ORIGINAL RESEARCH article

Front. Phys., 09 May 2025

Sec. Statistical and Computational Physics

Volume 13 - 2025 | https://doi.org/10.3389/fphy.2025.1569964

Analytical solutions for the forced KdV equation with variable coefficients

Ji Wang
Ji Wang1*Jia FuJia Fu2Jialin DaiJialin Dai3
  • 1School of Liberal Arts and Humanities, Sichuan Vocational College of Finance and Economics Chengdu, Chengdu, China
  • 2School of Mathematical Sciences and V.C. and V.R. Key Lab, Sichuan Normal University Chengdu, Chengdu, China
  • 3Pengzhou Tianfu Road Primary School Chengdu, Chengdu, Sichuan, China

This paper focuses on obtaining the exact solutions to the variable-coefficient forced Korteweg-de Vries (KdV) equation for modeling spatial inhomogeneity in fluids. By combining the direct similarity reduction-based CK method with the (G'/G) expansion method, three new similarity solutions are obtained for this variable-coefficient forced KdV equation.

1 Introduction

The forced KdV equation with variable coefficients plays a crucial role in researching the waves motion and nonlinear phenonmeno [1], and it attracts more and more research attentions [2]. In this paper, we examine the forced KdV equation with variable coefficients:

ut+atuux+btuxxx+ctu+dtux=fx,t,(1.1)

where u=u(x,t) is the wave function and x and t are scaled spatial and temporal coordinates, respectively. a(t) is a nonlinearity coefficient, b(t) is a dispersive coefficient, c(t) is a line-damping coefficient, d(t) is a dissipative coefficient, and f(x,t) represents the external force effect function. Under suitable selections of the coefficient functions, Equation 1.1 reduces to a sequence of integrable systems or describe the nonlinear waves in a fluid-filled tube [3], weakly nonlinear waves in the water of variable depth [4], and it models the spatial inhomogeneity in fluids [5]. The classical KdV equation was first derived from shallow water wave theory to describe the propagation of water waves in the long wave limit (surface gravity waves) [6]. The coefficients of variation in Equation 1.1 are due to geometric and physical inhomogeneities [3, 7].

In this context, we suppose that the external force effect function has the following form according to [5]:

fx,t=f1tx+f2t.(1.2)

In particular, when a(t)=μ1, b(t)=μ2, c(t)=0, d(t)=μ3(t)μ1μ(t), and f(x,t)=0, H.L. Demiray [8] obtained the solitary wave solution via coordinate transformation. When a(t)=3c32, b(t)=16c, c(t)=12c, d(t)=0, and f(x,t)=0, H.L. Demiray [9] obtained a progressive wave-type solution through the reductive perturbation method. When f1(t)=0, Zhang et al. [10] utilized the Wronskian technique and Hirota method to obtain a bilinear form and an analytic N-soliton-like solution. On the basis of symbolic computation, Tian et al. [11] obtained solutions for the Airy, Hermit and Jacobian elliptic functions [12]. Utilizing the Hirota bilinear method, Yu et al. [13] obtained an N-soliton solution and a type of analytic solution.

Various methods have been applied to search for exact solutions to nonlinear evolution equations (see [1423]), including the (G/G) expansion method [22, 24], the Hirota bilinear method [18], the inverse scattering transform method [16], the CK direct method [15], and the nonclassic Lie group method [14], among others.

In general, solving ordinary differential equations is easier than directly constructing partial differential equations. However, owing to variable coefficients, it remains difficult to solve an ordinary differential equation with variable coefficients. In the present work, first, by applying the direct similarity reduction-based CK method, we transform the partial differential equation shown in (1.1) into an ordinary differential equation. Then, solutions are obtained for the above ordinary differential equation via the (G/G) expansion method. Finally, we can obtain three new similarity solutions to the variable-coefficient forced KdV equation in (1.1) and express the graphics of these similarity solutions. This equation may represent the main profile of these solutions for Equation 1.1.

