatmasstransfer.2017.04.110 [DOI] [Google Scholar]
  • 48.Hu Z, Chu F, Shan H, Wu X, Dong Z, Wang R. Understanding and utilizing droplet impact on superhydrophobic surfaces: phenomena, mechanisms, regulations, applications, and beyond. Adv Mater. 2024;36(11):e2310177. doi: 10.1002/adma.202310177 [DOI] [PubMed] [Google Scholar]

Decision Letter 0

Xin Yong

5 Feb 2025

PONE-D-24-50755The numerical simulation of droplet impact on surfaces is conducted using the SPH-DEM methodPLOS ONE

Dear Dr. Bu,

Thank you for submitting your manuscript to PLOS ONE. We encountered some difficulties in securing sufficient reviews for your manuscript to make a decision. After careful consideration, we feel that it has merit but does not fully meet PLOS ONE’s publication criteria as it currently stands. The reviewers report significant concerns regarding the technical details of the work. In addition, the English language of the manuscript needs substantial improvements. Even the title of the manuscript is not written in an acceptable form. Therefore, we invite you to submit a revised version of the manuscript that addresses the points raised during the review process.

Please submit your revised manuscript by Mar 22 2025 11:59PM. If you will need more time than this to complete your revisions, please reply to this message or contact the journal office at plosone@plos.org . When you're ready to submit your revision, log on to https://www.editorialmanager.com/pone/ and select the 'Submissions Needing Revision' folder to locate your manuscript file.

Please include the following items when submitting your revised manuscript:

  • A rebuttal letter that responds to each point raised by the academic editor and reviewer(s). You should upload this letter as a separate file labeled 'Response to Reviewers'.

  • A marked-up copy of your manuscript that highlights changes made to the original version. You should upload this as a separate file labeled 'Revised Manuscript with Track Changes'.

  • An unmarked version of your revised paper without tracked changes. You should upload this as a separate file labeled 'Manuscript'.

If you would like to make changes to your financial disclosure, please include your updated statement in your cover letter. Guidelines for resubmitting your figure files are available below the reviewer comments at the end of this letter.

If applicable, we recommend that you deposit your laboratory protocols in protocols.io to enhance the reproducibility of your results. Protocols.io assigns your protocol its own identifier (DOI) so that it can be cited independently in the future. For instructions see: https://journals.plos.org/plosone/s/submission-guidelines#loc-laboratory-protocols . Additionally, PLOS ONE offers an option for publishing peer-reviewed Lab Protocol articles, which describe protocols hosted on protocols.io. Read more information on sharing protocols at https://plos.org/protocols?utm_medium=editorial-email&utm_source=authorletters&utm_campaign=protocols .

We look forward to receiving your revised manuscript.

Kind regards,

Xin Yong

Academic Editor

PLOS ONE

Journal Requirements:

When submitting your revision, we need you to address these additional requirements.

1.Please ensure that your manuscript meets PLOS ONE's style requirements, including those for file naming. The PLOS ONE style templates can be found at

https://journals.plos.org/plosone/s/file?id=wjVg/PLOSOne_formatting_sample_main_body.pdf and

https://journals.plos.org/plosone/s/file?id=ba62/PLOSOne_formatting_sample_title_authors_affiliations.pdf

2. Please note that PLOS ONE has specific guidelines on code sharing for submissions in which author-generated code underpins the findings in the manuscript. In these cases, we expect all author-generated code to be made available without restrictions upon publication of the work. Please review our guidelines at https://journals.plos.org/plosone/s/materials-and-software-sharing#loc-sharing-code and ensure that your code is shared in a way that follows best practice and facilitates reproducibility and reuse.

3. Please note that funding information should not appear in any section or other areas of your manuscript. We will only publish funding information present in the Funding Statement section of the online submission form. Please remove any funding-related text from the manuscript.

