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Article

The Period Function of the Generalized Sine-Gordon Equation and the Sinh-Poisson Equation

School of Mathematics and Statistics, Hunan First Normal University, Changsha 410205, China
*
Author to whom correspondence should be addressed.
Mathematics 2024, 12(16), 2474; https://doi.org/10.3390/math12162474
Submission received: 13 July 2024 / Revised: 5 August 2024 / Accepted: 7 August 2024 / Published: 10 August 2024
(This article belongs to the Section Dynamical Systems)

Abstract

:
In this paper, we consider the generalized sine-Gordon equation ψ t x = ( 1 + a x 2 ) sin ψ and the sinh-Poisson equation u x x + u y y + σ sinh u = 0 , where a is a real parameter, and σ is a positive parameter. Under different conditions, e.g., a = 0 , a 0 , and σ > 0 , the periods of the periodic wave solutions for the above two equations are discussed. By the transformation of variables, the generalized sine-Gordon equation and sinh-Poisson equations are reduced to planar dynamical systems whose first integral includes trigonometric terms and exponential terms, respectively. We successfully handle the trigonometric terms and exponential terms in the study of the monotonicity of the period function of periodic solutions.

1. Introduction

The sine-Gordon (sG) equation is a non-linear partial differential equation mainly applied in various fields of theoretical physics, including condensed matter physics, particle physics, and non-linear optics [1,2,3,4]. The sinh-Poisson (sP) equation has been used to study steady-state flows in an ideal incompressible liquid [5] and the dynamic behaviors of Kolmogorov flow. Cellular structures with square or hexagonal cells and quasi-crystal patterns of the sP equation are investigated in [6]. In this paper, we consider the generalized sG equation
ψ t x = ( 1 + a x 2 ) sin ψ ,
and the sP equation
u x x + u y y + σ sinh u = 0 ,
where a is a real parameter, ψ ( x , t ) , is a scalar valued function, u ( x , y ) represents the electrostatic potential, and σ is a positive parameter related to the plasma density and temperature.
In 1995, Fokas [7] first derived Equation (1) using the bi-Hamiltonian method. When a = 0 , Equation (1) becomes the standard sG equation. Ling and Sun [8] found multi-elliptic localized solutions, such as multi-elliptic kink solutions, multi-elliptic breather solutions, and multi-elliptic kink–breather solutions, using the Darboux–Bäcklund transformation method for a = 0 . When a 0 , many scholars have been devoted to study the dynamic behaviors of solitary waves in Equation (1). In the case where a < 0 , Equation (1) can be transformed into the sG equation using an appropriate Liouville-type transformation, and the behaviors of cusped and anti-cusped traveling-wave solutions to Equation (1) are discussed using conservation laws [9]. For a = 1 , Matsuno [10] constructed multi-soliton solutions in the form of parametric representation, and obtained many different solutions such as kinks, loop solitons, and breathers. For a = 1 , Matsuno [11] found that Equation (1) has kink and breather solutions but cannot have multi-valued solutions like loop solitons, as obtained in Ref. [10]. Gatlik et al. [12] studied the kink–inhomogeneity interaction for an sG equation. Carretero-González et al. [13] analyzed the interaction dynamics between kink and anti-kink stripes in a 2D sG equation. The integrable discretized system of Equation (1) has also been investigated. For instance, Feng et al. [14] constructed N-soliton solutions for the semi-discrete analogues of Equation (1) in the determinant form. In the continuous limit, they showed that the semi-discrete, generalized sG equation converged to the continuous generalized sG Equation (1). Sheng et al. [15] further found that in continuous, semi-discrete, and fully discrete cases, the generalized sG equation can be reduced into a short pulse equation. Xiang et al. [16] obtained some solutions and continuum limits to non-local, discrete sG equations using the bilinearization reduction method. Recently, Lührmann and Schlag [17] discussed the asymptotic stability of the kink solution for the sG equation under odd perturbations.
