Standard

Isomorphic substitutions in biomimetic carbonated fluorapatites. / Rosseeva, E. V.; Frank-Kamenetskaya, O. V.; Shwarts, U.; Kniep, R.

в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том 2009, № 3, 01.12.2009.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Rosseeva, EV, Frank-Kamenetskaya, OV, Shwarts, U & Kniep, R 2009, 'Isomorphic substitutions in biomimetic carbonated fluorapatites', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том. 2009, № 3.

APA

Rosseeva, E. V., Frank-Kamenetskaya, O. V., Shwarts, U., & Kniep, R. (2009). Isomorphic substitutions in biomimetic carbonated fluorapatites. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2009(3).

Vancouver

Rosseeva EV, Frank-Kamenetskaya OV, Shwarts U, Kniep R. Isomorphic substitutions in biomimetic carbonated fluorapatites. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2009 Дек. 1;2009(3).

Author

Rosseeva, E. V. ; Frank-Kamenetskaya, O. V. ; Shwarts, U. ; Kniep, R. / Isomorphic substitutions in biomimetic carbonated fluorapatites. в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2009 ; Том 2009, № 3.

BibTeX

@article{3f17a259455246b38cd1f6f13940a45c,
title = "Isomorphic substitutions in biomimetic carbonated fluorapatites",
abstract = "Biomimetic carbonated fluorapatite-gelatine composite were grown by a double-diffusion technique within a gelatine gel. In the biomimetic carbonated fluorapatite the carbonate ions replace the phosphate groups (so-called B-type substitution). The carbonate content in the synthetic fluorapatites varies from 0,05 to 7,5 wt.-%. Besides the {"}built-in{"} carbonate ion in the fluorapatite crystal structure we also determined sodium and hydrophoshate ions, water molecules and trace amounts of hydroxy! ions. The amount of vacancies on the calcium site as well as within the channels of the apatite crystal structure increases with the increase of carbonate content. The chemical composition and lattice parameters of the biomimetic carbonated fluorapatites are similar to those of apatite of hard tissues of some living and fossil organisms, but significantly different from apatite of sedimentary phosphorites.",
keywords = "Apatites of hard tissues of living and fossil organisms, Biomimetic synthesis, Carbonated fluorapatite, Isomorphism, Phosphorites",
author = "Rosseeva, {E. V.} and Frank-Kamenetskaya, {O. V.} and U. Shwarts and R. Kniep",
year = "2009",
month = dec,
day = "1",
language = "English",
volume = "2009",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "3",

}

RIS

TY - JOUR

T1 - Isomorphic substitutions in biomimetic carbonated fluorapatites

AU - Rosseeva, E. V.

AU - Frank-Kamenetskaya, O. V.

AU - Shwarts, U.

AU - Kniep, R.

PY - 2009/12/1

Y1 - 2009/12/1

N2 - Biomimetic carbonated fluorapatite-gelatine composite were grown by a double-diffusion technique within a gelatine gel. In the biomimetic carbonated fluorapatite the carbonate ions replace the phosphate groups (so-called B-type substitution). The carbonate content in the synthetic fluorapatites varies from 0,05 to 7,5 wt.-%. Besides the "built-in" carbonate ion in the fluorapatite crystal structure we also determined sodium and hydrophoshate ions, water molecules and trace amounts of hydroxy! ions. The amount of vacancies on the calcium site as well as within the channels of the apatite crystal structure increases with the increase of carbonate content. The chemical composition and lattice parameters of the biomimetic carbonated fluorapatites are similar to those of apatite of hard tissues of some living and fossil organisms, but significantly different from apatite of sedimentary phosphorites.

AB - Biomimetic carbonated fluorapatite-gelatine composite were grown by a double-diffusion technique within a gelatine gel. In the biomimetic carbonated fluorapatite the carbonate ions replace the phosphate groups (so-called B-type substitution). The carbonate content in the synthetic fluorapatites varies from 0,05 to 7,5 wt.-%. Besides the "built-in" carbonate ion in the fluorapatite crystal structure we also determined sodium and hydrophoshate ions, water molecules and trace amounts of hydroxy! ions. The amount of vacancies on the calcium site as well as within the channels of the apatite crystal structure increases with the increase of carbonate content. The chemical composition and lattice parameters of the biomimetic carbonated fluorapatites are similar to those of apatite of hard tissues of some living and fossil organisms, but significantly different from apatite of sedimentary phosphorites.

KW - Apatites of hard tissues of living and fossil organisms

KW - Biomimetic synthesis

KW - Carbonated fluorapatite

KW - Isomorphism

KW - Phosphorites

UR - http://www.scopus.com/inward/record.url?scp=73349098201&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:73349098201

VL - 2009

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 3

ER -

ID: 43672907