Compacton-like solutions in some nonlocal hydrodynamic-type models

Transcription

1 Compacton-like solutions in some nonlocal hydrodynamic-type models Vsevolod Vladimirov AGH University of Science and technology, Faculty of Applied Mathematics Protaras, October 26, 2008 WMS AGH Compactons in Relaxing hydrodynamic-type model 1 / 37

2 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

3 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

4 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

5 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

6 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

7 Plan of the talk: Historical background Solitons and compactons from the geometric point of view Non-local hydrodynamic-type models Compacton-like solutions in relaxing hydrodynamics Attractive features of compactons-like solutions Discussion, comments. WMS AGH Compactons in Relaxing hydrodynamic-type model 2 / 37

8 Rosenau-Hyman generaization of KdV hierarchy K(m, n) hierarchy(rosenau, Hyman, 1993): K(m, n) = u t + α (u m ) x + β (u n ) xxx = 0, m 2, n 2. (1) Solitary wave solution, corresponding to α = β = 1 and m = n = 2: u = { 4 V 3 cos 2 ξ 4 when ξ 2 π, 0 when ξ > 2 π, ξ = x V t. (2) WMS AGH Compactons in Relaxing hydrodynamic-type model 3 / 37

9 Rosenau-Hyman generaization of KdV hierarchy K(m, n) hierarchy(rosenau, Hyman, 1993): K(m, n) = u t + α (u m ) x + β (u n ) xxx = 0, m 2, n 2. (1) Solitary wave solution, corresponding to α = β = 1 and m = n = 2: u = { 4 V 3 cos 2 ξ 4 when ξ 2 π, 0 when ξ > 2 π, ξ = x V t. (2) WMS AGH Compactons in Relaxing hydrodynamic-type model 3 / 37

10 Main properties of KdV and K(m, n) equations solutions Solitons (compactons) forms a one-parameter family w.r.t. parameter V, see below; u = u = 12 V 2 sech 2[ V (x 4 V 2 t) ] KdV soliton β { 4 V 3 cos 2 x V t 4 when x V t 2 π, K(2, 2) compacton. 0 when ξ > 2 π, Maximal amplitude of the solitary wave is proportional to its velocity V. WMS AGH Compactons in Relaxing hydrodynamic-type model 4 / 37

11 Main properties of KdV and K(m, n) equations solutions Solitons (compactons) forms a one-parameter family w.r.t. parameter V, see below; u = u = 12 V 2 sech 2[ V (x 4 V 2 t) ] KdV soliton β { 4 V 3 cos 2 x V t 4 when x V t 2 π, K(2, 2) compacton. 0 when ξ > 2 π, Maximal amplitude of the solitary wave is proportional to its velocity V. WMS AGH Compactons in Relaxing hydrodynamic-type model 4 / 37

12 Smooth compact initial data create a finite number of solitons (compactons) WMS AGH Compactons in Relaxing hydrodynamic-type model 5 / 37

13 Evolution of an initial localized disturbance An initial pulse with a compact support, evolves in a series of sharply localized pulses compactons (length 5 mesh points) π/5 u ments time space

14 Solitons (compactons) restore their shapes after the mutual collisions Collision of compactons is accompanied by the creation of the low-amplitude compacton-anticompacton pair WMS AGH Compactons in Relaxing hydrodynamic-type model 6 / 37

15 Collisions Collision of compactons (here with velocities 0.2 and 0.9) is nearly elastic lacements field u n (t) time site n

16 Solitons and compactons from geometric point of view. Reduction of KdV equation In order to describe solitons, we use the TW reduction u(t, x) = U(ξ), with ξ = x V t. Inserting U(ξ) into the KdV equation u t + β u u x + u xxx = 0 we get, after one integration, Hamiltonian system: U(ξ) = W (ξ) = H W, (3) Ẇ (ξ) = β ( 2 U(ξ) U(ξ) 2 v ) = H U. β H = 1 2 (W 2 + β3 U 3 v U 2 ). (4) Every solutions of (3) can be identified with some level curve H = K. WMS AGH Compactons in Relaxing hydrodynamic-type model 7 / 37

