A Novel Neural Network-Based Symbolic Approach for Shallow-Water Waves with Surface Tension
Abstract
1. Introduction
2. Methodology and Algorithm
- Model I:In this context, denotes the weight that connects entry x to the i-th neuron of the hidden layer, while represents the weight that connects entry t to the same i-th neuron. Furthermore, represents the weight connecting each neuron in the hidden layer to the test function u (); ultimately, each denotes the biases.
- Model II:In this context, denotes the weight that connects entry x to the i-th neuron of the first hidden layer, while represents the weight that connects entry t to the same i-th neuron. The connection weights and , where , are for the first and second neurons in the first hidden layer and their links to the third and fourth neurons in the second hidden layer. Furthermore, represents the weight connecting each neuron in the second hidden layer to the test function u (); ultimately, each denotes the biases.
- Step 2: The neural network uses the R-function, derived as the solution to Equation (5), and some algebraic powers of it as the activation function in the first hidden layer.
- Step 4: By combining like terms of the algebraic equation, extracting the coefficients, and setting all coefficients to zero, we obtain an underdetermined system of nonlinear algebraic equations. This system requires careful analysis to identify potential solutions.
- Step 5: The derived system of nonlinear algebraic equations is computationally solved by using symbolic computation software. Examples of such software include Mathematica or Maple.
3. The Sixth-Order Boussinesq Equation
4. Adoption of the Suggested Methodology to Solve the 6BE
4.1. Solutions Using Model-I
4.2. Solutions Using Model-II
5. Visual Representation of Solutions
| Case | Value of m | Parameters | Type of Surface | Description |
|---|---|---|---|---|
| 1.1 | 5/2 | , , , , , , , , | Solitary wave | Figure 4 illustrates the solitary wave type corresponding to solution given by Equation (11). Solitary wave propagation is characterized by its stability and persistence over time. |
| 1.2 | 3/4 | , , , , , , , | Solitary wave | Figure 5 illustrates the solitary wave type corresponding to solution given by Equation (14). |
| 1.3 | 3/2 | , , , , , , | Shock wave (kink-type soliton) | Figure 6 illustrates the shock wave type corresponding to solution given by Equation (17). Shock wave propagation can be observed as it interacts with the surrounding medium, resulting in distinct changes in pressure and density profiles. |
| Case | Value of m | Parameters | Type of Surface | Description |
|---|---|---|---|---|
| 2.1 | 3/4 | , , , , , , , | Solitary wave | Figure 7 illustrates the solitary wave type corresponding to solution given by Equation (21). |
| 2.2 | 3/2 | , , , , , , , , | Shock wave (kink-type soliton) | Figure 8 illustrates the shock wave type corresponding to solution given by Equation (24). |
| 2.3 | 5/2 | , , , , , , , , | Solitary wave | Figure 9 illustrates the solitary wave type corresponding to solution given by Equation (27). |






6. Discussion of Results
- Figure 4 provides a visual representation of the solution derived from Equation (11), based on the parameters specified in Case 1.1 of Table 2. This case demonstrates that, when dispersion and surface tension have the same sign, the wave surface displays a low amplitude. The weights , , and regulate the temporal scaling of the soliton pulse width. The constraint inversely influences the propagation velocity in relation to the surface tension coefficient and directly depends on the nonlinearity coefficient c. Additionally, the constraint has a slight impact on the wave dispersion axis, which is directly proportional to the product of the dispersion coefficient and the surface tension coefficient . Furthermore, the wave amplitude is affected by the constraint .
- Figure 5 presents a visual representation of the solution derived from Equation (14), based on the parameters specified in Case 1.2 of Table 2. This case demonstrates that a sign change in a surface tension parameter leads to a significant increase in the surface level amplitude of the waves. The weight governs the temporal scaling of the soliton pulse width, while the surface tension parameters and influence the wave height. The constraints on the weights and impact the inclination of the wave axis in direct proportion to the dispersion and surface tension coefficients, respectively. Additionally, the constraint signifies that the wave amplitude is directly affected by the surface tension coefficient . Finally, the constraint indicates that the propagation speed is reduced in proportion to both and c.
