2020
DOI: 10.1080/19475705.2020.1861112
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Spatial–temporal evolution patterns of soil erosion in the Yellow River Basin from 1990 to 2015: impacts of natural factors and land use change

Abstract: This study optimized the slope and slope length factor (LS) and crop management factor (P) of the RUSLE model and then introduced the gravity centre model to analyze the spatial-temporal variation patterns of soil erosion in Yellow River Basin from a new perspective. Results showed that: (1) The improved model of RUSLE with optimized factors of LS and P had better applicability in Yellow River Basin; (2) The average erosion intensity was 2777.5 t/a, which belonged to moderate erosion. The soil erosion intensit… Show more

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Cited by 46 publications
(9 citation statements)
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“…This change has led to a significant increase in vegetation coverage, which has effectively controlled soil erosion intensity in the region. Remote sensing monitoring and soil erosion model estimation have confirmed these findings, demonstrating a clear correlation between changes in vegetation coverage and effective soil erosion control [28,29,35]. However, from a spatial perspective, soil erosion in small catchments in the Loess Plateau exhibits a distinct spatial distribution pattern that is closely associated with land use patterns and watershed topography factors.…”
Section: Discussionmentioning
confidence: 89%
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“…This change has led to a significant increase in vegetation coverage, which has effectively controlled soil erosion intensity in the region. Remote sensing monitoring and soil erosion model estimation have confirmed these findings, demonstrating a clear correlation between changes in vegetation coverage and effective soil erosion control [28,29,35]. However, from a spatial perspective, soil erosion in small catchments in the Loess Plateau exhibits a distinct spatial distribution pattern that is closely associated with land use patterns and watershed topography factors.…”
Section: Discussionmentioning
confidence: 89%
“…When SNDVI > 0, NDVI presents the increasing , and SNDVI<0 indicates declining in NDVI. Mann-Kendall used to determine the significance of trends [29], expressed by the following formula:…”
Section: Trend Analysis and Inspectionmentioning
confidence: 99%
“…The areas with a large negative effect of K ‐factor are concentrated in the central part of the eastern monsoon ecoregion, and the soil type is mainly loess soil. The low organic matter content, low water content, and weak soil erosion resistance of this region are mostly distributed in areas with fragmented topography, high slope, and intensive precipitation with poor soil retention effect (Yang et al, 2021), which has a coercive effect on VCS to a certain extent. The areas with a large positive effect of the K‐ factor are concentrated in the central part of the Tibetan alpine ecoregion, where the soil type is mainly felty soils.…”
Section: Discussionmentioning
confidence: 99%
“…Based on these policies, in the past 20 years, the ecological vulnerability level of the Yellow River Basin showed an irregular downward trend in the whole basin, and the decline was more evident in the middle and upper reaches [9]. The soil erosion intensity generally showed a trend of increasing and then decreasing [10].…”
Section: Introductionmentioning
confidence: 99%