Solitonic dispersive hydrodynamics: theory and observation

Solitonic dispersive hydrodynamics: theory and observation

Abstract

Ubiquitous nonlinear waves in dispersive media include localized solitons and extended hydrodynamic states such as dispersive shock waves. Despite their physical prominence and the development of thorough theoretical and experimental investigations of each separately, experiments and a unified theory of solitons and dispersive hydrodynamics are lacking. Here, a general soliton-mean field theory is introduced and used to describe the propagation of solitons in macroscopic hydrodynamic flows. Two universal adiabatic invariants of motion are identified that predict trapping or transmission of solitons by hydrodynamic states. The result of solitons incident upon smooth expansion waves or compressive, rapidly oscillating dispersive shock waves is the same, an effect termed hydrodynamic reciprocity. Experiments on viscous fluid conduits quantitatively confirm the soliton-mean field theory with broader implications for nonlinear optics, superfluids, geophysical fluids, and other dispersive hydrodynamic media.

Long wavelength, hydrodynamic theories abound in physics, from fluids Landau and Lifshitz (1987) to optics Carusotto and Ciuti (2013), condensed matter Fradkin (2013) to quantum mechanics Wyatt and Trahan (2005), and beyond. Such theories describe expansion and compression waves until breaking. When the physics at shorter wavelengths are predominantly dispersive, dispersive hydrodynamic theories Whitham (1974); El and Hoefer (2016) are used to describe shock waves of a spectacularly different character than their dissipative counterparts. Dispersive shock waves (DSWs) consist of coherent, rank-ordered, nonlinear oscillations that continually expand Gurevich and Pitaevskii (1974); El and Hoefer (2016). Observations in a wide range of physical media that include quantum matter Hoefer et al. (2006); Mo et al. (2013), optics Wan et al. (2007); Xu et al. (2017), classical fluids Trillo et al. (2016); Maiden et al. (2016) and magnetic materials Janantha et al. (2017) demonstrate the prevalence of DSWs.

Another celebrated feature of dispersive hydrodynamic media are localized, nonlinear solitary waves. When they exhibit particle-like properties such as elastic, pairwise interactions, solitary waves are called solitons Zabusky and Kruskal (1965) and have been extensively studied both theoretically Drazin and Johnson (1989) and experimentally Remoissenet (2013). The focus here is on solitary waves that exhibit solitonic behavior, i.e., elastic or near-elastic interaction, henceforth we refer to them as solitons. Despite their common origins, solitons and dispersive hydrodynamics have been primarily studied independently.

Utilizing the scale separation between extended hydrodynamic states and localized solitons (see Fig. 1), we propose in this work a general theory of solitonic dispersive hydrodynamics encapsulated by a set of effective partial differential equations for the hydrodynamic mean field, the soliton’s amplitude, and its phase. We identify two adiabatic invariants of motion and show that they lead to two pivotal predictions. First, the soliton trajectory is a characteristic of the governing equations that is directed by the mean field, a nonlinear analogue of wavepacket trajectories in quantum mechanics Wyatt and Trahan (2005). This implies that solitons are either trapped by or transmitted through a hydrodynamic state, depending on the relative amplitudes of the soliton and the hydrodynamic “barrier”.

The second prediction we term hydrodynamic reciprocity. Given an incident soliton amplitude and the far-field mean conditions, the adiabatic invariants are used to predict when the soliton is trapped or transmitted and, in the latter case, what its transmitted amplitude and phase shift are. Hydrodynamic reciprocity means that the trapping, transmission amplitude/phase relations are the same for soliton interactions with smooth, expanding rarefaction waves (RWs) and compressive, oscillatory DSWs.

Figure 1: Representative initial configuration and evolution (top to bottom) for solitonic dispersive hydrodynamics. The narrow soliton on the uniform mean field is transmitted through the broad hydrodynamic flow if it reaches and propagates freely on the uniform mean field . The hydrodynamic flow exhibits expansion (rarefaction) and compression that leads to a dispersive shock wave.
Figure 2: Experiments demonstrating soliton transmission and trapping with hydrodynamic states. Representative image sequences (a,c,e,g) and space-time contours (b,d,f,h) extracted from image processing are shown. The contour intensity scale is the dimensionless conduit cross-sectional area relative to the smallest area. a,b) Soliton-RW transmission. c,d) Soliton-RW trapping. e,f) Soliton-DSW transmission. g,h) Soliton-DSW trapping.