The sP Equation (2) originates from the mean field limit of ideal parallel line vortices with numerous interactions, and this model depicts a stream function configuration of a stationary 2D Euler flow [18]. Moreover, the sP Equation (2) is closely related to the long-time state of the 2D Navier–Stokes flow and some integrable soliton models, and the exact solutions of this equation play an important role in theoretic study and practice applications [19]. In past decades, the existence and multiplicity of solutions for Equation (2) have been investigated extensively, and the research topics involved equilibria and stability [20], boundary value problems [21,22], numerical calculations [23], and sign-changing solutions [24,25]. When σ was a sufficiently small positive constant, Bartolucci and Pistoia [26] obtained that Equation (2) has two pairs of nodal solutions under Dirichlet boundary conditions.
Currently, there is relatively little research on the behaviors of the periodic solutions of the sG equation and the sP equation. An important feature of the sG equation and sP equation is that both equations have soliton solutions and periodic solutions. A periodic solution is a special type of solution for non-linear wave equations, which is essentially different from the propagation of solitary wave solutions. In 2015, Li and Qiao [27] discussed the bifurcation and traveling wave solutions of Equation (1) and constructed some periodic wave solutions using the elliptic integral method. Recently, Zhang and Lou [28] considered the sG equation with some types of non-localities, and obtained two types of N-soliton solutions and six types of periodic solutions. Novkoski et al. [29] constructed periodic solutions of the sG equation and discussed their spectral signatures under both the large-amplitude and low-amplitude limits. Some authors have also discussed the existence of periodic solutions and quasi-periodic solutions for the sP equation [30,31,32,33]. Particularly, Wang and Zhou [34] discovered the existence of the periodic solutions for a discretized system of Equation (2) using critical point theory. In the current paper, our aim is to study the monotonicity of the period function of periodic solutions for Equations (1) and (2).
Consider a plane differential system
d x d ζ = A 1 ( x , y ) d y d ζ = A 2 ( x , y )
with the first integral H ( x , y ) = λ , where λ is a parameter called energy. Suppose that the origin O is the center (3). Let U O R 2 be the largest punctured neighborhood of O, which is filled with periodic orbits Υ λ encircling O. Define the period function by P ( λ ) : = Υ λ d ζ . The monotonicity of P ( λ ) is closely related to the existence and uniqueness of solutions of some boundary value, bifurcation, and the stability of periodic waves [35,36,37,38,39,40]. Many classical results regarding the monotonicity of the period function P ( λ ) have been obtained under the assumption that A 1 ( x , y ) and A 2 ( x , y ) are polynomials of x and y [41,42,43,44,45,46,47]. The knowledges of the Abelian integral, Picard–Fuchs equation, and structural features of polynomial are powerful tools for dealing with the monotonicity problems of the period function for polynomial systems. However, in our present paper, using traveling wave transformations, Equation (1) with a = 0 and Equation (2) can be written into Hamiltonian systems, in which trigonometric terms and exponential terms appear in the Hamiltonian function, respectively. When a 0 , Equation (1) can be written into a plane differential system that is not Hamiltonian, and the first integral contains trigonometric terms. Although the integrable system (1) can be transformed into a Hamiltonian form, the transformed Hamiltonian function is an implicit function for a 0 . The emergences of exponential terms, trigonometric terms, and implicit functions bring some difficulties for discussing the monotonicity of the period function. We handle these problems by utilizing some lemmas proposed by Chicone [48] and Sabatini [49].
The rest of this paper is arranged as follows. In Section 2, some criteria for the monotonicity of the period function are listed. In Section 3, the monotonicity of the period function for Equation (1) with a = 0 is discussed. In Section 4, the monotonicity of the period function for Equation (1) with a 0 is revealed. In Section 5, we study the monotonicity of the period function for Equation (2). In Section 6, the conclusion is summarized.

