Effects of Different Inflow Rate Patterns and Distributions of Grass Strips on Runoff and Sediment in an Engineering Accumulation Body

2021 ◽  
Author(s):  
Lou YongCai ◽  
Gao ZhaoLiang ◽  
Tong Wu ◽  
XingYuan Qi
Keyword(s):  
Water Loss ◽  
Sediment Yield ◽  
Water Conservation ◽  
Inflow Rate ◽  
Soil And Water Loss ◽  
Runoff Reduction ◽  
Strip Pattern ◽  
Sediment Reduction ◽  
Soil And Water ◽  
Grass Strip

Abstract Engineering accumulation bodies are critical sources of artificial soil and water loss. The objectives of this study were to evaluate the effects of different inflow rate patterns and distributions of grass strips on runoff and sediment in engineering accumulation bodies. A field runoff plot (20 m long, 1 m wide, and 0.5 m deep) was used for inflow simulation experiments under four inflow rate patterns (even, rising, falling, and rising-falling) and five grass strip patterns (patterns Ⅰ-Ⅴ). The results showed that the changing trends of runoff rate and sediment yield increased with increasing inflow rate and decreased with reduction for the same grass strip pattern. Although the inflow rate pattern affected runoff and sediment yield, it had no significant effect on the total runoff and sediment. The influence of the grass strip pattern on runoff and sediment was significantly higher than that of the inflow rate pattern. The runoff reduction and sediment reduction effects of grass strip patterns were 12.23 to 49.62% and 12.92 to 80.54%, respectively. When grass strips were distributed on a slope in bands (pattern Ⅴ), the soil and water conservation effects were ideal, reducing the average runoff and sediment by 44.98% and 58.09%, respectively. Sediment reduction caused by decreasing runoff (SRR) was the main factor controlling erosion and sediment yield. This study can guide the configuration of vegetation control measures for soil and water loss in engineering accumulation bodies.

scholarly journals Effects of water and soil conservation works on runoff and sediment variation in the areas with high and coarse sediment yield of the middle Yellow River

2018 ◽  
Vol 38 ◽  
pp. 01033
Author(s):  
Wei Ying Sun ◽  
Pan Zhang ◽  
Li Li ◽  
Jiang Nan Chen
Keyword(s):  
Sediment Yield ◽  
Water Conservation ◽  
Human Activities ◽  
Soil Conservation ◽  
Yellow River ◽  
Soil And Water Conservation ◽  
Contribution Rate ◽  
Rainfall Variation ◽  
Runoff Reduction ◽  
Soil And Water

The areas with high and coarse sediment yield of the middle Yellow River is well known for its severe erosion, high sediment yields. Since 1982 when the 8 key soil and water conservation harnessing regions has been built, the ecological environment has been gradually improved and the amount of sediment and runoff entering the Yellow River has been reduced continuously. Some researchers considered that it was owing to the water and soil conservation works (WSCW), while others believed that it was caused by the rainfall variation, but this has not been quantified for the effect respectively. This paper deals with the effects of WSCW on runoff and sediment variation. The study has been carried out in the Sanchuanhe River watershed, where was listed as one of the 8 key soil and water conservation harnessing regions. The results show that the contribution rate of human activities was 80.2% after 1st harnessing stage (1970-1979), 43.0% after 2nd harnessing stage (1980-1989), in 3rd harnessing stage (1990-1996) it reached 98.4%, and was 44.8% after 4th harnessing stage (1997-2006). With regard to the influence on runoff reduction in the watershed, the contribution rate of human activities was 62.5% compared with the natural factors after 1st harnessing stage (1970-1979), 28.4% after 2nd harnessing stage (1980-1989), in 3rd harnessing stage (1990-1996) it reached 69.6%, and was 37.0% after 4th harnessing stage (1997-2006). The results revealed that human activities exerted the largest effects on the sediment reduction and explained 66.6% of the variation in the specific sediment yield. This study suggests that a combination of human activities and rainfall variation effectively reduces runoff and sediment delivery of the Loess Plateau. Generally The runoff reduction and contribution of rainfall variation to runoff reduction in this area were as large as human activities. After many years' harnessing the great benefit have been obtained in water and soil loss control in this watershed.

