Journal
JOURNAL OF SOILS AND SEDIMENTS
Volume 14, Issue 7, Pages 1298-1310Publisher
SPRINGER HEIDELBERG
DOI: 10.1007/s11368-014-0903-7
Keywords
Physically basedmodel; Soil erosion; Soil management and conservation; Sediment yield
Categories
Funding
- FAPERGS-Fundacao de Amparo Pesquisa do Estado do Rio Grande do Sul
- CNPq-Conselho Nacional de Desenvolvimento Cientifico e Tecnologico
- SINDITABACO-Sindicato das Industrias do Tabaco
Ask authors/readers for more resources
Purpose Hydrosedimentological modeling is a tool that can be used to understand better important processes occurring at the catchment scale, such as runoff and sediment yield. The aim of this study was to use the Limburg Soil Erosion Model (LISEM) to describe the runoff and sediment yield during rainfall-runoff events in a small rural catchment in southern Brazil. Materials and methods The study was conducted in the Lajeado Ferreira Creek catchment (drainage area of 1.19 km(2)) where intense land use has caused a negative impact on water resources. Thirteen rainfall-runoff events that occurred in 2010 and 2011, including high-magnitude events, were used to model hydrosedimentological processes. Results and discussion Results from the calibration and validation stages indicate that the model had a good performance when representing the hydrograph, including events with greater complexity. The use of a second soil layer in the model increased its efficiency, which is in accordance with the importance of subsurface flow in this catchment and its sensitivity to the physical properties of the soil, which are essential for controlling hydrosedimentological processes at the catchment scale. The simulation of sediment yield was overestimated by the model, constrained by the lack of sensitivity of the model to soil cohesion and the stability of soil aggregates. During the model calibration stage, these parameters had values different from those measured in the field. Conclusions The LISEM model performed well in representing runoff for events of different magnitudes. The discretization of the physical-hydrologic properties in the soil profile enabled the evaluation of the effect of subsurface impediment layers on water infiltration and runoff. The simulation was less accurate for suspended sediment concentration than for runoff. This indicates the need for further studies to either identify other factors controlling erosion and sediment yield that have not been identified by the model, or identify if the representation of the physical parameters is inadequate, especially the values of soil cohesion and aggregate stability.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available