4. Thank you for stating the following financial disclosure:

“The work was supported by the National Natural Science Foundation of China (No. 52360031), Gansu Province higher education industry support plan project (No. 2022CYZC-32), and The Young Scholars Science Foundation of Lanzhou Jiaotong University (No. 1200061253).”

Please state what role the funders took in the study.  If the funders had no role, please state: "The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript."

If this statement is not correct you must amend it as needed.

Please include this amended Role of Funder statement in your cover letter; we will change the online submission form on your behalf.

5. We note that your Data Availability Statement is currently as follows: “All relevant data are within the manuscript and in Supporting Information files.”

Please confirm at this time whether or not your submission contains all raw data required to replicate the results of your study. Authors must share the “minimal data set” for their submission. PLOS defines the minimal data set to consist of the data required to replicate all study findings reported in the article, as well as related metadata and methods (https://journals.plos.org/plosone/s/data-availability#loc-minimal-data-set-definition).

For example, authors should submit the following data:

- The values behind the means, standard deviations and other measures reported;

- The values used to build graphs;

- The points extracted from images for analysis.

Authors do not need to submit their entire data set if only a portion of the data was used in the reported study.

If your submission does not contain these data, please either upload them as Supporting Information files or deposit them to a stable, public repository and provide us with the relevant URLs, DOIs, or accession numbers. For a list of recommended repositories, please see https://journals.plos.org/plosone/s/recommended-repositories.

If there are ethical or legal restrictions on sharing a de-identified data set, please explain them in detail (e.g., data contain potentially sensitive information, data are owned by a third-party organization, etc.) and who has imposed them (e.g., an ethics committee). Please also provide contact information for a data access committee, ethics committee, or other institutional body to which data requests may be sent. If data are owned by a third party, please indicate how others may request data access.

[Note: HTML markup is below. Please do not edit.]

Reviewers' comments:

Reviewer's Responses to Questions

Comments to the Author

1. Is the manuscript technically sound, and do the data support the conclusions?

The manuscript must describe a technically sound piece of scientific research with data that supports the conclusions. Experiments must have been conducted rigorously, with appropriate controls, replication, and sample sizes. The conclusions must be drawn appropriately based on the data presented.

Reviewer #1: No

Reviewer #2: Yes

**********

2. Has the statistical analysis been performed appropriately and rigorously?

Reviewer #1: No

Reviewer #2: Yes

**********

3. Have the authors made all data underlying the findings in their manuscript fully available?

The PLOS Data policy requires authors to make all data underlying the findings described in their manuscript fully available without restriction, with rare exception (please refer to the Data Availability Statement in the manuscript PDF file). The data should be provided as part of the manuscript or its supporting information, or deposited to a public repository. For example, in addition to summary statistics, the data points behind means, medians and variance measures should be available. If there are restrictions on publicly sharing data—e.g. participant privacy or use of data from a third party—those must be specified.

Reviewer #1: Yes

Reviewer #2: Yes

**********

4. Is the manuscript presented in an intelligible fashion and written in standard English?

PLOS ONE does not copyedit accepted manuscripts, so the language in submitted articles must be clear, correct, and unambiguous. Any typographical or grammatical errors should be corrected at revision, so please note any specific errors here.

Reviewer #1: Yes

Reviewer #2: Yes

**********

5. Review Comments to the Author

Please use the space provided to explain your answers to the questions above. You may also include additional comments for the author, including concerns about dual publication, research ethics, or publication ethics. (Please upload your review as an attachment if it exceeds 20,000 characters)

Reviewer #1: A numerical framework to simulate the high-speed impact of liquid droplets onto planar surfaces is here proposed and discussed.

The manuscript needs extensive revision, key messages need to be clarified. The abstract is concise while informative showing the background and applied methods. It might also bring results with key concrete values, supporting the feasibility of the adopted methodology.

The literature review is not comprehensive. It would benefit the discussion of recent reports on the simulation of droplets impact, e.g.

