Open AccessHIERARCHIC SKELETAL ORGANIZATION - A FACTOR REGULATING THE STRUCTURE OF FATIGUE INJURIES. PART II. HYPOTHETICAL MODEL OF FORMATION AND DISTRUPTION OF BONDS BETWEEN CRYSTALLITE ASSOCIATIONS
Author(s) -
А. С. Аврунин,
Р М Тихилов,
Л. К. Паршин,
Boris E. Melnikov
Publication year - 2010
Publication title -
travmatologiâ i ortopediâ rossii
Language(s) - English
Resource type - Journals
eISSN - 2542-0933
pISSN - 2311-2905
DOI - 10.21823/2311-2905-2010-0-1-48-57
Subject(s) - crystallite , mineralization (soil science) , geology , materials science , chemistry , crystallography , soil science , soil water
The authors discuss the questions concerning local structural-temporal changes in skeletal mineralization degree, local hyper-mineralization, the role of the spatial gradient of skeletal mineralization in forces distribution during locomotion, microstructural distribution of crystallite associations, ultrastructural mineral matrix transformation in the process of its formation. Hypothetical mechanisms of joining crystallite associations into a unified mineral complex are suggested; a hypothetical spatial structure of junction formation between the nearest crystallite associations is described, as well as a supposed schema of mineral massif destruction and restoration of disrupted connections.