Yuguo Han

Prof. Dr. Yuguo Han

Key Laboratory of State Forestry Administration on Soil and Water Conservation, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China

Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2013 in Chemosphere
Verified
Journal Article
Closed access
YHYuguo Han
Yuguo Han
XYXinxiao Yu
Xinxiao Yu
XWXiaoxue Wang
Xiaoxue Wang
YWYunqi Wang
Yunqi Wang
JTJinxia Tian
Jinxia Tian
CWChengzhi Wang
Chengzhi Wang

15 September 2012 in Environmental Earth Sciences
Verified
Journal Article
Closed access
PDF file
YHYuguo Han
Yuguo Han
XYXinxiao Yu
Xinxiao Yu
PYPeiling Yang
Peiling Yang
BLBo Li
Bo Li
LXLei Xu
Lei Xu
CWChengzhi Wang
Chengzhi Wang

1 June 2020 in Environmental Pollution
Verified
Journal Article
Closed access
WXWeimin Xing
Weimin Xing
YHYuguo Han
Yuguo Han
ZGZifan Guo
Zifan Guo
YZYue Zhou
Yue Zhou

12 January 2015 in Irrigation and Drainage
Verified
Journal Article
Closed access
PDF file
LYLinlin Yang
Linlin Yang
YHYuguo Han
Yuguo Han
PYPeiling Yang
Peiling Yang
CWChengzhi Wang
Chengzhi Wang
SYShengmin Yang
Shengmin Yang
CXCongying Xiao
Congying Xiao

26 September 2018 in Water
Verified
Journal Article
Open access
PDF file
YHYuguo Han
Yuguo Han
GFGary Feng
Gary Feng
Ying OuyangYing Ouyang
Ying Ouyang
Rainfall is a major dynamic source of soil erosion and nutrient loss on slopes. Soil and water conservation practices and agricultural activities can change the soil surface morphology and thus affect erosion and nutrient losses. This study focused on the effects of several typical soil and water conservation practices and agricultural land, for the purpose of: (1) determining how these practices prevent erosion and nutrient loss and identifying the hydrodynamic mechanisms; and (2) determining the application conditions for different practices. Runoff, sediment, total nitrogen (TN) and total phosphorus (TP) in fish-scale pits, agricultural land, narrow terraces, shrub cover and bare land, under rainfall events in rainy seasons (from May to November) during the 2010–2015 period, were monitored. Slope hydrodynamic mechanisms and application conditions of these practices were also investigated. The results showed that compared with bare land, fish-scale pits performed the best in preventing runoff, sediment, TN and TP, followed by 30% shrub coverage, narrow terraces and agricultural land, successively. Total runoff, sediment, TN and TP losses in fish-scale pits site were 19.70%, 2.03%, 10.10% and 35.97% of those in bare land of the same area, respectively. Soil and water conservation practices could change the hydraulic characteristics of slopes, decrease Re (Reynolds) and Fr (Froude) numbers, thereby decreasing runoff, sediment, TN and TP losses. Fish-scale pits were suitable for the areas with small single rainfall and good water permeability. When rainfall was greater than 60 mm, narrow terraces had highest efficiency in reducing sediment loss; therefore, they were suitable for the areas with relatively high rainfall intensity and soils similar to the sandy loams of the study area. As to the practice of covering land with plants, the effect was sustainable due to the plants’ long-term growth. Agricultural land was not recommended since the losses on it were relatively higher due to the impact of human activities. In reality, these practices may be applied in combination so as to effectively control water, soil and nutrient losses.

1 June 2019 in CATENA
Verified
Journal Article
Closed access
MAMiaoying An
Miaoying An
YHYuguo Han
Yuguo Han
LXLei Xu
Lei Xu
XWXiuru Wang
Xiuru Wang
CAChang Ao
Chang Ao
DPDanbo Pang
Danbo Pang