Cor do solo (Portuguese Wikipedia)

Analysis of information sources in references of the Wikipedia article "Cor do solo" in Portuguese language version.

refsWebsite
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2,523rd place
1st place
1st place
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agriculture.vic.gov.au

vro.agriculture.vic.gov.au

cecierj.edu.br

extensao.cecierj.edu.br

doi.org

dx.doi.org

  • Gonzalez-Perez, Jose A.; Gonzalez-Vila, Francisco J.; Almendros, Gonzalo; Knicker, Heike (2004). «The effect of fire on soil organic matter-a review» (PDF). Elsevier. Environment International. 30 (6): 855–870. PMID 15120204. doi:10.1016/j.envint.2004.02.003. Consultado em 4 de janeiro de 2019. As a whole, BC represents between 1 and 6% of the total soil organic carbon. It can reach 35% in Terra Preta Oxisols (Brazilian Amazonia) (Glaser et al., 1998, 2000) up to 45 % in some chernozemic soils from Germany (Schmidt et al., 1999), and up to 60% in black Chernozem from Canada (Saskatchewan) (Ponomarenko and Anderson, 1999) 

embrapa.br

ainfo.cnptia.embrapa.br

nih.gov

ncbi.nlm.nih.gov

  • Gonzalez-Perez, Jose A.; Gonzalez-Vila, Francisco J.; Almendros, Gonzalo; Knicker, Heike (2004). «The effect of fire on soil organic matter-a review» (PDF). Elsevier. Environment International. 30 (6): 855–870. PMID 15120204. doi:10.1016/j.envint.2004.02.003. Consultado em 4 de janeiro de 2019. As a whole, BC represents between 1 and 6% of the total soil organic carbon. It can reach 35% in Terra Preta Oxisols (Brazilian Amazonia) (Glaser et al., 1998, 2000) up to 45 % in some chernozemic soils from Germany (Schmidt et al., 1999), and up to 60% in black Chernozem from Canada (Saskatchewan) (Ponomarenko and Anderson, 1999) 

orst.edu

fsl.orst.edu

  • Gonzalez-Perez, Jose A.; Gonzalez-Vila, Francisco J.; Almendros, Gonzalo; Knicker, Heike (2004). «The effect of fire on soil organic matter-a review» (PDF). Elsevier. Environment International. 30 (6): 855–870. PMID 15120204. doi:10.1016/j.envint.2004.02.003. Consultado em 4 de janeiro de 2019. As a whole, BC represents between 1 and 6% of the total soil organic carbon. It can reach 35% in Terra Preta Oxisols (Brazilian Amazonia) (Glaser et al., 1998, 2000) up to 45 % in some chernozemic soils from Germany (Schmidt et al., 1999), and up to 60% in black Chernozem from Canada (Saskatchewan) (Ponomarenko and Anderson, 1999) 

uiuc.edu

webh2o.sws.uiuc.edu

web.archive.org