We confirm these predictions with experiments on the interfacial dynamics of a viscous fluid conduit, a model dispersive hydrodynamic medium Lowman and Hoefer (2013a) that has been used previously to investigate solitons Olson and Christensen (1986); Scott et al. (1986); Lowman et al. (2014) and DSWs Maiden et al. (2016). Although soliton-DSW interaction has been observed previously Maiden et al. (2016), the nature and properties of the interaction were not explained. We stress that the theory presented is general and applies to a wide range of physical media Hoefer et al. (2006); Wan et al. (2007); Mo et al. (2013); Maiden et al. (2016); Trillo et al. (2016); Xu et al. (2017); Janantha et al. (2017).

Experiments are performed on the interfacial dynamics of a buoyant, viscous fluid injected from below into a miscible, much more viscous fluid matrix. Due to negligible diffusion and high viscosity contrast, the two-fluid interface serves as the dispersive hydrodynamic medium Olson and Christensen (1986); Lowman and Hoefer (2013a). The experimental setup is similar to that described in Maiden et al. (2016) and consists of a tall acrylic column filled with glycerol (viscosity P, density g/cm). A nozzle at the column base serves as the injection point for the interior fluid (viscosity P, density g/cm), a miscible solution of glycerol, water, and black food coloring. By injecting at a constant rate (0.25 mL/min or 0.77 mL/min), the buoyant interior fluid establishes a vertically uniform fluid conduit. Although predicted to be unstable, our experiment operates in the convective regime Selvam et al. (2009). By varying the injection rate, conduit solitons, RWs, and DSWs can be generated at the interface between the interior and exterior fluids.

Observations of the hydrodynamic transmission and trapping of solitons resulting from their interaction with RWs and DSWs are depicted in Fig. 2. The contour plots in 2(b,f) show that transmitted solitons exhibit a smaller (larger) amplitude and faster (slower) speed post interaction with a RW (DSW). The transmitted solitons experience a phase shift due to hydrodynamic interaction, defined as the difference between the post and pre interaction spatial intercept. Our measurements show a negative (positive) phase shift for the soliton transmitted through a RW (DSW). Sufficiently small incident solitons in Fig. 2(d,h) do not emerge from the RW or DSW interior during the course of experiment, remaining trapped inside the hydrodynamic state.

We now present a theory to explain these observations by considering a general dispersive hydrodynamic medium with nondimensional scalar quantity (e.g., conduit cross-sectional area) governed by

(1)

is the long-wave speed, is an integro-differential operator, and Eq. (1) admits a real-valued, linear dispersion relation with frequency where is the wavenumber and is the background mean field. We assume so that the dispersive hydrodynamic system has convex flux El et al. (2017). The dispersion is assumed negative () for definiteness. We also assume that equation (1) satisfies the prerequisites for Whitham theory, an approximate description of modulated nonlinear waves that accurately characterizes dispersive hydrodynamics in a wide-range of physical systems Whitham (1974); El and Hoefer (2016).

Many models can be expressed in the form (1). In the Appendix, we perform calculations for the Korteweg-de Vries (KdV) equation , , a universal model of weakly nonlinear, dispersive waves, and the conduit equation , , an accurate model for our experiments Lowman and Hoefer (2013a).

The dynamics of DSWs, RWs, and solitons for Eq. (1) can be described using Whitham theory Whitham (1974), where a nonlinear periodic wave’s mean , amplitude , and wavenumber are assumed to vary slowly via modulation equations. The modulation equations admit an asymptotic reduction in the non-interacting soliton wavetrain regime Grimshaw (1979); Gurevich et al. (1990)

(2)

