Sentence examples for motion of soil from inspiring English sources

Working out the equation of surface of the mouldboard and using the analytical dependencies of the relative and absolute motion trajectories of the blade movement the mathematical models are received describing the patterns of motion of soil particles, at tillage with hulls with mouldboards of ripping type.

The response of the structure affects the motion of supporting soil and the movement of supporting soil influences the structural behaviour.

The motion of the soil is governed by Biot's dynamic poroelastic theory.

Those telltale vibrations are nothing like the motions of nearby soil or sticks that might be set humming by the waves.

The major cause of wind erosion is the jumping motion of the smaller soil particles, a process called saltation.

Open image in new window Fig. 5 Input sinusoidal wave sweep from 1 to 20 Hz at bedrock Open image in new window Fig. 6 Amplification of input motion at the surface of soil.

These findings reveal the importance of the asymmetric nature of the soil movement produced by mouldboard ploughing and the predominant effect of the lateral displacement dP on the actual trajectory of soil motion.

A general numerical model for the analysis of soil motion due to high-speed train passage and effects on nearby surface and underground structures is presented in this paper.

In contrast to the conventional method which deals with only a single ground motion for equivalent linearization of soil properties, a design response spectrum defined at the upper level (bottom of the surface ground) of an engineering bedrock can be handled as the target design earthquake in the present paper.

Note that for PGA > 200 cm/s2 or PGV > 20 cm/s, F p under strong motion becomes much smaller than under weak motion at most sites, representative of soil nonlinearity.

Note that fNL could not be identified at four sites (51MXT, 51XJD, 62SHW, and 62WIX) because of the small difference of the HVSR during strong and weak motions, implying the absence of soil nonlinearity.