2 Direct similarity reduction-based CK method

We hypothesize that the solution to Equation 1.1 takes the following form:

ux,t=Ux,t,wzx,t.(2.1)

Indeed, Equation 2.1 may represent the general form of the similarity solutions for Equation 1.1 (see [25]), and it is sufficient to consider the solutions for Equation 1.1 in the form of Equation 2.1. By substituting Equations 1.2, 2.1 into (1.1), we obtain

Ut+Uwwzt+atUUx+Uwwzx+ctU+dtUx+Uwwzx+btUxxx+3Uxxwwzx+Uwwww3zx3+Uxw3wzx2+3wzxx+Uww3wwzx3+3w2zxxzx+3Uxwww2zx2+Uwwzx3+3wzxxzx+wzxxx=f1tx+f2t,(2.2)

where w=dw/dz, w=d2w/dz2, and w=d3w/dz3. To reduce Equation 2.2 to an ordinary differential equation with respect to w(z), the derivatives of w(z) should be only functions of z and w. Moreover, when conducting normalization with a coefficient of w, namely, Uwzx3b(t), the coefficients of ww must satisfy

Uwzx3btΓ1w,z=btUwwzx3,(2.3)

where Γ1(w,z) is a function and can be determined as follows. From Equation 2.3, we have

Γ1w,z=UwwUw.

After an integration step, we obtain

Γ1w,zdw=lnUwlnβ0x,t,

where lnβ0(x,t) is the integral function. Letting lnΓ2(w,z)=Γ1(w,z)dw, we have

Γ2w,z=Uwβ0x,t.

After an integration process, we obtain

Γ2w,z=1β0x,tUα0x,t,(2.4)

where α0(x,t) is the function generated via integration. Let Γ3(w,z)=Γ2(w,z)dw; from Equation 2.4, we have that

U=β0x,tΓ3w,z+α0x,t.

Letting Γ3(w,z)=w(z), α0(x,t)=α(x,t), and β0(x,t)=β(x,t), we have

ux,t=αx,t+βx,twzx,t.(2.5)

Next, we compute α(x,t), β(x,t), and z(x,t). By substituting Equation 2.5 into Equation 2.2, we deduce that

btβzx3w+wbt3βxzx2+3βzxzxx+wβzt+atαβzx+dtβzx+bt3βxxzx+3βxzxx+βzxxx+wwatβ2zx+w2atββx+wβt+atαβx+αxβ+ctβ+dtβx+btβxxx+αt+atααx+αct+dtαx+btαxxxf1tx+f2t=0.(2.6)

For the above equation to reduce to a solvable equation with respect to w(z), the ratios of the coefficients w(z) and the derivatives of the equation must be dependent on z alone. This condition provides the relationships for α(x,t), β(x,t), and z(x,t), ensuring that any solution is a similarity reduction solution. Then, we introduce the following three footnotes (see [15]).

Remark 1. We adopt the coefficient of w (i.e., b(t)βzx3) as the normalizing factor and thus impose the condition that the other coefficients must take the form b(t)βzx3Γ(z), where Γ(z) is a function of z that needs to be determined.

Remark 2. Uppercase Greek letters are reserved for undetermined functions of z, ensuring that after performing operations (such as differentiation, integration, exponentiation, and rescaling), the result can still be denoted by the same letter. For example, the derivative of Γ(z) is denoted as Γ(z).

Remark 3. Three degrees of freedoms exist in the determination of α, β, z and w and can be exploited (without loss of generality) to keep the proposed method manageable:

(i) if α(x,t) is expressed as α=α0(x,t)+β(x,t)Ω(z), we can simplify it by setting Ω(z)=0, which is equivalent to performing the substitution w(z)w(z)Ω(z);

(ii) if β(x,t) is expressed as β=β0(x,t)Ω(z), we can simplify it by setting Ω(z)=1, which is equivalent to performing the substitution w(z)w(z)/Ω(z)];

(iii) if z(x,t) is determined by an equation with the form Ω(z)=z0(x,t), where Ω(z) is any invertible function, then we can take Ω(z)=z [by substituting zΩ1(z)].

