Документ взят из кэша поисковой машины. Адрес оригинального документа : http://www.mgumus.chem.msu.ru/publication/2007/kulikova-usage-2007.pdf
Дата изменения: Fri Sep 28 14:55:55 2007
Дата индексирования: Mon Oct 1 21:36:47 2012
Кодировка:
VIII Mendeleev Congress on General and Applied Chemistry, Moscow, 2007

2425

USAGE OF TRITUM LABELED HUMIC SUBSTANCES FOR THE STUDY OF THEIR INTERACTION WITH BIOMEMBRANES UNDER OPTIMUM AND SALT STRESS CONDITIONS Kulikova N.A.a, Badun G.A.b, Tyasto Z.A.b, Chernysheva M.G.b, Perminova I.V.
a

b

Department of Soil Science, Lomonosov Moscow State University, Moscow, Russia b Department of Chemistry, Lomonosov Moscow State University, Moscow, Russia

Humic substances (HS) are the natural organic compounds comprising 50 to 90% of the organic matter of peat, lignites, sapropels, as well as of the non-living organic matter of soil and water ecosystems. The beneficial effects of HS on living organisms have been numerously reported. The mechanism of their action remains unclear, and the ways of HS usage by organisms are also sophisticated. Problem of bioavailability of HS and their penetration into the cells is even more sophisticated due to difficulties in HS determination in the presence of other organic substances. In spite of many studies demonstrating HS adsorption onto different biological membranes, there are only a few data on quantitative estimation1,2 or influence of the environment conditions on this process. The most convenient way is a use of labeled compounds, and the availability of isotope-labeled HS is an important prerequisite to elucidate the fate of the heterogeneous organic matter in complex environments. Labeling of HS can be accomplished by the addition of a labeled precursor to an unlabeled soil sample during composting3 or by the synthesis of model polymeric compounds under defined conditions. The latter are synthesized either by enzyme mediated (usually initiated by adding H2O2 in the presence of horseradish peroxidase) oxidative polymerization of phenolic compounds4, or by their spontaneous polymerization in the presence of oxygen or other oxidants, usually at alkaline pH.5 Usage of those techniques, however, does not allow producing labeled preparation completely identical in their properties to the native preparations. Some methods of the direct labeling of HS were therefore developed including labeling of HS with 3H.6 The main advantage of the direct labeling of HS is an opportunity to produce a broad spectrum of isotope-labeled native humics varying significantly in both their origin and properties. The objective of the study was to quantify HS interaction with biomembrane using tritium labeled HS and bacteria Escherichia coli as a model under optimum and salt stress conditions. Six samples of HS originated from coal, peat and soil were examined. Observed values of bioconcentration factor of HS by Escherichia coli under optimum and salt stress conditions varied in the range 0.9-13.1 or 0.2-130 l kg-1, respectively, depending considerably on the HS preparation. Surface activity of HS was demonstrated to be a leading factor determining their both sorption and uptake by bacteria cells.
This research was supported by the grants of the Russian Foundation for Basic Research (#06-03-33036 and #06-0449017a).

References
1. 2. 3. 4. 5. 6. L. Parent, M.R. Twiss, P.G. Campbell, P.G., Environ. Sci. Technol. 1996, 30, 1713-1720. J.B. Fein, J.-F. Boily, K. Guclu, E. Kaulbach, Chem. Geol. 1999, 162, 33-45. K.M. Haider, J.P. Martin, Soil Biol Biochem. 1988, 20, 425­429. A. Kappler, R. Ji, A. Brune Soil Biol Biochem. 2000, 32, 1271­1280. K.T. Steffen, A. Hatakka, M. Hofrichter, Appl. Environ. Microbiol. 2002, 68, 3442-3448. G.A. Badun, V.Yu. Pozdnyakova, A.V. Kudryavtsev, I.V. Perminova, Bulg. J. of Ecol. Sci. 2003, 2(3-4), 26-27.