17 Solitons and compactons from geometric point of view. Reduction of KdV equation In order to describe solitons, we use the TW reduction u(t, x) = U(ξ), with ξ = x V t. Inserting U(ξ) into the KdV equation u t + β u u x + u xxx = 0 we get, after one integration, Hamiltonian system: U(ξ) = W (ξ) = H W, (3) Ẇ (ξ) = β ( 2 U(ξ) U(ξ) 2 v ) = H U. β H = 1 2 (W 2 + β3 U 3 v U 2 ). (4) Every solutions of (3) can be identified with some level curve H = K. WMS AGH Compactons in Relaxing hydrodynamic-type model 7 / 37

18 Solitons and compactons from geometric point of view. Reduction of KdV equation In order to describe solitons, we use the TW reduction u(t, x) = U(ξ), with ξ = x V t. Inserting U(ξ) into the KdV equation u t + β u u x + u xxx = 0 we get, after one integration, Hamiltonian system: U(ξ) = W (ξ) = H W, (3) Ẇ (ξ) = β ( 2 U(ξ) U(ξ) 2 v ) = H U. β H = 1 2 (W 2 + β3 U 3 v U 2 ). (4) Every solutions of (3) can be identified with some level curve H = K. WMS AGH Compactons in Relaxing hydrodynamic-type model 7 / 37

19 Solitons and compactons from geometric point of view. Reduction of KdV equation In order to describe solitons, we use the TW reduction u(t, x) = U(ξ), with ξ = x V t. Inserting U(ξ) into the KdV equation u t + β u u x + u xxx = 0 we get, after one integration, Hamiltonian system: U(ξ) = W (ξ) = H W, (3) Ẇ (ξ) = β ( 2 U(ξ) U(ξ) 2 v ) = H U. β H = 1 2 (W 2 + β3 U 3 v U 2 ). (4) Every solutions of (3) can be identified with some level curve H = K. WMS AGH Compactons in Relaxing hydrodynamic-type model 7 / 37

20 Solitons and compactons from geometric point of view. Reduction of KdV equation In order to describe solitons, we use the TW reduction u(t, x) = U(ξ), with ξ = x V t. Inserting U(ξ) into the KdV equation u t + β u u x + u xxx = 0 we get, after one integration, Hamiltonian system: U(ξ) = W (ξ) = H W, (3) Ẇ (ξ) = β ( 2 U(ξ) U(ξ) 2 v ) = H U. β H = 1 2 (W 2 + β3 U 3 v U 2 ). (4) Every solutions of (3) can be identified with some level curve H = K. WMS AGH Compactons in Relaxing hydrodynamic-type model 7 / 37

21 Level curves ( of the Hamiltonian H = 1 2 W 2 + β U 3 v U 2) = K = const 3 Solution to KdV, corresponding to the homoclinic trajectory WMS AGH Compactons in Relaxing hydrodynamic-type model 8 / 37

22 Reduction of K(m, n) equation Inserting ansatz u(t, x) = U(ξ) U(x v t) into K(m, n) u t + α (u m ) x + β (u n ) xxx = 0, we obtain, after one integration and employing the integrating multiplier ϕ[u] = U n 1, the Hamiltonian system: { n β U 2(n 1) d U d ξ = n β U 2(n 1) W = H W, n β U 2(n 1) d W d ξ = U n 1 [ v U + αu m + n(n 1) β U n 2 W 2] = H U. Every trajectory of the above system can be identified with some level curve H = const of the Hamiltonian H = α m + n U m+n v n + 1 U n+1 + β n 2 U 2(n 1) W 2. WMS AGH Compactons in Relaxing hydrodynamic-type model 9 / 37

23 Reduction of K(m, n) equation Inserting ansatz u(t, x) = U(ξ) U(x v t) into K(m, n) u t + α (u m ) x + β (u n ) xxx = 0, we obtain, after one integration and employing the integrating multiplier ϕ[u] = U n 1, the Hamiltonian system: { n β U 2(n 1) d U d ξ = n β U 2(n 1) W = H W, n β U 2(n 1) d W d ξ = U n 1 [ v U + αu m + n(n 1) β U n 2 W 2] = H U. Every trajectory of the above system can be identified with some level curve H = const of the Hamiltonian H = α m + n U m+n v n + 1 U n+1 + β n 2 U 2(n 1) W 2. WMS AGH Compactons in Relaxing hydrodynamic-type model 9 / 37