The first equation is for the decoupled mean field, which is governed by the dispersionless, , equation (1). The second equation describes the soliton amplitude , which is advected by the mean field according to the soliton amplitude-speed relation and the coupling function . The final equation expresses wave conservation Whitham (1974) and describes a train of solitons with spacing . The soliton train here is a useful, yet fictitious construct because we will only consider the soliton limit of solutions to Eq. (2). Equation (2) with and corresponds to the soliton limit of the KdV-Whitham system of modulation equations, shown in El et al. (2007) to be equivalent to the soliton modulation equations determined by other means Grimshaw (1979) with application to shallow water soliton propagation over topography in Grimshaw (1979); El et al. (2012); Grimshaw et al. (2016, 2016). The general case of Eq. (2) was derived in Gurevich et al. (1990) and can be interpreted as a mean field approximation for the interaction of a soliton with the hydrodynamic flow. In contrast to standard soliton perturbation theory where the soliton’s parameters evolve temporally Kivshar and Malomed (1989), solitonic dispersive hydrodynamics require the soliton amplitude be treated as a spatio-temporal field. We note that the equations in (2) can be solved sequentially by the method of characteristics Grimshaw (1979).

It will be physically revealing to diagonalize the system of equations in (2) by identifying its Riemann invariants Whitham (1974). Owing to the special structure of (2) with just two characteristic velocities , it is always possible to find a change of variables to Riemann invariant form that diagonalizes the system. The mean field equation is already diagonalized with the Riemann invariant associated to the velocity . The second Riemann invariant, is associated with the velocity . can be found by integrating the differential form Whitham (1974) (see the Appendix). For KdV, , whereas for the conduit equation

(3)

The third Riemann invariant is found by direct integration of the wavenumber equation to be the quantity given by

(4)

where . For KdV, . The change of variables and diagonalizes (2)

(5)

We seek solutions to Eq. (5) subject to an initial mean field profile and an initial soliton of amplitude located at . But we require initial soliton and wavenumber fields and for all in order to give a properly posed problem for (2). Admissible initial conditions are obtained by recognizing this as a special solution, a simple wave in which all but one of the Riemann invariants are constant Whitham (1974). The non-constant Riemann invariant must be to satisfy the initial condition and therefore satisfies . The initial soliton amplitude and position determine the constant Riemann invariant . An initial wavenumber determines the other constant Riemann invariant . As we will show, the value of is not relevant so can be arbitrarily chosen. We now show how this solution physically describes soliton-mean field interaction.

A smooth, initial mean field, e.g., in Fig. 1, will evolve according to the obtained implicit solution until wavebreaking occurs. Our interest is in the interaction of a soliton with the expansion and compression waves that result. In dispersive hydrodynamics, the simplest examples of these are RWs and DSWs, respectively, which are most conveniently generated from step initial data. We therefore analyze the obtained general solution subject to step initial data

(6)

that model incident and transmitted soliton amplitudes and through the mean field transition to for soliton train wavenumbers and . The mean field dynamics depend upon the ordering of and . When , the mean field equation admits a RW solution, otherwise an unphysical, multi-valued solution. Short-wave dispersion regularizes such behavior and leads to the generation of a DSW. We consider each case in turn.

The transmission of a soliton through a RW is shown experimentally in Fig. 2(a,b). The incident soliton “climbs” the RW and emerges from the interaction with altered amplitude and speed. The mean field is the self-similar, RW solution with for and

(7)

where and is the inverse of . Constant and correspond to adiabatic invariants of the soliton-mean field dynamics that yield constraints on the amplitude, mean field, and wavenumber parameters we call the transmission and phase conditions

(8)

The first adiabatic invariant determines the transmitted soliton amplitude in terms of the incident soliton amplitude and the mean fields . The second adiabatic invariant determines the ratio , which in turn yields the soliton’s phase shift due to hydrodynamic interaction. Equation (8) is the main theoretical result of this work and describes the trapping or transmission of a soliton through a RW and a DSW.

The necessary and sufficient condition for soliton transmission is a positive transmitted soliton amplitude , which places a restriction on the incident soliton amplitude . For the conduit equation, Eq. (3) implies . For KdV, . In both cases, we find that the transmitted soliton’s amplitude is decreased, and its speed is increased, . More generally, and (see Appendix).

The soliton phase shift is where are the -intercepts of the soliton pre () and post () hydrodynamic interaction. Given the initial soliton position , the contraction/expansion of the soliton train determines the phase shift as . Hence, the ratio in the phase condition (8), not the arbitrary initial wavenumber , determines the soliton phase shift. Our use of a fictitious soliton train is therefore justified.

