3 results

Sediment source tracing in a Brazilian subtropical catchment using diffuse reflectance: Effect of spectral ranges, pre-processing techniques, and multivariate model

Rafael Ramon ORCID logo , Olivier Evrard ORCID logo , Jean Paolo Gomes Minella ORCID logo , Cláudia Alessandra Peixoto de Barros ORCID logo , Jean Michel Moura-Bueno ORCID logo , Gabriela Naibo ORCID logo , [...]

11/Oct/2024

ABSTRACT Agriculture intensification in Southern Brazil’s subtropical regions combined with the frequent occurrence of erosive rainfall has rendered the area a global water erosion hotspot. In this scenario, understanding and regulating erosion processes at the river catchment scale is critical for mitigating soil and water resource degradation. Traditional methods for tracing sediment sources are expensive and time-consuming and justify the development of alternative approaches. Therefore, in this study, we employed diffuse reflectance spectroscopy analyses in the ultraviolet-visible (UV-VIS), near-infrared (NIR), […]

Visual Abstract

Interril erosion from area under burned and green sugarcane harvested by hand and mechanically

Marcos Vinícios Garbiate, Antonio Carlos Tadeu Vitorino, Bruno Andrade Tomasini, Anderson Cristian Bergamin, Elói Panachuki

01/Dec/2011

Although a number of studies related to environmental issues address air pollution, the increased use of biotechnology and mechanical harvesting of sugar cane, less attention has been paid to the negative environmental impacts caused by laminar erosion. This study aimed to determine the levels of organic matter (OM) and nutrients (P, K, Ca and Mg) in sediment and runoff water from interrill erosion from different sugarcane harvest systems (green and burnt cane), on a loamy Dystrophic Red Latosol (Oxisol). The […]

Flow hydraulics and sediment transport in rills of a sandy clay loam soil

José Ramon Barros Cantalice, Elemar Antonino Cassol, José Miguel Reichert, Ana Luiza de Oliveira Borges

01/Jul/2005

Rill erosion is characterized by concentrated surface water flow, with enough shear stress and detachment capacity to deform the rill and alter flow hydraulics, responsible for rill formation dynamics. The objective of this study was to evaluate flow hydraulic conditions that can provide important information on erosion relationships, soil erodibility and sediment transport in furrows of a recently-tilled Palleudult. Rills were pre-formed in a sandy clay loam soil with an average slope of 0.067 m m-1. Simulated rainfall with an intensity of […]