EGU23-122, updated on 22 Feb 2023
https://doi.org/10.5194/egusphere-egu23-122
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Harmonic dynamic of the Earth (C)

xianwu xin
xianwu xin
  • Anshan city qianshan district government, qianshan district science and technology bureau, China. (xinxianwu@126.com)

Abstract.

In this paper, the physical simulation of the meridional movement of the crust is carried out by experiments; According to the geometry relationship between the peak point of the earth's crust and the earth's rotation under the action of tidal force, a mathematical model of the meridional movement of the crust is established. The velocity field of global continental drift is calculated using the meridional motion equation derived from the model, and is compared with the measured value of ITRF2000. It can be seen from the comparison between adjacent calculated values and measured values that the magnitude and direction of the two velocity vectors are basically the same. It follows that the meridional movement of the crust is a reciprocating harmonic movement. The continent and the ocean floor, under the action of the reciprocating harmonic dynamic process, float back and forth along the meridian. Due to the difference between forward and reverse resistance, there will be fixed displacement in one direction. So far, the series of papers on "Harmonic dynamic of the Earth (C)" have completed the kinematic analysis, driving force calculation, energy conversion calculation and verification of observation results of the earth harmonic dynamic process. Velocity field, driving force and energy consumption are the three basic indicators of mechanical power process. Many possibilities of geophysical evolution mechanism determine that the study of its main dynamic mechanism is inseparable from the detailed discussion of the three major indicators.

How to cite: xin, X.: Harmonic dynamic of the Earth (C), EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-122, https://doi.org/10.5194/egusphere-egu23-122, 2023.

Supplementary materials

Supplementary material file