3.5.2. Theoretical Representation of Vortex Ring Formation and Propagation
The vortex ring at the main stage of the propagation trajectory is a steady-state aerodynamic structure consisting of a toroidal vortex, inside which almost all the vorticity is concentrated, and the “atmosphere” of the vortex—the region surrounding the core and moving with it. The ring moves in the environment with the preservation of geometric proportions, the main of which is illustrated in
Figure 8.
Vortices are formed where the flow velocities change rapidly along the normal values to the fluid flow lines: in these places, large forces of viscous friction arise. In a viscous medium, there can be no sharp boundary between two flows, so there is a transition layer with rapidly changing velocities. The thickness of this layer is less, the lower the viscosity of the medium. Additionally, vortices are often formed when the velocity changes sharply in the direction that leads to the formation of interfaces. Here, too, there is a velocity gradient along the normal to the fluid flow lines and the formation of viscous friction forces that cause small gas particles to rotate first and then larger volumes. When the air is pushed out of the cavity, a boundary layer with significant vorticity is formed on the walls of the cavity nozzle due to viscous adhesion. The formation of the vortex begins when the jet front exits the nozzle into an undisturbed medium. The boundary layer under the action of the velocity field turns into a spiral. The leading edge of the mushroom head of the vortex is the boundary of the liquid that was in the pipe before the start of the jet outflow process. It follows from the results of the experiments that during the main time of the jet outflow, the velocity of the leading edge extension is approximately equal to half of the jet velocity. The jet that feeds the vortex retains its cylindrical shape even after exiting the hole, and only when entering the vortex does its cross section decrease. At high Reynolds numbers, the boundary layer is thin and practically represents a tangential discontinuity, due to the instability of which (Kelvin–Helmholtz instability) the structure of the boundary layer is destroyed. The layers are mixed, which leads to the formation of a vortex core. It is worth noting that the core of the vortex forms only the front part of the boundary layer, and the rest of the latter enters the atmosphere of the vortex, where it spreads more or less evenly by turbulent pulsations and then gradually passes into the vortex path.
Figure 9 shows the scheme of vortex ring formation.
It is experimentally defined that the core and the “atmosphere” of the vortex, respectively, account for 7.7% and 92.3% of the total mass of the medium carried by the vortex (at least after its formation), i.e., the mass of the core exceeds the mass of the “atmosphere” by about 12 times [
14]. Thus, assuming
R/
a =
k, where
k is the experimental coefficient, and the ratio of the volumes of the atmosphere and the core equal to 12 (the density of the vortex medium is determined by the density of the “atmosphere”), we obtain the following estimate:
b2 = 41.22(1/
k)
2b1, i.e., on average, one half-axis of the ellipsoid exceeds the other by 1.5 times.
Let us take a closer look at the VR structure. The maximum velocities
vx of each of the sections lie in the plane x = 0 passing through the circular axis of the vortex (
Figure 10). In this plane, |
vx| > |
v0| except for the area close to the circular axis. At infinity,
vx tends asymptotically to
v0. The maximum values of the
vr velocities are localized on the cylinder
r =
D/2, vanishing at
x = 0. At infinity,
vr tends to 0.
Next, we provide a justification for the statement about the possibility of transferring various additives (f. e. smoke particles) by the ring [
15]. The velocity in the circulation flow, in contrast to the rotational velocity of a solid, decreases along the hyperbola with increasing radius. The pressure, on the contrary, according to the Bernoulli equation decreases from the periphery to the center.
On the axis of the vortex, the potential flow is disturbed: the vortex core of the circulation flow, having a small diameter, rotates already as a solid body and the Bernoulli equation is not applicable here. In the core, the linear velocity increases from the center to the periphery in proportion to the distance to the boundary between the vortex core and the atmosphere. The position of this boundary depends on the angular velocity of the core.
