1. Introduction
The interaction of shock waves with combustion products containing particles of a condensed phase is an important problem in the combustion chambers of rocket engines. The challenges of capturing high-speed processes are linked to the limitations of experimental diagnostic tools. The high cost of processor time and the imprecision of mathematical models restrict the possibilities of the numerical modeling of high-speed flows [
1,
2].
Continuum or continuum–discrete models are widely used in computational practice to describe the interaction of a dense layer of particles with a shock wave. To enhance description of fluid flow in porous or granular media, the interaction between a supersonic fluid flow and various shaped solids has been conducted [
3]. These works generally focus on the computational or experimental modeling of flow around stationary bodies, as well as the study of interference effects during joint flow around solids.
Experimental and numerical studies of the interaction of a shock wave with layer of particles are presented in [
4]. The impact of the dispersed phase on air pressure distribution and shock wave structure was investigated. The volume concentration of particles reached 0.35. The effectiveness of various numerical techniques was then assessed using the obtained experimental data [
5,
6,
7,
8].
The work [
9] investigates physical conditions and dynamics of shock wave propagating through an array of solids and the formation of a collective bow shock in front of them. Two types of shock wave structures that experiments recorded corresponded to regular and Mach reflections of shock waves from each sphere onto the other. Quantitative conditions were established for the existence of various regimes and their transitions to a bow shock wave.
A continuum–discrete array of laminar particle-laden flow is used in [
10] to study shock wave propagation through an array of particles. The volumetric fraction of the dispersed phase varied from 0.1 to 3%. The results obtained showed the modification of shock wave structure in supersonic flow with particles. Bow shocks are formed at low particle concentrations on each particle. If the concentration of particles increases, neighboring shock waves interact with each other, overlap, and generate a common bow shock.
The data presented in [
11] confirm that the polydispersity of particles has a small impact on flow pattern (eight fractions, particle diameters varied from 60 to 130 µm with a step of 10 µm). Flow constraint effects happen in a supersonic nozzle if
while, in low-speed flows, they happen if
[
10].
The works [
12,
13] model, in two dimensions, the interaction of a shock wave with a dense layer of solid particles. Particles of a dispersed phase had a volume fraction of 0.15 and were assumed to be immobile. The configuration under investigation agreed qualitatively with the quantities of the experimental work [
14]. Two-dimensional calculations were used to obtain qualitative descriptions of multi-dimensional effects. The results were compared with calculations using a one-dimensional formulation, demonstrating how important it is to take into account multi-dimensional effects associated with Reynolds stresses in turbulent wake and within a particle cloud. It was shown that there exist both transmitted and reflected shock waves, and a fan of rarefaction waves in the layer of particles. A contact discontinuity forms at the trailing edge of the layer as the shock wave exits. The Reynolds stresses in momentum transport equations are comparable to static pressure, both within and outside the particle cloud. Flow kinetic energy and turbulent kinetic energy are equal in this region.
The interaction of a shock wave with a group of particles in a horizontal cylindrical shock tube is covered in [
15]. The particles’ reflection of the shock wave causes the pressure to increase. The intensity of the reflected shock wave increases if the particle loading increases and the particle size decreases. The shock wave becomes less intense as it passes through the particle layer. If the particle loading increases and particle diameter decreases, the shock wave attenuates.
The study [
16] compares data acquired using different collisional models of gas suspension flow. When big (1 mm in diameter) particles collide, the impact of gas-dynamic forces is negligible in comparison to the impact of collision forces.
Shock wave propagation through a layer of particles in the air is simulated in [
17] for Mach numbers up to 10. When a shock wave passes through the particle layer, it becomes more powerful at each new particle. A multiscale technique for modeling the dynamics of multiphase flows under shock waves is developed in [
18]. This technique makes it possible to examine how a cloud of particles evolves and to show how the particle gas-dynamic interaction affects cloud motion. Calculations were conducted for various particle sizes, volumetric concentrations of those particles, and Mach numbers. The results of the three-dimensional simulation are presented in [
19]. Particle trajectories were calculated with the Lagrangian method. The computations altered the cloud size and particle volume concentration.
The works [
20,
21] construct high-order finite-difference schemes for a mixed Eulerian–Lagrangian description of particle-laden flow. The results computed were in reasonable agreement with experimental data. Particle dispersion was analyzed with respect to the initial cloud geometry, and it was discovered that the layer shape plays a significant role in calculations of the transverse direction of particle dispersion.
