Laboratory apparatuses for the analysis of infiltration and runoff enable studies under controlled environments and at reduced costs. Unfortunately, the design and construction of such systems are complex and face difficulties associated with the scale factor. This paper presents the design, construction, and evaluation of a portable rainfall and runoff simulator. The apparatus allows the evaluation of unsaturated soils with and without vegetation cover, under a wide range of simulation scenarios. The apparatus also enables the control of the intensity, size, and uniformity of simulated raindrops for variable surface slope, specimen thickness, and length conditions. The monitoring of the volumetric water content and matric suction and a rigorous computation of water balance are ensured. The obtained results indicate that the automated rainfall generator produces raindrops with Christiansen uniformity coefficients higher than 70%, and with an adequate distribution of raindrop sizes under a range of rainfall intensities between 86.0 and 220.0 mm h⁻¹. The ideal rainfall generator conditions were established for a relatively small area equal to or lower than 1.0 m² and considering rainfall events with return periods of 10 to 100 years.

Interception by vegetation is one of the main variables controlling hydrological and geo-environmental problems such as erosion, landslides and floods. Interception, along with precipitation and evapotranspiration, is required for the modeling of infiltration, percolation and runoff. Unfortunately, the measurement of interception in the field is time consuming, burdensome and subject to testing parameters with relatively high variability. In this context, experiments using rainfall simulators (RSs) have the potential to provide an alternative approach that addresses most of the limitations of field experiments. This paper presents a new approach to evaluate interception that combines a RS and the monitoring of the wetting front using pore-water pressure instrumentation at specific locations of the specimen. Two specimens are required, one with and another without vegetation. The proposed approach was applied to Paspalum notatum (bahiagrass) and a tropical soil. The results indicated an average interception of 5.1 mm of the simulated rainfall for a slope at 15 degrees, rainfall intensity of 86 mm h⁻¹, and duration of 60 min. Furthermore, the vegetation decreased the surface runoff that contributes to erosion. The proposed method will enable studies on the interception mechanisms and the various involved variables, with benefits to the modeling of soil-vegetation-atmosphere interaction.

RESUMO O crescimento desordenado das cidades e o excesso de impermeabilização são problemáticas dos grandes centros urbanos, tendo como consequência principal a ocorrência de inundações e alagamentos. Nesse contexto, a modelagem hidrodinâmica pode ser uma importante ferramenta para a determinação de áreas inundáveis, permitindo estimar as cotas de inundação para diferentes cenários de tempos de retorno (TR) e chuvas de projetos, permitindo, assim, representar mais fielmente a realidade e minimizar erros decorrentes de projetos hidráulicos. Trabalhando em conjunto com o Sistema de Informações Geográficas (SIG), em que a geometria do canal é extraída por meio do Modelo Digital do Terreno (MDT) de alta precisão gerado por levantamento com técnica LiDAR (Light Detection and Ranging) e software de modelagem hidrodinâmica (Hydrologic Engineering Center — River Analysis System — HEC-RAS), foi possível avaliar diferentes cenários de inundações no trecho canalizado em concreto, no córrego Botafogo, em Goiânia, Goiás. Com os resultados da modelagem hidrodinâmica foi possível avaliar o comportamento da propagação das vazões geradas, constatando-se que para precipitações com TR de 50 anos ou mais, os limites da canalização não suportam os volumes gerados e transportados, provocando inundações em seis trechos críticos. Os dados obtidos pelo HEC-RAS puderam ser validados a partir de registros fotográficos divulgados pela imprensa local e levantamento topográfico dos locais inundados, de modo que a integração entre o SIG e a modelagem hidrodinâmica se mostrou eficiente para o estudo de áreas inundáveis.

The phenomena of infiltration and the percolation of water in the soil are of fundamental importance for the evaluation of runoff, groundwater recharge, evapotranspiration, soil erosion and transport of chemical substances in surface and groundwater. Within this context, the quantitative determination of the infiltration values is extremely important for the different areas of knowledge, in order to evaluate, mainly the surface runoff. Several types of changes in vegetation cover and topography result in significant changes in the infiltration process, making it necessary to use mathematical models to assess the consequences of these changes. Thus, this article aims to implement the Green-Ampt model using two numerical methods - Newton-Raphson method and W-Lambert function - to determine soil permeability parameters - K and matric potential multiplied by the difference between initial and of saturation - comparing them to the real data obtained in simulations using an automatic rainfall simulator from the Federal University of Goiás - UFG. The Green-Ampt model adjusted well to the data measured from the rain simulator, with a determination coefficient of 0.978 for the Newton-Raphson method and 0.984 for the W-Lambert function.