2. Criteria for the Monotonicity of the Period Function

In order to more logically prove the main results (Theorems 1–4) of the monotonicity of the period function for Equations (1) and (2), we first introduce some technical lemmas.
Lemma 1
([48]). Consider a plane Hamiltonian system
d z d ζ = y , d y d ζ = S ( z )
with Hamiltonian H ( z , y ) = 1 2 y 2 + S ( z ) , where S ( z ) is a smooth potential function with a non-degenerate relative minimum at the origin. Let
K ( λ ) = z R | S ( z ) λ ,
where λ is energy defined as ( 0 , λ * ) . Set
L ( z ) : = S ( z ) ( S ( z ) ) 2 .
Then, one has the following:
(1) If function L ( z ) 0 for all z K ( λ ) , the period function P ( λ ) satisfies P ( λ ) 0 for λ ( 0 , λ * ) .
(2) If function L ( z ) 0 for all z K ( λ ) , the period function P ( λ ) satisfies P ( λ ) 0 for λ ( 0 , λ * ) .
Lemma 2
([49]). Consider a plane Hamiltonian system:
d x d ζ = G ( y ) , d y d ζ = Q ( x ) ,
where G ( y ) and Q ( x ) are C 1 in a neighborhood of the origin O. Suppose that the origin O is the center (5). Let x = r cos θ , y = r sin θ . Then, Equation (5) becomes
d r d ζ = ρ ( r , θ ) , d θ d ζ = ω ( r , θ ) .
Assume that there exists a star-shaped set Δ U O , such that ω ( r , θ ) 0 for all ( r , θ ) Δ ρ , where Δ ρ is a set in the polar coordinate corresponding to Δ. Let r Δ ( θ ) : = sup { r | ( r , θ ) Δ ρ } . Denote Υ Δ : = { λ | λ Υ λ } by the set of cycles contained in Δ . Then, one has the following:
(1) 
If there exist a zero-measure set  A [ 0 , 2 π ) , such that for all  θ [ 0 , 2 π ) A ,   | ω ( r , θ ) | r 0  for  r ( 0 , r Δ ( θ ) ) , then  P ( λ ) 0  for  λ Υ Δ .
(2) 
If there exist a zero-measure set  A [ 0 , 2 π ) , such that for all  θ [ 0 , 2 π ) A ,   | ω ( r , θ ) | r 0  for  r ( 0 , r Δ ( θ ) ) , then  P ( λ ) 0  for  λ Υ Δ .
Remark 1.
In the following, we introduce two simple examples to illustrate the application of the above two lemmas.
Example 1.
Consider the cubic potentials system
d z d ζ = y , d y d ζ = 2 z 3 z 2
with Hamiltonian H ( z , y ) = 1 2 y 2 + z 2 + z 3 = λ . It is easy to verify that the origin is the center point. There exists a set of periodic orbits encircling the center at the origin. Taking L ( z ) = z 2 + z 3 ( 2 z + 3 z 2 ) 2 = 1 + z ( 2 + 3 z ) 2 , it yields that L ( z ) = 6 ( 3 z + 5 ) ( 3 z + 2 ) 4 . Thus, we obtain L ( z ) 0 for z > 2 3 . Since the periodic orbits encircling the origin are confined to the region z > 2 3 , using Lemma 1, we obtain that the period function P ( λ ) > 0 for λ ( 0 , 27 4 ) .
Example 2.
Consider the polynomial system
d x d ζ = y , d y d ζ = 2 x 4 x 3 ,
with Hamiltonian H ( x , y ) = 1 2 y 2 + x 2 + x 4 = λ . We can verify that the origin is the center point as there exists a set of periodic orbits encircling the center at the origin. Let x = r cos θ , y = r sin θ . Then, Equation (7) becomes
d r d ζ = ρ ( r , θ ) = r sin θ cos θ 4 r 2 cos 2 θ + 1 , d θ d ζ = ω ( r , θ ) = 4 r 2 cos 4 θ sin 2 θ 2 cos 2 θ .
Obviously, | ω ( r , θ ) | r = 8 r ( cos θ ) 4 0 for all r ( 0 , + ) , and by using Lemma 2, we obtain that the period function P ( λ ) 0 for λ ( 0 , + ) .

3. The Monotonicity of the Period Function for the Generalized sG Equation in the Case of a = 0

When a = 0 , Equation (1) becomes the standard sG equation [8], which can be directly written into a Hamiltonian system. For this, in the following we consider the case with a = 0 for Equation (1).
Let
ψ ( x , t ) = ψ ( x c t ) = z ( ζ ) ,
