METHANE EMISSION FROM NATURAL COMPLEXES OF THE ZAKAMYE LOWLANDS IN THE TERRITORY OF UDMURTIA

  • A.V. Semakina
    • Udmurt State University
  • L.R. Sharipov
    • Direction for Environmental Protection and Nature Management of the Ministry of Natural Resources of the UR
  • I.Yu. Gagarina
    • Udmurt State University
  • I.Yu. Rubtsova
    • Udmurt State University
  • G.R. Platunova
    • Udmurt State University
Keywords: methane, emission, Zakamye lowlands, Udmurt Republic

Abstract

The methane content largely determines the oxidizing properties of the atmosphere, including greenhouse gases and polluting components. The purpose of this study is to estimate the amount of methane emissions from natural sources. The volumes of methane emission from a typical section of the swamp massif within the Zakamye lowlands in the Udmurt Republic were obtained experimentally. Analyzing the results obtained in the course of this work, it can be concluded that the most intensive methane supply is observed in the tracts located in the floodplain of the Kama River and its tributaries. These tracts are characterized by a high level of soil moisture, and as a consequence, active anaerobic processes in the soil during the warm season. Slope and watershed landscapes are characterized by minimum methane emissions, which is associated with a greater degree of aeration of soils of these territorial units.

References


  1. Isidorov V.A. Ekologicheskaya khimiya [Ecological chemistry], SPb.: Himizdat Publ., 2001, 116 p. (in Russ.).

  2. Karol' I.L., Kiselev A.A. [Atmospheric methane and global climate], in Priroda, Moscow: Nauka Publ., 2004, no. 7, pp. 47-52 (in Russ.).

  3. Prirodnye zakonomernosti soderzhaniya metana v ugol'nykh plastakh [Natural patterns of methane in coal beds], Kolesnichenko E.A. et al. (ed.), Moscow: Gornaya kniga Publ., 2011, 325 p. (in Russ.).

  4. Baird A.J., Beckwith C.W., Waldron S., Waddington J.M. 2004 Ebullition of methane-containing gas bubbles from near-surface Sphagnum peat, in Geophysical Research Letters, 2004, vol. 31, L21505. DOI: 10.1029/2004GL021157.

  5. Happell J.D., Chanton J.P. Carbon Remineralization in a North Florida Swamp Forest: Effects of Water Level on the Pathways and Rates of Soil Organic Matter Decomposition, in Global Biogeochemical Cycles, 1993, vol. 7, pp. 475-490.

  6. Happell J.D., Chanton J.P., Whiting G.J., Showers W.J. Stable Isotopes as Tracers of Methane Dynamics in Everglades Marshes With and Without Active Populations of Methane Oxidizing Bacteria, in Journal of Geophysical Research, 1993, vol. 98, no. D8, pp. 14771-14782.

  7. Chen Y.-K, Prinn R.G. Estimation of atmospheric methane emissions between 1996 and 2001 using a three-dimensional global chemical transport model, in Journal of Geophysical Research, 2006, D10307, DOI: 10.1029/2005JD006058.

  8. Bazhin N.M. Metan v okruzhayushchej srede [Methane in the environment], Moscow: Khimiya Publ., 2005, 87 p. (in Russ.).

  9. Walter B.P., Heimann M., Shannon R.D., White J.R. A process-based model to derive methane emissions from natural wetlands, in Geophysical Research Letters, 1996, vol. 23, pp. 3731-3734.

  10. Kazancev V.S. [Methane emission from swamp ecosystems of northern Western Siberia], Cand. Biol. sci. diss., Moscow, 2013, 137 p. (in Russ.).

  11. Christensen T. Seasonal emission of methane from the active layer of organic tundra soils-scale and controlling factors, in Joint Russian-American seminar on Cryopedology and global change (November 15-16, 1992, Pushchino). Pushchino: Pushchino Research Centre, 1993, pp. 325-341.

  12. Geoekologicheskie problemy Udmurtii [Geoenvironmental problems of Udmurtia], Sturman V.I. (ed), Izhevsk: Izd-vo Udmurt. Univ., 1997, 167 p. (in Russ.).

  13. Geograficheskiy atlas Udmurtskoy Respubliki [Geographical Atlas of the Udmurt Republic], Rysina I.I. (ed), 2nd ed., Moscow: DIK Publ., 2010, 40 p. (in Russ.).

  14. Rysin I.I. [Physical-geographical (landscape) zoning of Udmurtia, in Udmurt. Univ., 1996, no. 3, pp. 131-150 (in Russ.).

Received 2020-03-06
Published 2020-05-08
Section
Short communications
Pages
112-118