Hydrologic Response to Land Use and Land Cover Change Scenarios: An Example from the Paraopeba River Basin Based on the SWAT Model
Human land use land cover changes (LULCCs) can cause impacts on watershed lands and on water resources. The regions with land use conflict suffer more intense erosion processes due to their high slope and drainage density. The study intends to evaluate scenarios with an absence of land use conflict...
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Veröffentlicht in: | Water (Basel) 2023-04, Vol.15 (8), p.1451 |
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creator | Costa, Renata Cristina Araújo Santos, Regina Maria Bessa Fernandes, Luís Filipe Sanches Carvalho de Melo, Marília Valera, Carlos Alberto Valle Junior, Renato Farias do Silva, Maytê Maria Abreu Pires de Melo Pacheco, Fernando António Leal Pissarra, Teresa Cristina Tarlé |
description | Human land use land cover changes (LULCCs) can cause impacts on watershed lands and on water resources. The regions with land use conflict suffer more intense erosion processes due to their high slope and drainage density. The study intends to evaluate scenarios with an absence of land use conflict and verify if it can contribute to reductions in surface runoff, avoiding the carriage of tailings to river channels. In the study, the SWAT model was used in the hydrological modeling of the Paraopeba River watershed affected by the rupture. The results show that the SWAT model was able to reproduce the flow data with good and very good performances. The quality indicators in the calibration step were NSE = 0.66, R2 = 0.69, PBIAS = 5.2%, and RSR = 0.59, and in the validation, step were NSE = 0.74, R2 = 0.77, PBIAS = 13.5%, and RSR = 0.51. The LULCC from 2000 to 2019 led to a 70% increase in lateral runoff (LATQ) and a 74% decrease in aquifer groundwater. The scenario of land use capability and no conflict can reduce lateral runoff by 37% and increase water infiltration by 265%, minimizing the point and diffuse contamination of the tailings in the Paraopeba river channel. |
doi_str_mv | 10.3390/w15081451 |
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The regions with land use conflict suffer more intense erosion processes due to their high slope and drainage density. The study intends to evaluate scenarios with an absence of land use conflict and verify if it can contribute to reductions in surface runoff, avoiding the carriage of tailings to river channels. In the study, the SWAT model was used in the hydrological modeling of the Paraopeba River watershed affected by the rupture. The results show that the SWAT model was able to reproduce the flow data with good and very good performances. The quality indicators in the calibration step were NSE = 0.66, R2 = 0.69, PBIAS = 5.2%, and RSR = 0.59, and in the validation, step were NSE = 0.74, R2 = 0.77, PBIAS = 13.5%, and RSR = 0.51. The LULCC from 2000 to 2019 led to a 70% increase in lateral runoff (LATQ) and a 74% decrease in aquifer groundwater. The scenario of land use capability and no conflict can reduce lateral runoff by 37% and increase water infiltration by 265%, minimizing the point and diffuse contamination of the tailings in the Paraopeba river channel.</description><identifier>ISSN: 2073-4441</identifier><identifier>EISSN: 2073-4441</identifier><identifier>DOI: 10.3390/w15081451</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Agricultural production ; Agriculture ; Aquifers ; Brazil ; Calibration ; Contamination ; drainage ; Drainage density ; Drinking water ; Groundwater ; humans ; Hydrology ; Land cover ; Land use ; land use and land cover maps ; Land use planning ; Mine tailings ; Precipitation ; River basins ; Rivers ; Runoff ; Soil and Water Assessment Tool model ; Soil erosion ; Surface runoff ; Tailings ; Topography ; Water infiltration ; Water quality ; Water resources ; Watersheds</subject><ispartof>Water (Basel), 2023-04, Vol.15 (8), p.1451</ispartof><rights>COPYRIGHT 2023 MDPI AG</rights><rights>2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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The regions with land use conflict suffer more intense erosion processes due to their high slope and drainage density. The study intends to evaluate scenarios with an absence of land use conflict and verify if it can contribute to reductions in surface runoff, avoiding the carriage of tailings to river channels. In the study, the SWAT model was used in the hydrological modeling of the Paraopeba River watershed affected by the rupture. The results show that the SWAT model was able to reproduce the flow data with good and very good performances. The quality indicators in the calibration step were NSE = 0.66, R2 = 0.69, PBIAS = 5.2%, and RSR = 0.59, and in the validation, step were NSE = 0.74, R2 = 0.77, PBIAS = 13.5%, and RSR = 0.51. The LULCC from 2000 to 2019 led to a 70% increase in lateral runoff (LATQ) and a 74% decrease in aquifer groundwater. 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The regions with land use conflict suffer more intense erosion processes due to their high slope and drainage density. The study intends to evaluate scenarios with an absence of land use conflict and verify if it can contribute to reductions in surface runoff, avoiding the carriage of tailings to river channels. In the study, the SWAT model was used in the hydrological modeling of the Paraopeba River watershed affected by the rupture. The results show that the SWAT model was able to reproduce the flow data with good and very good performances. The quality indicators in the calibration step were NSE = 0.66, R2 = 0.69, PBIAS = 5.2%, and RSR = 0.59, and in the validation, step were NSE = 0.74, R2 = 0.77, PBIAS = 13.5%, and RSR = 0.51. The LULCC from 2000 to 2019 led to a 70% increase in lateral runoff (LATQ) and a 74% decrease in aquifer groundwater. The scenario of land use capability and no conflict can reduce lateral runoff by 37% and increase water infiltration by 265%, minimizing the point and diffuse contamination of the tailings in the Paraopeba river channel.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/w15081451</doi><orcidid>https://orcid.org/0000-0002-7633-0714</orcidid><orcidid>https://orcid.org/0000-0002-2399-5261</orcidid><orcidid>https://orcid.org/0000-0001-8261-2470</orcidid><orcidid>https://orcid.org/0000-0001-5096-0550</orcidid><orcidid>https://orcid.org/0000-0001-8454-5400</orcidid><orcidid>https://orcid.org/0000-0003-0774-5788</orcidid><orcidid>https://orcid.org/0000-0002-9486-7160</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Agricultural production Agriculture Aquifers Brazil Calibration Contamination drainage Drainage density Drinking water Groundwater humans Hydrology Land cover Land use land use and land cover maps Land use planning Mine tailings Precipitation River basins Rivers Runoff Soil and Water Assessment Tool model Soil erosion Surface runoff Tailings Topography Water infiltration Water quality Water resources Watersheds |
title | Hydrologic Response to Land Use and Land Cover Change Scenarios: An Example from the Paraopeba River Basin Based on the SWAT Model |
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