Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity (2019)
- Authors:
- Autor USP: BARCELLOS, DIEGO - ESALQ
- Unidade: ESALQ
- DOI: 10.1007/s11368-018-2068-2
- Subjects: DIFRAÇÃO POR RAIOS X; ESPECTROSCOPIA DO MOSSBAUER; FERRO; HORIZONTES DO SOLO; MINERALOGIA DO SOLO
- Keywords: Profundidade do solo
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Publisher place: Heidelberg
- Date published: 2019
- Source:
- Título: Journal of Soils and Sediments
- ISSN: 1614-7480
- Volume/Número/Paginação/Ano: v. 19, p. 785-797, 2019
- Este periódico é de assinatura
- Este artigo é de acesso aberto
- URL de acesso aberto
- Cor do Acesso Aberto: green
- Licença: other-oa
-
ABNT
CHEN, Chunmei et al. Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity. Journal of Soils and Sediments, v. 19, p. 785-797, 2019Tradução . . Disponível em: https://doi.org/10.1007/s11368-018-2068-2. Acesso em: 28 dez. 2025. -
APA
Chen, C., Barcellos, D., Richter, D. D., Schroeder, P. A., & Thompson, A. (2019). Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity. Journal of Soils and Sediments, 19, 785-797. doi:10.1007/s11368-018-2068-2 -
NLM
Chen C, Barcellos D, Richter DD, Schroeder PA, Thompson A. Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity [Internet]. Journal of Soils and Sediments. 2019 ; 19 785-797.[citado 2025 dez. 28 ] Available from: https://doi.org/10.1007/s11368-018-2068-2 -
Vancouver
Chen C, Barcellos D, Richter DD, Schroeder PA, Thompson A. Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity [Internet]. Journal of Soils and Sediments. 2019 ; 19 785-797.[citado 2025 dez. 28 ] Available from: https://doi.org/10.1007/s11368-018-2068-2 - 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: 10.1007/s11368-018-2068-2 (Fonte: oaDOI API)
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