Soil and Water Conservation Society and the Construction of Ecological Civilization City

2014 ◽  
Vol 977 ◽  
pp. 290-294 ◽  
Author(s):  
Zhi Qiang Yu ◽  
Qiang Gao ◽  
Wen Feng Ding
Keyword(s):  
Soil Erosion ◽  
Social Construction ◽  
Water Loss ◽  
Water Conservation ◽  
Soil And Water Conservation ◽  
Ecological Civilization ◽  
Soil And Water Loss ◽  
The Social ◽  
The City ◽  
Soil And Water

In recent years , with the acceleration of the process of China's modernization cities , soil erosion and lead to many more serious environmental problems . This paper describes the harm to the social construction of ecological civilization city soil and water loss,analyzed the causes of soil erosion,and finally illustrates the importance of soil and water conservation of the city and puts forward some suggestions for the construction of soil and water conservation.

Characterization and Evaluation of Soil Erosion in Shenzhen: Using Environmental Radionuclides

2014 ◽  
Vol 522-524 ◽  
pp. 211-222
Author(s):  
Jun Jie Li ◽  
Ding Qiang Li ◽  
Mu Ning Zhuo
Keyword(s):  
Soil Erosion ◽  
Water Loss ◽  
Water Conservation ◽  
Urban Soil ◽  
Land Development ◽  
Wide Distribution ◽  
Distribution Area ◽  
Soil And Water Loss ◽  
Unique Method ◽  
Soil And Water

Nuclear tracer technology is quantitative and it has a high priority, which provides a unique method for understanding the mechanism of urban soil and water loss.137Cs +210Pbexcombination tracer was applied to study the characterization and evaluation of soil Erosion in Shenzhen. The results indicate that the following: 1)Disturbances from urbanization has greatly changed surface soil in Shenzhen.137Cs background inventory in Shenzhen range at 99 Bq/m2-653 Bq/m2. 2)210Pbexbackground inventory increase with altitude rise, which is attributed to the movement of water vapor. 3)Soil erosion in Shenzhen has a wide distribution area and exacerbated by severe human disturbance. Land development and steep orchard are key factors that influence urban soil and water loss. 4)Shenzhen should strictly carry out projects for soil and water conservation, such as returning steep slopes into forests and grasslands, and other ecological management reforms.

scholarly journals Study on Soil and Water Conservation and Governance of Urban Inland Rivers: A Case Study of Nakau River Basin Governance

2020 ◽  
Vol 145 ◽  
pp. 02032
Author(s):  
Yiyuan Zhang ◽  
Dong Li ◽  
Yan Sun ◽  
Ronghua Tang ◽  
Yongxin Nong
Keyword(s):  
River Basin ◽  
Water Loss ◽  
Water Conservation ◽  
Soil Conservation ◽  
Control Measure ◽  
Effective Prevention ◽  
Soil And Water Loss ◽  
Water And Soil Conservation ◽  
Inland Rivers ◽  
Soil And Water

Taking the Nakau River Basin Governance Project as the research area, the problems existing in the Nakau River Basin, the key and difficult points of water and soil conservation management, and the measures and implementation effects of water and soil conservation in urban rivers are discussed. According to the characteristics of soil and water loss in the inland rivers of the city, an effective prevention and control measure system was proposed, which ultimately effectively prevented human-induced soil and water loss during the construction of the project, protected water and soil resources, guaranteed the safe operation of the main project, and maintained and improved the regional ecology surroundings.

scholarly journals Research Progress on Soil Erosion and Socioeconomic Correlation