The general similarity reduction of Equation 1.1 can be determined via this method.

For Equation 2.2 to be reduced to an ordinary differential equation in terms of w(z), the ratios of the various derivatives of w(z) must depend on the functions of w and z. When implementing normalization with the coefficient of w, namely, b(t)βzx3, the coefficients of ww must satisfy certain conditions.

btβzx3Γ4z=atβ2zx,

where Γ4(z) is a function to be determined. From Remark 3 (ii), we have

β=btatzx2.(2.7)

The coefficient of w2 requires that

btβzx3Γ5z=atββx,(2.8)

where Γ5(z) is a function to be determined. By substituting Equation 2.8 into Equation 2.7, we obtain

zx2Γ5z=2zxx.

From Remark 2, after applying a scale transformation, we have

zxΓ5z+zxxzx=0.

An integration step yields the following:

Γ5z+lnzx=Θt,

where Θ(t) is the integration function. From Remark 2, this can be exponentiated:

zxΓ5=Θt.

Integrating again gives

Γ5=xΘt+Σt,

where Σ(t) is another integration function. We obtain the following equation through Remark 3 (iii).

z=xθt+σt,(2.9)

where θ(t) and σ(t) are functions to be determined.

By substituting Equation 2.9 into Equation 2.7, we have that

β=btatθt2.(2.10)

With the coefficient of w, we have

btβzx3Γ6z=βzt+atαβzx+dtβzx+bt3βxxzx+3βxzxx+βzxxx.

where Γ6(z) is a function to be determined. From Equations 2.9, 2.10, we have

btθ3Γ6z=xdθdt+dσdt+atαθ+dtθ,

From Remark 3(i), we obtain

α=1atθxdθdt+dσdtdtat.(2.11)

Substituting Equations 2.92.11 into (Equation 2.2), we have

θ5b2tatw+ww+watbtθ2+2btθdθdtatbtθ2at2btθatdθdt+btctθ2at+1θxdθdt+dσdt+dt1atθdθdtct1atθxdθdt+dσdt+dtatxd2θdt2+d2σdt2atθ+xdθdt+dσdtdθdtat+atθθ2a2tdtatdtata2tf1tx+f2t=0.(2.12)

We proceed to transform Equation 2.12 into an ordinary differential equation for w(z). By using the coefficients of w and ww (i.e., θ5b2(t)a(t)), we deduce that the coefficients of w and w0 must satisfy

θ5b2tatγ1z=atbtθ2+2btθdθdtatbtθ2a2tbtθatdθdt+btctθ2at,(2.13)
θ5b2tatγ2z=1θxdθdt+dσdt+dt1atθdθdtct1atθxdθdt+dσdt+dtatxd2θdt2+d2σdt2atθ+xdθdt+dσdtdθdtat+atθθ2a2tdtatdtata2tf1tx+f2t,(2.14)

where γ1(z) and γ2(z) are functions to be determined. Since z=xθ(t)+σ(t) and the right-hand side of Equation 2.14 is linear in terms of x, we can assume that γ2(z)=Az+B, where A and B are constants. From Equation 2.14, we have that

θ5b2tatAxθ+σ+B=1θxdθdt+dσdt+dt1atθdθdtct1atθxdθdt+dσdt+dtatxd2θdt2+d2σdt2atθ+xdθdt+dσdtdθdtat+atθθ2a2tdtatdtata2tf1tx+f2t.(2.15)

By comparing the coefficients of x, we obtain

Aθ6b2tat=1atθd2θdt2+1a2tθ2dθdtdθdtat+atθ+1atθ2dθdt2ctatθdθdtf1t,(2.16)
θ5b2tatAσ+B=1atθd2σdt2+1a2tθ2dσdtdθdtat+atθ1a2tθ2dtatdtat+1θdθdt+dt1atθdθdt+ct1atθdσdtdtatf2t.(2.17)

