Articles | Volume 14, issue 2
https://doi.org/10.5194/bg-14-467-2017
https://doi.org/10.5194/bg-14-467-2017
Research article
 | 
27 Jan 2017
Research article |  | 27 Jan 2017

Soil methane oxidation in both dry and wet temperate eucalypt forests shows a near-identical relationship with soil air-filled porosity

Benedikt J. Fest, Nina Hinko-Najera, Tim Wardlaw, David W. T. Griffith, Stephen J. Livesley, and Stefan K. Arndt

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Cited articles

Ashworth, J., Keyes, D., Kirk, R., and Lessard, R.: Standard procedure in the hydrometer method for particle size analysis, Commun. Soil. Sci. Plan., 32, 633–642, 2001.
Ball, B. C., Dobbie, K. E., Parker, J. P., and Smith, K. A.: The influence of gas transport and porosity on methane oxidation in soils, J. Geophys. Res.-Atmos., 102, 23301–23308, 1997.
Boeckx, P., van Cleemput, O., and Villaralvo, I.: Methane oxidation in soils with different textures and land use, Nutr. Cycl. Agroecosys., 49, 91–95, 1997.
Born, M., Dorr, H., and Levin, I.: Methane consumption in aerated soils of the temperate zone, Tellus B, 42, 2–8, https://doi.org/10.1034/j.1600-0889.1990.00002.x, 1990.
Butterbach-Bahl, K. and Papen, H.: Four years continuous record of CH4-exchange between the atmosphere and untreated and limed soil of a N-saturated spruce and beech forest ecosystem in Germany, Plant. Soil., 240, 77–90, 2002.
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