where ζ = x c t and c is a real constant. Then, Equation (1) yields
sin z + c z = 0
at a = 0 , where z = d z d ζ and z = d 2 z d ζ 2 . We write Equation (9) as
d z d ζ = y , d y d ζ = sin z c ,
with Hamiltonian
H ( z , y ) = 1 2 y 2 1 c cos z + 1 c = λ .
System (10) has infinite equilibrium points O k ( k π , 0 ) , where k Z , and Z represents the set of integers.
In the following, we provide the main result of this section.
Theorem 1.
In the case that a = 0 and c > 0 , there are corresponding period annulus of the infinite number of centers at the points O 2 k ( 2 k π , 0 ) for Equation (9). The period function P ( λ ) satisfies P ( λ ) 0 for λ ( 0 , 2 c ) . Moreover, lim λ 0 P ( λ ) = 2 c π and lim λ 2 c P ( λ ) = + .
Proof. 
Let M 0 ( 0 , 0 ) be the coefficient matrix of the linearized system (10) at equilibrium point O 0 ( 0 , 0 ) and define J = det M 0 ( 0 , 0 ) . Then,
M 0 ( 0 , 0 ) = 0 1 1 c 0 , J = 1 c .
Using the theory of planar dynamical systems [50], we know that for an equilibrium point O 0 ( 0 , 0 ) of a planar dynamical system, if J < 0 , then the equilibrium point is a saddle point; if J > 0 and Trace ( M 0 ( 0 , 0 ) ) = 0 , then the equilibrium point is the center point.
When c > 0 , we have J > 0 and Trace ( M 0 ( 0 , 0 ) ) = 0 , which implies the equilibrium point O 0 ( 0 , 0 ) is the center point. Using trigonometric identity sin 2 k π = sin 0 = 0 , it follows that the equilibrium points O 2 k ( 2 k π , 0 ) are centers. Similarly, we obtain that the points O 2 k + 1 ( 2 k π + π , 0 ) are saddles for c > 0 . The phase portrait of system (10) is shown in Figure 1, and we can see that there exists a class of periodic orbits surrounding the infinite number of centers O 2 k ( 2 k π , 0 ) if λ satisfies λ ( 0 , 2 c ) . When c > 0 , the numerical simulation of periodic waves of system (10) is plotted in Figure 2.
Since sin z is the function with a period of 2 π with respect to z, the monotonicity of the period function of periodic solutions surrounding the centers O 2 k ( 2 k π , 0 ) are the same, we only need to consider the center point O 0 ( 0 , 0 ) . Let
S ( z ) = 1 c cos z + 1 c , L ( z ) = S ( z ) ( S ( z ) ) 2 = c 1 + cos z .
A straightforward computation shows that
L ( z ) = 1 4 c ( cos z 2 ) sec 4 z 2 0
holds for all z ( π , π ) . Using Lemma 1, we complete the proof of the first part of Theorem 1.
Next, we consider the asymptotic analysis. Recall that
1 2 y 2 1 c cos z + 1 c = λ
is a first integral of system (10). Let y = 0 , then Equation (12) yields z 1 , 2 = ± arccos ( 1 c λ ) .
P ( λ ) = 2 z 1 z 2 d z λ + 1 c cos z 1 c = 2 c arccos ( 1 c λ ) arccos ( 1 c λ ) d z c λ + cos z 1 .
Let
z = w arccos ( 1 c λ ) ,
then
P ( λ ) = 2 c 1 1 arccos ( 1 c λ ) c λ + cos w arccos ( 1 c λ ) 1 d w .
Let c λ = h . Then, we have h 0 as λ 0 . Using the Taylor series in h, we have
arccos ( 1 c λ ) c λ + cos w arccos ( 1 c λ ) 1 = 2 1 w 2 + h 2 w 2 + 2 12 1 w 2 + O h 2 .
Therefore,
lim λ 0 P ( λ ) = lim h 0 2 c 1 1 2 1 w 2 + O h d w = 2 c π .
Let arccos ( 1 c λ ) = l , then we obtain l π as λ 2 c . Let l w = q . Then, using (15), we have
lim λ 2 c P ( λ ) = lim l π 2 c 1 1 l cos w l cos l d w = lim l π 2 c l l 1 cos q cos l d q = + .
This completes the proof of the second part of Theorem 1.
When c = 1 , the graph of the period function P ( λ ) of system (10) at λ ( 0 , 2 ) is shown in Figure 3, and it indicates that the numerical result is consistent with the theoretical analysis result.