24 Reduction of K(m, n) equation Inserting ansatz u(t, x) = U(ξ) U(x v t) into K(m, n) u t + α (u m ) x + β (u n ) xxx = 0, we obtain, after one integration and employing the integrating multiplier ϕ[u] = U n 1, the Hamiltonian system: { n β U 2(n 1) d U d ξ = n β U 2(n 1) W = H W, n β U 2(n 1) d W d ξ = U n 1 [ v U + αu m + n(n 1) β U n 2 W 2] = H U. Every trajectory of the above system can be identified with some level curve H = const of the Hamiltonian H = α m + n U m+n v n + 1 U n+1 + β n 2 U 2(n 1) W 2. WMS AGH Compactons in Relaxing hydrodynamic-type model 9 / 37

25 Reduction of K(m, n) equation Inserting ansatz u(t, x) = U(ξ) U(x v t) into K(m, n) u t + α (u m ) x + β (u n ) xxx = 0, we obtain, after one integration and employing the integrating multiplier ϕ[u] = U n 1, the Hamiltonian system: { n β U 2(n 1) d U d ξ = n β U 2(n 1) W = H W, n β U 2(n 1) d W d ξ = U n 1 [ v U + αu m + n(n 1) β U n 2 W 2] = H U. Every trajectory of the above system can be identified with some level curve H = const of the Hamiltonian H = α m + n U m+n v n + 1 U n+1 + β n 2 U 2(n 1) W 2. WMS AGH Compactons in Relaxing hydrodynamic-type model 9 / 37

26 Level curves of the Hamiltonian H = α U m+2 v U 3 + β U 2 W 2 = L = const, m+2 3 corresponding to the reduced K(m, 2) equation Generalized solution to K(m, 2) equation (nonzero part corresponds to the homoclinic trajectory): WMS AGH Compactons in Relaxing hydrodynamic-type model 10 / 37

27 Conclusion: Compacton-like TW solution is represented in the phase space of the factorized system by the trajectory bi-asymptotic to a (topological) saddle.lying on a singular manifold of dynamical system WMS AGH Compactons in Relaxing hydrodynamic-type model 11 / 37

28 Modeling system Let s consider balance equations for mass and momentum in lagrangean coordinates: { ut + p x = F, Using the closing equation ρ t + ρ 2 u x = 0, p = β m + 1 ρm+1 characteristic for local processes,we get the Euler-type system { ut + β ρ m ρ x = F, ρ t + ρ 2 (6) u x = 0, No solitary waves, no compactons for physically justified case p/ ρ > 0 (5) WMS AGH Compactons in Relaxing hydrodynamic-type model 12 / 37

29 Modeling system Let s consider balance equations for mass and momentum in lagrangean coordinates: { ut + p x = F, Using the closing equation ρ t + ρ 2 u x = 0, p = β m + 1 ρm+1 characteristic for local processes,we get the Euler-type system { ut + β ρ m ρ x = F, ρ t + ρ 2 (6) u x = 0, No solitary waves, no compactons for physically justified case p/ ρ > 0 (5) WMS AGH Compactons in Relaxing hydrodynamic-type model 12 / 37

30 Modeling system Let s consider balance equations for mass and momentum in lagrangean coordinates: { ut + p x = F, Using the closing equation ρ t + ρ 2 u x = 0, p = β m + 1 ρm+1 characteristic for local processes,we get the Euler-type system { ut + β ρ m ρ x = F, ρ t + ρ 2 (6) u x = 0, No solitary waves, no compactons for physically justified case p/ ρ > 0 (5) WMS AGH Compactons in Relaxing hydrodynamic-type model 12 / 37

31 Modeling system Let s consider balance equations for mass and momentum in lagrangean coordinates: { ut + p x = F, Using the closing equation ρ t + ρ 2 u x = 0, p = β m + 1 ρm+1 characteristic for local processes,we get the Euler-type system { ut + β ρ m ρ x = F, ρ t + ρ 2 (6) u x = 0, No solitary waves, no compactons for physically justified case p/ ρ > 0 (5) WMS AGH Compactons in Relaxing hydrodynamic-type model 12 / 37

32 Closing equation taking into account non-local effects: t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. (7) Using the kernel K [ t, t ; x, x ] = δ(x x ) e t t τ describing the effects of temporal non-localities and the polynomial functions f(ρ) = χ τ ρn, g(ρ) = σ ρ n we can get the relaxing hydrodynamics system 1 u t + p x = F, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p (8) 1 Cf. Lyakhov, 1983; Danylenko et al., 1995 WMS AGH Compactons in Relaxing hydrodynamic-type model 13 / 37

