Atributos físicos e infiltração de água no solo sob eucalipto e pastagem

• Autor(a) principal: Pola, Lunalda Aparecida Vaz
• Data de Publicação: 2024
• Tipo de documento: Dissertação
• Idioma: por
• Título da fonte: Repositório Institucional da Universidade Federal do Espírito Santo (riUfes)
• Texto Completo: http://repositorio.ufes.br/handle/10/17458
• topic: Área(s) do conhecimento do documento (Tabela CNPq); Infiltrômetro de anéis; Latossolo; modelos de infiltração; mudança de uso de solo; subject.br-rjbn

Understanding water infiltration into the soil is of great importance for adopting the best soil and water management practices. Therefore, this study aimed to evaluate the physical attributes and infiltration behavior in a soil under eucalyptus compared to its previous use as pastureland. Infiltration was determined through ring infiltrometer tests at three different positions in the terrain, with three infiltration tests conducted at each position. To characterize the soil, soil density, total porosity, macroporosity, microporosity, particle size distribution, total organic carbon, and penetration resistance were determined. Instantaneous infiltration equations were adjusted using the Kostiakov, Kostiakov-Lewis, Horton, and Philip models. The β values found for Horton were used to calculate the average β and applied to the equations along with field data; the same approach was used with the average β along with the average Tie. Exploratory analysis included clustering of points by Euclidean Distance, Principal Component Analysis, and Pearson correlation. To evaluate the difference between terrain positions, the data underwent ANOVA and Tukey's test at a 5% significance level. The difference between land uses was assessed using the ANOVA F-test at a 5% significance level. Model performance was assessed using the coefficient of determination (R²), Nash-Sutcliffe efficiency coefficient (NSE), square root of the mean squared error (RMSE) and mean absolute error (MAE). There was no statistical difference between the lower, middle, and upper positions of the areas, indicating homogeneity. Stable infiltration rates were moderate for both areas, with no statistical difference (63.13 and 95.16 mm h-1 , for eucalyptus and pasture, respectively). Area differences were more related to their physical properties, especially macroporosity, microporosity, clay, and sand content. The adjustments made showed good performance in most study points for the Kostiakov, Kostiakov-Lewis, and Horton models, with Horton being the most faithful to infiltration. The Philip model did not fit the field data well and performed the worst, with a mean MAE of 25.48 mm h-1 for the eucalyptus area and 47.98 mm h-1 for the pasture area. Adjustments of the Horton equation using the average β resulted in an MAE of 15.64 mm h-1 for the eucalyptus area and 33.95 mm h-1 for the pasture area. Using the average β along with the average Tie increased the MAE to 25.54 mm h-1 for eucalyptus and 68.05 mm h-1 for the pasture area, therefore, its application is recommended only for the area under eucalyptus.