Let

f1t=1atθ2A2+Aatθ+2A2ata2tθ2ActatθAθ6b2tat,(2.18)

and

f2t=θ5b2tatAσ+B+1a2tθ2BAat+atθ1a2tθ2dtatdtat+1θA+dt1atθA+ct1atθBdtat.(2.19)

It follows from Equations 2.18, 2.19, 2.16, 2.17 that

θ=At+A0,σ=Bt+B0,(2.20)

where A0 and B0 are integral constants. For the convenience of the calculation process, we assume that

atatbtbtθ=A+ctθAθ4bt.(2.21)

By substituting Equations 2.202.21 into Equation 2.13, we obtain γ1(z)=A. Then, substituting γ1(z)=A and γ2(z)=Az+B into Equation 2.12 yields

w+ww+Aw+Az+B=0,(2.22)

where A and B are arbitrary constants. Upon substituting Equations 2.92.11 and (Equation 2.20) into Equation 2.5, we can deduce that

u=btatAt+A02wz1atAt+A0xA+Bdtat,z=xAt+A0+Bt+B0,(2.23)

where w(z) satisfies Equation 2.22.

Next, we try to compute the exact solutions for Equation 2.22 based on the (G/G) expansion method. More precisely, we suppose that Equation 2.22 has solutions in the following form:

wz=i=1maizG/G,

where mN. To balance w and ww, we can take m=2, and then we have

wz=a0Z+a1zG/G+a2zG/G2,(2.24)

where G satisfies the following ordinary differential equation:

G+λG+μG=0,(2.25)

where λ and μ are constants. By substituting Equation 2.24 and Equation 2.25 into Equation 2.22 and comparing their coefficients, we deduce that

24a22a22=0,34a2+a1+10a2λ+6a224a2λ+a2a1a1λ2μa22a1a2=0,2a22a14λa2+3λa1+8a2μ+4a2λ24a2+2a1+10a2λ3λ4a2+2a1+10a2λ24a2μ2a0a2+a1a1a1λ2a2μ+a2a1λa12a2μ=0,a12a1λ4a2μ+a1λ2+6a2λμ+2a1μ+a22a14a2λ+3a1λ+8a2μ+4a2λ22λa22a14a2λ+8a2μ+4a2λ23μ4a2+2a1+10a2a0a1a1λ2a2μ+a1a1a1λ2a2μ+a2a0a1μ+Aa2=0,a12a1λ4a2μ+a1λ2+6a2λμ+2a1μλa12a1λ4a2μ+a1λ+6a2λμ+2a1μ2μa22a14a2λ+3a1λ+8a2μ+4a2λ2+a1a0a1μa0a1a1λ2a2μ+Aa1=0,a0a1μμa1a1λ2a2μμa12a1λ4a2μ+a1λ2+6a2λμ+2a1μ+Aa0+Az+B=0.

Then, we obtain

a0z=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z,a1z=6λ24μ22λ+3e2λ+3z,a2z=12.(2.26)

The following exact solution forms exist for Equation 2.22, and they can be acquired by substituting Equation 2.26 into Equation 2.24.

Case 1.If λ24μ>0, then

w1z=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3zλ24μ2A1coshλ24μ2z+A2sinhλ24μ2zA1sinhλ24μ2z+A2coshλ24μ2zλ212λ24μ2A1coshλ24μ2z+A2sinhλ24μ2zA1sinhλ24μ2z+A2coshλ24μ2zλ22.(2.27)

Case 2.If λ24μ<0, then

w2z=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3z4μλ22A1sin4μλ22z+A2cos4μλ22zA1cos4μλ22z+A2sin4μλ22zλ2124μλ22A1sin4μλ22z+A2cos4μλ22zA1cos4μλ22z+A2sin4μλ22zλ22.(2.28)

Case 3. If λ24μ=0, then

w3z=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3zA2A1+A2zλ212A2A1+A2zλ22.(2.29)

3 Conclusion

Substitute Equation 2.272.29 into Equation 2.23 and the following forms of similarity solutions exist for Equation 1.1.

