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To model hydrosedimentological dynamics, the SWAT (Soil and Water Assessment Tool) model was used to identify erosion-prone areas, predict soil erosion in the watershed, and evaluate flow and sediment yield at different locations of the river network.
Three types of soil erosion models can be distinguished: theoretical, physics-based, and empirical or statistical models. These models can be divided into three categories based on the physical processes they replicate, the model algorithms that represent these processes, and how much they rely on data [14].
SWAT is a quasi-physically based hydrological model which evaluates the hydrologic balance at the Hydrological Response Unit (HRU) level. HRUs are a subdivision of the watershed that represents homogeneous spatial entities in terms of land use, management, and soil types.
SWAT is a comparatively small-scale model that limits the size of a small watershed or river basin. It can simulate the quality and quantity of surface- and groundwater, and can deliver high-quality spatial description by dividing watershed into numerous subwatersheds.
SWAT is a public domain hydrology model with the following components: weather, surface runoff, return flow, percolation, evapotranspiration, transmission losses, pond and reservoir storage, crop growth and irrigation, groundwater flow, docHub routing, nutrient and pesticide loading, and water transfer.
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The Soil and Water Assessment Tool (SWAT) model is a quasi-physically-based water quality simulation model that predicts the impact of management decisions on water, sediment, and agricultural chemicals in watersheds (Arnold et al., 1998).
SWAT is a physical model that uses mathematical equations to represent watershed processes such as hydrology, soil erosion, crop growth, and nutrient cycling on the land and in the stream network on a daily time scale. The model is spatially-referenced to a specific watershed or sub-watershed.

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