33 Closing equation taking into account non-local effects: t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. (7) Using the kernel K [ t, t ; x, x ] = δ(x x ) e t t τ describing the effects of temporal non-localities and the polynomial functions f(ρ) = χ τ ρn, g(ρ) = σ ρ n we can get the relaxing hydrodynamics system 1 u t + p x = F, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p (8) 1 Cf. Lyakhov, 1983; Danylenko et al., 1995 WMS AGH Compactons in Relaxing hydrodynamic-type model 13 / 37

34 Closing equation taking into account non-local effects: t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. (7) Using the kernel K [ t, t ; x, x ] = δ(x x ) e t t τ describing the effects of temporal non-localities and the polynomial functions f(ρ) = χ τ ρn, g(ρ) = σ ρ n we can get the relaxing hydrodynamics system 1 u t + p x = F, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p (8) 1 Cf. Lyakhov, 1983; Danylenko et al., 1995 WMS AGH Compactons in Relaxing hydrodynamic-type model 13 / 37

35 Closing equation taking into account non-local effects: t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. (7) Using the kernel K [ t, t ; x, x ] = δ(x x ) e t t τ describing the effects of temporal non-localities and the polynomial functions f(ρ) = χ τ ρn, g(ρ) = σ ρ n we can get the relaxing hydrodynamics system 1 u t + p x = F, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p (8) 1 Cf. Lyakhov, 1983; Danylenko et al., 1995 WMS AGH Compactons in Relaxing hydrodynamic-type model 13 / 37

36 Closing equation taking into account non-local effects: t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. (7) Using the kernel K [ t, t ; x, x ] = δ(x x ) e t t τ describing the effects of temporal non-localities and the polynomial functions f(ρ) = χ τ ρn, g(ρ) = σ ρ n we can get the relaxing hydrodynamics system 1 u t + p x = F, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p (8) 1 Cf. Lyakhov, 1983; Danylenko et al., 1995 WMS AGH Compactons in Relaxing hydrodynamic-type model 13 / 37

37 Let us consider closing equation p = f(ρ) + with the kernel t { + K [ t, t ; x, x ] } g(ρ) d x d t. K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. describing effects of spatial non-locality. When f(ρ) = B ρ n+1, and g(ρ) = ˆσ ρ n+1 then we get the system describing e.g. solids with microcracks 2 : { ut + β ρ n ρ x + σ (ρ n ρ x ) xx = 0, ρ t + ρ 2 (9) u x = 0, System (9) possesses a one-parameter family of soliton-like TW solutions (Vladimirov, 2003), and does not possess compacton-like solutions (Vladimirov, 2008). 2 cf. Peerlings, de Borst, Geers et al., 2001 WMS AGH Compactons in Relaxing hydrodynamic-type model 14 / 37

38 Let us consider closing equation p = f(ρ) + with the kernel t { + K [ t, t ; x, x ] } g(ρ) d x d t. K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. describing effects of spatial non-locality. When f(ρ) = B ρ n+1, and g(ρ) = ˆσ ρ n+1 then we get the system describing e.g. solids with microcracks 2 : { ut + β ρ n ρ x + σ (ρ n ρ x ) xx = 0, ρ t + ρ 2 (9) u x = 0, System (9) possesses a one-parameter family of soliton-like TW solutions (Vladimirov, 2003), and does not possess compacton-like solutions (Vladimirov, 2008). 2 cf. Peerlings, de Borst, Geers et al., 2001 WMS AGH Compactons in Relaxing hydrodynamic-type model 14 / 37

39 Let us consider closing equation p = f(ρ) + with the kernel t { + K [ t, t ; x, x ] } g(ρ) d x d t. K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. describing effects of spatial non-locality. When f(ρ) = B ρ n+1, and g(ρ) = ˆσ ρ n+1 then we get the system describing e.g. solids with microcracks 2 : { ut + β ρ n ρ x + σ (ρ n ρ x ) xx = 0, ρ t + ρ 2 (9) u x = 0, System (9) possesses a one-parameter family of soliton-like TW solutions (Vladimirov, 2003), and does not possess compacton-like solutions (Vladimirov, 2008). 2 cf. Peerlings, de Borst, Geers et al., 2001 WMS AGH Compactons in Relaxing hydrodynamic-type model 14 / 37