4. The Monotonicity of the Period Function for the Generalized sG Equation in the Case of a 0

In this section, we consider the generalized sG Equation (1) in the case with a 0 . When a cos z + c 0 , using the traveling wave transformation (8), Equation (1) can be written as
sin z a cos z + c ( z ) 2 a sin z a cos z + c + z = 0 .
Equation (17) is equivalent to the following planar dynamical system:
d z d ζ = y , d y d ζ = ( a y 2 1 ) sin z c + a cos z ,
with the first integral
H ( z , y ) = y 2 ( c + a cos z ) 2 ( a cos 2 z + 2 c cos z 2 c a ) = λ .
It should be mentioned that system (18) is not a Hamiltonian system but it can be transformed into the form of a Hamiltonian. Note that z ( ζ ) is a solution of (18) if and only if v ( ζ ) is a solution of the following planar Hamiltonian system
d v d ζ = y , d y d ζ = W ( v ) ,
where the implicit function W ( v ) = sin z c + a satisfies the equation
c z + a sin z = ( c + a ) v .
Since W ( v ) in Hamiltonian system (20) is an implicit function and it cannot be represented explicitly, it is difficult to analyze the monotonicity of the period function using Lemma 1. However, we can tackle this problem using Lemma 2.
Theorem 2.
In the case that  a + c > 0 , there are corresponding period annulus surrounding the center points  O 2 k ( 2 k π , 0 )  for Equation (18), where  k Z .
(1) 
If  c > a > 0 ,  or in the case that  c > a > 0 ,  the corresponding period function  P ( λ )  satisfies  P ( λ ) 0  for  0 < λ < 4 c .
(2) 
If  a > c > 0 ,  then  P ( λ ) 0  for  0 < λ < ( a + c ) 2 a .
(3) 
If  a > c > 0 ,  then  P ( λ ) 0  for  0 < λ < ( a + c ) 2 a .
Proof. 
Obviously, the points O 2 k ( 2 k π , 0 ) are equilibria of (18). Since
sin z = sin ( z + 2 k π ) , cos z = cos ( z + 2 k π ) ,
from the expression of (18), we only need to consider the point O 0 ( 0 , 0 ) . Since the linear coefficient matrix of (18) at the origin is
0 1 1 a + c 0 ,
using the theory of planar dynamical system, it follows that the point O 0 ( 0 , 0 ) is the center of a + c > 0 . The phase portrait of system (18) is shown in Figure 4 under different parametric conditions.
Using identities
sin z = 2 sin z 2 cos z 2 , 1 cos 2 z = sin 2 z , cos z 1 = 2 sin 2 z 2 ,
Equation (19) can be rewritten as
H ( z , y ) = y 2 ( c + a cos z ) 2 + ( 4 a + 4 c ) sin 2 z 2 4 a sin 4 z 2 = λ .
When c > a > 0 , or in the case that c > a > 0 , there exists a set of period orbits surrounding the center O 0 ( 0 , 0 ) for 0 < λ < 4 c , and the abscissa of the intersection point between the periodic orbit and the z-axis satisfies π < z < π ; see Figure 4a,c.
Since systems (18) and (20) have the same monotonicity of the period function defined in the neighborhood of origin, we only consider system (20). Since W ( 0 ) = 0 , one can set
W ( v ) = W ( 0 ) v + W 1 ( v ) .
Using polar coordinate transformation v = r cos θ , y = r sin θ , system (20) becomes
d r d ζ = r cos θ sin θ sin θ W ( r cos θ ) = ρ ( r , θ ) , d θ d ζ = W ( 0 ) cos 2 θ sin 2 θ cos θ W 1 ( r cos θ ) r = ω ( r , θ ) .
Note that
r 2 ω ( r , θ ) = r 2 d θ d ζ = W ( 0 ) v 2 y 2 v W 1 ( v ) = v W ( v ) y 2 .
Using (21), we obtain
v W ( v ) = v sin z c + a = ( c z + a sin z ) sin z ( c + a ) 2 .
When c > a > 0 , or in the case that c > a > 0 , we obtain that v W ( v ) > 0 for z ( π , 0 ) ( 0 , π ) .
Using (25), we have r 2 ω ( r , θ ) < 0 for z ( π , 0 ) ( 0 , π ) . Thus,
| ω ( r , θ ) | r = ω ( r , θ ) r = cos θ W 1 ( r cos θ ) r r = r 2 cos 2 θ W 1 ( r cos θ ) r cos θ W 1 ( r cos θ ) r 3 = v 2 W 1 ( v ) v W 1 ( v ) ( v 2 + y 2 ) 3 2
for θ [ 0 , 2 π ) and θ π 2 , 3 π 2 . Using (21) and (23), it can be deduced that
W 1 ( v ) = W ( v ) W ( 0 ) = cos z c + a cos z 1 c + a .
Hence,
v 2 W 1 ( v ) v W 1 ( v ) = v 2 cos z c + a cos z 1 c + a v sin z c + a 1 c + a v = v v cos z c + a cos z sin z c + a = c ( a + c ) 2 ( z cos z sin z ) ( a sin z + c z ) a cos z + c .
