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Importantly, the Y-L PINN method can directly solve the Young-Laplace equation with a discontinuous wetting boundary, eliminating the need for additional techniques. This work provides valuable insights for material wettability assessments, microstructure preparation, and advances in microfluidics research, ...
Experimentally measured FI flux when estimating the target scatterer’s x position (flux_theta_x sheet) and y position (flux_theta_y sheet). On both sheets, the first columns correspond to the x and y coordinates of the measurement point (in metres). The next two columns correspond to the...
Double–clickon thehorizontal axis. It will open theFormat Axisoptions on the right side of the sheet. Set theMinimumvalue to0andMaximumvalue to1.2in theBoundssection. PressEnter. Double–clickon thevertical axis. Set theMinimumvalue to0.3andMaximumvalue to0.65in theBoundssection. ...
One method for estimating the sediment transport from sheet andrill erosionis a loading function based on theuniversal soil loss equation(USLE) (11.1)A = R × K ×LS × C ×P, where A= soil loss (ton/acre–year), ...
First demonstration of an asymmetric kinetic equilibrium for a thin current sheet. Phys. Plasmas 20, 110702 (2013). Article ADS Google Scholar Allanson, O., Wilson, F., Neukirch, T., Liu, Y.-H. & Hodgson, J. D. B. Exact Vlasov–Maxwell equilibria for asymmetric current sheets. ...
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temperature distributions, electrostatic potentials, and fluid flow, to name just a few. The special case involving Laplace equation with satisfied boundary values is known as the Dirichlet problem. Solving Dirichlet problems is of paramount importance in applied mathematics, engineering, and physics. ...
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