Cite
Isotope fractionation factors controlling isotopocule signatures of soil-emitted N2O produced by denitrification processes of various rates.
MLA
Lewicka, Szczebak, Dominika, et al. “Isotope Fractionation Factors Controlling Isotopocule Signatures of Soil-Emitted N2O Produced by Denitrification Processes of Various Rates.” Rapid Communications in Mass Spectrometry: RCM, vol. 29, no. 3, Feb. 2015, pp. 269–82. EBSCOhost, https://doi.org/10.1002/rcm.7102.
APA
Lewicka, S. D., Well, R., Bol, R., Gregory, A. S., Matthews, G. P., Misselbrook, T., Whalley, W. R., & Cardenas, L. M. (2015). Isotope fractionation factors controlling isotopocule signatures of soil-emitted N2O produced by denitrification processes of various rates. Rapid Communications in Mass Spectrometry: RCM, 29(3), 269–282. https://doi.org/10.1002/rcm.7102
Chicago
Lewicka, Szczebak, Dominika, Reinhard Well, Roland Bol, Andrew S. Gregory, G. Peter Matthews, Tom Misselbrook, W. Richard Whalley, and Laura M. Cardenas. 2015. “Isotope Fractionation Factors Controlling Isotopocule Signatures of Soil-Emitted N2O Produced by Denitrification Processes of Various Rates.” Rapid Communications in Mass Spectrometry: RCM 29 (3): 269–82. doi:10.1002/rcm.7102.