Traçando a origem de sedimentos de reservatórios usando propriedades magnéticas no Sudeste do Brasil
DOI:
https://doi.org/10.5433/1679-0359.2020v41n3p847Palavras-chave:
Ambiente tropical, Erosão do solo, Fontes de sedimentos, Recursos naturais.Resumo
Determinar a origem de solos erodidos é essencial para projetar estratégias efetivas de controle da erosão do solo que preservem os recursos do solo, aumentem a produtividade agrícola e reduzam os impactos negativos da erosão do solo, em campo e fora dele. As propriedades magnéticas têm sido amplamente utilizadas em ambientes temperados para identificar fontes, vias e elos de sedimentos, mas existem pouquíssimas aplicações em ambientes tropicais. Portanto, neste trabalho investigamos fontes de sedimentos de reservatórios na Bacia do Alto Rio Grande, Sudeste do Brasil, utilizando técnicas de rastreamento de sedimentos baseadas em parâmetros magnéticos (suscetibilidade magnética de baixa e alta freqüência, susceptibilidade dependente da freqüência). Os diferentes materiais de origem e condições de intemperismo tropical resultaram em solos com diferentes minerais de óxido de Fe e teores de óxidos de Fe, promovendo variabilidade magnética que permitiu a comparação e identificação de possíveis fontes de sedimentos de reservatórios para reduzir os impactos da erosão hídrica. Os resultados indicam a adequação das propriedades magnéticas como um traçador para estudos de erosão do solo em ambientes tropicais.Downloads
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Dearing, J. A. (1999). Environmental magnetic susceptibility: using the Bartington MS2 system (2nd ed.). Kenilworth: Chi Publishing.
Dearing, J. A., Bird, P. M., Dann, R. J. L., & Benjamin, S. F. (1997). Secondary ferrimagnetic minerals in Welsh soils: a comparison of mineral magnetic detection methods and implications for mineral formation. Geophysical Journal International, 130(3), 727-736. doi: 10.1111/j.1365-246X.1997.tb01867.x
Deasy, C., Titman, A., & Quinton, J. N. (2014). Measurement of flood peak effects as a result of soil and land management, with focus on experimental issues and scale. Journal of Environmental Management, 132(2014), 304-312. doi: 10.1016/j.jenvman.2013.11.027
Environmental Systems Research Institute (2010). ArcGIS Desktop: Release 10.1. Redlands, CA: Environmental Systems Research Institute.
Ferreira, M. M., Fernandes, B., & Curi, N. (1999). Influência da mineralogia da fração argila nas propriedades físicas de Latossolos da região sudeste do Brasil. Revista Brasileira de Ciência do Solo, 23(3), 515-524. doi: 10.1590/S0100-06831999000300004
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Guzmán, G., Quinton, J. N., Nearing, M. A., Mabit, L., & Gómez, J. A. (2013). Sediment tracers in water erosion studies: current approaches and challenges. Journal of Soils and Sediments, 13(4), 816-833. doi: 10.1007/s11368-013-0659-5
Hatfield, R. G., & Maher, B. A. (2008). Suspended sediment characterization and tracing using a magnetic fingerprinting technique: Bassenthwaite Lake, Cumbria, UK. The Holocene, 18(1), 105-115. doi: 10.1177/0959683607085600
Hatfield, R. G., & Maher, B. A. (2009). Fingerprinting upland sediment sources: particle size‐specific magnetic linkages between soils, lake sediments and suspended sediments. Earth surface processes and landforms, 34(10), 1359-1373. doi: 10.1002/esp.1824
Jain, S. K., & Singh, V. P. (2003). Water resources systems planning and management. Amsterdam: Elsevier.
Kämpf, N., & Curi, N. (2000). Óxidos de ferro: indicadores de ambientes pedogênicos e geoquímicos. In R. F. Novais, V. H. Alvarez, & C. E. G. R. Schaefer (Eds.), Tópicos em ciência do solo, 1 (pp. 107-138). Viçosa, MG: Sociedade Brasileira de Ciência do Solo.
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2020-04-07
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Lima, P. L. T., Silva, M. L. N., Quinton, J., Armstrong, A., Inda, A. V., Batista, P. V. G., … Curi, N. (2020). Traçando a origem de sedimentos de reservatórios usando propriedades magnéticas no Sudeste do Brasil. Semina: Ciências Agrárias, 41(3), 847–864. https://doi.org/10.5433/1679-0359.2020v41n3p847
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