{"title":"[Microprobe study of bones in the determination of individual age].","authors":"F Kósa, I Farkas, G Wittman","doi":"","DOIUrl":null,"url":null,"abstract":"<p><p>Potassium and phosphorus levels and the Ca: P ratio were determined in autopsy material taken from the compact bone substance of the right femur of 25 individuals of various age and either sex. Studies were made under a Tesla BS-300 scanning electron microscope connected to an EDAX-149-10 X-ray detector and a BMG-38100 X-ray analyser using 15 kV accelerating voltage, 100 pA test-current and 20 s measuring time. Different bone substances (lamellae, Haversian canals, interstitial bone) showed similatr Ca: P ratios (p greater than 0.05). However, mean mol-ratio was found to decrease with age and this was still significant (p greater than 0.05) at 95% level. The equation of the regression line was: y = -0.0013x + 1.8275, where y represents Ca: P ratio x the age. There was a close correlation between the molar ratio of Ca and P which enables this method to be applied for the assessment of individual age in forensic medicine and paleoanthropology.</p>","PeriodicalId":19047,"journal":{"name":"Morphologiai es igazsagugyi orvosi szemle","volume":"29 3","pages":"227-32"},"PeriodicalIF":0.0000,"publicationDate":"1989-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Morphologiai es igazsagugyi orvosi szemle","FirstCategoryId":"1085","ListUrlMain":"","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Potassium and phosphorus levels and the Ca: P ratio were determined in autopsy material taken from the compact bone substance of the right femur of 25 individuals of various age and either sex. Studies were made under a Tesla BS-300 scanning electron microscope connected to an EDAX-149-10 X-ray detector and a BMG-38100 X-ray analyser using 15 kV accelerating voltage, 100 pA test-current and 20 s measuring time. Different bone substances (lamellae, Haversian canals, interstitial bone) showed similatr Ca: P ratios (p greater than 0.05). However, mean mol-ratio was found to decrease with age and this was still significant (p greater than 0.05) at 95% level. The equation of the regression line was: y = -0.0013x + 1.8275, where y represents Ca: P ratio x the age. There was a close correlation between the molar ratio of Ca and P which enables this method to be applied for the assessment of individual age in forensic medicine and paleoanthropology.