Biogeochemistry

, Volume 34, Issue 3, pp 113–132

Soil environmental variables affecting the flux of methane from a range of forest, moorland and agricultural soils

  • Jannette A. MacDonald
  • Ute Skiba
  • Lucy J. Sheppard
  • Kenneth J. Hargreaves
  • Keith A. Smith
  • David Fowler
Article

Abstract

Measurements of the net methane exchange over a range of forest, moorland, and agricultural soils in Scotland were made during the period April to June 1994 and 1995. Fluxes of CH4 ranged from oxidation −12.3 to an emission of 6.8 ng m−2 s−1. The balance between CH4 oxidation and emission depended on the physical conditions of the soil, primarily soil moisture. The largest oxidation rates were found in the mineral forest soils, and CH4 emission was observed in several peat soils. The smallest oxidation rate was observed in an agricultural soil. The relationship between CH4 flux and soil moisture observed in peats (FluxCH4 = 0.023 × %H2O (dry weight) − 7.44, p > 0.05) was such that CH4 oxidation was observed at soil moistures less than 325%( ± 80%). CH4 emission was found at soil moistures exceeding this value. A large range of CH4 oxidation rates were observed over a small soil moisture range in the mineral soils. CH4 oxidation in mineral soils was negatively correlated with soil bulk density (FluxCH4 = −37.35 × bulk density (g cm−3) + 48.83, p > 0.05). Increased nitrogen loading of the soil due to N fixation, atmospheric deposition of N, and fertilisation, were consistently associated with decreases in the soil sink for CH4, typically in the range 50 to 80%, on a range of soil types and land uses.