40 Let us consider closing equation p = f(ρ) + with the kernel t { + K [ t, t ; x, x ] } g(ρ) d x d t. K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. describing effects of spatial non-locality. When f(ρ) = B ρ n+1, and g(ρ) = ˆσ ρ n+1 then we get the system describing e.g. solids with microcracks 2 : { ut + β ρ n ρ x + σ (ρ n ρ x ) xx = 0, ρ t + ρ 2 (9) u x = 0, System (9) possesses a one-parameter family of soliton-like TW solutions (Vladimirov, 2003), and does not possess compacton-like solutions (Vladimirov, 2008). 2 cf. Peerlings, de Borst, Geers et al., 2001 WMS AGH Compactons in Relaxing hydrodynamic-type model 14 / 37

41 Let us consider closing equation p = f(ρ) + with the kernel t { + K [ t, t ; x, x ] } g(ρ) d x d t. K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. describing effects of spatial non-locality. When f(ρ) = B ρ n+1, and g(ρ) = ˆσ ρ n+1 then we get the system describing e.g. solids with microcracks 2 : { ut + β ρ n ρ x + σ (ρ n ρ x ) xx = 0, ρ t + ρ 2 (9) u x = 0, System (9) possesses a one-parameter family of soliton-like TW solutions (Vladimirov, 2003), and does not possess compacton-like solutions (Vladimirov, 2008). 2 cf. Peerlings, de Borst, Geers et al., 2001 WMS AGH Compactons in Relaxing hydrodynamic-type model 14 / 37

42 Compactons appears in case when we slightly modify the state equation t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. Now we use the same function g(ρ) = ˆσ ρ n+1 and the same kernel of non-locality K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. and some unspecified function f( ρ) f(ρ ρ 0 ). This way we obtain system {ut + f( ρ) ρ x + σ ( ρ n ρ x ) xx = 0, ρ t + ρ 2 (10) u x = 0. Under certain conditions system (10) possesses compacton-like TW solutions (Vladimirov, 2008). WMS AGH Compactons in Relaxing hydrodynamic-type model 15 / 37

43 Compactons appears in case when we slightly modify the state equation t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. Now we use the same function g(ρ) = ˆσ ρ n+1 and the same kernel of non-locality K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. and some unspecified function f( ρ) f(ρ ρ 0 ). This way we obtain system {ut + f( ρ) ρ x + σ ( ρ n ρ x ) xx = 0, ρ t + ρ 2 (10) u x = 0. Under certain conditions system (10) possesses compacton-like TW solutions (Vladimirov, 2008). WMS AGH Compactons in Relaxing hydrodynamic-type model 15 / 37

44 Compactons appears in case when we slightly modify the state equation t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. Now we use the same function g(ρ) = ˆσ ρ n+1 and the same kernel of non-locality K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. and some unspecified function f( ρ) f(ρ ρ 0 ). This way we obtain system {ut + f( ρ) ρ x + σ ( ρ n ρ x ) xx = 0, ρ t + ρ 2 (10) u x = 0. Under certain conditions system (10) possesses compacton-like TW solutions (Vladimirov, 2008). WMS AGH Compactons in Relaxing hydrodynamic-type model 15 / 37

45 Compactons appears in case when we slightly modify the state equation t { + p = f(ρ) + K [ t, t ; x, x ] } g(ρ) d x d t. Now we use the same function g(ρ) = ˆσ ρ n+1 and the same kernel of non-locality K [ t, t ; x, x ] = δ(t t ) e (x x ) 2 L. and some unspecified function f( ρ) f(ρ ρ 0 ). This way we obtain system {ut + f( ρ) ρ x + σ ( ρ n ρ x ) xx = 0, ρ t + ρ 2 (10) u x = 0. Under certain conditions system (10) possesses compacton-like TW solutions (Vladimirov, 2008). WMS AGH Compactons in Relaxing hydrodynamic-type model 15 / 37

46 Compactons in relaxing hydrodynamic-type model We consider relaxing hydrodynamic-type system u t + p x = F = γ = const, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p In the following we assume that n = 1. Introducing the variable V = 1 (describing the specific volume) we get ρ (11) u t + p x = γ, V t u x = 0 (12) [ τ p t + χ ] τ V 2 u x = κ V p. We are going to state that the set of self-similar solutions of system (12) contains a compacton WMS AGH Compactons in Relaxing hydrodynamic-type model 16 / 37

47 Compactons in relaxing hydrodynamic-type model We consider relaxing hydrodynamic-type system u t + p x = F = γ = const, ρ t + ρ 2 u x = 0, τ [ p t χ ] τ (ρn ) t = κ ρ n p In the following we assume that n = 1. Introducing the variable V = 1 (describing the specific volume) we get ρ (11) u t + p x = γ, V t u x = 0 (12) [ τ p t + χ ] τ V 2 u x = κ V p. We are going to state that the set of self-similar solutions of system (12) contains a compacton WMS AGH Compactons in Relaxing hydrodynamic-type model 16 / 37

