Relações entre precipitação, escoamento e sedimentos suspensos na bacia do Rio das Antas, Goiás

• Autor(a) principal: Didonet, Thais Teodoro dos Santos Cordeiro
• Data de Publicação: 2017
• Tipo de documento: Dissertação
• Idioma: por
• Título da fonte: Repositório Institucional da UFG
• dARK ID: ark:/38995/001300000d28s
• Texto Completo: http://repositorio.bc.ufg.br/tede/handle/tede/7881
• topic: Histerese; Granulometria; Hidrossedimentologia; Concentração média do evento; Hysteresis; Granulometry; Hydrosedimentology; Event mean concentration; ENGENHARIA HIDRAULICA::HIDROLOGIA

Sediments transported by surface runoff and by rivers are essential components in the comprehension of changes in a river basin and the quality of aquatic systems. The high variability of rainfall events, the SSC and the relation between them produce complex behavioral dynamics difficult to interpret but the study of these aspects is a useful and frequently used tool in the quantification of impacts due to erosive and hydrossedimentological processes. The main objective of this study was to characterize and quantify the hydrological, sedimentological and granulometric characteristics of the urban watercourse of the Rio das Antas basin, located in Anápolis, Goiás, wich faces various erosion processes. Continuous monitoring of precipitation, flow rates, sediment concentrations and turbidity was performed using pluviographs, linigraphs, an automatic sampler and a laser granulometer during most of a rainy season, where samples were collected and 14 events were analyzed. Descriptive statistical analyzes, identification of hysteresis patterns, Event Mean Concentration, “first flush” phenomenon effects and grain size distribution and their relationships with precipitations and flow rates were performed. The peak concentration of total sediments reached 3,380 mg L -1 , and approximately 83% were suspended sediments. No “first flush" has been recorded in any event. The highest mean concentration observed for suspended sediments was 1,714.6 mg/m3 and the mean of the events was 1,001.3 mg/m3, values considered to be high when compared to river basin flows, where the highest was 15.49 m 3 s -1 . The maximum flow rates were determinant in the total sediment, however, the same flow range carried very different amounts of suspended sediments during the floods. This behavior suggests that the variation also depends on precipitation characteristics and sediment sources. In the hysteresis analyzes, it can be verified that these sources are located farther from the monitoring point, but are also the river itself, since the most frequent hysteresis loop was "Figure Eight" followed by the"Counter Clock-wise” type. There were complex hysteretic loops characterized by multiple peaks of flow and sediments. The size of particles carried by the flow varies throughout the rainy season. The suspended sediment particles had dimensions between 0.0019 mm and 0.990 mm being characterized as sandy silt material. The small and medium particles were more frequent in final events and larger particles occurred in the middle of the period. Finner particles were more present during the rise of the hydrograph and in the recession phase the amount of particles with dimensions between 0.2 mm e 0.6 mm increased in some events. Particles larger than 0.6 mm were not related to precipitation. It was also observed that the amount of dissolved solids decreases with increasing particle size and may indicate that larger particles have less capacity to absorb/adsorb other pollutants. It is observed that the suspended sediments vary between the events and within the same event and depends on the hydrological behavior, the characteristics of the water body and the type of monitoring.