Using the equation of gas element equilibrium in a steady circulation flow around a single vortex and bearing in mind that in the core
v = ω
r, where ω is the vorticity (s
−1), we obtain the following:
The sign of Δp coincides with the sign of Δr, therefore, inside the vortex core, the pressure continues to decrease from the periphery to the center (although the speed also decreases toward the center). Thus, a strong suction occurs in the core, due to which outer particles are drawn (sucked) into the core.
The parameters of the vortex torus can be described using the model of a cylindrical vortex with a finite core of a circular cross section of radius
a, in which the vorticity ω is constant—the Rankin vortex [
16] (
Figure 11). Outside the core, the current is assumed to be vortex-free. Such a vortex can be approximated by a continuous distribution of rectilinear vortex filaments in the core. Then, the cross-sectional element of the core d
S gives a contribution to the circulation dΓ equal, according to Stokes theorem, to dΓ = ωd
S. The circulation along any contour that once covers the entire core of the vortex is Γ = ωπ
a2 = const.
If we take into account the axial symmetry of the problem, i.e., the presence of only the circumferential component of the velocity
vr =
vr(
r), then from the Stokes theorem for a circle of radius
r > 0 we have 2π
rvr = ωπ
a2, from where, taking into account the expression for circulation, we find an expression for the velocity in the region of the vortex-free (potential) flow.
Inside the core, we similarly obtain 2π
rvr = π
r2ω or
The average velocity in the VR core can be estimated as the ratio of the linear velocity at the boundary of the core to the radius of the core. From experimental data [
8], at the Reynolds number Re = 7.5 × 10
4, the angular velocity of rotation in the core reaches 35,000 rpm. The forward speed of the ring is 11 m/s. In experiments conducted with the help of a shock tube, rings with a translational velocity of more than 100 m/s were obtained (in particular, at the speed of the outgoing jet of 198 m/s and the radius of the generator nozzle of 25 mm, a ring with a radius of 33 mm moving at a speed of 99 m/s was obtained).
The radial distribution of static pressure is characterized by its sharp decrease in the vortex core. To calculate the pressure profile, we apply the Euler equation, which in polar coordinates, taking into account the axial symmetry, will take the form
, from where
, where ρ is the density of the medium;
the pressure at infinity. Substituting the velocity profiles in the expression for pressure, we find the pressure distribution
The minimum pressure is achieved on the axis of the vortex as follows:
For an infinitely thin vortex thread of intensity Γ, the pressure on the axis tends to (−∞), as can be seen with a tending to 0.
To determine the initial geometric parameters of the vortex ring, we can write a closed system of equations as follows:
where
Dn is the exit diameter of the nozzle,
R0 is the initial radius of the ring,
a0 is the initial radius of the ring core;
b1 and
b2 are the dimensions of the sides of the “atmosphere” of the vortex (taken as an ellipsoid),
k1 = 1.1…1.3 experimental coefficient that determines the expansion of the ring at the exit from the generator nozzle (when the ring is formed inside the generator,
k1 can be taken equal to 1), and
k is the coefficient.
Since the vortex is a stable structure, we assume that its geometric parameters change proportionally on the trajectory.
To determine the kinematic characteristics of a vortex ring, we consider a physical model of its motion in the environment.
For further discussion, we will take the following notation: U is the forward velocity of the vortex ring; u is the rate of expansion of the vortex ring along the y axis; vel is the velocity modulus of the vortex element; ρ1 is the density of the medium outside the ring (since the motion of the ring at the earth’s surface is considered, we can take ρ1 = 1.29 kg/m3—the density of air under normal conditions); ρ is the density of the medium inside the ring (determined by the density of the “atmosphere”); Γ is the velocity circulation; S is the area of the midsection of the vortex; M is the mass of gas in the vorticity region; M1 is the mass of gas in the “atmosphere”.