We also determine the soliton-RW trajectory. A soliton with position propagates through the mean field along a characteristic of the modulation system (2)

(9)

where the soliton amplitude varies along the trajectory according to the adiabatic invariant . The phase shift from integration of (9) equals from the adiabatic invariant in (8), as expected.

When in (8), the soliton is trapped by the RW, as in experiment, Fig. 2(c,d).

If , a DSW is generated. Soliton-DSW transmission is experimentally depicted in Fig. 2(e,f). An incident soliton propagates through the DSW, exhibiting a highly non-trivial interaction, ultimately emerging with altered amplitude and speed.

Figure 3: Graphical depictions of hydrodynamic reciprocity. (a) Space-time contour plot of soliton-DSW () and soliton-RW () interaction with two solitons satisfying the transmission condition (8). For sufficiently large, the soliton speeds are the same. (b) If the soliton post DSW interaction (top, left to right) is used to initialize soliton-RW interaction (bottom, right to left), the post RW interaction soliton has the same properties as the pre DSW interaction soliton.

In contrast to the soliton-RW problem, the modulation equations (2) are no longer valid throughout the soliton-DSW interaction. Instead, the mean field equation is replaced by the DSW modulation equations Gurevich and Pitaevskii (1974); El and Hoefer (2016). We seek a simple wave solution for soliton-DSW modulation. Because DSW generation occurs only for , the soliton-DSW modulation system for reduces exactly to Eq. (2), i.e., that of soliton-RW modulation. For , the adiabatic invariants (8) hold. By continuity of the modulation solution, these conditions must hold for as well. In particular, soliton-RW and soliton-DSW interaction both satisfy the same transmission and phase conditions (8). This fact, termed hydrodynamic reciprocity, is due to time reversibility of the governing equation (1) and is depicted graphically in Fig. 3.

Equations (3) and (8) for the conduit equation indicate that solitons incident upon DSWs exhibit a decreased transmitted speed and an increased transmitted amplitude . and are precisely the amplitude and speed of the DSW’s soliton leading edge Lowman and Hoefer (2013b). Hydrodynamic reciprocity therefore implies that the transmitted soliton’s amplitude is decreased (increased), its speed is increased (decreased), and its phase shift is negative (positive) relative to the soliton incident upon the RW (DSW), as observed experimentally in Fig. 2. Using the transmission and phase conditions (8), we accurately predict the conduit soliton trajectory post DSW interaction without any detailed knowledge of soliton-DSW interaction (see Appendix).

In contrast to soliton-RW transmission, solitons with amplitude initially placed to the right of the step will interact with the DSW if . Then the transmission condition (8) implies , i.e., the soliton cannot transmit back through the DSW. Instead, the soliton is effectively trapped as a localized defect in the DSW interior as observed experimentally in Fig. 2(g,h).

Figure 4: Transmitted soliton properties due to conduit soliton-RW and DSW interaction for a hydrodynamic transition from to . a) Soliton amplitude from eq. (8) (curve), experiment (filled squares, triangles), and numerical simulations (open squares, triangles). b) Soliton phase shift from eq. (8) (curves) and numerical simulations (symbols).

The transmission and phase conditions (8) for the conduit equation are shown in Fig. 4. For soliton-RW interaction, the abscissa and ordinate are and , respectively reversed for soliton-DSW interaction. Hydrodynamic reciprocity implies that the transmission condition on these axes is the same for soliton-RW and DSW transmission. Reciprocity is confirmed by experiment and numerical simulations of the conduit equation in Fig. 4(a), that slightly deviate from soliton-mean field theory as the amplitudes increase, consistent with previously observed discrepancies Lowman and Hoefer (2013b); Maiden et al. (2016). Reciprocity of the phase shift is also confirmed by conduit equation numerics in Fig. 4(b). Our experiments provide definitive evidence of soliton-hydrodynamic transmission, trapping, reciprocity, and the theory’s efficacy.

We have introduced a general framework for soliton-mean field interaction. The dynamics exhibit two adiabatic invariants that describe soliton trapping or transmission. The existence of the same adiabatic invariants for soliton-mean field interactions of compression (DSW) and expansion (RW) imply hydrodynamic reciprocity. This describes a conceptually new notion of hydrodynamic soliton “tunneling” where the potential barrier is the mean field, obeying the same equations as the soliton Sprenger (2018).

