A method for detecting anomalies of Earth's gravitational field in laboratory WORKS

摘要

1.method u0432u044bu00a0u0432u043bu0435u043du0438u00a0 anomalies of gravitational earth u043fu043eu043bu00a0 (apps) in the laboratory work, based on the use of at least one outer ap parata (ka), u043du0430u0445u043eu0434u00a0u0449u0435u0433u043eu0441u00a0 in orbit measurement of coordinates and velocities u0434u0432u0438u0436u0435u043du0438u00a0 centre of gravity, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0, further u0438u0437u043cu0435u0440u00a0u044eu0442 coordinates and velocity. u0438u0436u0435u043du0438u00a0 centre of gravity, with a significantly greater mass, for example.u043eu0442u0434u0435u043bu0438u0432u0448u0435u0439u0441u00a0 part of the last stage of the launch u043du043eu0441u0438u0442u0435u043bu00a0 (- rn), u0434u0432u0438u0436u0443u0449u0435u0439u0441u00a0 on the same orbit, u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 u043fu043eu0441u0442u043eu00a0u043du043du0443u044e total energy (in) each j th point interval, ism u0435u0440u0435u043du0438u0439 t u0434u043bu00a0 each i-th ka (hu043au0430ij) and mos ph hu043eu0447u0440Hj formula;where v = (Vx2 + Vy2 + V2z) 0.5 (r = (x2 + Y2 + z2) 0.5.;- u0433u0440u0430u0432u0438u0442u0430u0446u0438u043eu043du043du0430u00a0 u043fu043eu0441u0442u043eu00a0u043du043du0430u00a0 (u0434u043bu00a0 spherical models of the earth = 398602105 km3 / s2);;Vx, check, Vz, x, y, z is measured the actual speed and position the center of gravity of each i-th ka and mos ph, respectively, for each j in the interval of measurements of t, where;i = 1 i think... - number ka of the laboratory work.;mr. j = 1, the number of points on the interval u0438u0437u043cu0435u0440u0435u043du0438u00a0 t, in which u043fu0440u043eu0432u043eu0434u00a0u0442u0441u00a0 u0438u0437u043cu0435u0440u0435u043du0438u00a0, and, in u043fu043eu00a0u0432u043bu0435u043du0438u0438 u043du0430u0440u0443u0448u0435u043du0438u00a0 u0443u0441u043bu043eu0432u0438u00a0 u043fu043eu0441u0442u043eu00a0u043du0441u0442u0432u0430 (1), u043du0435u0441u043eu0432u043fu0430u0434u0435u043du0438u00a0 calculated values in u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 gravitational parameter values ij u0434u043bu00a0 each i-th ka and mos ph, j - x points, of the formula (1).;u0441u043eu0441u0442u0430u0432u043bu00a0u044eu0442 u0443u0441u0440u0435u0434u043du0435u043du043du0443u044e difference values of parameter;and identify the station as anomalous, and the ij identify as additional gravitational disturbance capacity of the u043fu0440u0438u0442u00a0u0436u0435u043du0438u00a0 apps.;2. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that the location of the anomalies in the orbit u0434u0432u0438u0436u0435u043du0438u00a0 ka u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 of u0443u0441u043bu043eu0432u0438u00a0 u043du0430u0440u0443u0448u0435u043du0438u00a0 u0443u0441u043bu043eu0432u0438u00a0 u043fu043eu0441u0442u043eu00a0u043du0441u0442u0432u0430 (h = v2 - 2 / rconst and length from the u0443u0441u043bu043eu0432u0438u00a0 u043fu0440u0435u043au0440u0430u0449u0435u043du0438u00a0 u0432u043eu0437u0434u0435u0439u0441u0442u0432u0438u00a0 gravity u0432u043eu0437u043cu0443u0449u0435u043du0438u00a0). u043eu0431u043du0443u043bu0435u043du0438u00a0 ij = 0.