In the framework of the physical model of the process used, based on [
17], we assume the following assumptions:
- -
The gas heated to a certain temperature and located in the generator chamber exits the nozzle in a uniform laminar flow, the core of the vortex is completely formed from this gas, and the “atmosphere” of the vortex is formed from the surrounding cold air;
- -
During the movement of the vortex, there is a constant mass exchange of the gas forming the “atmosphere” of the vortex with the external environment due to turbulent mixing;
- -
The air in the core of the vortex does not flow out; therefore, as the size of the core increases, colder air from the “atmosphere” flows into it, which leads to a gradual cooling of the core.
When the ring moves, the following three forces act on it:
- (3)
The power of Zhukovsky
The Zhukovsky force acts perpendicular to the gas element motion direction; its vertical component stretches the ring, and the horizontal component slows down its movement (for a circular vortex ring FZh = 2πρ1ΓvelR);
- (4)
Hydrodynamic drag force
where
Cx is the coefficient of resistance of the vortex, and
S is the area of its midsection. The force due to the pressure difference in front of and behind the ring and the viscous friction on the surface of the body, determined by the disruption of the flow from the back side (friction at the boundary, as already noted, is small) and directed opposite to the forward velocity of the ring;
- (5)
The Archimedean force, which arises from the difference in the densities of the air inside the ring and in the atmosphere,
where
Vrot is the volume of the “atmosphere” of the vortex.
Thus, it is possible to obtain the equations of ring motion in projections on orthogonal coordinate axes as follows:
Analyzing the large array of experimental data obtained, we can conclude that the most acceptable form of estimating the change in the radius of the vortex ring on the trajectory is the formula
where α =
R/
L is the expansion coefficient determined from the experiment (for estimated calculations, we can take α ≈ 0.01). Thus, the rate of expansion of the ring is constant over the entire trajectory of its motion, and in System (2), we can take
u = α
U, and then consider only the first equation of the system, in which the approximation
U ≈
vel will be valid.
When decomposing the left part of the equation, we can distinguish the mass transfer factor
, where
m = 1.08
M1 is the total mass of the vortex ring, taken from the condition
M1/
M = 12. Let us assume that mass exchange with the environment occurs only in the “atmosphere,” and in the core of the ring, the environment remains unchanged during movement. Estimates for the mass transfer factor
dm/
dt are semiempirical. Considering the motion of the vortex ring in the form of an ellipse of rotation with a major semiaxis
b1 =
R/0.9 and with a mass
m = 1.08
M1 = 1.08π
RcgSell, where
Rcg is the coordinate of the center of gravity of the half of the ellipse, and
Sell = π
b1b2, and taking the postulate of preserving the shape of the vortex, as well as the linear dependence of the increasing radius on the distance traveled, we obtain the ratio
Thus, the mass of the turbulent vortex ring increases linearly in accordance with the distance traveled by the vortex, due to the involvement of media from the environment in the vortex motion. As a result of this process, the kinetic energy is lost, and the vortex is decelerated.
The relationship between the density of the gas forming the vortex and the temperature can be determined using the Clapeyron–Mendeleev equation.
The temperature of the vortex ring at the current time can be defined as
where
V0 is the initial volume of the vortex ring, which can be assumed to be equal to the volume of the generator chamber;
T0 is the initial temperature of the gas in the ring;
Tinv is the ambient temperature.
The circulation of the medium in the vortex ring can be determined by the Burgers formula
Thus, from the first equation of the System (1), we finally obtain the differential equation
where
—coefficient of geometric dimensions of the ring;
—coefficient of the geometric shape of the ring;
—mass transfer coefficient.
The visualization technique considered in this paper may be used to verify the developed model of the motion of the vortex ring, which is the subject of a separate study. Here, for example, we will present a specific result of comparing theoretical representations with experimental results.
Figure 12 shows a comparison of the velocity calculated from (8) with the experimental data. A rather large spread of experimental data is explained by the difficulty of accurately selecting a certain point of the ring for “tracking” the speed.