2020 ◽  
Vol 145 ◽  
pp. 02031
Author(s):  
Yan Sun ◽  
Junbo Xiao ◽  
Yiyuan Zhang ◽  
Wenhao Lai ◽  
Min Wei ◽  
...  
Keyword(s):  
Soil Erosion ◽  
Social Development ◽  
Water Loss ◽  
Water Conservation ◽  
Water Environment ◽  
Soil And Water Conservation ◽  
Research Progress ◽  
Soil And Water Loss ◽  
The One ◽  
Soil And Water

Soil erosion and socio-economic interacts with each other. Soil and water loss destroys land resources, causes non-point source pollution, affects the recycling and utilization of water resources, worsens the water environment, and even causes natural disasters such as collapse, landslides, and debris flows. Soil erosion affects regional socio-economic development. On the one hand, economic and social development has caused a sharp increase in people’s demand for the development and utilization of natural resources, which has increased the occurrence of soil and water loss; on the other hand, economic and social development has promoted people’s understanding of soil erosion and soil and water conservation, enabling people to consciously change their production and lifestyle, and having sufficient funds to invest in soil and water conservation and reduce soil erosion.

scholarly journals Effect of Biochar on Soil and Water Loss on Sloping Farmland in the Black Soil Region of Northeast China during the Spring Thawing Period

2021 ◽  
Vol 13 (3) ◽  
pp. 1460
Author(s):  
Pengfei Yu ◽  
Tianxiao Li ◽  
Qiang Fu ◽  
Dong Liu ◽  
Renjie Hou ◽  
...  
Keyword(s):  
Soil Erosion ◽  
Water Loss ◽  
Water Conservation ◽  
Field Experiments ◽  
Field Capacity ◽  
Application Rate ◽  
Frozen Soil ◽  
Soil And Water Loss ◽  
Sloping Farmland ◽  
Soil And Water

Biochar, as a kind of soil amendment, has attracted wide attention from scholars in various countries, and the effects of biochar on soil and water loss have been well reported. However, soil erosion is significantly affected by geographical conditions, climate, and other factors, and research on the characteristics of soil erosion and the effects of biochar application in seasonally frozen soil areas is currently unclear. The purpose of this study was to explore the effect of corn straw biochar application on soil and water conservation during the spring thawing period. Specifically, through field experiments, the addition of 0, 6, and 12 kg m−2 biochar on slopes of 1.8, 3.6, 5.4, and 7.2° and the effects on runoff and the soil erosion rate of farmland were analyzed. The results showed that in the 6 and 12 kg m−2 biochar addition treatments, the saturated water content of the soil increased by 24.17 and 42.91%, and the field capacity increased by 32.44 and 51.30%, respectively. Compared with the untreated slope, with an increase in biochar application rate, runoff decreased slightly, and soil erosion decreased significantly. This study reveals that biochar can be used as a potential measure to prevent soil and water loss on sloping farmland in cold regions.

scholarly journals Vulnerability Assessment of Soil and Water Loss in Loess Plateau and Its Impact on Farmers’ Soil and Water Conservation Adaptive Behavior

2018 ◽  
Vol 10 (12) ◽  
pp. 4773 ◽  
Author(s):  
Xiaohui Huang ◽  
Lili Wang ◽  
Qian Lu
Keyword(s):  
Soil Erosion ◽  
Loess Plateau ◽  
Water Loss ◽  
Water Conservation ◽  
Positive Impact ◽  
Soil And Water Conservation ◽  
The Loess Plateau ◽  
Soil And Water Loss ◽  
Conservation Technology ◽  
Soil And Water