The works [
22,
23,
24] study the propagation of particles in accelerating flow behind the front of a normal shock wave, the impact of flow direction on particle dispersion for clouds of elliptical and rectangular shapes, and the ratio of the cloud’s longitudinal size to its transverse size. The area occupied by the particle cloud remained constant while the shape changed. The volume concentration of particles was 4%. A high-order finite-difference monotonic scheme was used for the numerical solution. In comparison to a rectangular cloud, the elliptical cloud has less dispersion. The speed of cloud convection in the flow direction increases as the ratio of the cloud’s longitudinal to transverse dimensions decreases.
The work [
25] uses continuum models to describe two-phase flow. The works [
14,
26,
27,
28] consider the interaction of a layer of particles with a shock wave. The particle volume concentration corresponded to a regime of dense packing of a dispersed phase (volume concentration of particles was 0.21). Experimental studies were conducted for a dense filling of particles (volume concentration of particles was 0.48) in [
29].
Numerical methods for the simulation of shock wave interaction with both a single particle and a layer of particles are developed in [
30]. The configuration of particles at a cubic lattice of nodes and face centers is examined. Particles were assumed to be stationary. This led to a rarefaction of the particle array at the beginning of its movement due to a more intense movement of the cloud’s rear edge. This phenomenon occurred for all volume fractions for small Mach numbers of the incident shock wave, where particles’ drag downstream was greater than that of particles at the leading edge of the array. This effect was less noticeable for high incident shock wave Mach numbers (the particle system moved nearly as a single unit). Only media with a low fraction of the dispersed phase are suitable for using correlations for the drag of an individual particle to account for the motion of the particle layer [
9].
The propagation of a shock wave through a layer of regularly positioned squares and circles is considered in [
31]. The impact of various drag correlations on the outcomes of the interaction of a shock wave with particles is assessed in [
32]. Only media with a low fraction of the dispersed phase are suitable for using correlations for the drag coefficient of an individual sphere to account for the motion of a cloud of particles [
9]. The studies [
33,
34] demonstrate how little the Magnus and Saffman forces affect particle dynamics in supersonic flows.
The work [
35] presents results of a simulation of the rise of particles behind a shock wave reflected from the tube end and sliding over a layer of particles. Particles rise in a vortex that forms in the air subsequent to the shock wave’s reflection off the wall. Due to the inhomogeneity of air flow behind the transmitted shock wave, the reflected shock wave forms a
-shaped structure leading to the formation of a vortical flow. The problem of a plane shock wave propagating over a square cavity with particles is discussed in [
36]. The shock waves in a cavity become weaker and transform into compression waves if the particle concentration increases. The flow pattern and wave structure are influenced by particle size. The flow approaches the structure of air flow for large particle diameters of about 250 µm. The problem of suppressing a shock wave in a layer of inert particles is considered in [
37]. Ignoring volume occupied by particles, results of simulation are presented in [
38].
The propagating of a shock wave through a layer of particles is solved numerically in [
39] to identify types of interactions of shock waves in front of bodies. Different flow modes around particles are realized depending on the distance between spheres and speed of the supersonic flow behind the shock wave. When bodies are in close proximity to each other while a shock wave is passing through, the flow regime varies from regular reflection to a Mach interaction of shock waves and, finally, to a common shock wave [
40].
Numerous practical issues remain unresolved, even with the advancements made. The influence of a particle on the structure of the bow shock and the transmitted, reflection of the shock wave from a group of particles, the presence of secondary shock waves, and the intense vortex flows behind the layer of particles are among them. The intricacy of this issue demands the creation of theories and use of mathematical modeling techniques to explain the dynamics of multiphase flow. It also calls for thorough investigations of scientific and technical issues utilizing cutting-edge computational experimentation and mathematical modeling technologies. This study examines the characteristics of the numerical solution for the shock wave propagation problem in a mixture of inert particles and air using a Eulerian–Eulerian approach. The results of the interaction between a shock wave and a dense layer of particles were compared with a full-scale experiment [
4]. The distribution of the fraction of particles and shock wave structure were examined, and the results were contrasted with available experimental and computational observations.