48 Lemma.System (12) admits the local group, generated by the following operators: ˆX 1 = t, ˆX 2 = x, ˆX 3 = x x + p p V V. Based on these symmetry generators one can build up the following ansatz u = U(ω), V = R(ω) x 0 x, p = (x 0 x) P (ω), (13) x 0 ω = tξ + ln x 0 x, leading to the reduction of the system of PDEs. Note that the parameter ξ plays the role of velocity! WMS AGH Compactons in Relaxing hydrodynamic-type model 17 / 37

49 Lemma.System (12) admits the local group, generated by the following operators: ˆX 1 = t, ˆX 2 = x, ˆX 3 = x x + p p V V. Based on these symmetry generators one can build up the following ansatz u = U(ω), V = R(ω) x 0 x, p = (x 0 x) P (ω), (13) x 0 ω = tξ + ln x 0 x, leading to the reduction of the system of PDEs. Note that the parameter ξ plays the role of velocity! WMS AGH Compactons in Relaxing hydrodynamic-type model 17 / 37

50 Lemma.System (12) admits the local group, generated by the following operators: ˆX 1 = t, ˆX 2 = x, ˆX 3 = x x + p p V V. Based on these symmetry generators one can build up the following ansatz u = U(ω), V = R(ω) x 0 x, p = (x 0 x) P (ω), (13) x 0 ω = tξ + ln x 0 x, leading to the reduction of the system of PDEs. Note that the parameter ξ plays the role of velocity! WMS AGH Compactons in Relaxing hydrodynamic-type model 17 / 37

51 Lemma.System (12) admits the local group, generated by the following operators: ˆX 1 = t, ˆX 2 = x, ˆX 3 = x x + p p V V. Based on these symmetry generators one can build up the following ansatz u = U(ω), V = R(ω) x 0 x, p = (x 0 x) P (ω), (13) x 0 ω = tξ + ln x 0 x, leading to the reduction of the system of PDEs. Note that the parameter ξ plays the role of velocity! WMS AGH Compactons in Relaxing hydrodynamic-type model 17 / 37

52 Inserting ansatz (13) into the system (12), we get the first integral U = ξr + const and the dynamical system DS: ξ (R)R = R [σr P κ + τξrγ], (14) ξ (R) P = ξ {ξr (R P κ) + χ ( P + γ)}, where ( ) = d ( ) /dω, (R) = τ(ξr) 2 χ, σ = 1 + τξ. Figure: Stationary points of system (14): A(R 1, P 1 ), R 1 = κ/γ, P 1 = γ; B (R 2, P 2 ), R 2 = χ κ τξγ R2 τξ, P 2 2 = (1+τ ξ) R 2 ; C(0, γ) WMS AGH Compactons in Relaxing hydrodynamic-type model 18 / 37

53 Inserting ansatz (13) into the system (12), we get the first integral U = ξr + const and the dynamical system DS: ξ (R)R = R [σr P κ + τξrγ], (14) ξ (R) P = ξ {ξr (R P κ) + χ ( P + γ)}, where ( ) = d ( ) /dω, (R) = τ(ξr) 2 χ, σ = 1 + τξ. Figure: Stationary points of system (14): A(R 1, P 1 ), R 1 = κ/γ, P 1 = γ; B (R 2, P 2 ), R 2 = χ κ τξγ R2 τξ, P 2 2 = (1+τ ξ) R 2 ; C(0, γ) WMS AGH Compactons in Relaxing hydrodynamic-type model 18 / 37

54 Inserting ansatz (13) into the system (12), we get the first integral U = ξr + const and the dynamical system DS: ξ (R)R = R [σr P κ + τξrγ], (14) ξ (R) P = ξ {ξr (R P κ) + χ ( P + γ)}, where ( ) = d ( ) /dω, (R) = τ(ξr) 2 χ, σ = 1 + τξ. Figure: Stationary points of system (14): A(R 1, P 1 ), R 1 = κ/γ, P 1 = γ; B (R 2, P 2 ), R 2 = χ κ τξγ R2 τξ, P 2 2 = (1+τ ξ) R 2 ; C(0, γ) WMS AGH Compactons in Relaxing hydrodynamic-type model 18 / 37