10.1007/s10409-024-24165-x

10.1016/j.oceaneng.2024.118730

10.1016/j.ijadhadh.2024.103734

Amend r_ij = |r_ij|

eta = 0.01 h^2 is not added in the equation.

In the coupling procedure, clarify the role of the adsorption force induced by capillary action, as it seems relevant in light of the claimed application concerning the droplet impact on surfaces.

“The critical time step in the DEM model should be associated with the propagation speed of Rayleigh Waves along the surface of solid particles”

This position should be strengthen at least by give References.

Fig. 3 While wettability is overall in a fairly good agreement, the impact process returns different shapes in Fig. 2, if not below 4.5 ms. Energy conversion should be further investigated, along which numerical values of ruling parameters.

Fig. 4. Particle distribution along the deformed free surfaces seems to show excessive irregularity. Bouncing effects should be the cause. A further investigation of this behaviour would be needed.

Fig. 10. Droplet diffusion process. Molecular diffusion? Any validation?

Reviewer #2: This study developed a SPH-DEM model to simulate the liquid drop impacting on the granule. The results by the proposed method are agreement with the published data. I recommend the publishment of the manuscript after a minor revision. The suggestions are given as follows.

1, In Eq. (6), what does the variable ν0 mean?

2, For the free surface flow, it usually uses the so-called artificial viscous scheme to discretize the viscous term of fluid instead of the physical viscous scheme because the artificial viscous scheme can satisfy the free surface boundary condition, as described in the published papers (https://doi.org/10.1016/j.coastaleng.2024.104569), (https://doi.org/10.1063/5.0236386) and (https://doi.org/10.1002/nme.5608). Please cite these papers and give a comment on the viscous scheme of SPH.

3, In Eq. (7), what does the variable mean?

4, In Eq. (8), what does the variable mean?

5, How to solve the symbol m in the term a/m?

6, It is necessary to cite the reference when introducing the DEM method.

7, How to solve the symbols cn and ct in Eq. (14)?

8, what does the variable c in Eq. (15) mean? And, how to solve the symbols k and m in Eq. (15)?

9, I think the right term of Eq. (19) is equal to μft. Why does the authors use a complex form to express the term of Eq. (19)?

10, For Eqs. (20), (21), (22), (23) and (24), the symbols used to represent solid and fluid particles are too mixed. Please carefully review and modify these formulas.

11, For figure 1, why is the evolution of the surface by the current method different from the published results? Is it possible that the difference is caused by the viscous discrete format? I suggest that the authors check it carefully.

**********

6. PLOS authors have the option to publish the peer review history of their article (what does this mean? ). If published, this will include your full peer review and any attached files.

If you choose “no”, your identity will remain anonymous but your review may still be made public.

Do you want your identity to be public for this peer review? For information about this choice, including consent withdrawal, please see our Privacy Policy .

Reviewer #1: No

Reviewer #2: Yes:  Can Huang

**********

[NOTE: If reviewer comments were submitted as an attachment file, they will be attached to this email and accessible via the submission site. Please log into your account, locate the manuscript record, and check for the action link "View Attachments". If this link does not appear, there are no attachment files.]

While revising your submission, please upload your figure files to the Preflight Analysis and Conversion Engine (PACE) digital diagnostic tool, https://pacev2.apexcovantage.com/ . PACE helps ensure that figures meet PLOS requirements. To use PACE, you must first register as a user. Registration is free. Then, login and navigate to the UPLOAD tab, where you will find detailed instructions on how to use the tool. If you encounter any issues or have any questions when using PACE, please email PLOS at figures@plos.org . Please note that Supporting Information files do not need this step.

