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Studying of crystallization with participation synovial of the liquid of the person
- Source :
- Vestnik Otdelenia nauk o Zemle RAN. 3:1-7
- Publication Year :
- 2011
- Publisher :
- Geophysical Center of the Russian Academy of Sciences, 2011.
-
Abstract
- In live organisms of biological liquids are formed various органоминеральные units (a bone and tooth fabric, nephritic, salivary and scales in a human body etc.). It is known that the major property of any liquid is its viscosity. Viscosity renders a great influence for speed of movement of a liquid, resistance which it renders to particles at their moving, thereby defines a direction and intensity of many biochemical reactions, including processes of formation of mineral phases in vivo. Change is viscous – elastic properties influences a number of physical and chemical parametres of biological system, affects speed of the chemical reactions proceeding in bioliquids. Such bioliquid is synovial a liquid (SL, synovial) the person, it is one of the basic components of a joint and substantially defines its morfo-functional condition, carries out the important role in realisation of functions of a joint and maintenance of its communication with other fabrics. The key characteristic of the given bioliquid is its viscosity which provides normal mobility of a joint, reduces a friction and provides functional congruence. Viscosity синовии considerably fluctuates depending on рН, concentration of salts, temperatures. In comparison with other bioliquids viscosity synovial liquids is high enough [Veresov, etc., 2004,], in communication, with what the purpose given work is the establishment of influence of viscosity of modelling solution synovial on processes of a bone mineralization. According to earlier spent thermodynamic calculation [Lemeshev, 2010], it is shown that within the limits of the chosen thermodynamic model in an investigated range рН in solutions probably formation of following substances (tab. 1): Са10 (РО4) 6 (IT) 2, β-Ca3 (РО4) 2, MgHPO4·3Н2О, Ca4H(РО4)3·2.5Н2О, СaHРО4·2Н2О, CaCO3-kaltsit, CaCO3-aragonite, α-Ca3 (РО4) 2. Thus for each system of value рН the sedimentation beginnings slightly soluble connections are various.
Details
- ISSN :
- 18196586
- Volume :
- 3
- Database :
- OpenAIRE
- Journal :
- Vestnik Otdelenia nauk o Zemle RAN
- Accession number :
- edsair.doi...........3e6dc0abf0a5430ca88be1bcc730f7c5
- Full Text :
- https://doi.org/10.2205/2011nz000150