55 Our further steps are the following: We are looking for the conditions assuring that the point A(R 1, P 1 ) is a center while simultaneously the point B (R 2, P 2 ) is a saddle. Next we apply the Andronov-Hopf-Floquet theory in order to state the conditions assuring the appearance of limit cycle in proximity of the critical point A; WMS AGH Compactons in Relaxing hydrodynamic-type model 19 / 37

56 Figure: Birth of the limit cycle in proximity of the critical point A WMS AGH Compactons in Relaxing hydrodynamic-type model 20 / 37

57 Finally we investigate (numerically) the interaction of the limit cycle with the saddle point B, hoping that the growth of the limit cycle will finally lead to the homoclinic trajectory appearance. WMS AGH Compactons in Relaxing hydrodynamic-type model 21 / 37

58 Figure: Interaction of limit cycle with unmovable saddle B would lead to the homoclinic loop creation WMS AGH Compactons in Relaxing hydrodynamic-type model 22 / 37

59 Lemma If R 1 < R 2 then in vicinity of the critical value ξ cr = χ + χ 2 + 4κR1 2. (15) 2R 2 1 a stable limit cycle appears in system (14). Lemma Stationary point B(R 2, P 2 ) is a saddle lying in the first quadrant for any ξ > ξ cr if the following inequalities hold: τ ξ cr R 2 < R 1 < R 2. (16) WMS AGH Compactons in Relaxing hydrodynamic-type model 23 / 37

60 Figure: Changes of phase portrait of system (14): (a) A(R 1, P 1 ) is the stable focus; (b) A(R 1, P 1 ) is surrounded by the stable limit cycle; (c) A(R 1, P 1 ) is surrounded by the homoclinic loop; (d) A(R 1, P 1 ) is the unstable focus; WMS AGH Compactons in Relaxing hydrodynamic-type model 24 / 37

61 Main features of the compacton solution of system (12) 1. The family of TW solutions to relaxing hydrodynamic system (12) includes a compacton in case when an external force is present (more precisely, when γ < 0 ). 2. To our best knowledge, no one of the classical (local) hydrodynamic-type models does not possesses this type of solution. 3. In contrast to the equations belonging to the K(m, n) hierarchy, compacton solution to system (12) occurs merely at selected values of the parameters: for fixed κ, γ and χ: there is the unique compacton-like solution, corresponding to the value ξ = ξ cr2. WMS AGH Compactons in Relaxing hydrodynamic-type model 25 / 37

62 Main features of the compacton solution of system (12) 1. The family of TW solutions to relaxing hydrodynamic system (12) includes a compacton in case when an external force is present (more precisely, when γ < 0 ). 2. To our best knowledge, no one of the classical (local) hydrodynamic-type models does not possesses this type of solution. 3. In contrast to the equations belonging to the K(m, n) hierarchy, compacton solution to system (12) occurs merely at selected values of the parameters: for fixed κ, γ and χ: there is the unique compacton-like solution, corresponding to the value ξ = ξ cr2. WMS AGH Compactons in Relaxing hydrodynamic-type model 25 / 37

63 Main features of the compacton solution of system (12) 1. The family of TW solutions to relaxing hydrodynamic system (12) includes a compacton in case when an external force is present (more precisely, when γ < 0 ). 2. To our best knowledge, no one of the classical (local) hydrodynamic-type models does not possesses this type of solution. 3. In contrast to the equations belonging to the K(m, n) hierarchy, compacton solution to system (12) occurs merely at selected values of the parameters: for fixed κ, γ and χ: there is the unique compacton-like solution, corresponding to the value ξ = ξ cr2. WMS AGH Compactons in Relaxing hydrodynamic-type model 25 / 37

64 Stability and attracting features of the compacton-like solution to system (12) RESULTS OF NUMERICAL SIMULATION WMS AGH Compactons in Relaxing hydrodynamic-type model 26 / 37

65 Figure: Temporal evolution of the compacton-like solution: t = 0 corresponds to initial TW solution; graphs t = 20, 40, 60 are obtained by means of the numerical simulation WMS AGH Compactons in Relaxing hydrodynamic-type model 27 / 37

66 Non-invariant initial (Cauchý) data Following family of the initial perturbations have been considered in the numerical experiments p 0 (x 0 x) when x (0, a) (a + l, x 0 ) p = (p 0 + p 1 )(x 0 x) + w(x a) + h when x (a, a + l), u = 0, V = κ/p. (17) WMS AGH Compactons in Relaxing hydrodynamic-type model 28 / 37