Attachment

Submitted filename: Comments on PONE-D-24-51781.pdf

pone.0323418.s001.pdf (115.6KB, pdf)
PLoS One. 2025 Jun 2;20(6):e0323418. doi: 10.1371/journal.pone.0323418.r003

Author response to Decision Letter 1


25 Mar 2025

Dear Editors and Reviewers:

The co-authors and I would like to thank you for the precious time and effort spent in reviewing the manuscript entitled “The numerical simulation of droplet impact on surfaces is conducted using the SPH-DEM method” (Manuscript No. PONE-D-24-50755).

Those comments are all very valuable and helpful for revising and improving this manuscript, as well as the important guiding significance to our researches. We have studied every comment carefully and have made correction which we hope meet with approval. Revised portion are marked in yellow highlight in the manuscript. The main corrections in the manuscript and the responds to the reviewers’ comments are as flowing�

Reviewer #1:

1. The literature review is not comprehensive. It would benefit the discussion of recent reports on the simulation of droplets impact, e.g.

10.1007/s10409-024-24165-x

10.1016/j.oceaneng.2024.118730

10.1016/j.ijadhadh.2024.103734

Answer�Thank you for pointing out the deficiencies in the literature review and providing crucial references. We have carefully studied these three recent publications and incorporated their core contributions into the discussion section of the revised manuscript to enhance both the comprehensiveness and cutting-edge nature of this study. Below are the specific additions and modifications made:

In recent years, droplet impact simulation methods have achieved remarkable progress in multi-physics field coupling and complex interface handling. For instance, He et al. [25] revealed the aggregation effect of liquid metal droplets on elastic substrates through SPH method, providing novel insights into energy dissipation mechanisms at soft material interfaces; Dong et al. [26] developed a dual-core SPH model that effectively suppresses tensile instability, laying methodological foundations for contact time regulation of macrostructurally structured surfaces; Meanwhile, Huo et al. [27] comparatively demonstrated the robustness of Lagrangian framework-based fluid-solid coupling simulations by contrasting FEM-SPH and SPH-SPH approaches in elastic beam vibration analysis.

[25] He, Z., Xiao, R. & Qu, S. A study on the impact of liquid metal droplets onto metal and elastomer substrates. Acta Mech. Sin. 41, 224165 (2025). https://doi.org/10.1007/s10409-024-24165-x

[26] Huo, Y., et al., Modeling and simulation of droplet impact on an elastic beam based on FEM-SPH and SPH-SPH FSI methods. Ocean Engineering, 2024. 310: p. 118730.

https://doi.org/10.1016/j.oceaneng.2024.118730

[27] Dong, X., L. Feng and Q. Zhang, Droplet asymmetry bouncing on structured surfaces: A simulation based on SPH method. International Journal of Adhesion and Adhesives, 2024. 132: p. 103734. https://doi.org/10.1016/j.ijadhadh.2024.103734

2. Amend r_ij = |r_ij|

Answer�The relevant formulas have been modified in the revised manuscript.

rij=∣rij∣

3. eta = 0.01 h^2 is not added in the equation.

Answer�Thank you for your meticulous review. Equation (6) in the original manuscript did contain a typographical error. We have conducted a thorough re-examination of the equations and implemented necessary corrections.

�6�

4. In the coupling procedure, clarify the role of the adsorption force induced by capillary action, as it seems relevant in light of the claimed application concerning the droplet impact on surfaces.

Answer�Thank you for your attention to the role of adsorption forces in the coupled model. The capillary-induced adsorption force plays a crucial role in the dynamic process of droplet impact on particle surfaces, particularly during the stages of droplet spread, retraction, and particle engulfment. The following sections will elaborate on the physical significance of adsorption forces and their impact on droplet behavior from two aspects:

(1) The mathematical model of adsorption force and its physical significance

In the SPH-DEM coupling procedure, the adsorption force induced by capillary action plays a critical role in governing the interaction between the droplet and particle surfaces. This force arises from the capillary pressure within the interstitial voids between particles, which is influenced by the wettability of the particles and the local saturation of the fluid. The adsorption force is modeled to account for capillary effects caused by fluid infiltration into the gaps between particles. This force acts as an indirect attraction between the fluid and solid particles, driven by the wetting properties of the particles (quantified by the wetting coefficient ζ) and the pore pressure near the particle surfaces. The wetting coefficient is determined by the particle material property and the local saturation (Sa), which is calculated based on the density of fluid particles within the support domain (Eq. 21–22). The adsorption force is integrated into the SPH-DEM coupling equations (Eq. 20, 23–24) as part of the total interaction force between fluid and solid particles. It directly affects the momentum exchange between the droplet and particles during spreading and retraction phases. For instance, during droplet spreading, capillary forces enhance fluid-particle adhesion, while during retraction, they contribute to the "pull-back" effect driven by surface tension, influencing droplet rebound dynamics.

(2) Impact on Droplet Behavior:

Spreading Phase: The adsorption force facilitates fluid infiltration into particle gaps, increasing the contact area and energy dissipation. This aligns with the observed dependency of maximum spreading diameter on particle size (Fig. 13), where smaller particles (e.g. d=20μm) exhibit faster retraction due to stronger capillary interactions.

Retraction Phase: The interplay between capillary forces and surface tension governs the rebound rate. Higher adsorption forces (e.g., in smaller particles or higher impact velocities) accelerate retraction by intensifying momentum exchange between fluid and particles (Fig. 11–13).

Particle encapsulation phenomenon: Adsorption forces drive the encapsulation of particles by the surface of a droplet (Fig. 10-12), simulating the experimentally observed "drop-encased particle" nucleation process. This mechanism is crucial for achieving uniform particle distribution in coating processes.

5. “The critical time step in the DEM model should be associated with the propagation speed of Rayleigh Waves along the surface of solid particles” This position should be strengthen at least by give References.

Answer�Thank you for your suggestion. We have already supplemented the relevant references in the manuscript.

[39] Rayleigh, L., (1885) On Waves Propagated along the Plane Surface of an Elastic Solid. Proceedings of the London Mathematical Society, s1-17(1): p. 4-11. https://doi.org/10.1112/plms/s1-17.1.4

6. Fig. 3 While wettability is overall in a fairly good agreement, the impact process returns different shapes in Fig. 2, if not below 4.5 ms. Energy conversion should be further investigated, along which numerical values of ruling parameters.

Answer�We appreciate the reviewer’s insightful observation regarding the differences in droplet shapes during the impact process (Fig. 2) and the need for further investigation into energy conversion and parameter sensitivity. Below, we address these points in detail:

�1� Discrepancies in Droplet Shapes Below 4.5 ms (Fig. 2):

The observed differences in droplet morphology during the early impact phase (0–4.5 ms) can be attributed to the following factors:

a. Dynamic Surface Tension Effects:

While the SPH model incorporates a surface tension term (Eq.7–9), the current implementation assumes a constant surface tension coefficient (σ=0.04N/m). However, during high-speed droplet impact, dynamic surface tension effects may arise due to rapid deformation, which are not explicitly modeled. This simplification could lead to deviations in droplet spreading dynamics compared to experiments.

b. Viscous Dissipation and Strain Rate Dependence:

The viscous term in Eq. 6 employs a constant dynamic viscosity. At the high strain rates encountered during impact, non-Newtonian behavior or strain-rate-dependent viscosity might influence energy dissipation. Future work will explore strain-rate-dependent viscosity models to better match experimental observations.

c. Boundary Condition Simplifications:

The hydrophobic wall is modeled using a fixed wetting coefficient (ζ) derived from saturation Sa (Eq. 21). However, transient contact angle hysteresis and slip boundary effects during rapid spreading are not fully resolved. Incorporating dynamic contact angle models (e.g., Cox-Voinov theory) could improve accuracy during the initial impact phase.