- Figure 6 illustrates the shock wave type corresponding to the solution given by Equation (17), based on the parameters specified in Case 1.3 of Table 2. Shock wave propagation can be observed as it interacts with the surrounding medium, resulting in distinct changes in pressure and density profiles. This case shows how nonlinear power affects waveform shape. The weight and the value of c determine the kink-type shape of the shock wave. Meanwhile, the surface tension parameters and influence the wave height. The constraints on the weights and affect the slope of the wave axis in direct proportion to the value of the wave number; furthermore, the constraint also affects the axis of evolution in proportion to the coefficient of the surface tension parameter . The constraint decreases the speed of evolution inversely proportional to the dispersion coefficient . Finally, the wave velocity is affected in inverse proportion to the surface tension coefficient through the constraints on the weights and .
- Figure 7 illustrates the solitary wave type corresponding to the solution given by Equation (21) based on the parameters outlined in Case 2.1 of Table 3. The selection of surface tension and dispersion parameters results in the wave traveling to the right over time while sustaining a large amplitude. The weights and , combined with the signs of and , determine the amplitude of the wave. Meanwhile, the surface tension parameters and control the wave height. The constraint governs the inclination of the line of evolution in direct proportion to the dispersion and surface tension coefficients and , respectively. Additionally, the constraint indicates that the dispersion velocity is directly proportional to the surface tension coefficient .
- Figure 8 illustrates the type of shock wave corresponding to the solution provided by Equation (24) based on the parameters outlined in Case 2.2 of Table 3. Due to the selection of the nonlinearity power, these waves manifest as stable solitary solutions that converge to a constant value at infinity. The parameters , along with the values of k and c, determine the kink-like shape of the shock wave. Additionally, the surface tension parameters and affect the height of the wave. The slope of the wave axis arises from the constraint , indicating that it is proportional to the dispersion coefficient and the nonlinearity coefficient c. The constraints and govern the dispersion velocity of the wave, which is directly proportional to the dispersion coefficient and the surface tension coefficient .
- Figure 9 illustrates the type of solitary wave corresponding to the solution provided by Equation (27), based on the parameters specified in Case 2.3 of Table 3. The chosen surface tension and dispersion parameters lead to the wave traveling to the right over time while maintaining a low amplitude. The weights and , along with the signs of and , dictate the wave’s amplitude. Meanwhile, the surface tension parameters and control the wave height. The restriction influences the wave’s axis of development, which is directly proportional to the spatiotemporal dispersion coefficient and the surface tension coefficient . Additionally, the relationships and suggest that wave velocity is directly proportional to both and , while it is inversely proportional to the nonlinearity coefficient c and the surface tension coefficient , respectively.
7. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
Appendix A. Algebraic System Corresponding to Case 1.1
Appendix B. Symbolic Verification of the Solution u1.1 to Case 1.1
Appendix C. The Activation Functions in the Methods Presented in [33,34,35,36,37,38]
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González-Gaxiola, O.; Hart-Simmons, M.; Ahmed, H.M.; Biswas, A. A Novel Neural Network-Based Symbolic Approach for Shallow-Water Waves with Surface Tension. Fluids 2026, 11, 100. https://doi.org/10.3390/fluids11040100
González-Gaxiola O, Hart-Simmons M, Ahmed HM, Biswas A. A Novel Neural Network-Based Symbolic Approach for Shallow-Water Waves with Surface Tension. Fluids. 2026; 11(4):100. https://doi.org/10.3390/fluids11040100
Chicago/Turabian StyleGonzález-Gaxiola, Oswaldo, Milisha Hart-Simmons, Husham M. Ahmed, and Anjan Biswas. 2026. "A Novel Neural Network-Based Symbolic Approach for Shallow-Water Waves with Surface Tension" Fluids 11, no. 4: 100. https://doi.org/10.3390/fluids11040100
APA StyleGonzález-Gaxiola, O., Hart-Simmons, M., Ahmed, H. M., & Biswas, A. (2026). A Novel Neural Network-Based Symbolic Approach for Shallow-Water Waves with Surface Tension. Fluids, 11(4), 100. https://doi.org/10.3390/fluids11040100