Appendix A Appendix A: Riemann invariants of solitonic hydrodynamics

In this section, we provide the derivation of the Riemann invariants for the soliton train modulation system

(A10a)
(A10b)
(A10c)

enabling its reduction to the diagonal form

(A11a)
(A11b)
(A11c)

To elucidate the general procedure, we perform explicit calculations for the KdV equation along with the conduit equation, our primary example.

First, we notice that equations (A10a) and (A10b) are decoupled from (A10c), and have two distinct, real characteristic velocities . This subsystem of quasi-linear equations is thus strictly hyperbolic and can be diagonalized for any coupling function Whitham (1974).

The mean field equation is already in diagonal form with the Riemann invariant associated with the velocity . The second Riemann invariant, , depends on , and is associated with the characteristic velocity . It can be found by integrating (see, e.g., Ref. Whitham (1974)). Another way of finding is to look for a simple wave relation of the subsystem (A10a) and (A10b).

The coupling function is not always readily available, and its direct computation generally requires the determination of a singular, soliton limit in the full system of Whitham modulation equations for the dispersive hydrodynamics Gurevich et al. (1990). Below, we use a convenient change of variables proposed in Ref. El (2005) that enables one to circumvent explicit determination of the coupling function in the derivation of the Riemann invariant , utilizing only the known linear dispersion relation and the soliton amplitude-speed relation .

Following Ref. El (2005), we introduce a conjugate (soliton) wavenumber , implicitly determined via the soliton amplitude-speed relation

(A12)

where is the conjugate dispersion, whose phase velocity coincides with the speed of a soliton. The conjugate dispersion relation is realized by linearizing the governing dispersive hydrodynamic equation, Eq. (1), with respect to the soliton solution in the far-field. Very often, one can explicitly determine the soliton amplitude-speed relation hence also the change of variables via Eq. (A12).

As a simple example, for the KdV equation we have , , therefore .

For the conduit equation, the dispersion and soliton amplitude-speed relations are Maiden et al. (2016)

(A13)

The conjugate wavenumber transformation (A12) then yields .

In the variables , simple wave solutions of Eqs. (A10a) and (A10b) satisfy the ordinary differential equation (ODE) El (2005)

(A14)
Figure 5: Numerical simulations of the conduit equation (contours) and corresponding predicted soliton trajectories (dashed curves). a) Soliton-RW transmission for , , and . The dashed curve is the integration of Eq. (A11). b) Soliton-RW trapping for , , and . The dashed curve is the integration of Eq. (A11). c) Soliton-DSW transmission for , , and . The two dashed curves correspond to the predicted soliton trajectory pre and post DSW interaction. The post interaction trajectory is determined by the adiabatic invariants and . The difference between the intercepts of these lines is the soliton-DSW phase shift. d) Soliton-DSW trapping for , , and .

For the KdV equation, the ODE (A14) is readily integrated to yield , where is a constant.

For the conduit equation, integration of (A14) gives an implicit determination of

(A15)

where , again, is a constant of integration.

Generally, is constant along the characteristic , where , and so is a Riemann invariant satisfying Eq. (A11b). For the KdV equation, we find and . For the conduit equation, we obtain and (Eq. (5)).

Having determined two Riemann invariants, and , of the system (A10), the third Riemann invariant, labeled and also associated with the characteristic velocity , is readily found in the form where is given by the general expression (4).

The constancy of and lead to the transmission conditions in Eq. (8). These conditions completely determine the soliton’s trajectory post RW or DSW interaction. They also determine the conditions for soliton-hydrodynamic trapping. All four possible interaction types (soliton-RW, soliton-DSW trapping and transmission) are shown in the numerical simulations compared with theoretical predictions in Fig. 5.

Appendix B Appendix B: Amplitude property of soliton transmission

Conduit soliton transmission through a RW has the following property. The amplitude of the transmitted soliton, , is always smaller than the amplitude of the incident soliton, . The same result readily follows for KdV soliton transmission using the first condition (8) and the expression for the Riemann invariant derived in Sec. A. We now derive the extension of this result to the general dispersive hydrodynamic system Eq. (1), assuming .

