Studies on properties of montmorillonite-amino acid complexes
Three montmorillonite-amino acid complexes (montmorillonite-glicine, montmorillonitearginine and montmorillonite-lysine) were prepared. The complexes were studied by DTA, X-ray and IR-spectroscopy. DTA measurements indicate a strong interaction between montmorillonite and organic material. .There is...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1977
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| Sorozat: | Acta mineralogica-petrographica
23 No. 1 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24625 |
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| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Berlinger H. | |
| 245 | 1 | 0 | |a Studies on properties of montmorillonite-amino acid complexes |h [elektronikus dokumentum] / |c Berlinger H. |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1977 | ||
| 300 | |a 159-164 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 23 No. 1 | |
| 520 | 3 | |a Three montmorillonite-amino acid complexes (montmorillonite-glicine, montmorillonitearginine and montmorillonite-lysine) were prepared. The complexes were studied by DTA, X-ray and IR-spectroscopy. DTA measurements indicate a strong interaction between montmorillonite and organic material. .There is a mutual stabilization as evidenced by the shift of peak temperatures of both the structural decomposition of the montmorillonite and the decomposition of the organic material. X-ray measurements support the results obtained by other methods. IR-spectra support the existence of the montmorillonite-organic material interactions. Complex formation brings about such conjugational relationships which result in the appearance of a new absorption band in the IR-spectra. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 700 | 0 | 1 | |a Grasselly Gyula |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24625/1/mineralogica_023_fasc_001_159-164.pdf |z Dokumentum-elérés |