Key words

methane oxidation methane emission soil nitrogen 

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References

  1. Adamsen APS & King GM (1993) CH4 consumption in temperate and subarctic forest soils: rates, vertical zonation and responses to water and nitrogen. App. & Env. Microbiol. 59: 485–490Google Scholar
  2. Bender M & Conrad R (1994) CH4 oxidation activity in various soils and freshwater sediments: Occurrence, characteristics, vertical profiles, and distribution on grain size fractions. J. Geophys. Res. 99: 16531–16540Google Scholar
  3. Blake DR & Rowland FS (1988) Continuing worldwide increase in atmospheric CH4. Science 239: 2181–2187Google Scholar
  4. Brady NC (1990) The Nature and Properties of Soils. Macmillan Publishing Co., New YorkGoogle Scholar
  5. Brown CJ & Shipley BM (1982) Soil Survey of Scotland: South East Scotland. Aberdeen University Press, AberdeenGoogle Scholar
  6. Castro MS, Steudler PA, Melillo JM, Aber JD & Millham S (1993) Exchange of N2O & CH4 between the atmosphere and soils in spruce-fir forests in the northeastern United States. Biogeochemistry 18: 119–135PubMedGoogle Scholar
  7. Castro MS, Peterjohn WT, Melillo JM & Steudler PA (1994) Effects of N fertilisation on the fluxes of N2O, CH4 and CO2 from soils in a Florida slash pine plantation. Can. J. For. Res. 24: 9–13Google Scholar
  8. Cicerone RJ & Oremland RS (1988) Biogeochemical aspects of atmospheric CH4. Global Biogeochem. Cycles 2: 299–327Google Scholar
  9. Clayton H, Arah JRM & Smith KA (1994) Measurement of N2O emissions from fertilised grassland using closed chambers. J. Geophys. Res. 99: 16599–16607Google Scholar
  10. Crill PM (1991) Seasonal patterns of CH4 uptake and CO2 release by a temperate woodland soil. Global Biogeochem. Cycles 5: 319–334Google Scholar
  11. Crossley A, Wilson DB & Milne R (1992) Pollution in the upland environment. Environ. Pollut. 75: 81–87Google Scholar
  12. Crooke WM & Simpson WE (1971) Determination of ammonia in Kjeldal digests of crops by an automated procadure. J. Sci. Food Agric. 22: 9–10Google Scholar
  13. Dunfield P, Knowles R, Dumont R & Moore T (1993) CH4 production and consumption in temperate and subarctic peat soils: response to temperature and pH. Soil Biol. Biochem. 25: 321–326Google Scholar
  14. Dobbie KE, Smith KA, Prieme A, Christensen S, Degorska A & Orlanski P (1996) Effect of land use on the rate of CH4 uptake by surface soils in Northern Europe. Atmospheric Environment 30: 1005–1011Google Scholar
  15. Dorr H, Katruff L & Levin I (1993) Soil texture parameterisation of the CH4 uptake in aerated soils. Chemosphere 26: 697–713Google Scholar
  16. Fowler D, Cape JN & Unsworth MH (1989) Deposition of atmospheric pollutants on forests. Phil. Trans. R. Soc. Lond. B324: 247–265Google Scholar
  17. Hansen S, Maehlum JE & Bakken LR (1993) N2O and CH4 fluxes in soil influenced by fertilisation and tractor traffic. Soil Biol. Biochem. 25: 621–630Google Scholar
  18. Henrikson A & Selmer-Olsen AR (1970) Automatic methods for determining nitrate and nitrite in water and soil extracts. Analyst 95: 514–518Google Scholar
  19. Hornung M (1985) Acidification of soils by trees and forests. Soil Use and Management 1: 24–28Google Scholar
  20. Hutsch BW, Webster CP & Powlson DS (1994) CH4 oxidation in soil as affected by land use, soil pH and N fertilisation. Soil Biol. Biochem. 26: 1613–1622Google Scholar
  21. Hyman MR & Wood PM (1983) CH4 oxidation by Nitrosomonas europaea. Biochem. J. 212: 31–37Google Scholar
  22. IPCC (1990) Climate Change, The IPCC Scientific Assessment. In: Houghton JT, Jenkins GJ & Ephraums JJ (Eds) Cambridge University Press, CambridgeGoogle Scholar
  23. IPCC (1994) Radiative Forcing of Climate Change and an Evaluation of the IPCC IS92 Emission Scenarios. In: Houghton JT, Meira Filho LG, Bruce J, Hoesung Lee, Callander BA, Haites E, Harris N & Maskell K (Eds) Cambridge University Press, CambridgeGoogle Scholar
  24. Khalil MAK & Rasmussen RA (1990) Constraints on the global sources of CH4 and an analysis of recent budgets. Tellus 42B: 229–236Google Scholar
  25. Khalil MAK & Rasmussen RA (1983) Sources, sinks and seasonal cycles of atmospheric CH4. J. Geophys. Res. 88: 5131–5144Google Scholar
  26. Keller M, Mitre ME & Stallard RF (1990) Consumption of atmospheric CH4 in soils of central Panama: effects of agricultural developement. Global Biogeochem. Cycles 4: 21–27Google Scholar
  27. Keller M & Reiners WA (1994) Soil atmosphere exchange of N2O, NO and CH4 under secondary succession of pasture to forest in the Atlantic lowlands of Costa Rica. Global Biogeochem. Cycles 8: 399–409Google Scholar
  28. Lessard R, Rochette P, Popp E, Pattey E, Desjardins RL & Beaumont G (1994) CH4 and CO2 fluxes from poorly drained adjacent cultivated and forest sites. Can. J. Soil Science 74: 139–146Google Scholar
  29. Mosier A, Schimel D, Valentine D, Bronson K & Parton W (1991) CH4 and N2O fluxes in native, fertilised and cultivated grasslands. Nature 350: 330–332Google Scholar
  30. Ojima DS, Valentine DW, Mosier AR, Parton WJ & Schimel DS (1993) Effect of land use change on CH4 oxidation in temperate forest and grassland soils. Chemosphere 26: 675–685Google Scholar
  31. O'Neill JG & Wilkinson JF (1977) Oxidation of ammonia by CH4 oxidising bacteria and the effects of ammonia on CH4 oxidation. J. Gen. Microbiol. 100: 407–412Google Scholar
  32. Rowell DL (1994) Soil Science: Methods & Applications. Longman Group Ltd., HarlowGoogle Scholar
  33. Schutz H & Seiler W (1989) CH4 flux measurements: methods and results. In: Andreae MO & Schimel DS (Eds) Exchange of Trace Gases Between Terrestrial Ecosystems and the Atmosphere (pp 209–228). WileyGoogle Scholar
  34. Schnell S & King GM (1994) Mechanistic analysis of ammonium inhibition of atmospheric methane consumption in forest soils. App. & Environ. Microbiol. 60: 3514–3521Google Scholar
  35. Sheppard LJ (1993) Performance of red alder provenances at Glencorse. Report ref. DCY/CK/Red AlderGoogle Scholar
  36. Sitaula BK & Bakken LR (1993) N2O release from spruce forest soil, relation with nitrification, CH4 uptake, temperature, moisture and fertilisation. Soil Biol. Biochem. 25: 1415–1421Google Scholar
  37. Smith KA & Arah JRM (1986) Anaerobic micro-environments in soil and the occurence of anaerobic bacteria. In: Jensen V, Kjoller A & Sorensen LH (Eds) Microbial Communities in Soil. F.E.M.S. Symposium 33 (pp 247–261) Elsevier Press, LondonGoogle Scholar
  38. Steudler PA, Bowden RD, Melillo JM & Aber JD (1989) Influence of N fertilisation on CH4 uptake in temperate forest soils. Nature 341: 314–315CrossRefGoogle Scholar
  39. Streigl RG, McConnaughey TA, Tharston DC, Weeks EP & Woodward JC (1992) Consumption of atmospheric CH4 by desert soils. Nature 357: 145–147Google Scholar
  40. Whalen SC, Reeburgh WS & Sandbeck KA (1990) Rapid CH4 oxidation in a landfill cover soil. App. & Environ. Microbiol. 56: 3405–3411Google Scholar
  41. Whalen SC, Reeburgh WS & Kizer KS (1991) CH4 consumption & emission by taiga. Global Biogeochem. Cycles 5: 261–273Google Scholar
  42. Whalen SC & Reeburgh WS (1990) Consumption of atmospheric CH4 by tundra soils. Nature 346: 160–162Google Scholar
  43. Whittenbury R, Phillips KC & Wilkinson JF (1970) Enrichment, isolation and some properties of CH4 utilising bacteria J. Gen. Microbiol. 61: 205–218Google Scholar
  44. Yavitt JB, Downey DM, Lang GE & Sexstone AJ (1990) CH4 consumption in two temperate forest soils. Biogeochemistry 9: 39–52Google Scholar
  45. Zahniser MS, Nelson DD, McManus JB & Kebabian PL (1995) Measurements of trace gas fluxes using tunable diode laser spectroscopy. Phil. Trans. R. Soc. Lond. A 351: 371–381Google Scholar

Copyright information

© Kluwer Academic Publishers 1996

Authors and Affiliations

  • Jannette A. MacDonald
    • 1
    • 2
  • Ute Skiba
    • 1
  • Lucy J. Sheppard
    • 1
  • Kenneth J. Hargreaves
    • 1
  • Keith A. Smith
    • 3
  • David Fowler
    • 1
  1. 1.Edinburgh Research StationInstitute of Terrestrial EcologyPenicuikUK
  2. 2.Soils DepartmentScottish Agricultural CollegeWest Mains RoadUK
  3. 3.Institute of Ecology and Resource ManagementUniversity of EdinburghWest Mains RoadUK

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