In the mean field, simple wave approximation, the transmission of a soliton through a RW is determined by the conservation of the second Riemann invariant, , of the solitonic hydrodynamic system (A10) (see the first condition in Eq. (8)). We are interested in the sign of the derivative in the course of soliton transmission. Expressing , we obtain (since is constant). Now, using Eq. (7), we have . Next, . Hence, and therefore, assuming , . Say, for KdV so as already observed. By hydrodynamic reciprocity, the amplitude change for soliton-DSW transmission is opposite to that of soliton-RW transmission.

In a similar manner, the acceleration or deceleration of soliton-RW transmission can be determined by the positivity or negativity of . By a similar argument, . For KdV, , and for the conduit equation, , so a transmitted soliton in both cases is accelerated by the RW. By hydrodynamic reciprocity, a soliton is decelerated by a DSW.

Appendix C Appendix C: Fluid Conduit Experimental Details

The experimental setup is similar to that described in Maiden et al. (2016) and consists of a square acrylic column with dimensions cm. The column is filled with glycerol, a highly viscous, transparent, exterior fluid. A nozzle installed at the base of the column allows for the injection of the interior fluid. To eliminate surface tension effects, the interior fluid is a miscible solution of glycerol, water, and black food coloring. As a result, the interior fluid has both lower density and viscosity than the exterior fluid. The properties of the interior and exterior fluids are dynamic viscosity cP, cP and density g/cm, and g/cm with a superscript denoting interior/exterior.

Interior fluid is drawn from a reservoir and injected through the nozzle via a computer controlled high precision piston pump. By injecting at a constant rate, the buoyant interior fluid establishes a stable, vertically uniform fluid conduit. By varying the injection rate in a precise manner, conduit solitons, RWs, and DSWs can be reliably generated. For each trial, a volumetric flow rate profile is generated based on these fluid properties that results in a long box followed by a soliton of chosen amplitude. The smaller conduit diameter is set by the background flow rate mL/min. The maximum flow rate for the long box is mL/min. These two flow rates correspond to a nondimensional jump in cross-sectional area from 1 to 1.75 that defines . The box is sufficiently long that the trailing edge acts as a RW and leading edge acts as a DSW at the time of their respective interactions with the soliton.

The cross-sectional area of the fluid conduit corresponds to the dispersive hydrodynamic medium of interest. Data acquisition of and is performed using three high resolution cameras, two equipped with macro lenses and one with a zoom lens. The macro lens cameras are near the bottom and top of the conduit, and the zoom lens near the middle, for extracting precise conduit diameter and soliton amplitude information. The cameras take several high-resolution images of the soliton as it passes through their respective viewscreens, as well as pictures of the background conduit before and after the hydrodynamic structure has passed. Correction for the refractive index of glycerin is calibrated via images of a cylinder of known height and width dropped into the center of the apparatus before the experiment.

The camera images are processed in Matlab to extract the conduit edges by taking a horizontal row of pixels and calculating the maximum and minimum derivatives for each row. As the background is white and the conduit is black, this finds the approximate boundary. The conduit’s slight variability from vertical gets enhanced during image processing so we use a background subtraction method to extract the measured non-dimensional conduit area from the images reported in Figs. 2 and 4. Prior to inducing interfacial dynamics, we take ten images, extract non-dimensional edge data, average all the edges and subtract this from edges extracted for the trial. The data is then sent through a low-pass filter to reduce noise from the pixelation of the photograph and any impurities (such as bubbles) in the exterior fluid. After converting to area and rescaling the smaller background area to unity, we then determine the soliton amplitudes before and after tunneling. Calculations suggest that density variations of 1% in the exterior fluid can lead to a 10% change in the background conduit diameter. We observe an increase in the conduit diameter for the top camera, relative to the bottom and middle cameras by 10.1%, which we attribute to density variation of the external fluid. Because the model assumes no density variation, we accommodate this discrepancy by scaling all amplitude measurements from the top camera by the factor .

Acknowledgements.
This work was supported by NSF CAREER DMS-1255422 (DVA, NAF, MAH), the NSF GRFP (MDM), NSF EXTREEMS-QED DMS-1407340 (DVA), and EPSRC grant EP/R00515X/1 (GAE). GAE and MAH gratefully acknowledge the London Mathematical Society for supporting a Research in Pairs visit.

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This is a comment super asjknd jkasnjk adsnkj
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