The proposed approach is based on governing equations of the hyperbolic type for gas and particles. This allows to extend the computational algorithms designed for pure gas to the solution of gas dynamics problems with solid particles. The presence of secondary shock waves may lead to the inefficient use of the layer of particles to protect the objects from a destructive effect of shock waves. The proposed approach enables an optimization of the coating process at the impingement of a supersonic gas–particle flow onto an obstacle.
2. Mathematical Model
The Lagrangian approach to the simulation of particle dynamics is too expensive from a computational point of view. It involves the simulation of
particles [
41], where
N is the number of mesh cells,
D is the dimension. A lower estimation of a number of particles is about six particles per mesh cell in each coordinate direction [
42,
43]. These particle number requirements become unnecessarily high for fine meshes. The Eulerian approach requires less degrees of freedom than the Lagrangian approach [
25].
A model of interpenetrating continua was applied to describe fluid flow with particles (Eulerian–Eulerian approach). This approach led to conservation equations of mass, momentum, and energy for each phase. Semi-empirical correlations for the drag and heat flux of individual particles were applied to close governing equations. The Baer–Nunziato model proposed in [
44] and expanded in [
5,
6] supposes the existence of two velocities and two pressures of gas and solid phases. Depending on how the model is applied, different pressures and velocities are chosen at the interface between two phases.
A mixture of two continua, each with its own pressure, velocity, and temperature, is referred to as a two-phase medium. The continuity, momentum, and energy equations are derived for each phase with an additional equation describing the transport of the volumetric fraction of the dispersed phase. The viscosity and thermal conductivity of the air are considered when the air interacts with particles.
- 2.
Transport equations of particles
- 3.
Transport equation of the volume fraction of particles
Here,
t is time,
x is the Cartesian coordinate,
is the
ith phase volume fraction and
,
is the
ith phase density,
is the
ith phase velocity,
is the
ith phase pressure,
is the
ith phase-specific total energy, and
is the
ith phase dynamic viscosity. The subscripts
g and
p correspond to air and particles. The dynamic viscosity of the dispersed phase characterizes pressure relaxation on the interface. The total energies of the air and particles are found as
where
is the ratio of the specific heat capacities at a constant pressure and constant volume. The equation of the state of the ideal gas,
, where
R is gas constant, yields gas pressure. Assuming that solid particles are weakly compressible, the dispersed phase is described by a two-term equation of state containing quantities
and
(
,
Pa).
The source terms in governing Equations (
1)–(
7) take into account processes on the interphase. The interphase pressure and velocity,
and
, are averaged over the control volume of two-phase flow. The closing relations used in order to calculate these quantities are represented as
On the interface, the phase pressures are equal (
). This condition is imposed in the presence of an interphase boundary, rather than assuming the equality of phase pressures, which would violate the hyperbolicity of the governing equations.
The particle Equations (
4)–(
6) and gas Equations (
1)–(
3) are inter-related with source terms. The relationship yields the drag force applied per unit volume
where
is particle diameter. The drag coefficient is found as
where
corresponds to the Stokes law. The correction function depends on the relative Reynolds and Mach numbers and accounts for compressibility and inertia effects
The heat flux between the gas and particles is
where
is the thermal conductivity. The Nusselt number depends on the Reynolds and Prandtl numbers. It is calculated as
where
. The relative velocities of gas and particles are used to compute the Reynolds and Mach numbers
where
a is the speed of sound.
3. Numerical Method
The convective terms are found in the left-hand sides of the mass and momentum equations. The terms associated with the non-conservative parts of the governing equations, and , are moved to the right-hand sides. The equations of state are applied to determine pressures of the gas and particles. The governing equations are composed of a hyperbolic part and, in order to account for the interfacial interaction, pressure and velocity relaxation terms are added.
The unsteady one-dimensional particle-laden flow is described by equation
The vector of flow quantities and flux vector have the form
The source terms on the right-hand side are
The splitting into physical processes is applied to discretize the transport equations of gas and the dispersed phase. In the first step, the transport is integrated if (hyperbolic step, indicated by the operator ). In the second step, the pressure relaxation process (represented by the operator ) is accounted. The third step involves accounting for non-differential source terms (represented by the operator ) that are responsible for the interphase interaction.