Case 1. If λ24μ>0, then

u1x,t=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3zλ24μ2A1coshλ24μ2z+A2sinhλ24μ2zA1sinhλ24μ2z+A2coshλ24μ2zλ212λ24μ2A1coshλ24μ2z+A2sinhλ24μ2zA1sinhλ24μ2z+A2coshλ24μ2zλ22btatAt+A021atAt+A0xA+Bdtat.(3.1)

The similar solution corresponding to Case 1 is expressed in Figure 1.

The values determined for u1(x,t) when λ=1,μ=1,A1=100,A2=A=B=A0=B0=a(t)=b(t)=d(t)=1.

Case 2. If λ24μ<0, then

u2x,t=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3z4μλ22A1sin4μλ22z+A2cos4μλ22zA1cos4μλ22z+A2sin4μλ22zλ2124μλ22A1sin4μλ22z+A2cos4μλ22zA1cos4μλ22z+A2sin4μλ22zλ22btatAt+A021atAt+A0xA+Bdtat.(3.2)
Figure 1
www.frontiersin.org

Figure 1. The values determined for u1(x, t) when λ = 1, μ = −1, A1 = 100, A2 = A = B = A0 = B0 = a(t) = b(t) = d(t) = 1.

The similar solution corresponding to Case 2 is expressed in Figure 2.

Figure 2
www.frontiersin.org

Figure 2. The values determined for u2(x, t) when λ = 1, μ = 1, A1 = 100, A2 = A = B = A0 = B0 = a(t) = b(t) = d(t) = 1.

The values determined for u2(x,t) when λ=1,μ=1,A1=100,A2=A=B=A0=B0=a(t)=b(t)=d(t)=1.

Case 3. If λ24μ=0, then

u3x,t=11λ28μ+3λ12μ2μ6λ24μ2λ+3e2λ+3z+1+2λ2+3λ242λ+312λ48μ2e22λ+3z+6λ24μ22λ+3e2λ+3zA2A1+A2zλ212A2A1+A2zλ22btatAt+A021atAt+A0xA+Bdtat.(3.3)

The similar solution corresponding to Case 3 is expressed in Figure 3.

Figure 3
www.frontiersin.org

Figure 3. The values determined for u3(x, t) when λ = 2, A1 = 100, μ = A2 = A = B = A0 = B0 = a(t) = b(t) = d(t) = 1.

The values determined for u3(x,t) when λ=2,A1=100,μ=A2=A=B=A0=B0=a(t)=b(t)=d(t)=1.

According to the above discussion, the shape of the graphic is sensitive to the values of x and t. Indeed, we can clearly see the change trends exhibited by these three graphs, which are in exponential form. The constraints on the solution of the variable coefficient equation obtained by Method 1 are simple and less categorical than those of the previous article [26].

In the present work, we investigate the variable-coefficient forced KdV equation. As a result, this paper not only reduces the equation to an ordinary differential equation via the direct similarity reduction-based CK method but also obtains similarity solutions from the solutions of the above ordinary differential equation. This provides a simpler method for studying the variable-coefficient forced KdV equation. It simplifies the mathematical solution process and facilitates fluctuation control and application design in engineering practice. Many other variable-coefficient nonlinear partial differential equations can also be investigated via this method.

Data availability statement

The original contributions presented in the study are included in the article/supplementary material, further inquiries can be directed to the corresponding author.

Author contributions

JW: Conceptualization, Writing – original draft, Writing – review and editing. JF: Writing – review and editing, Visualization. JD: Visualization, Writing – original draft, Writing – review and editing.

Funding

The author(s) declare that no financial support was received for the research and/or publication of this article.

