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Autor:
T. Diem, N. J. Morley, A. J. Ccahuana Quispe, L. P. Huaraca Quispe, E. M. Baggs, P. Meir, M. I. A. Richards, P. Smith, Y. A. Teh
Publikováno v:
Biogeosciences, Vol 14, Pp 5077-5097 (2017)
Current bottom–up process models suggest that montane tropical ecosystems are weak atmospheric sources of N2O, although recent empirical studies from the southern Peruvian Andes have challenged this idea. Here we report N2O flux from combined fi
Externí odkaz:
https://doaj.org/article/257538fc6ddd4a2fac3886356a38c82c