A series of operators act to produce the solution to Equation (
8), in accordance with the splitting into physical processes procedure
Subscript
j is related to the mesh cell, and superscript
n is related to the time layer. Three steps are involved in finding a solution on a new time layer: (i) calculation of the gas-dynamic process, (ii) calculation of the velocity relaxation, and (iii) calculation of the pressure relaxation.
Step 1. Calculation of the gas-dynamic component. Without accounting for pressure and velocity relaxations, the model describing two-phase flow is hyperbolic. A Godunov-type scheme proposed in [
45] was applied to discretize it. However, the hyperbolic equations have one non-conservative equation for the volume fraction of particles and non-conservative terms.
The equation describing the flow is
A mathematical analysis of the hyperbolic part of the governing equations written in one-dimensional form is performed in [
46]. The Jacobian eigenvalues are
,
,
,
, and
. The relation yields the sound speed
Here,
is a specific internal energy. Equation (
10) is hyperbolic, and the Jacobian eigenvalues are real and distinct.
A higher order of accuracy Godunov-type method is applied to make the hyperbolic step with the HLLC (Harten–Lax–van Leer–Contact) method to solve the Riemann problem and the minmod limiter.
The finite-volume scheme scheme for Equation (
10) is
where
is the vector of flow quantities in cell
j at time later
n, and
is the numerical flux on the cell face. The flux of conservative variables through face
is
where
, and
. The additional factor is
Step 2. Calculation of the velocity relaxation. To find the flow quantities at the velocity relaxation step, the following equation is used:
Various techniques of integration of ordinary differential equations including Euler or Runge–Kutta methods are applied to solve (
11).
Step 3. Pressure relaxation computation. The equation used to determine the flow quantities is as follows:
Various techniques of integration of ordinary differential equations including Euler or Runge–Kutta methods are applied to solve (
12).
The fluxes are discretized with a 2nd-order numerical scheme, and integration over time is conducted with a 3rd-order Runge–Kutta scheme. The employed Runge–Kutta scheme is positive (if the numerical solution is positive on time layer n, it remains positive on time layer ). The numerical scheme on hyperbolic step satisfies the TVD condition.
4. Results and Discussion
A vertical shock tube with a cross-section area of cm2 and a length of 6 m was considered. Under normal circumstances, the shock tube contained pure air () at normal atmospheric conditions. Air density was kg/m3, and air pressure was Pa. The air was in a stationary state () at the initial time. The tube inlet section was situated one meter away from the dividing partition. A 2 cm thick layer of particles was situated 3.055 m away from the dividing wall. The particles had a diameter of 1.5–2 mm and were solids made of either nylon ( kg/m3) or glass ( kg/m3). The particles were packed, and the volume fraction of air was 0.36. At the initial time, the particles were not moving.
The shock wave with a Mach number of 1.29 was created when a diaphragm was destroyed. A shock wave traveled from the bottom to the top of the tube, and there was a rarefaction wave that propagated in the opposite direction. The air quantities behind the shock wave front were as follows: the pressure was 18,289 Pa, density was kg/m3, and velocity was m/s. The tube end walls reflected both the shock and rarefaction waves at different points in time. There were two pressure sensors in the tube. The pressure sensor 1 was positioned 11 cm below the particle layer. The pressure sensor 2 was positioned 4.3 cm above the particle layer.
Figure 1 provides an explanation of the computational domain and the experimental setup from the work [
4] (lengths are given in meters, and scale is not observed). The initial coordinate of the shock wave front at time
is
. There are two pressure sensors inside the shock tube. Pressure sensors 1 and 2 are situated 4.3 cm above the particle layer (
m) and 11 cm below it (
m). The reflected shock wave is detected by sensor 1. Sensor 2 captures the transmitted shock wave. The layer of particles is two centimeters thick. It is considered that a two-phase medium fills the computational domain. Particles in the layer have an initial concentration of 0.65, while those outside the layer have an initial concentration of
. No penetration boundary conditions are specified on the upper boundary, and the flow quantities are specified on the lower boundary. On a mesh with 1000 cells, calculations are conducted up until 4.6 ms (before the rarefaction wave arrives).
Figure 2 illustrates pressure distribution in pure air. The pressure sensor 2 is situated 4.3 cm above the particle layer. Solid lines represent the computation results, and symbols • represent the experimental data from [
4]. The computational and experimental data agree well with each other.
Section 2 and
Section 4 correspond to rarefaction waves, while
Section 1 and
Section 3 correspond to incident and reflected shock waves.