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Generative AI statement

The author(s) declare that no Generative AI was used in the creation of this manuscript.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

References

1. Tian SF, Zhang HQ. On the integrability of a generalized variable-coefficient forced Korteweg-de Vries equation in fluids. Stud Appl Math (2014) 132(3):212–46. doi:10.1111/sapm.12026

CrossRef Full Text | Google Scholar

2. Mohammed WW, Al-Askar FM. New stochastic solitary solutions for the modified Korteweg-de Vries equation with stochastic term/random variable coefficients. AIMS Math (2024) 9(8):20467–81. doi:10.3934/math.2024995

CrossRef Full Text | Google Scholar

3. Demiray H. The effect of a bump on wave propagation in a fluid-filled elastic tube. Int J Eng Sci (2004) 42(2):203–15. doi:10.1016/s0020-7225(03)00284-2

CrossRef Full Text | Google Scholar

4. Holloway PE, Pelinovsky E, Talipova T. A generalized Korteweg-de Vries model of internal tide transformation in the coastal zone. J Geophys Res C (1999) 104:18333–50. doi:10.1029/1999jc900144

CrossRef Full Text | Google Scholar

5. Yu X, Sun ZY, Zhou KW, Shen YJ. Spacial inhomogeneity and nonlinear tunneling for the forced KdV equation. Appl Math Lett (2018) 75:30–6. doi:10.1016/j.aml.2017.05.015

CrossRef Full Text | Google Scholar

6. Korteweg DJ, de Vries G. On the change of form of long waves advancing in a rectangular canal and on a new tipe of long stationary waves. Phil Mag 39(1895):422–43. doi:10.1080/14786449508620739

CrossRef Full Text | Google Scholar

7. Xu F. Application of exp-function method to symmetric regularized long wave (SRLW) equation. Phys Lett A (2008) 372:252–7. doi:10.1016/j.physleta.2007.07.035

CrossRef Full Text | Google Scholar

8. Demiray HL. Forced KdV equation in a fluid-filled elastic tube with variable initial stretches. Chaos Solitons Fractals (2009) 42(3):1388–95. doi:10.1016/j.chaos.2009.03.067

CrossRef Full Text | Google Scholar

9. Demiray HL. Weakly nonlinear waves in water of variable depth: variable-coefficient Korteweg-de Vries equation. Comput Math Appl (2010) 60(6):1747–55. doi:10.1016/j.camwa.2010.07.005

CrossRef Full Text | Google Scholar

10. Zhang CY, Yao ZZ, Zhu HW, Xu T, Li J, Meng XH, et al. Exact AnalyticN-soliton-like solution in wronskian form for a generalized variable-coefficient Korteweg-de Vries model from plasmas and fluid dynamics. Chin Phys Lett (2007) 24:1173–6. doi:10.1088/0256-307x/24/5/013

CrossRef Full Text | Google Scholar

11. Tian B, Wei GM, Zhang CY, Shan WR, Gao YT. Transformations for a generalized variable-coefficient Korteweg-de Vries model from blood vessels, Bose-Einstein condensates, rods and positons with symbolic computation. Phys Lett A (2006) 356(1):8–16. doi:10.1016/j.physleta.2006.03.080

CrossRef Full Text | Google Scholar

12. Khalique CM, Adeyemo OD, Monashane MS. Exact solutions, wave dynamics and conservation laws of a generalized geophysical Korteweg de Vries equation in ocean physics using Lie symmetry analysis. Adv Math Models Appl (2024) 9:147–72. doi:10.62476/amma9147

CrossRef Full Text | Google Scholar

13. Yu X, Gao YT, Sun ZY, Liu Y. Solitonic propagation and interaction for a generalized variable-coefficient forced Korteweg-de Vries equation in fluids. Phys Rev E (2011) 83:056601. doi:10.1103/physreve.83.056601

PubMed Abstract | CrossRef Full Text | Google Scholar

14. Bluman GW, Cole JD. The general similarity solution of the heat equation. J Math Fluid Mech (1969) 18:1025–42. doi:10.1512/iumj.1969.18.18074

