Evaluating erosion in an Inceptisol (soil) in Tunja (Boyacá department, Colombia) having different coverage regarding the impact of simulated rainfall
Evaluación de la erosión de un Inceptisol de Tunja con diferentes coberturas al impacto de lluvias simuladas
DOI:
https://doi.org/10.15446/ing.investig.v29n3.15188Keywords:
soil loss, simulator, rainfall, runoff, infiltration (en)pérdida de suelo, simulador, precipitación, escorrentía, infiltración (es)
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The area surrounding the city of Tunja in the Boyacá department has a heterogeneous climate and adverse conditions facilitating erosion. Scarce vegetation cover does little to reduce the impact of the rain and increases runoff. This study was aimed at analysing different types of rainfall coverage, intensity and duration by simulation. A experimental 3x3 Latin square design was used, with 3 rainfall intensities (10, 20 and 30 mm•h-1), 3 rainfall durations (1, 2 and 3 hours) and 3 types of soil coverage (kikuyo, natural coverage, bare). Each Latin square had 3 repetitions, giving a total of 27 experimental units. Significant differences were found between rainfall intensities evaluated; 30 mm•h-1 rainfall intensity generated 2,218.6 kg•ha-1 of soil loss caused by run-off. Kikuyo coverage was the vegetal cover presenting the least soil loss and greatest infiltration (1,019.1 kg•ha-1 soil loss by run-off and 0.88 cm accumulated infiltration). Rainfall duration did not affect soil loss due to run-off and infiltration. Tunja’s annual rainfall pattern showed that 2006 presented the greatest soil loss (46,663 kg•ha-1 for bare soil). This meant that corrective action must be taken quickly by implementing vegetal cover to mitigate the effects of rainfall on exposed soil to reduce the loss of such valuable resource.
Los alrededores de la ciudad de Tunja presentan condiciones climáticas heterogéneas y adversas que posibilitan el proceso de erosión. La poca presencia de cubierta vegetal no disminuye el impacto de las lluvias y favorece fenómenos como la escorrentía. Este estudio tuvo como objetivo analizar diferentes coberturas, intensidades y duraciones de lluvia mediante simulación. Se realizó un diseño experimental de cuadrado latino de 3 x 3, con 3 intensidades de lluvia (10, 20 y 30 mm•h-1), 3 duraciones de lluvia (1, 2 y 3 horas), y 3 tipos de cobertura de suelo (kikuyo, cobertura natural, descubierto), cada cuadrado latino con 3 repeticiones, para un total de 27 unidades experimentales. Se presentaron diferencias significativas entre las intensidades de lluvia evaluadas, la intensidad de 30 mm•h-1de lluvia generó 2.218,6 kg•ha-1 de suelo perdido por escorrentía. La cubierta vegetal que presentó la menor pérdida de suelo y la mayor infiltración fue la cobertura de kikuyo, con valores de 1.019,1 kg•ha-1 de suelo perdido por escorrentía y 0,88 cm de infiltración acumulada. Las duraciones de lluvia no afectaron la pérdida de suelo por escorrentía e infiltración. El patrón anual de lluvias de Tunja mostró que el año 2006 presentó la mayor pérdida de suelo, con 46.663 kg•ha-1 para el suelo descubierto, lo que implica que se deben tomar acciones correctivas rápidamente, mediante la implementación de coberturas vegetales que atenúen el efecto de la precipitación sobre el suelo a libre exposición con el fin de disminuir la pérdida del recurso.
References
Assouline, S., Ben-Hur, M., Effects of rainfall intensity and slope gradient on the dynamics of interrill erosion during soil surface sealing., Catena 66, 2006, pp. 211–220.
Castro, H. E., Fundamentos para el conocimiento y manejo de suelos agrícolas., Produmedios. Tunja, Colombia, 1998, 360p.
De Lima, J. L. M. P., Singh, V. P., Isabel, M., The influence of storm movement on water erosion: storm direction and velocity effects., Catena 52, 2003, pp. 39–56.
De Luis, M., González-Hidalgo, J. C., Raventós, J., Efectos erosivos de una lluvia torrencial en suelos afectados por quemas experimentales de diferente severidad., Rev.C.&G., NO.17, 2003, pp. 57-67.
Ekern, P. C., Rainfall intensity as a measure of storm erosivity., Soil Science Society of America, Proceedings No.18, 1954, pp. 212-216.
Flanagan, D. C., Foster, Moldenhauer, G. R., W.C. Storm pattern effect on infiltration, runoff and erosion., Transactions of the American Society of Agricultural Engineers, Vol. 31, No. 2, 1987, pp. 414–420.