Figure 3 shows the
diagram of propagation of gas-dynamic discontinuities. With an initial velocity of zero, the incident shock wave interacts with contact discontinuity, which separates the region of pure air from the region occupied by particles. The interaction creates two shock waves: (i) a transmitted wave that travels along the two-phase region before exiting into the pure air region, and (ii) a reflected shock wave that travels towards the inlet section.
Simulations of trajectories of individual particles were also performed with a Lagrangian approach to verify the accuracy of the sub-model describing the interphase momentum exchange.
Figure 4 displays the trajectory of a single particle (solid lines) in comparison to the data obtained from the physical experiment [
4] (symbols • and symbols ∘). Line 1 and symbols • denote particles of nylon measuring 2 mm in diameter, while line 2 and the symbols ∘ denote particles of glass measuring the same diameter. Times
and
ms correspond to the start of the interaction of the incident shock wave with particles and the appearance of a rarefaction wave.
Figure 5 displays concentration profiles of the dispersed phase at various times. Vertical dotted lines represent the particle layer position [
4]. Transmitted and reflected waves are created when the incident shock wave interacts with the layer of particles. The array then starts to move as a result of the pressure difference to its left and right and the interfacial interaction force.
The difference between the current solution and computational results from [
4] is explained by physical and numerical effects. Physical effects include the impact of viscosity and thin boundary layers on wall tubes. The simulation of particle motion requires the use of semi-empirical correlations for the drag of individual particles. These correlations are usually available for a sphere in uniform flow. One of the unresolved issues is how finite particle volume concentration can affect drag and heat transfer of each particle in the cloud.
The air pressure behind the transmitted shock wave and above the upper boundary of the backfill area is roughly 1.2 a.m., while the air pressure behind the reflected shock wave and in front of the lower boundary is about 3 a.m. A pressure differential of roughly 1.8 a.m. is felt by the layer of particles, which causes it to start moving upward. Due to the force of viscous friction, the air that has been displaced by the transmitted shock wave moves in relation to initially stationary particles and displaces them. A two-phase flow toward the second pressure sensor appears as a result of both effects. In this instance, the particle layer is smeared, meaning that the area it occupies is shifting and getting larger.
Figure 6 (solid lines) illustrates how the lower and upper boundaries of the particle layer change over time (blurring of the layer boundaries) in comparison to data from the physical experiment from [
4] (symbols • and symbols ∘). A one-millimeter diameter glass particle is used in the calculations. The lower boundary of the layer is represented by line 2 and symbols ∘, while the upper boundary is represented by line 1 and symbols •. The boundaries of the particle layer are significantly blurred, with the upper boundary of the layer being more so than the lower.
Figure 7 displays pressure distributions (solid lines) compared to data from the physical experiment [
4] (symbols • and ∘). Pressure sensors 1 and 2 are represented by line 1 and • and ∘ icons, respectively. As compared to the experiment, the pressure behind the transmitted shock wave is higher and the pressure behind the reflected shock wave is lower [
4]. The figure displays average values of pressure. The experimental curve reported in the work [
4] has pulsations that are not present in the computed curve.
For the entire time range, the pressure distribution over time at the first sensor agrees well with experimental measurements. Sensor 1 records the incident shock wave traveling through it at time ms, and the reflected shock wave traveling through it at time ms. As the sensor passes through, the air pressure behind the reflected wave reaches 2.964 a.m. As the shock tube is being unloaded, a two-phase flow occurs, causing the air pressure to gradually drop. A total of 3.149 a.m. of pressure is behind the shock wave that is reflected off the solid wall.
On sensor 2, there is a little less agreement between computational and experimental data. At the beginning of the process, there is a qualitative coincidence in the results. A weak transmitted shock wave enters the second pressure sensor at ms. The pressure behind the shock wave front is about 1.18 a.m., and it gradually rises to 1.25 a.m. over time. A flow of air and particles arrives at the second sensor location at time ms. The pressure rises in 1.5 ms to 2.4 a.m. Then, as a result of unloading, the pressure in the vicinity of the second sensor starts to gradually drop.
The observed discrepancy between computational and experimental data is explained by presence of a boundary layer near the tube walls, which leads to the distortion of the particle layer near the walls in the experimental photographs presented in [
4,
29].