Anthropogenic mountain forest degradation and soil erosion recorded in the sediments of Mayinghai Lake in northern China

CATENA ◽  
2021 ◽  
Vol 207 ◽  
pp. 105597
Author(s):  
Xiaozhong Huang ◽  
Xiuxiu Ren ◽  
Xuemei Chen ◽  
Jun Zhang ◽  
Xiaosen Zhang ◽  
...  
2020 ◽  
Author(s):  
Chengzhong Pan ◽  
Lan Ma

<p>The aim of this study was to investigate how the spatial distribution of grass influenced run-off and erosion from a hillslope with loess and cinnamon soils in the rocky area of Northern China. We set up a trial to test the two soils with different treatments, including bare soil (BS), grass strips on the upper (UGS) and lower (DGS) parts of the slope, grass cover over the entire slope (GS), and a grass carpet on the lower part of the slope (GC), under simulated rainfall conditions. The results showed that the run-off coefficients for the loess and cinnamon soils decreased by between 4% and 20% and by between 2% and 37%, respectively, when covered with grass. Grass spatial distribution had little effect on the run-off, but more effect on erosion than vegetation coverage degree. The most effective location of grass cover for decreasing hillslope erosion was at the foot, and the high efficiency was mainly due to controlling of rill formation and sediment deposition. The soil loss from GS, DGS, and GC on the loess and cinnamon soils was between 77% and 93% less and 55% and 80% less, respectively, compared with the loss from BS. However, the soil characteristics had little effect on soil erosion for well-vegetated slopes. The results highlight the importance of vegetation re-establishment at the foot of hillslope in controlling soil erosion.</p>


Geoderma ◽  
2006 ◽  
Vol 136 (3-4) ◽  
pp. 838-851 ◽  
Author(s):  
Chun Chang Huang ◽  
Yaofeng Jia ◽  
Jiangli Pang ◽  
Xiaochun Zha ◽  
Hongxia Su

Water ◽  
2021 ◽  
Vol 13 (17) ◽  
pp. 2334
Author(s):  
Haiyan Fang

Total nitrogen (TN) and total phosphorous (TP) are the main pollutants affecting the water quality of the Miyun Reservoir, Beijing. However, few studies have been conducted on their responses to implemented soil conservation measures at a slope scale in northern China. To explore the impact of soil conservation measures on TN and TP losses, field monitored data from 18 runoff plots under natural rainfalls were used to analyze the changing characteristics of runoff, soil loss, and nutrient losses during 2014–2019. The results indicated that runoff, soil erosion, as well a TN and TP losses from the plots varied significantly, depending on land use and soil conservation measures. Bare plots suffered the highest soil, TN, and TP losses, followed by cultivated plots without soil conservation measures, cultivated plots with contour tillage, and other plots. Event-averaged runoff and soil loss rates ranged from 0 to 7.9 mm and from 0 to 444.4 t km−2 yr−1, and event-averaged TN and TP losses from cultivated plots were the highest, with values of 39.8 and 3.0 kg km−2, respectively. Bare and cultivated plots were the main sediment and nutrient sources. Among the cultivated plots, the terraced plot had the lowest soil and nutrient losses. The vegetated plots had insignificantly lower soil and nutrient losses. Most TN and TP were lost in particulate status from the plots, especially from the plots with soil conservation measures. Soil conservation measures can effectively prevent TN and TP losses. To guarantee water resource use, contour tillage is preferred for the bare and cultivated lands in the study region.


2013 ◽  
Author(s):  
B.K. Sitaula ◽  
P.L. Sankhayan ◽  
B.R. Singh ◽  
O. Hofstad ◽  
N.R. Gurung

2013 ◽  
Vol 726-731 ◽  
pp. 3807-3810
Author(s):  
Zi Jun Li ◽  
Qiao Qin Liu

Soil erosion has been the most prominent issue in Chinas ecological environment. The rocky mountain area of Northern China is an important typical area of soil erosion and one of the most dangerous regions of potential erosion in China characterized by more stones in thinner soils and the land surface is easily reduced to sand gravel or rocky desertification. Concentrated rainfall with frequent rainstorms, broken topography with steep slope and highly dense gully are important natural factors resulting in soil erosion. However, unreasonable land utilization especially slope farmland aggravates soil erosion. Soil erosion results in land degradation, threatens regional water resources security, intensifies regional poverty and restricts socio-economic development. Sloping cultivated land transformation will be the necessary choice for soil and water conservation and ecological construction in this region.


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