Water is a natural resource essential for the origin and preservation of life, and despite being a renewable resource, in the last few years there has been an intense concern about its scarcity, since it has lost its ability to recover in a natural way, as many sources of water have been exhausted by improper use. According to Tocantins (2008), the population supply represents 71% of the water demand in the current scenario. According to UNESCO (2017), the approximately percentage of 12% is equivalent to the entire amount of potable water of the world concentrated in the Brazilian territory. Urbanization, soil sealing and the consequent deforestation by soybean monoculture in the municipality of Porto Nacional, result in a number of environmental problems, such as: soil erosion, basin siltation and climate change. The degree of siltation suffered by these impoundments in recent years has been decreasing its useful volume, with consequences on the quality and quantity of water available for abstraction. In this context, it is of great importance the study of methods that quantify the degree of sedimentation of these impoundments (Silveira, et al., 2009). The sediment is of extreme importance as an indicator of the level of pollution when it is considered that the crop launches the agrochemicals or the industries launch their dumping in the aquatic environments, especially when there is no inspection. According to Esteves (2011), the sediment can register the pollution occurred in the water in the previous days. The mineralogical characteristics are defined according to NBR-6508, the granulometric scale that divides the soils into the following fractions: clay, silt, fine sand, medium sand, coarse sand and gravel. The granulometric analysis, quantified in sediment samples, is related to the evaluation of the mineralogical characteristics that compose the limnological matrix, to verify the presence of silt, sand and clay. According to CETESB (2007), a greater quantity of fines, represented by high amounts of silt, clay and smaller sand, constitute a significant possibility of finding contaminants that allow the measurement of the quality of the sediment present in the water body, since the size of the particle influences the adsorption and retention of contaminants, as there is the tendency that when the grain decreases, the concentrations of nutrients and contaminants increase.