Comparative IR spectral characteristics of humic acids from peats of different origin in the Tomsk area; Pharmaceutical Chemistry Journal; Vol. 43, iss. 7

מידע ביבליוגרפי
Parent link:Pharmaceutical Chemistry Journal
Vol. 43, iss. 7.— 2009.— [P. 418-421]
מחברים אחרים: Gostishcheva M. V., Belousov M. V. Mikhail Valerievich, Yusubov M. S. Mekhman Suleiman-Ogly (Suleimanovich), Ismatova R. R., Dmitruk S. E.
סיכום:Title screen
Results obtained from comparative studies of the structures of humic acids from peats of different origins in the Tomsk area by infrared spectroscopy are presented. These data showed that the IR spectra of humic acids extracted from different types of peat had high levels of similarity, demonstrating similarities in their chemical structures. Humic acid from lowland woody-grassy peat had very significant differences from other types of peat and consisted of compounds with high proportions of aliphatic fragments and, perhaps, lower benzenoid levels, as well as higher contents of active acid groups (carboxyl, hydroxyl).
Режим доступа: по договору с организацией-держателем ресурса
שפה:אנגלית
יצא לאור: 2009
נושאים:
גישה מקוונת:http://dx.doi.org/10.1007/s11094-009-0323-y
פורמט: אלקטרוני Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=647735
תיאור
סיכום:Title screen
Results obtained from comparative studies of the structures of humic acids from peats of different origins in the Tomsk area by infrared spectroscopy are presented. These data showed that the IR spectra of humic acids extracted from different types of peat had high levels of similarity, demonstrating similarities in their chemical structures. Humic acid from lowland woody-grassy peat had very significant differences from other types of peat and consisted of compounds with high proportions of aliphatic fragments and, perhaps, lower benzenoid levels, as well as higher contents of active acid groups (carboxyl, hydroxyl).
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1007/s11094-009-0323-y