The collection of analytical and experimental data makes it possible to consider the existence of three common scientific principles for solid body consolidation to be proved. One of them, the identity principle, formulates the degree of generality between properties and the behavior of a porous, consolidating or consolidated body, and a normal body; two others, i.e. the principle of self-regulation and the transmission principle, formulate features of the properties and behavior of powder bodies. The identity principle may be formulated as follows. The properties and behavior of any compact element of a porous body are the same as for the substance of a compact pore-free body with the condition of an identical chemical composition, degree of strain hardening, and test conditions. The self-regulation principle may be formulated as follows. During consolidation there are processes of non-self-regulation (intraparticle, consolidating, increasing and fixing the contacts and equilibrium) loading deformation and self-regulating (intraparticle, deconsolidating, reducing and breaking contacts and body equilibrium) unloading deformation; non-self-regulation consolidating deformation increases, and self-regulation deconsolidating deformation reduces compaction resistance; flow of particles substance is intermediate in nature between entirely continuous and entirely localized flow in contact areas. The greater the degree of consolidation, the lower is the level of self-regulation for its processes. The transmission principle may be formulated as follows. Consolidating stresses applied to a consolidating self-regulating body are transmitted by their elastic balancing in a continuous critical zone lying entirely within the solid phase of a body with equally large interparticle (contact) and intraparticle (critical) sections normal to the loading direction. These stresses and elastic loading are only transmitted through fixed, and not through broken, contact sections at this instant of consolidation, and consequently through fixed critical sections in a fixed critical zone.