When c > a > 0 , or in the case that c > a > 0 , we can directly verify that v 2 W 1 ( v ) v W 1 ( v ) < 0 for z ( π , 0 ) ( 0 , π ) . Using (26), we obtain | ω ( r , θ ) | r 0 for almost all θ [ 0 , 2 π ) . From Lemma 2, we have P ( λ ) 0 for 0 < λ < 4 c .
Similarly, when a > c > 0 , we have v 2 W 1 ( v ) v W 1 ( v ) < 0 for z ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . Using (26) again, we obtain | ω ( r , θ ) | r 0 for z ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . From Lemma 2, we have P ( λ ) 0 for 0 < λ < ( a + c ) 2 a .
When a > c > 0 , we have v 2 W 1 ( v ) v W 1 ( v ) > 0 for z ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . Using (26), it yields | ω ( r , θ ) | r 0 for z ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . From Lemma 2, we obtain P ( λ ) 0 for 0 < λ < ( a + c ) 2 a .
Taking c = 2 and a = 1 , the plot of P ( λ ) for λ ( 0 , 4 c ) is presented in Figure 5a. Taking c = 2 and a = 1 , the plot of P ( λ ) for λ ( 0 , 4 c ) is shown in Figure 5b. Taking a = 2 and c = 1 , the plot of P ( λ ) for λ ( 0 , ( a + c ) 2 a ) is presented in Figure 5c. Taking a = 2 and c = 1 , the plot of P ( λ ) for λ ( 0 , ( a + c ) 2 a ) is shown in Figure 5d. The numerical simulation verifies the qualitative analytical results of Theorem 2.
Theorem 3.
In the case that a > c > 0 , there are corresponding period annulus surrounding the center points O 2 k + 1 ( 2 k π + π , 0 ) for Equation (18), where k Z . The corresponding period function P ( λ ) satisfies P ( λ ) 0 for 4 c < λ < ( a c ) 2 a .
Proof. 
It is straightforward to verify that the points O 2 k + 1 ( 2 k π + π , 0 ) are equilibria of (18). We make a translation to move the equilibrium points O 2 k + 1 ( 2 k π + π , 0 ) to the origin. Let z ( 2 k π + π ) = z ^ and y 0 = y ^ . Then, system (18) becomes
d z ^ d ζ = y ^ , d y ^ d ζ = ( 1 a y ^ 2 ) sin z ^ c a cos z ^ .
The linear coefficient matrix of (29) at the origin is as follows:
0 1 1 c a 0 .
Using the theory of the planar dynamical system, it follows that the points O 2 k + 1 ( 2 k π + π , 0 ) are centers for a > c > 0 . From Figure 4d, we can see that there are corresponding period annulus surrounding the center points O 2 k + 1 ( 2 k π + π , 0 ) for Equation (18).
Note that z ^ ( ζ ) is a solution of (29) if and only if v ^ ( ζ ) is a solution of the planar Hamiltonian system:
d v ^ d ζ = y ^ , d y ^ d ζ = W ^ ( v ^ ) ,
where the implicit function W ^ ( v ^ ) = sin z ^ a c satisfies the following equation:
c z ^ + a sin z ^ = ( a c ) v ^ .
Since W ^ ( 0 ) = 0 , we set
W ^ ( v ^ ) = W ^ ( 0 ) v ^ + W ^ 1 ( v ^ ) .
Let v ^ = r ^ cos θ ^ , y = r ^ sin θ ^ . Then, system (30) becomes
d r ^ d ζ = r ^ cos θ ^ sin θ ^ sin θ ^ W ^ ( r ^ cos θ ^ ) = ρ ^ ( r ^ , θ ^ ) , d θ ^ d ζ = W ^ ( 0 ) cos 2 θ ^ sin 2 θ ^ cos θ ^ W ^ 1 ( r ^ cos θ ^ ) r ^ = ω ^ ( r ^ , θ ^ ) .
Obviously,
r ^ 2 ω ^ ( r ^ , θ ^ ) = r ^ 2 d θ ^ d ζ = v ^ W ^ ( v ^ ) y ^ 2 .
Using (31), we obtain
v ^ W ^ ( v ^ ) = v ^ sin z ^ a c = ( c z ^ + a sin z ^ ) sin z ^ ( a c ) 2 .
When a > c > 0 , we obtain that v ^ W ^ ( v ^ ) > 0 for z ^ ( π , 0 ) ( 0 , π ) . Using (34), we have r ^ 2 ω ^ ( r ^ , θ ^ ) < 0 for z ^ ( π , 0 ) ( 0 , π ) . Thus,
| ω ^ ( r ^ , θ ^ ) | r ^ = ω ^ ( r ^ , θ ^ ) r ^ = v ^ 2 W ^ 1 ( v ^ ) v ^ W ^ 1 ( v ^ ) ( v ^ 2 + y ^ 2 ) 3 2
for z ^ ( π , 0 ) ( 0 , π ) . Using (31), we have
W ^ 1 ( v ^ ) = W ^ ( v ^ ) W ^ ( 0 ) = cos z ^ c + a cos z ^ 1 a c .
Therefore,
v ^ 2 W ^ 1 ( v ^ ) v ^ W ^ 1 ( v ^ ) = c ( a c ) 2 ( z ^ cos z ^ sin z ^ ) ( a sin z ^ c z ^ ) a cos z ^ c .
When a > c > 0 , we can verify that v ^ 2 W ^ 1 ( v ^ ) v ^ W ^ 1 ( v ^ ) < 0 for z ^ ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . Using (35), we obtain | ω ^ ( r ^ , θ ^ ) | r ^ < 0 for z ^ ( arccos ( c a ) , 0 ) ( 0 , arccos ( c a ) ) . Returning to Equations (18) and (19), using Lemma 2, we have P ( λ ) 0 for 4 c < λ < ( a c ) 2 a .
Taking a = 2 and c = 1 , the plot of P ( λ ) for λ ( 4 c , ( a c ) 2 a ) is presented in Figure 6. The numerical simulation verifies the qualitative analytical results of Theorem 3.