�2�Energy Conversion Mechanisms

Thank you for your insightful comments on the importance of studying energy conversion mechanisms. The issues you raised regarding energy transformation and key parameter quantification during droplet impact processes are indeed critical for gaining a deeper understanding of droplet dynamic behavior. We fully agree with your viewpoint and have incorporated this topic as a core focus for our future research. Below is our detailed explanation and implementation plan:

The SPH-DEM coupled model has preliminarily validated the correlation between droplet spreading-retraction behavior and surface tension, particle wettability (Fig. 8-9). However, the multiphase coupling between droplets and particulate beds involves dynamic interconversion among kinetic energy, surface energy, viscous dissipation, and particle frictional energy. To address this, we are developing specialized energy tracking algorithms (e.g., particle-level energy tagging method), which is currently under active development and debugging. The current version has not yet implemented systematic quantification of energy conversion processes.

In response to your valuable suggestion, we plan to integrate energy conservation equations into the SPH-DEM framework in our next phase of work. This will enable real-time calculation of four critical energy components during droplet-particle interactions:

Droplet kinetic energy (Ek), Surface energy (Es), Viscous dissipation energy (Ev), Particle frictional energy (Ef). The governing equations will be formulated as follows:

where, A represents the drop surface area, Fij denotes the particle contact force, and δij corresponds to the relative displacement. Subsequently, we will quantify the effects of the Weber number (We), particle diameter (dp), and wetting coefficient (ζ) on the energy allocation ratio, combined with theoretical models from literature for validation.

7. Fig. 4. Particle distribution along the deformed free surfaces seems to show excessive irregularity. Bouncing effects should be the cause. A further investigation of this behaviour would be needed.

Answer: We sincerely appreciate the reviewer’s observation regarding the irregular particle distribution along the deformed free surfaces in Fig. 4 and their suggestion to investigate potential bouncing effects. Below, we provide a detailed explanation and outline steps for further analysis:

The DEM model employs the Hertz-Mindlin contact theory (Eq. 16–19) with a damping coefficient derived from the restitution coefficient e=0.92 (Section 2.2). While this setup effectively captures energy dissipation during collisions, it may oversimplify microscale particle interactions in dense granular flows. Specifically, the linear spring-dashpot model assumes idealized elastic-plastic collisions, which might not fully resolve multibody collisions or particle rearrangement dynamics during rapid collapse.

We attempted to reduce the coefficient of restitution of the particles (e=0.8), and the simulation results showed that smoother particle distributions (attached supplementary figure). This suggests that optimizing damping parameters can mitigate irregularity.

�b�

The following research, we are going to address the bouncing effect through parameter optimization and the implementation of advanced contact mechanics, with the aim of enhancing the physical fidelity in particle dynamics simulations. We sincerely appreciate the reviewers' valuable feedback, which will significantly strengthen the robustness of our model.

8. Fig. 10. Droplet diffusion process. Molecular diffusion? Any validation?

Answer�Thank you for your question. Here we confirm that there are inaccuracies in the formulation of the ‘droplet diffusion process’ in Fig. 10. The term ‘diffusion’ in our manuscript refers to the macroscopic spreading of the droplet driven by inertia and surface tension, rather than molecular-scale diffusion processes. The latter is negligible in the studied millimeter-scale droplet impact dynamics due to the dominance of advection and capillary forces.

We made revisions to the relevant statements in the revised manuscript.

Thanks to you for your comments and suggestions again.

Reviewer #2:

1. In Eq. (6), what does the variable ν0 mean?,

Answer: Thank you for your meticulous review. Equation (6) in the original manuscript did contain a typographical error. We have conducted a thorough re-examination of the equations and implemented necessary corrections.

(6)

where vij= vi-vj, rij =ri-rj, rij = |rij|. h is the smoothing length. The third term on the right side of the Eq. (6) is the viscous term. μ is the dynamic viscosity of the fluid. g denotes the body force acting on the fluid, such as gravitational force. The term η = 0.01h2 was added to prevent the singularity of the viscous term when two particles approach each other infinitely.

