The collision of polymer composite parts with a steel hammer is simulated using grid-characteristic method. To verify the method a comparison with analytics for distribution of spherical explosion in a homogeneous medium is given. The potential fracture zones in composite parts are analyzed.
By means of mathematical two-dimensional nonstationary model mechanisms of formation of longitudinal effect in a middle-latitude ionosphere are probed and is shown that one of main engines is the thermosphere wind in combination with earth magnetic field geometry. Model calculations of dependence of longitudinal effects in middle-latitude F-area from levels of geomagnetic and solar activity are carried out. It is shown that with increase in a geomagnetic disturbance the behavior of electronic concentration as a whole corresponds to the negative phase of a substorm. However, in some longitudinal sectors increase of electronic concentration that is explained by hobby of ionospheric plasma for a termosphere wind is watched. Thus DYE amplitude is supervised by changes of absolute value, amplitude and a phase of longitudinal profiles of the meridional and zonal components of speed of a neutral wind. To growth of solar activity there is an increase in electronic concentration in a maximum of F2 of a layer, also inc reases hmF2.
It was considered a two-dimensional model of the interaction of a charged micro satellite and thermal plasma. The method of molecular dynamics used as a modeling method. Ion concentration distributions near SC were calculated for 10 and 102 protons in cm2 and the two values of relative satellite velocity and plasma were considered — 8 and 20 km s-1, respectively. It is shown that an increase in velocity and concentration of particles of ion shadow behind the satellite becomes more expressed.
A numerical model of equatorial F-layer of ionosphere on simulating of ionosphere irregularities with object scale from 1 km during to the instability development is constructed.
The restoration factor is experimentally defined at blow of ball about a motionless oblique surface. It is shown that the restoration factor is function of an angle of slope.