Experimental research on the chemical composition of hydroxyapatite in bones
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F13%3A00071842" target="_blank" >RIV/00216224:14310/13:00071842 - isvavai.cz</a>
Výsledek na webu
<a href="http://www.geopilsen2013.com/" target="_blank" >http://www.geopilsen2013.com/</a>
DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Experimental research on the chemical composition of hydroxyapatite in bones
Popis výsledku v původním jazyce
In the mineral structure of OHAp numerous substitutions may occur which cause changes in physical processes in OHAp. Bioapatite in fossil teeth and bone tissue can be highly affected by the character of natural environment, especially by the mineralogy,geochemistry, and hydrology of the rock background. Dissected samples of turtle humerus (Testudo graeca) were used for experiment. Several samples of bone tissue remained with collagen, while the other were deproteinated. Numerous simulation experimentswere realised (fresh samples vs. deproteinated samples immersed in solutions of Ba, Sr and Zn) to determine the ability of selected elements to incorporate in the bone tissue and/or the structure of bioapatite. The samples were analysed by the method ofelectron microprobe and X-ray diffraction. The crystallinity of deproteinated bone is slightly higher due to the lower content of organic components (e.g. collagen).
Název v anglickém jazyce
Experimental research on the chemical composition of hydroxyapatite in bones
Popis výsledku anglicky
In the mineral structure of OHAp numerous substitutions may occur which cause changes in physical processes in OHAp. Bioapatite in fossil teeth and bone tissue can be highly affected by the character of natural environment, especially by the mineralogy,geochemistry, and hydrology of the rock background. Dissected samples of turtle humerus (Testudo graeca) were used for experiment. Several samples of bone tissue remained with collagen, while the other were deproteinated. Numerous simulation experimentswere realised (fresh samples vs. deproteinated samples immersed in solutions of Ba, Sr and Zn) to determine the ability of selected elements to incorporate in the bone tissue and/or the structure of bioapatite. The samples were analysed by the method ofelectron microprobe and X-ray diffraction. The crystallinity of deproteinated bone is slightly higher due to the lower content of organic components (e.g. collagen).
Klasifikace
Druh
O - Ostatní výsledky
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/ED1.1.00%2F02.0068" target="_blank" >ED1.1.00/02.0068: CEITEC - central european institute of technology</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů