EVOLUTION OF VENUS IN THEORETICAL PLANETOLOGY
The Empirical Theory of Universe (ETU) is formulated for the description of solar system on the basis of existing theories of a field. Three new fundamental constants for ETU are calculated on the observant data of body’s Solar system. The received simple properties of the universe are based theoretical planetology. The problem of theoretical planetology will consist in an establishment of laws evolution of planets with atmospheres under modern characteristics of Venus, the Earth and Mars. The linear increase in the linear sizes of bodies and results spaces in very dynamical evolution of parameters planets. The affinity of Venus to the Sun has led to a heat on its surface. The big radius of Venus has led to low pressure of an atmosphere. The temperature and pressure are compared to values of critical point water. Water on Venus and through 4 billion years will not appear. Now Venus is interesting by the beginning of formation an oceanic bark. The age of the most ancient minerals is estimated in 2.23 billion years.