Analyzing vulnerability and adaptation to soil and water loss is an important part of the study on the human–environment relationship in the Loess Plateau. It has also provided a new perspective for studying the farmers’ adoption behavior of soil and water conservation technology in the soil erosion area of the Loess Plateau. Based on the Turner vulnerability framework, this paper constructs a household-scale index system of soil and water loss vulnerability in the Loess Plateau and evaluates the soil and water loss vulnerability in the Loess Plateau using the field survey data of the Loess Plateau applied entropy method. Finally, we use the binary logistic model to estimate the impact mechanism of farmers’ soil erosion vulnerability on farmers’ adoption behavior of soil and water conservation technology. The main conclusions are as follows: (1) In the total sample, susceptibility > exposure > adaptability, whereas in the Shaanxi and Gansu subsample, susceptibility > adaptability > exposure. The Ningxia subsample was similar to the total sample. For each index, Ningxia > Gansu > Shaanxi; (2) The exposure and susceptibility of soil and water loss have a positive impact on farmers’ adoption behavior of soil and water conservation technology, and natural capital has a positive impact on farmers’ adoption behavior of soil and water conservation technology. Physical capital has a positive impact on farmers’ adoption behavior of biological measures. Financial capital has a negative impact on farmers’ adoption behavior of biological measures and farming measures. Social capital has a positive impact on farmers’ adoption behavior of engineering measures and biological measures; (3) Overall, the marginal effect of the adoption behavior of farmers’ soil and water conservation techniques, adaptability > susceptibility > exposure. Therefore, it is necessary to strengthen the monitoring of soil and water loss, encourage the government and farmers to respond in time, and reduce the losses caused by soil erosion. Enriching the capital endowment of farmers, breaking through the endowment restriction of farmers’ adoption of soil and water conservation technology.

scholarly journals Research Progress on Soil and Water Loss and Soil and Water Conservation in Karst Areas

2020 ◽  
Vol 145 ◽  
pp. 02030
Author(s):  
Yan Sun ◽  
Yiyuan Zhang ◽  
Sigao Li ◽  
Nan Zhang ◽  
Junming Wang
Keyword(s):  
Soil Erosion ◽  
Water Loss ◽  
Water Conservation ◽  
Clean Energy ◽  
Soil And Water Conservation ◽  
Karst Area ◽  
Research Progress ◽  
Soil And Water Loss ◽  
Karst Areas ◽  
Soil And Water

Based on the research of soil erosion and soil and water conservation in karst areas in China in recent years, the status and progress of soil erosion and soil and water conservation in karst areas in China are discussed. The results show that the soil and water loss in the karst area mainly has two types of soil erosion: surface soil erosion and underground soil erosion. Soil and water loss management in karst areas mainly adopts measures to adjust land use structure, increase vegetation coverage, carry out slope-to-ladder construction, and promote clean energy applications. Different governance models should be adopted for different landform types, different landform parts, different slopes, and different levels of rocky desertification in karst areas.

Effect of Eco-Grass Planting on Soil and Water Conservation on the Bare Slope of Mountainous Area in Beijing

2012 ◽  
Vol 518-523 ◽  
pp. 4695-4700
Author(s):  
Tie Jun Sun ◽  
Baderihu Tajilake
Keyword(s):  
Water Loss ◽  
Water Conservation ◽  
Chemical Properties ◽  
Ecological Engineering ◽  
Soil And Water Conservation ◽  
Mountainous Area ◽  
Soil Infiltration ◽  
Soil And Water Loss ◽  
Reservoir Watershed ◽  
Soil And Water

There was less vegetation on the bare slope of mountainous area due to sterile soil in Beijing than other places. Soil and water loss was so serious that vegetation restoration became important one of ecological engineering. So experiment was executed to plant eco-grass on the bare slope in Miyun reservoir watershed and Guanting reservoir watershed, and study effect of eco-grass on soil and water conservation. The results indicated that vegetation restored quickly on the bare slope of mountainous area after eco-grass planted for a year, roughness length on the earth’s surface increased, and soil and water loss reduced clearly. Meanwhile soil bulk density reduced, and soil infiltration and available nutrients increased obviously. So soil physical and chemical properties improved batter in a short time than no eco-grass.

Sign in / Sign up

Export Citation Format

Share Document