Theoretical constraints on fe reduction rates in upland soils as a function of hydroclimatic conditions (2020)
- Authors:
- Autor USP: BARCELLOS, DIEGO - ESALQ
- Unidade: ESALQ
- DOI: 10.1029/2020JG005894
- Subjects: CHUVA; CICLO DO CARBONO; FERRO; UMIDADE DO SOLO
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Source:
- Título: Journal of Geophysical Research: Biogeosciences
- ISSN: 2169-8961
- Volume/Número/Paginação/Ano: v. 125, n. 12, art. e2020JG005894, p. 1-18, 2020
- Este periódico é de assinatura
- Este artigo NÃO é de acesso aberto
- Cor do Acesso Aberto: closed
-
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: 28 dez. 2025. -
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:10.1029/2020JG005894 -
NLM
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 2025 dez. 28 ] Available from: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005894 -
Vancouver
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 2025 dez. 28 ] Available from: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JG005894 - Influence of po2on iron redox cycling and anaerobic organic carbon mineralization in a humid tropical forest soil
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Informações sobre o DOI: 10.1029/2020JG005894 (Fonte: oaDOI API)
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