Calabrese, Salvatore; Barcellos, Diego 
; Thompson, Aaron; Porporato, Amilcare
Source: Journal of Geophysical Research: Biogeosciences. Unidade: ESALQ
Subjects: CHUVA, CICLO DO CARBONO, FERRO, UMIDADE DO SOLO
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ABNT
CALABRESE, Salvatore et al. Theoretical constraints on fe reduction rates in upland soils as a function of hydroclimatic conditions. Journal of Geophysical Research: Biogeosciences, v. 125, n. 12, p. 1-18, 2020Tradução . . Disponível em: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005894. Acesso em: 02 jun. 2024.APA
Calabrese, S., Barcellos, D., Thompson, A., & Porporato, A. (2020). Theoretical constraints on fe reduction rates in upland soils as a function of hydroclimatic conditions. Journal of Geophysical Research: Biogeosciences, 125( 12), 1-18. doi:10.1029/2020JG005894NLM
Calabrese S, Barcellos D, Thompson A, Porporato A. Theoretical constraints on fe reduction rates in upland soils as a function of hydroclimatic conditions [Internet]. Journal of Geophysical Research: Biogeosciences. 2020 ; 125( 12): 1-18.[citado 2024 jun. 02 ] Available from: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005894Vancouver
Calabrese S, Barcellos D, Thompson A, Porporato A. Theoretical constraints on fe reduction rates in upland soils as a function of hydroclimatic conditions [Internet]. Journal of Geophysical Research: Biogeosciences. 2020 ; 125( 12): 1-18.[citado 2024 jun. 02 ] Available from: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005894
