The experimental implementation of split-lens configurations carry the difficulty of physically fabricating the different lens sectors with sufficient quality and precision.
The generation of the light structures is based on the implementation of split-lens schemes, which allow us to vary some spatial properties of the light-cavities just by modifying some control parameters of simple physical interpretation.
A new implementation of the split-operator method for calculating the time-evolution of Dirac wave functions is presented.
The main part of the code presented in this work represents an implementation of the split-operator method [J.A. Fleck, J.R. Morris, M.D. Feit, Appl. Phys. 10 (1976) 129 160; R. Heather, Comput. Phys. Comm. 63 (1991) 446] for calculating the time-evolution of Dirac wave functions.
The design and implementation of a split-plot experimental test-matrix provided a mechanism for addressing the existing technical randomization restrictions of ex vivo ultrasonic scalpel performance testing, while preserving the ability to examine the potential effects of independent factors or variables.
From this investigation, it was determined that the design and implementation of a split-plot experimental test-matrix provided a mechanism for addressing the existing technical randomization restrictions in a statistically meaningful way, while preserving the ability to examine the potential combinatorial effects of independent factors or variables that can be assessed in ex vivo testing.
The data segmentation is in fact the implementation of the function split, where H = split ( D ) (3). = ( d 1, d 2, …, d n ) (4).
The implementation of multi-stage splitting integrators is essentially the same as the implementation of the familiar Strang/Verlet method.
A parallel implementation of the Shardlow splitting algorithm (SSA) for Dissipative Particle Dynamics (DPD) simulations is presented.
Here, a new fourth-order implementation of the Fourier split-step algorithm is described for problems possessing azimuthal symmetry in 3 + 1-dimensions.
The present paper addresses the practical implementation of such a splitting for the case of isopycnic ocean modeling, in which the vertical coordinate is density or some other related quantity.
