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• W4313367958 endingPage "106810" @default.
• W4313367958 startingPage "106810" @default.
• W4313367958 abstract "Benggang is a unique soil erosion landform in the subtropical hilly granite area of South China that seriously endangers the local ecology and environment. In this study, a developing Benggang in South China was selected to explore the spatial variability and the driving factors of the soil saturated hydraulic conductivity (Ks). The results demonstrated that the soil properties of Benggang landforms varied with the soil layer depth and slope position. Only the sand content increased with decreasing distance from the collapsing wall, while the soil organic matter (SOM) content, free iron oxide (Fed) content and cation exchange capacity (CEC) exhibited the opposite trend. Particularly, these parameters exhibited the most significant variation between the middle slope (MS) and lower slope (LS) I and II positions. The Ks values at the LS positions were significantly higher than those at the upper slope (US) and middle slope (MS) positions, and the Ks values first decreased and then increased as the soil layer depth increased. Among the slope positions, the variation in Ks values followed the order of LS II > LS I > US > MS. The Ks values in different directions exhibited notable multifractal characteristics, and the heterogeneity was stronger in the vertical direction than in the horizontal direction. The soil Ks values significantly differed between the different directions at four slope positions, and the values along the vertical direction were higher than those along the horizontal direction at the US and MS sites. However, the values along the horizontal direction were higher than those along the vertical direction at the LS I and LS II sites. Especially at the LS II site, the difference in the soil Ks values between the two directions was extremely significant (P < 0.01). The correlation coefficient values between Ks and the number, area ratio and mean volume of soil macropores were > 0.8. Path analysis revealed that the mean volume of macropores was the main factor affecting the Ks variation. The difference in the soil Ks values at the LS positions could effectively explain the mechanism of headward erosion on the Benggang slope. This study provides a theoretical basis for Benggang erosion control and the prevention of soil erosion in South China." @default.
• W4313367958 created "2023-01-06" @default.
• W4313367958 creator A5003383142 @default.
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• W4313367958 date "2023-03-01" @default.
• W4313367958 modified "2023-10-15" @default.
• W4313367958 title "Variability and driving factors of the soil saturated hydraulic conductivity along the horizontal and vertical directions in the upper catchment of Benggang" @default.
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• W4313367958 cites W1876652137 @default.
• W4313367958 cites W1918071029 @default.
• W4313367958 cites W1965505512 @default.
• W4313367958 cites W1966183442 @default.
• W4313367958 cites W1967496689 @default.
• W4313367958 cites W1967590934 @default.
• W4313367958 cites W1979094291 @default.
• W4313367958 cites W1982235412 @default.
• W4313367958 cites W1988039264 @default.
• W4313367958 cites W1994623683 @default.
• W4313367958 cites W1996885644 @default.
• W4313367958 cites W1996948463 @default.
• W4313367958 cites W2000652503 @default.
• W4313367958 cites W2002920449 @default.
• W4313367958 cites W2005772849 @default.
• W4313367958 cites W2014787799 @default.
• W4313367958 cites W2015726067 @default.
• W4313367958 cites W2017080781 @default.
• W4313367958 cites W2017234021 @default.
• W4313367958 cites W2019469273 @default.
• W4313367958 cites W2021560332 @default.
• W4313367958 cites W2029608510 @default.
• W4313367958 cites W2033732901 @default.
• W4313367958 cites W2033811990 @default.
• W4313367958 cites W2036133799 @default.
• W4313367958 cites W2036589170 @default.
• W4313367958 cites W2038375805 @default.
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• W4313367958 cites W2046268814 @default.
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• W4313367958 cites W2060855932 @default.
• W4313367958 cites W2062733797 @default.
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• W4313367958 cites W2064596878 @default.
• W4313367958 cites W2068810943 @default.
• W4313367958 cites W2069556228 @default.
• W4313367958 cites W2070547953 @default.
• W4313367958 cites W2071796285 @default.
• W4313367958 cites W2082480262 @default.
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• W4313367958 cites W2152615519 @default.
• W4313367958 cites W2167218073 @default.
• W4313367958 cites W2169577049 @default.
• W4313367958 cites W2516519514 @default.
• W4313367958 cites W2547321789 @default.
• W4313367958 cites W2553570509 @default.
• W4313367958 cites W2560130654 @default.
• W4313367958 cites W2614583352 @default.
• W4313367958 cites W2743615736 @default.
• W4313367958 cites W2746634979 @default.
• W4313367958 cites W2802433047 @default.
• W4313367958 cites W2902893073 @default.
• W4313367958 cites W2903229089 @default.
• W4313367958 cites W2905260761 @default.
• W4313367958 cites W2944419715 @default.
• W4313367958 cites W2961088451 @default.
• W4313367958 cites W2965099054 @default.
• W4313367958 cites W2981645372 @default.
• W4313367958 cites W2989326560 @default.
• W4313367958 cites W3014706317 @default.
• W4313367958 cites W3017071916 @default.
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• W4313367958 doi "https://doi.org/10.1016/j.catena.2022.106810" @default.
• W4313367958 hasPublicationYear "2023" @default.
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