CrossRef Full Text | Google Scholar

15. Clarkson PA, Kruskal MD. New similarity reductions of the Boussinesq equation. J Math Phys (1989) 30(10):2201–13. doi:10.1063/1.528613

CrossRef Full Text | Google Scholar

16. Gardner CS, Greene JM, Kruskal MD, Martin DK, Robert MM. Method for solving the Korteweg-de Vries equation. Phys Rev Lett (1967) 19(19):1095–7. doi:10.1103/physrevlett.19.1095

CrossRef Full Text | Google Scholar

17. Guo Q, Liu J. New exact solutions to the nonlinear Schrödinger equation with variable coefficients. Results Phys (2020) 16:102857. doi:10.1016/j.rinp.2019.102857

CrossRef Full Text | Google Scholar

18. Hirota R. Exact solution of the kortewegde Vries equation for multiple collisions of solitons. Phys Rev Lett (1971) 27(18):1192–4. doi:10.1103/physrevlett.27.1192

CrossRef Full Text | Google Scholar

19. Wu GC, Xia TC. A new method for constructing soliton solutions and periodic solutions of nonlinear evolution equations. Phys Lett A (2008) 372(5):604–9. doi:10.1016/j.physleta.2007.07.064

CrossRef Full Text | Google Scholar

20. Wu GC, Xia TC. Uniformly constructing exact discrete soliton solutions and periodic solutions to differential-difference equations. Comput Math Appl (2009) 58:2351–4. doi:10.1016/j.camwa.2009.03.022

CrossRef Full Text | Google Scholar

21. Wu GC. Uniformly constructing soliton solutions and periodic solutions to Burgers-Fisher equation. Comput Math Appl (2009) 58:2355–7. doi:10.1016/j.camwa.2009.03.023

CrossRef Full Text | Google Scholar

22. Wang ML, Li XZ, Zhang JL. The (G/G)-expansion method and travelling wave solutions of nonlinear evolution equations in mathematical physics. Phys Lett A (2008) 372(4):417–23. doi:10.1016/j.physleta.2007.07.051

CrossRef Full Text | Google Scholar

23. Adeyemo OD, Khalique CM, Gasimov YS, Villecco F. Variational and non-variational approaches with Lie algebra of a generalized (3+ 1)-dimensional nonlinear potential Yu-Toda-Sasa-Fukuyama equation in Engineering and Physics. Alexandria Eng J (2023) 63:17–43. doi:10.1016/j.aej.2022.07.024

CrossRef Full Text | Google Scholar

24. Koç DA, Gasimov YS, Bulut H. A study on the investigation of the traveling wave solutions of the mathematical models in physics via (m + (1/G))-expansion method. Adv Math Models Appl (2024) 9(1):5–13. doi:10.62476/amma9105

CrossRef Full Text | Google Scholar

25. Bluman GW, Cole JD. Similarity methods for differential equations. Berlin: Springer (1974).

Google Scholar

26. Lu DC, Hong BJ, Tian LX. Explicit and exact solutions to the variable coefficient combined KdV equation with forced term (2006). p. 5617–22.

Google Scholar

Keywords: forced KdV equation, direct similarity reduction-based CK method, variable coefficient, similarity solution, exact solution

Citation: Wang J, Fu J and Dai J (2025) Analytical solutions for the forced KdV equation with variable coefficients. Front. Phys. 13:1569964. doi: 10.3389/fphy.2025.1569964

Received: 02 February 2025; Accepted: 25 March 2025;
Published: 09 May 2025.

Edited by:

Jisheng Kou, Shaoxing University, China

Reviewed by:

Yusif Gasimov, Azerbaijan University, Azerbaijan
Segun Oke, Alabama A and M University, United States

Copyright © 2025 Wang, Fu and Dai. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Ji Wang, MTM5ODA1Nzk0NDlAMTYzLmNvbQ==

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.