Though riparian areas generally have a shallow water table and higher soil moisture compared to upslope areas, climatic seasonality may trigger water repellency in tropical riparian forests, which, if persistent, could negatively affect essential ecosystem functions related to water resources protection such as reduced overland-flow, sediment transport, and nutrient filtration. The objective of this study was to answer the following: can tropical riparian forests develop water repellency? If so, does water repellency affect infiltration on a seasonal basis? For this, water repellency and infiltration were measured in a grid of 72 points during a dry and a wet month of a tropical riparian forest with a shallow water table in a region with highly marked climatic seasonality. Water repellency and infiltration were significantly different between the wet and dry months. Water repellency affected negatively infiltration in the dry month, its effect in the wet month was insignificant. As a result, a higher infiltration capacity was observed over the wet period. Previous research has claimed that the development and persistence of repellency in soils could promote other hydrological processes such as overland flow. The findings shown here demonstrate that such phenomenon does not persist longer than the dry season.

The Brazilian savanna, regionally known as Cerrado is an important water source due to its spatial position in the highlands known as Planalto Central of Brazil. Yet, the hydrological functioning of such complex ecosystems and its many variations is poorly understood. In this paper, we characterized the soil surface permeability to water under in one of the most common vegetation types: the Cerrado típico which is a type of savanna. In doing so, we measured infiltration capacity using the Mini-Disk infiltrometer (n = 15) and soil resistance to penetration using the Stolf penetrometer (n = 7) in a Latossolo (oxisol) under Cerrado típico located in Brasília (Planaltina), Distrito Federal, Brazil. Our results indicated a high infiltration capacity under Cerrado típico which is potentially associated with a low penetration resistance. This fact might highlight the importance of the natural undisturbed ecosystems, in this case Cerrado típico, as a land-cover which favors hydrological processes which, in turn, promotes soil-groundwater recharge that are inportant to maintain water bodies and reservoirs in the region.

Water infiltration is a key process in groundwater-river recharge. However, it is poorly known in the Brazilian Tropical Savanna (biome with different natural ecosystems, such as savannas, native grasslands, and forests). Thus, we carried out a review on soil water infiltration in different natural ecosystem types within the domains of the Brazilian Tropical Savanna. We collected articles from the Web of Science, Periódicos CAPES, and Scholar Google databases. We found 15 articles (including 22 assays) with studies prevailing in the Midwest region of Brazil. The mean and median infiltration capacity of all studies was 792 and 567 mm h-1, respectively. The majority of the studies (12 articles) did not clearly define which specific type of ecosystem was studied. Furthermore, most of the studies were carried out in Oxisols. Generally, the studies had a low sample size to characterize soil properties. A better description of ecosystem type, as well as a more significant sample size, are needed to understand infiltration in natural ecosystems of the Brazilian Tropical Savanna. Given the limitations of the studies available, our review showed that it is still too early to synthesize and to make an in-depth discussion on such topic in such huge and heterogeneous biome. Infiltração de água nos domínios da Savana Tropical Brasileira: o que realmente sabemos? R E S U M OA infiltração de água é um processo chave na recarga de rios e aquíferos. Entretanto, é pouco conhecido no Cerrado brasileiro (bioma com diferentes ecossistemas naturais, tais como as formações savânicas, campestres e florestais). Assim, realizou-se uma revisão sobre a infiltração de água no solo em diferentes tipos de ecossistemas dentro dos domínios do Cerrado brasileiro. Os artigos coletados foram das bases de dados Web of Science, Periódicos CAPES e Google escolar. Foram encontrados 15 artigos (que incluem 22 ensaios) presentes em sua maioria na região Centro-oeste do Brasil. A média e a mediana da capacidade de infiltração de todos os estudos foram 792 e 567 mm h-1, respectivamente. A maioria dos estudos (12 estudos) não define claramente qual o tipo de ecossistema foi avaliado. Além disso, a maioria dos estudos foram realizados em Latossolos. Em geral, os estudos tiveram um número amostral baixo para caracterizar as propriedades do solo. Diante disso, uma melhor descrição do tipo de ecossistema avaliado, bem como um número amostral mais significativo são necessários para compreender a infiltração de água nos ecossistemas naturais do Cerrado brasileiro. Em razão das limitações dos estudos encontrados, essa revisão mostrou que ainda é cedo para sintetizar e aprofundar a discussão deste tema em um bioma tão grande e heterogêneo.Palavras-chave: fitofisionomia, solo, vegetação nativa.

Plant composition, diversity and structure of riparian forests of Central Brazil are well known. However, little is known about soil physical properties under these forests. This knowledge is important as a baseline for biodiversity restoration and ecosystem services that occur in riparian zones. In order to bridge this gap, here we assessed the infiltration capacity and soil penetration resistance in a plinthic soil under gallery forest in Planaltina, Distrito Federal, Brazil. We measured infiltration capacity (Mini-Disk infiltrometer) and soil penetration resistance (Stolf penetrometer) following linear transects. The plinthic soil had high infiltration capacity and low penetration resistance. Our infiltration estimate is in the middle range when compared to other permeability studies in tropical forests. Like their counterparts, high biological activity along with the lack of disturbance are the likely explanations for such high topsoil permeability to water.