5. The Monotonicity of the Period Function for the sP Equation

Let
ξ = k 1 x + k 2 y ,
where k 1 and k 2 are constants. Substituting (38) into Equation (2) yields
k 1 2 d 2 u d ξ 2 + k 2 2 d 2 u d ξ 2 = σ e u e u 2 .
Equation (39) can be written as a plane Hamiltonian system:
d u d ξ = p , d p d ξ = N ( u ) ,
with Hamiltonian
H ( u , p ) = 1 2 p 2 b 2 ( e u + e u ) + b = λ ,
where N ( u ) = b e u e u 2 , b = σ k 1 2 + k 2 2 , and k 1 2 + k 2 2 0 . Since σ > 0 , we have b < 0 .
Theorem 4.
In the case that b < 0 , there is a class of periodic solutions in a neighborhood of the point O ( 0 , 0 ) for Equation (40). The period function satisfies P ( λ ) 0 for λ ( 0 , + ) . Moreover, lim λ 0 P ( λ ) = 2 π b and lim λ + P ( λ ) = 0 .
Proof. 
When b 0 , there is an equilibrium point O ( 0 , 0 ) of system (40). Since the linear coefficient matrix of (40) at equilibrium point O ( 0 , 0 ) is
0 1 b 0 ,
by the theory of the planar dynamical system, we know that the equilibrium point O ( 0 , 0 ) is a center point for b < 0 . With numerical simulations, the phase portrait of system (40) is plotted in Figure 7, and the periodic waves are plotted in Figure 8.
From Figure 7, we can see that if b < 0 and λ > 0 , then there is a class of periodic orbits in a neighborhood of the center O ( 0 , 0 ) . Using (41), we have
P ( λ ) = Υ λ d u p = 2 u 1 u 2 d u λ + b 2 ( e u + e u ) b ,
where u 1 and u 2 are the roots of equation b 2 ( e u + e u ) + b = λ , and u 1 < 0 < u 2 . Since H ( u , p ) is an even function with respect to u and p, it yields that u 1 = u 2 .
Since N ( 0 ) = 0 , we set
N ( u ) = N ( 0 ) u + N 1 ( u ) .
Using the polar coordinate transformation u = r ˜ cos θ ˜ , p = r ˜ sin θ ˜ , system (40) becomes
d r ˜ d ξ = r ˜ cos θ ˜ sin θ ˜ sin θ ˜ N ( r ˜ cos θ ˜ ) = ρ ˜ ( r ˜ , θ ˜ ) , d θ ˜ d ξ = N ( 0 ) cos 2 θ ˜ sin 2 θ ˜ cos θ ˜ N 1 ( r ˜ cos θ ˜ ) r ˜ = ω ˜ ( r ˜ , θ ˜ ) .
Note that
r ˜ 2 ω ˜ ( r ˜ , θ ˜ ) = r ˜ 2 d θ ˜ d ξ = N ( 0 ) u 2 p 2 u N 1 ( u ) = u N ( u ) p 2 .
When b < 0 , we have
u N ( u ) = b u e u e u 2 > 0
for u R { 0 } . Using (45), we obtain r ˜ 2 ω ˜ ( r ˜ , θ ˜ ) < 0 for u R { 0 } .
Thus,
| ω ˜ ( r ˜ , θ ˜ ) | r ˜ = ω ˜ ( r ˜ , θ ˜ ) r ˜ = cos θ ˜ N 1 ( r ˜ cos θ ˜ ) r ˜ r ˜ = u 2 N 1 ( u ) u N 1 ( u ) ( u 2 + p 2 ) 3 2
for θ ˜ [ 0 , 2 π ) and θ ˜ π 2 , 3 π 2 . Obviously,
N 1 ( u ) = N ( u ) N ( 0 ) = b e u + e u 2 + b .
Thus,
u 2 N 1 ( u ) u N 1 ( u ) = u 2 b e u + e u 2 + b u b e u e u 2 + b u = b u sinh u u cosh u .
When b < 0 , we have u 2 N 1 ( u ) u N 1 ( u ) > 0 for u R { 0 } . Using (46), we obtain | ω ˜ ( r ˜ , θ ˜ ) | r ˜ 0 for θ ˜ [ 0 , 2 π ) and θ ˜ π 2 , 3 π 2 . From Lemma 2, we have P ( λ ) 0 for λ ( 0 , + ) .
Next, we discuss the asymptotic behavior of P ( λ ) . Recall that
P ( λ ) = 2 u 1 u 2 d u λ + b 2 ( e u + e u ) b
and u 1 = u 2 . Since u 1 and u 2 are the roots of equation
b 2 ( e u + e u ) + b = λ
and u 1 = u 2 , it deduces that lim λ 0 u 1 = 0 = lim λ 0 u 2 . Let
u = u 2 w .
Then, Equation (49) becomes
P ( λ ) = 2 1 1 u 2 d w λ + b 2 ( e w u 2 + e w u 2 ) b .
Using (50) and the Taylor expansion with respect to u 2 , we have
u 2 λ + b 2 ( e w u 2 + e w u 2 ) b = 2 b 1 w 2 u 2 2 w 2 + 1 12 2 b 1 w 2 + O u 2 2 .
Thus, using (51) and (52), we obtain
lim u 2 0 P = 2 1 1 2 d w b ( 1 w 2 ) = 2 b π .
It follows that P 2 b π as λ 0 .
We also can obtain that lim λ + P ( λ ) = 0 . The proof process of the asymptotic property of λ + is similar to that of λ 0 , so we omit it here. □
Taking b = 2 , the plot of P ( λ ) for λ ( 0 , b ) is presented in Figure 9a, and the plot of P ( λ ) for λ ( b , 100 b ) is presented in Figure 9b, the plot of P ( λ ) at infinity is also presented in Figure 9c. The numerical simulation verifies the qualitative analytical results of Theorem 4.
Remark 2.
If Lemma 1 is used to analyze the monotonicity of the period function (42), then we can only obtain that P ( λ ) 0 for λ ( 0 , b ) , but the monotonicity of P ( λ ) on ( b , + ) cannot be theoretically proven directly. In fact, choosing S ( u ) = b 2 ( e u + e u ) + b , we have
L ( u ) = S ( u ) ( S ( u ) ) 2 = 2 ( e u + e u ) + 4 b ( e u e u ) 2 .
Taking the derivative of L ( u ) twice, it yields
L ( u ) = 2 e u e 2 u 4 e u + 1 b e u + 1 4 .
A short calculation revealed that for u ( ln ( 2 + 3 ) , ln ( 2 + 3 ) ) , L ( u ) < 0 holds. From Lemma 1, it implies that P ( λ ) 0 for λ ( 0 , b ) . However, Equation (55) yields that L ( u ) > 0 for u > ln ( 2 + 3 ) . Thus, L ( u ) < 0 is impossible for all u ( ln ( 2 + 3 ) , + ) , and the condition of Lemma 1 is not satisfied.

