EARTH MULTISCALING PROCESSES: ACTUAL INTERACTION BETWEEN DYNAMIC PARAMETER SYSTEMS AND SYSTEMS OF HETEROGENEOUS MATERIAL BEHAVIOR

In order to understand the current dynamic processes presentable database from well explored different scale fields of the world has been comparably investigated. We have revealed that multisystem mechanisms depend on certain connected systems shown on the empirically created diagram. The first is an octave system of material parameter groups interaction. It consists of the most important dynamic parameter groups divided into initial energy-forming C-G-P-T and derivative power controlling t-r-p-v classes, where C-is composition, G-gravity, P-pressure, T-temperature, t-timing, r-relief of key surfaces, p-permeability, v-viscosity. Each of the parameter groups involves some measurements closely associated with the key parameters. So, t is also velocity and trends of processes. Qualitative changing of the parameters is marked by types of the lines. The next is space-time system of heterogeneous geomaterial fields, scaling from mineral to global and displaying on the diagram as windows 1-4, contoured by lines of its dominant parameters influencing similar to thosecould be seen on a P-T-t-v paths of window-1.Using the four types of the three-dimensions seems to be a practical application of 4 of 8 octants into which euclidean space can be divided. Each of the fields hasits own formats for timing of key events and surfaces correlation as well as mass material composing and behavior control. These lead to form two other systems. Global timing formats system /external doted line 1-4/ and material mass moving system /inner around arrows 1-4/. Processes 1-4 proceed under impact of solar space-time-5.