کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4571005 1629216 2016 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Responses of soil erosion processes to land cover changes in the Loess Plateau of China: A case study on the Beiluo River basin
ترجمه فارسی عنوان
پاسخ های فرآیند فرسایش خاک به تغییرات پوشش زمینی در ورقه لوز چینی: مطالعه موردی حوضه رودخانه بیولو
کلمات کلیدی
تغییرات زمین پوشش، فرآیند فرسایش خاک، شاخص کنتراست موقعیت جغرافیایی، لس پلوتو
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• The vegetation cover experienced a rapid increasing trend in the basin.
• A significant positive correlation exists between LCIs and sediment load modulus.
• Slope gradient and flow length are two important factors in soil erosion processes.
• VC pattern became more reasonable but high risk of soil erosion still exists.

Understanding the responses of soil erosion processes to land cover changes would benefit catchment ecological management. Landsat thematic mapper images in 1987, 1995, and 2007 were collected to obtain the historical normalized difference vegetation index and land cover data of the Beiluo River basin, one of the catchments in the Loess Plateau. The sediment load data of five subcatchments were collected in the corresponding periods. A set of location-weighted landscape contrast indices was used to analyze the effect of land cover changes on soil erosion processes, as specified by the following indices: slope gradient, flow path length, relative altitude, and relative distance. Results showed that vegetation cover (VC) notably increased from 41.12% to 63.43% in the basin from 1987 to 2007. The increased VC was mainly concentrated in the hilly-gully area from 18.40% in 1987 and 20.21% in 1995 to 41.65% in 2007. The mean annual sediment load modulus in the region over the same periods significantly decreased by 90%. All the indices for each subcatchment exhibited a decreasing trend. The change extent of the indices revealed a significantly positive correlation with that of sediment load modulus. Slope gradient and flow path length were the most important influential factors on soil erosion. Results implied that the improvement in land cover in the Beiluo River basin from 1987 to 2007 led to sediment entrapment in the sink area and changed the soil erosion processes, especially the slope gradient and flow length of the soil erosion source area. This study contributed to improving catchment ecological management and evaluating erosion control practices in the Loess Plateau.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: CATENA - Volume 136, January 2016, Pages 118–127
نویسندگان
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