2. For the free surface flow, it usually uses the so-called artificial viscous scheme to discretize the viscous term of fluid instead of the physical viscous scheme because the artificial viscous scheme can satisfy the free surface boundary condition, as described in the published papers (https://doi.org/10.1016/j.coastaleng.2024.104569), (https://doi.org/10.1063/5.0236386) and (https://doi.org/10.1002/nme.5608). Please cite these papers and give a comment on the viscous scheme of SPH.

Answer: We appreciate your insightful suggestion regarding the artificial viscous scheme for free surface flows. In this study, the physical viscous scheme (Morris’ formulation [41], Eq. 6) was adopted to prioritize numerical stability and direct alignment with the Navier-Stokes equations, as validated in Section 3.1 (square droplet oscillation) and Section 3.2 (droplet impact on hydrophobic walls). While artificial viscosity is widely used to suppress numerical oscillations near free surfaces, our tests confirmed that the current scheme sufficiently stabilizes simulations without compromising accuracy for the studied cases. Artificial viscosity demonstrates notable advantages in complex free-surface scenarios such as wave breaking and splash [2–4]. We recognize its potential value and will systematically compare both methodologies in subsequent studies to optimize the model and expand its applicability to broader computational domains.

References:

[41] Morris J P, Fox P J, Zhu Y. Modeling low Reynolds number incompressible flows using SPH, Journal of Computational Physics 136 (1997) 214-226.

[28] He, F., et al., Multi-phase SPH-FDM and experimental investigations on the hydrodynamics of an oscillating water column wave energy device. Coastal Engineering, 2024. 192: p. 104569. https://doi.org/10.1016/j.coastaleng.2024.104569

[29] Wang, X.J., et al., Study on hydrodynamic characteristics of multiple fish based on smoothed particle hydrodynamics. Physics of Fluids, 2024. 36(11): p. 111915.

https://doi.org/10.1063/5.0236386

[30] Huang, C., Zhang, D. H., Shi, Y. X., Si, Y. L., & Huang, B. (2018). Coupled finite particle method with a modified particle shifting technology. International Journal for Numerical Methods in Engineering, 113(2), 179-207. https://doi.org/10.1002/nme.5608

3. In Eq. (7), what does the variable mean?

Answer: Following your suggestions, the variables in Eq. (7) have been clarified and incorporated into the revised manuscript.

(7)

where v is the fluid velocity, p is the fluid pressure, μ is the dynamic viscosity of the fluid, and g denotes the body force acting on the fluid, such as gravitational force. vij= vi-vj, rij =ri-rj, rij = |rij|. The term η

Attachment

Submitted filename: Response to Reviewers.docx

pone.0323418.s003.docx (234.1KB, docx)

Decision Letter 1

Xin Yong

8 Apr 2025

The numerical simulation of droplet impact on surfaces is conducted using the SPH-DEM method

PONE-D-24-50755R1

Dear Dr. Bu,

We’re pleased to inform you that your manuscript has been judged scientifically suitable for publication and will be formally accepted for publication once it meets all outstanding technical requirements.

Within one week, you’ll receive an e-mail detailing the required amendments. When these have been addressed, you’ll receive a formal acceptance letter and your manuscript will be scheduled for publication.

An invoice will be generated when your article is formally accepted. Please note, if your institution has a publishing partnership with PLOS and your article meets the relevant criteria, all or part of your publication costs will be covered. Please make sure your user information is up-to-date by logging into Editorial Manager at Editorial Manager®  and clicking the ‘Update My Information' link at the top of the page. If you have any questions relating to publication charges, please contact our Author Billing department directly at authorbilling@plos.org.