González-Hidalgo, J. C., Los índices de agresividad de la lluvia y su aplicación en la valoración de la erosión del suelo., Sociedad Española de Geomorfología, Geoforma, Logroño, 1996, pp. 37.
Hillel, D., Environmental Soil Physics., Academic Press, New York, 1998.
Jiao, J., Wang, W., Hao, X., Precipitation and erosion features of rainstorms in different patterns on the Chinese Loess Plateau., Journal of Arid Land Resources end Environment, Vol.13, No. 1, (in Chinese with English abstract), 1999, pp. 34–41.
Joseph, L., Pikul, J., Kristian, J. A., Water infiltration and storage affected by subsoiling and subsequent tillage., Soil Sci. Soc. Am. J., Vol. 67, 2003, pp. 859–867.
Kinnell, P. I. A., Raindrop impact induced erosion processes and prediction: a review., Hydrol. Process., Vol. 19, 2005, pp. 2815– 2844.
Kinderknecht, G. A., Paparotti, F., O., Saluzzio F. M., Estudio de la erosionabilidad de un suelo Vertisol mediante el uso de un simulador de lluvia., INTA-EEA Paraná. 2004, pp. 1-11.
Li, Y., Zhu, X. M., Tian, J. Y., Effectiveness of plant roots to increase the antis-scouribility of soil on the Loess Plateau., Chin. Sci. Bull. Vol. 36, (in Chinese), 1991, pp. 2077–2082.
Marqués, M. J., Bienes, R., Jimenez, L., Pérez-Rodríguez, R., Effect of vegetal cover on runoff and soil erosion under light intensity events. Rainfall simulation over USLE plots., Instituto Madrileño de Investigación en
Desarrollo Agrario y Alimentario, Revista Science of the total Environment, 2007, pp. 161-165.
Márques, M. J., Jiménez, L., Alonso-Blázquez, N., García-Estríngana, P., Alegre, J., Bienes, R. Evaluación de la contaminación difusa por metales pesados originada por erosión hídrica en suelos enmendados con lodos de depuradora., In: Bienes R, Marqués MJ, editors. Proceedings of I Simposio Nacional Sobre Control de la Erosión y Degradación del Suelo, Madrid, 2003, pp. 417–21.
Martens, D. A., Relationship between plant phenolic acids released during soil mineralization and aggregate stabilization., Soil Sci. Soc. Am. J., Vol. 66, 2002, pp. 1857-1867.
Martínez-Mena, M., Abadia, R., Castillo, V., Albaladejo, J., Diseño experimental mediante lluvia simulada para el estudio de los cambios en la erosión del suelo durante la tormenta., Rev. C&G, Vol. 15, 2001, pp.1-2.
Meyer, L. D., Rainfall simulators for soil conservation research. En: Soil Erosion Research Methods., R. Lal (ed.), Soil and Water Conservation Society, Ankeny, Iowa, Chapter 4, 1988.
Meyer, G. A., Pierce, J. L., Wood, S. H., Jull, A. J. T., Fire, storms, and erosional events in the Idaho batholith., Hydrological Processes, Vol. 15, 2001, pp. 3025-3038.
Nicolau, J. M., Bienes, R., Guerrero-Campo, J., Aroca, J. A., Gómez, B., Espigares, T., Runoff coefficient and soil erosion rates in croplands in a Mediterranean-continental region, in Central Spain. In: Rubio JL, Morgan RPC, Andreu V, editors., Proceedings of the third International Congress Man and Soil at the Third Millenium, Logroño, Geoforma ediciones, 2002, pp. 1359-68.
Peterson, A. E., Bubenzer, G. D., In: Klute, A. (Ed.), Methods of Soil Analysis., Am. Soc. Agron, Madison, WI. Monograph, No. 9, 1986.
Scott, V. H., Houston, C. E., Measuring Irrigation Water., California Agric. Expt. Station, Circular 473, 1959.
Scott, H. D., Soil Physics., Iowa State University Press, Ames, 2000.
Stomph, T. J., De Ridder, N., Steenhuis, T S., Van de Giesen, N. C., Scale effects of hormonian overland flow and rainfall-runoff dynamics: laboratory validation of a process-based model., Earth Surf Process Landf, 2002, No. 261, pp.1-23.
Wu, W. D., Zheng, S. Z., Lu, Z. H., Effect of plant roots on penetrability and anti-scouribility of red soil derived from Granite., Pedosphere, Vol. 10, 2000, pp. 183–188.
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