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ACTIVITIES OF ENZYMES PARTICIPATION IN REDOX POTENTIALIN THE TWO DEPTHS OF TAGAN PEATLAND L.W. Szajdak, L.I. Inisheva, T. Meysner, W. Gaca, K. Styla

  * Institute for Agricultural and Forest Environment, Polish Academy of Science, Poznan, Poland,

szajlech@man.poznan.pl

**Testing Agroecology Laboratory, Tomsk State Pedagogical University, Tomsk, Russia, inisheva@mail.ru

The redox potential is a critical environmental factor because it governs the chemical and biochemical form of many compounds and their availability for plants and soil microorganisms.

Soil organic matter transformation is strongly effected by the activities of soil microorganisms, which use many enzymes in their metabolic pathways. As is well known, the role of enzymes in coupling reactions leading to polymerization is limited to the oxidation of the substrates.

Soils samples were taken from four places marked as No 1, 2, 3 and 4 each from two depth 0-25 and 50-75 cm of the peatland Tagan. Peatlands Tagan is located near Tomsk, West Siberia, Russia. Place No 1 in both layers represents grasses peat with the degree of the decomposition ranged from 25 to 35 % (pH 6.31-7.95). Point 2 is characterized by wooden and wooden grasses peat with 35 % degree of the decomposition (pH 5.16-9.31). There is buckbean peat in the points 3 and 4 (pH 6.4-6.49). However, 1,5 m depth of sapropel is located in point 4.

Dissolved organic matter and total organic matter, reductase, xanthine oxidase, phenol oxidase and peroxidase activity were determined in the soil samples. It is known that organic matter is capable of inducing reduction and oxidation reactions, hence affecting the redox system in the environment. Our research showed that the dissolved organic carbon concentration ranged from 5,67 to 10,92 g kg-1 and total organic matter from 314,0 to 436,8 g kg-1 in all of sampling.

Nitrate reductase is enzyme involved in the process of denirification. Nitrogen present in the structure of this enzyme acts as a terminal acceptor of electrons instead of molecular O2 by bacteria and is irreversible once NO is formed. The investigation has shown that nitrate reductase activity in the soils reached from 0.11 to 0.68 pgN 24h-1 g-1 in all of sampling.

An important role in redox processes in soil plays xanthine oxidase. This enzyme is a metal-flavoprotein containing FAD, molybdenum and iron in the ratio of 2:2:8. Xanthine oxidase is the last enzyme in the pathway of the degradation of purine derivatives from nucleic acids and is assumed to be a rate-limiting step in purine metabolism. These studies indicated that xanthine oxidase activity in the soils increased with depth and ranged from 22,93 to 40,43 pmol h-1 g-1 at 0-25 cm and from 33,61 to 54,75 pmol h-1 g-1 at 50-75 cm depth in all of sampling Similar trend was shown for the activity of phenol oxidase and peroxidase in the points 2, 3 and 4. The phenol oxidase is enzyme that catalyzes the oxidation of phenolic compounds to quinones, participates in the formation of humic acids, and indicates the capacity of the microflora degrade recalcitrant organic substances. These studies indicated that phenol oxidase activity ranged from 10,85 to 15,77 pmol h-1 g-1 at 0-25 cm and from 6,18 to 46,01 pmol h-1 g-1 at 50-75 cm depth. Peroxidases are present in natural soil, and may originate from microorganisms, plants or other organisms. This enzyme catalyzes the oxidation of phenols and aromatic amines in the presence of hydrogen peroxide as an electron acceptor in the reactions. It was observed that activity of peroxidase was from 1,50 to 6,64 nmol h-1 g-1 at 0-25 cm and from 4,30 to 7,52 nmol h-1 g-1 at 50-75 cm depth in all of sampling. In the soil profiles activity of xanthine oxidase, phenol oxidase and peroxidase increased with depth in the points 2, 3 and 4.

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Источник: Л. И. Инишева. Болота и биосфера : материалы VII Всероссийской с международным участием научной школы. 2010

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