PEDOSPHEREEffect of Land Use on Soil Erosion and Nutrients in Dianchi Lake Watershed, China
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Cited by (30)
Novel sediment source fingerprinting quantifying erosion-induced total nitrogen and total phosphorus outputs from an intensive agricultural catchment, North China
2023, International Soil and Water Conservation ResearchCitation Excerpt :The previous studies have supported our findings. By comparing soil erosion and its effects on soil nutrients under different land use types (forestland, abandoned land, arable land and grassland) in the Shuanglongliu Area of Dianchi Lake, researchers found that the greatest loss of nutrients is due to erosion during tillage in the cultivated farmland (Niu et al., 2015). The study of erosion on small watershed in hilly and gully region of Loess Plateau revealed that the TN and TP in farmland soil decreased in the last 18 years.
An extreme drought event homogenises the diatom composition of two shallow lakes in southwest China
2020, Ecological IndicatorsCitation Excerpt :There are several factors that can affect the binding and mobility of 137Cs in lake sediments. Catchment disturbances and erosion increase the influx of soil material and 137Cs (e.g., Niu et al., 2015). Depending on the mineral composition of the soil material, the binding of 137Cs in soils and lake sediments can be increased or decreased.
<sup>137</sup>Cs estimates of soil erosion rates in a small catchment on a channelized river floodplain in the lower reaches of Yangtze River, China
2019, Journal of Environmental RadioactivityCitation Excerpt :In the last decades, the use of 137Cs measurements in China has focused on 137Cs activity concentrations in soil around a Nuclear Power Plant (NPP) (Lu et al., 2006), determining the 137Cs reference inventory (Tang et al., 2006), investigating the spatial distribution of 137Cs inventory (Zhao et al., 2012), developing the 137Cs simplified erosion and transport models (Yin and Ji, 2015). The method has also been used to estimate soil erosion and deposition rates in weak soil-resistance regions, such as the Tibet Plateau (Wang et al., 2014), the Loess Plateau (Feng et al., 2010), the Three Gorges Reservoir (Ju et al., 2013), the Karst region (Yan et al., 2012; Feng et al., 2016), as well as regions of different soil types including black soils (An et al., 2014), red soils (Niu et al., 2015), and alpine meadows soils (Wang et al., 2017). A significant number of natural and human-induced factors affecting soil erosion have been discussed in relation to rainfall, slope gradient, slope length, soil properties, land use and land cover change (LUCC), tillage depth and pattern, and soil sampling style (Li M et al., 2009; Fang et al., 2012; Li Y et al., 2015).