If your institution or institutions have a press office, please notify them about your upcoming paper to help maximize its impact. If they’ll be preparing press materials, please inform our press team as soon as possible -- no later than 48 hours after receiving the formal acceptance. Your manuscript will remain under strict press embargo until 2 pm Eastern Time on the date of publication. For more information, please contact onepress@plos.org.

Kind regards,

Xin Yong

Academic Editor

PLOS ONE

Additional Editor Comments (optional):

Please revise the title of the accepted manuscript to an acceptable form, for example "Numerical simulations of droplet impact on surfaces using SPH-DEM method"

Reviewers' comments:

Reviewer's Responses to Questions

Comments to the Author

1. If the authors have adequately addressed your comments raised in a previous round of review and you feel that this manuscript is now acceptable for publication, you may indicate that here to bypass the “Comments to the Author” section, enter your conflict of interest statement in the “Confidential to Editor” section, and submit your "Accept" recommendation.

Reviewer #1: All comments have been addressed

Reviewer #2: All comments have been addressed

**********

2. Is the manuscript technically sound, and do the data support the conclusions?

The manuscript must describe a technically sound piece of scientific research with data that supports the conclusions. Experiments must have been conducted rigorously, with appropriate controls, replication, and sample sizes. The conclusions must be drawn appropriately based on the data presented.

Reviewer #1: Yes

Reviewer #2: Yes

**********

3. Has the statistical analysis been performed appropriately and rigorously?

Reviewer #1: N/A

Reviewer #2: Yes

**********

4. Have the authors made all data underlying the findings in their manuscript fully available?

The PLOS Data policy requires authors to make all data underlying the findings described in their manuscript fully available without restriction, with rare exception (please refer to the Data Availability Statement in the manuscript PDF file). The data should be provided as part of the manuscript or its supporting information, or deposited to a public repository. For example, in addition to summary statistics, the data points behind means, medians and variance measures should be available. If there are restrictions on publicly sharing data—e.g. participant privacy or use of data from a third party—those must be specified.

Reviewer #1: Yes

Reviewer #2: Yes

**********

5. Is the manuscript presented in an intelligible fashion and written in standard English?

PLOS ONE does not copyedit accepted manuscripts, so the language in submitted articles must be clear, correct, and unambiguous. Any typographical or grammatical errors should be corrected at revision, so please note any specific errors here.

Reviewer #1: Yes

Reviewer #2: Yes

**********

6. Review Comments to the Author

Please use the space provided to explain your answers to the questions above. You may also include additional comments for the author, including concerns about dual publication, research ethics, or publication ethics. (Please upload your review as an attachment if it exceeds 20,000 characters)

Reviewer #1: Dear Authors,

The reviewer is satisfied with the revised version of the manuscript: I acknowledge the efforts made. Some unknown characters appear in the pdf file, e.g., page 9 "、λ=0.25 [7]、f is ...": could be a matter of some issues in the pdf generation.

Kind regards

Reviewer #2: The authors have well answered my all questions. I would like to recommend publication of this manuscript.

**********

7. PLOS authors have the option to publish the peer review history of their article (what does this mean? ). If published, this will include your full peer review and any attached files.

If you choose “no”, your identity will remain anonymous but your review may still be made public.

Do you want your identity to be public for this peer review? For information about this choice, including consent withdrawal, please see our Privacy Policy .

Reviewer #1: No

Reviewer #2: No

**********

Associated Data

    This section collects any data citations, data availability statements, or supplementary materials included in this article.

    Supplementary Materials

    Attachment

    Submitted filename: Comments on PONE-D-24-51781.pdf

    pone.0323418.s001.pdf (115.6KB, pdf)
    Attachment

    Submitted filename: Response to Reviewers.docx

    pone.0323418.s003.docx (234.1KB, docx)

    Data Availability Statement

    We have uploaded the data into an online database, which can be found at the link below. https://doi.org/10.6084/m9.figshare.28659227


    Articles from PLOS One are provided here courtesy of PLOS

    RESOURCES