Assessment of soil erosion by RUSLE in the Ecuadorian basins (2001−2020) based on GIS and high-resolution satellite data: Main drivers and changes on soil erosion

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Daniel Delgado , Mahrez Sadaoui , Wolfgang Ludwig , Williams Méndez , Eduardo Ortiz-Hernández , Pablo Farfán-Intriago
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引用次数: 0

Abstract

Soil erosion is a significant environmental problem that can have devastating impacts on ecosystems and the sustainability of agricultural lands, including landscape degradation and biodiversity loss. Estimating erosion rates requires the installation of measurement devices such as sediment traps and runoff collectors or the use of erosion plots considering soil texture and vegetation cover. However, these procedures have significant spatial and temporal limitations, in addition to high implementation costs. The objective of this study was to analyze soil erosion in Ecuadorian basins using the Revised Universal Soil Loss Equation (RUSLE) based on Geographic Information System (GIS) and high-resolution satellite data from 2001 to 2020. The methodology involved delineating and evaluating the environmental characteristics of Ecuadorian basins, precipitation data, soil physical and chemical properties, identification of the Normalized Difference Vegetation Index (NDVI), land use, Digital Elevation Model (DEM) selection and assigning values based on slope raster. Basin delineation was obtained from regional literature; precipitation data from GPM-IMERG web servers; sand, clay, silt, and Soil Organic Carbon (SOC) content from SoilGrids web servers; DEM from SRTM database; spatial-temporal distribution of NDVI and land use from MODIS database; and P Factor value ranges based on slope from global literature. Recorded erosion rates ranged from 0.28 t/ha year to 2373.85 t/ha year, with the highest values identified in the Andes Mountains due to steep slopes. The main driver of soil erosion in Ecuadorian basins was the R-Factor, followed by LS and C. Land use variations indicated a loss of 9771 km2 of forests and 80 km2 of cultivated lands between 2001 and 2020, while semi-natural vegetation increased by 9851 km2. These results provide relevant information to assist land managers in making decisions to address this natural phenomenon.
以地理信息系统和高分辨率卫星数据为基础,通过 RUSLE 评估厄瓜多尔流域(2001-2020 年)的土壤侵蚀情况:土壤侵蚀的主要驱动因素和变化
土壤侵蚀是一个严重的环境问题,会对生态系统和农业用地的可持续性造成破坏性影响,包括景观退化和生物多样性丧失。估算水土流失率需要安装沉积物收集器和径流收集器等测量装置,或使用考虑到土壤质地和植被覆盖的侵蚀地块。然而,这些方法除了实施成本高昂外,还存在很大的空间和时间限制。本研究的目的是根据地理信息系统 (GIS) 和 2001 年至 2020 年的高分辨率卫星数据,使用修订的通用土壤流失方程 (RUSLE) 分析厄瓜多尔流域的土壤侵蚀情况。该方法涉及厄瓜多尔盆地环境特征的划分和评估、降水数据、土壤物理和化学特性、归一化植被指数(NDVI)的确定、土地利用、数字高程模型(DEM)的选择以及基于坡度栅格的赋值。流域划分来自区域文献;降水数据来自 GPM-IMERG 网络服务器;沙、粘土、粉土和土壤有机碳 (SOC) 含量来自 SoilGrids 网络服务器;DEM 来自 SRTM 数据库;归一化差异植被指数 (NDVI) 的时空分布和土地利用情况来自 MODIS 数据库;基于坡度的 P 因子值范围来自全球文献。记录的侵蚀率从 0.28 吨/公顷/年到 2373.85 吨/公顷/年不等,其中安第斯山脉的陡坡侵蚀率最高。土地利用的变化表明,2001 年至 2020 年期间,森林面积减少了 9771 平方公里,耕地面积减少了 80 平方公里,而半自然植被面积增加了 9851 平方公里。这些结果提供了相关信息,有助于土地管理者做出应对这一自然现象的决策。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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