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Application of a second order accurate finite-difference method to problems of diffraction of elastic waves by gradient layers for the boundary-value problem describing diffraction of elastic waves by gradient isotropic and transversely
The Optical Path Method for the Problem of Oblique Incidence of a Plane Electromagnetic Wave on a Plane-Parallel Scatterer of radiation on a plane-parallel scatterer. For such problems, an approximate method of integrating the Maxwell
Conjugate of Natural Bacteriochlorin with Doxorubicin for Combined Photodynamic and Chemotherapy of chemotherapeutic agents limits the possibilities of this method, making it necessary to search for new approaches
Second-Order Accurate Finite-Difference Scheme for Solving the Problem of Elastic Wave Diffraction by the Anisotropic Gradient Layer differential equations of the given form. The finite-difference scheme is obtained by the method
Body size variation of ground beetles (Coleoptera: Carabidae) in latitudinal gradient shape variation in latitude gradient in studied species of Ground Beetles. Material and methods: Six
Modern software capabilities for shape optimization of shells three gradient-based methods: IPOPT (Interior Point OPTimizer), SNOPT (Sparse Nonlinear OPTimizer
An exact analytical solution of an R-linear conjugation problem for a n-phased concentric circular heterogeneous structureAn exact analytical solution of an R-linear conjugation problem for a n-phased concentric circular
Direct realization of the pseudospectral method of calculating waveguide modeOften in the applied problems of integrated optics we use regular open gradient (general) planar
Easily implementable iterative methods for variational inequalities with nonlinear diffusion-convection operator and constraints to the gradient of solution-convection operator and constraints to the gradient of solution. Implementation of every iteration of these methods
Diffraction of a plane elastic wave by a gradient transversely isotropic layerThe problem of diffraction of a plane elastic wave by a gradient transversely isotropic layer
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