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  • Bone mineral density in children in different age periods

    Редакция | 2013, Original articles, Practical medicine 06 (13) Pediatrics | 25 ноября, 2013

    S.V. MALTSEV, G.Sh. MANSUROVA, T.V. KOLESNICHENKO, N.A. ZOTOV
    Kazan State Medical Academy

    Maltsev  Stanislav Viktorovich
    Doctor of Medical Science, Professor, Head of the department of Pediatrics with a course of polyclinic pediatrics
    18 Volkova Str., Kazan 420012
    tel. (843) 236-96-88, e-mail: maltc@mail.ru 

    The article presents the results of a study of bone mineral density in children aged 0 to 18 years, conducted by dual-energy X—ray absorptiometry (DXA), X-ray densitometry using a computer analysis program of film radiographs (XRay Analysis) and quantitative ultrasound. Reduced bone mineral density in children was found in all age groups, the largest deviations were set at tender age and puberty.

    Key words: bone mineral density in children, osteopenia in children, osteoporosis.

     

    REFERENCES

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    3. Korovina N.A., Svincickaja V.I. Varianty osteopenij pri tubulointersticial’nyh zabolevanijah pochek u detej // Pediatrija. — 2010. — № 6. — S. 12-16.

    4. Mal’cev S.V., Arhipova N.N., Shakirova Je.M. Vitamin D, kal’cij i fosfaty u zdorovyh detej i pri patologii. — Kazan’, 2012. — 120 s.

    5. Nauchno-prakticheskaja programma «Deficit kal’cija i osteopenicheskie sostojanija u detej: diagnostika, lechenie, profilaktika» Mezhdunarodnogo fonda ohrany zdorov’ja materi i rebenka / pod red. N.A. Korovinoj i V.A. Peterkovoj. — M.: Mezhdunarodnyj fond ohrany materi i rebenka, 2006. — 46 s.

    6. Gajdarova T.A., Fedotova M.V., Eremina N.A., Inshakov D.V., Litvinova T.K. Metod ispol’zovanija rentgenomorfometrii dlja ocenki mineral’noj plotnosti kostnoj tkani al’veoljarnoj kosti // Bjulleten’ VSNC SO RAMN. — 2006. — № 5 (51). — S. 46-49.

    Метки: bone mineral density in children, G.Sh. MANSUROVA, N.A. ZOTOV, osteopenia in children, osteoporosis., Practical medicine 06 (13) Pediatrics, S.V. MALTSEV, T.V. KOLESNICHENKO

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