Szczegóły publikacji
Opis bibliograficzny
Spectroscopic study of biologically active glasses / M. SZUMERA, I. WACŁAWSKA, W. MOZGAWA, M. SITARZ // Journal of Molecular Structure ; ISSN 0022-2860. — 2005 — vols. 744–747, s. 609–614. — Bibliogr. s. 614, Abstr. — Publikacja dostępna online od: 2005-03-03. — XXVIIth European Congress on Molecular Spectroscopy : Krakow, Poland, September 5-10, 2004
Autorzy (4)
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 22650 |
|---|---|
| Data dodania do BaDAP | 2005-06-16 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.molstruc.2005.01.023 |
| Rok publikacji | 2005 |
| Typ publikacji | referat w czasopiśmie |
| Otwarty dostęp |  |
| Czasopismo/seria | Journal of Molecular Structure |
Abstract
It is known that the chemical activity phenomenon is characteristic for some inorganic glasses and they are able to participate in biological processes of living organisms (plants, animals and human bodies). An example here is the selective removal of silicate-phosphate glass components under the influence of biological solutions, which has been applied in designing glasses acting as ecological fertilizers of controlled release rate of the nutrients for plants. The structure of model silicate-phosphate glasses containing the different amounts of the glass network formers, i.e. Ca2+ and Mg2+, as a binding components were studied. These elements besides other are indispensable of the normal growth of plants. In order to establish the function and position occupied by the particular components in the glass structure, the glasses were examined by FTIR spectroscopy (with spectra decomposition) and XRD methods. It has been found that the increasing amount of MgO in the structure of silicate-phosphate glasses causes the formation of domains the structure of which changes systematically from a structure of the cristobalite type to a structure corresponding to forsterite type. Whilst the increasing content of CaO in the structure of silicate-phosphate glasses causes the formation of domains the structure of which changes from a structure typical for cristobalite through one similar to the structure of calcium orthophosphate, to a structure corresponding to calcium silicates. The changing character of domains structure is the reason of different chemical activity of glasses. (c) 2005 Elsevier B.V. All rights reserved.