6. Conclusions

In this paper, we considered the monotonicity of the period function of the generalized sine-Gordon Equation (1) and the sinh-Poisson Equation (2). Using Lemma 1, we obtained the monotonicity of the period function of Equation (1) for a = 0 , and the result can be found in Theorem 1. Using Lemma 2, we obtained the monotonicity of the period function of Equation (1) for a 0 , and the results can be found in Theorems 2 and 3. Using Lemma 2, the monotonicity of the period function of Equation (2) was provided, and the result can be found in Theorem 4. The numerical simulations were used, and the results of the numerical simulations were consistent with the theoretical analysis. In the future, we will further investigate the stability of the periodic solutions of Equations (1) and (2).

Author Contributions

Conceptualization and methodology, X.H.; writing—original draft, L.L.; writing—review and editing, X.Z. All authors have read and agreed to the published version of the manuscript.

Funding

This research is supported by the Excellent Youth Project of the Education Department of Hunan Province (No. 22B0886), the Natural Science Foundation of Hunan Province (No. 2023JJ30179), the National Natural Science Foundation of China (No. 12275350), and the Hunan Provincial Natural Science Foundation of China (No. 2024JJ6171).

Data Availability Statement

Data are contained within the article.

Acknowledgments

The authors wish to thank the anonymous reviewers for their helpful comments and suggestions.

Conflicts of Interest

The authors declare no conflicts of interest.

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Figure 1. The phase portrait of system (10) for c > 0 .
Figure 1. The phase portrait of system (10) for c > 0 .
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Figure 2. Periodic waves of system (10) for c > 0 .
Figure 2. Periodic waves of system (10) for c > 0 .
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Figure 3. The graph of the period function P ( λ ) of system (10) for c = 1 .
Figure 3. The graph of the period function P ( λ ) of system (10) for c = 1 .
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Figure 4. Phase portraits of system (18) for a + c > 0 .
Figure 4. Phase portraits of system (18) for a + c > 0 .
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Figure 5. When a + c > 0 , the plots of P ( λ ) are associated with the center O 0 ( 0 , 0 ) for system (18).
Figure 5. When a + c > 0 , the plots of P ( λ ) are associated with the center O 0 ( 0 , 0 ) for system (18).
Mathematics 12 02474 g005aMathematics 12 02474 g005b
Figure 6. When a = 2 and c = 1 , the plot of P ( λ ) associated with the center O 1 ( π , 0 ) for system (18).
Figure 6. When a = 2 and c = 1 , the plot of P ( λ ) associated with the center O 1 ( π , 0 ) for system (18).
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Figure 7. Phase portrait of (40) for b < 0 .
Figure 7. Phase portrait of (40) for b < 0 .
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Figure 8. Periodic waves of (40) for b < 0 .
Figure 8. Periodic waves of (40) for b < 0 .
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Figure 9. The plots of P ( λ ) at b = 2 .
Figure 9. The plots of P ( λ ) at b = 2 .
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Lu, L.; He, X.; Zhou, X. The Period Function of the Generalized Sine-Gordon Equation and the Sinh-Poisson Equation. Mathematics 2024, 12, 2474. https://doi.org/10.3390/math12162474

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Lu L, He X, Zhou X. The Period Function of the Generalized Sine-Gordon Equation and the Sinh-Poisson Equation. Mathematics. 2024; 12(16):2474. https://doi.org/10.3390/math12162474

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Lu, Lin, Xiaokai He, and Xing Zhou. 2024. "The Period Function of the Generalized Sine-Gordon Equation and the Sinh-Poisson Equation" Mathematics 12, no. 16: 2474. https://doi.org/10.3390/math12162474

APA Style

Lu, L., He, X., & Zhou, X. (2024). The Period Function of the Generalized Sine-Gordon Equation and the Sinh-Poisson Equation. Mathematics, 12(16), 2474. https://doi.org/10.3390/math12162474

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