In this contribution a new procedure for parameter identification for the material characterisation of rubber blends is proposed which is based on genetic algorithms. Such a model has to consider the effect of wall slippage on the viscous properties as well as the identification of a new material parameter regarding die swell. As basis serves an experimental investigation of the viscous propert...

Abstract Between 5% and 25% of the total momentum transferred between atmosphere ocean is transmitted via growth long surface gravity waves called “swell.” In this paper, we use large-eddy simulations to show that swell-transmitted excites near-inertial drives turbulent mixing deepens a rotating, stratified, boundary layer. We find currents are less effective at producing turbulence layer than ...

abstract: one the most important problems in recent sensitive loads is the quality of voltage. for this challenge custom power devices are used in distribution systems. dynamic voltage restorer (dvr) is a custom power device that improves voltage, decrease power distortion, filter harmonics and balance distributed generations (dgs) with low voltage distribution system. in this paper, a new algo...

Abstract Growing application of artificial intelligence in geotechnical engineering has been observed; however, its ability to predict the properties and nonlinear behaviour reactive soil is currently not well considered. Although previous studies provided linear correlations between shrink–swell index Atterberg limits, obtained model accuracy values were found unsatisfactory results. Artificia...

The molecular identity of the channels producing swelling-activated Cl conductance (g swell) is of great interest since this physiologic response to swelling is common to many cells. the question of whether the observed g swell represents a family of channel proteins is presently unanswered, but to be included in this family a channel must be activated by cell swelling and conduct Cl. Determini...

[1] A long-standing question in geodynamics is the cause of deviations of ocean depth or seafloor topography from the prediction of a cooling half-space model (HSC). Are the deviations caused entirely by mantle plumes or lithospheric reheating associated with sublithospheric small-scale convection or some other mechanisms? In this study we analyzed the age and geographical dependences of ocean ...