67 Hyperbolicity of system (12) causes that any compact initial perturbation splits into two pulses moving into opposite directions. Numerical experiments show that under certain conditions one of the wave packs created by the perturbation (namely that one which runs downwards towards the direction of diminishing pressure) in the long run approaches compacton solution. It does occur when the total energy of initial perturbation E tot is close to some number E(κ, χ, γ...) depending on the parameters of the system. WMS AGH Compactons in Relaxing hydrodynamic-type model 29 / 37

68 Hyperbolicity of system (12) causes that any compact initial perturbation splits into two pulses moving into opposite directions. Numerical experiments show that under certain conditions one of the wave packs created by the perturbation (namely that one which runs downwards towards the direction of diminishing pressure) in the long run approaches compacton solution. It does occur when the total energy of initial perturbation E tot is close to some number E(κ, χ, γ...) depending on the parameters of the system. WMS AGH Compactons in Relaxing hydrodynamic-type model 29 / 37

69 Hyperbolicity of system (12) causes that any compact initial perturbation splits into two pulses moving into opposite directions. Numerical experiments show that under certain conditions one of the wave packs created by the perturbation (namely that one which runs downwards towards the direction of diminishing pressure) in the long run approaches compacton solution. It does occur when the total energy of initial perturbation E tot is close to some number E(κ, χ, γ...) depending on the parameters of the system. WMS AGH Compactons in Relaxing hydrodynamic-type model 29 / 37

70 For κ = 10, χ = 1.5, γ = 0.04, τ = 0.07 and x 0 = 120 E(κ, χ, γ...) is close to 45. WMS AGH Compactons in Relaxing hydrodynamic-type model 30 / 37

71 Figure: Left: initial perturbation on the background of the compacton-like solution (dashed). Right: evolution of the wave pack caused by the initial perturbation on the background of the compacton-like solution (dashed). WMS AGH Compactons in Relaxing hydrodynamic-type model 31 / 37

72 Figure: Left: initial perturbation on the background of the compacton-like solution (dashed). Right: evolution of the wave pack caused by the initial perturbation on the background of the compacton-like solution (dashed). WMS AGH Compactons in Relaxing hydrodynamic-type model 32 / 37

73 Figure: Left: initial perturbation on the background of the compacton-like solution (dashed). Right: evolution of the wave pack caused by the initial perturbation on the background of the compacton-like solution (dashed). WMS AGH Compactons in Relaxing hydrodynamic-type model 33 / 37

74 Figure: Evolution of the wave pack caused by the initial perturbation which does not satisfy the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 34 / 37

75 Figure: Evolution of the wave pack caused by the initial perturbation which does not satisfy the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 35 / 37

76 Colclusions and discussion Numerical investigations of relaxing hydrodynamics system (12) reveal that: 1. Compacton encountering in this particular model evolves in a stable self-similar mode. 2. A wide class of initial perturbations creates wave packs tending to the compacton. 3. Convergency only weakly depend on the shape of initial perturbation and is mainly caused by fulfillment of the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 36 / 37

77 Colclusions and discussion Numerical investigations of relaxing hydrodynamics system (12) reveal that: 1. Compacton encountering in this particular model evolves in a stable self-similar mode. 2. A wide class of initial perturbations creates wave packs tending to the compacton. 3. Convergency only weakly depend on the shape of initial perturbation and is mainly caused by fulfillment of the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 36 / 37

78 Colclusions and discussion Numerical investigations of relaxing hydrodynamics system (12) reveal that: 1. Compacton encountering in this particular model evolves in a stable self-similar mode. 2. A wide class of initial perturbations creates wave packs tending to the compacton. 3. Convergency only weakly depend on the shape of initial perturbation and is mainly caused by fulfillment of the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 36 / 37

79 Colclusions and discussion Numerical investigations of relaxing hydrodynamics system (12) reveal that: 1. Compacton encountering in this particular model evolves in a stable self-similar mode. 2. A wide class of initial perturbations creates wave packs tending to the compacton. 3. Convergency only weakly depend on the shape of initial perturbation and is mainly caused by fulfillment of the energy criterion. WMS AGH Compactons in Relaxing hydrodynamic-type model 36 / 37

80 THANKS FOR YOUR ATTENTION WMS AGH Compactons in Relaxing hydrodynamic-type model 37 / 37