Study on mechanism of regulation measures on water erosion process in the slope system

Author(s):  
Guo-qiang Yu ◽  
Zhan-bin Li ◽  
Liang Pei ◽  
Peng Li ◽  
Xia Zhang
Author(s):  
U. Akbarova

The distribution area of water erosion has been determined, factors causing creation and intensification of erosion process have been identified in Lankaran region in this article. It was known that a main reason in intensification of erosion process in Lankaran region is anthropogenic factor. Trus, ill-considered human economic activity, replacement of natural forest cover with agricultural crops, untimely and improper organization of antierosion control measures have led to a decrease in soil quality and productivity, as well as accelerated erosion processes.  The mountainous, foothill and plain areas of Lankaran region, which are the object of research, are at risk of water erosion. The total area of the region is 636,3 thousand hectares. Of this, 266,5 thousand hectares, or 41,9% were subject to various degrees of erosion. 


Fractals ◽  
1996 ◽  
Vol 04 (03) ◽  
pp. 385-392 ◽  
Author(s):  
R. LI ◽  
H. TAKAYASU ◽  
H. INAOKA

We study numerically the water erosion process under a variety of conditions. The water erosion model that we use leads to a universal exponent describing the fractal basin area distribution in the steady state.


2021 ◽  
Author(s):  
Pan Zhang ◽  
pingqing Xiao

<p>Coarse sediment of the Yellow River in the complex erosion area of the Pisha sandstone region of the Ordos Plateau is deposited on the downstream riverbed, posing a threat to the flood control safety of the river. The study of sediment particles in this erosion process can deepen the understanding of the erosion process, provide a theoretical basis for the establishment of an erosion prediction model, reveal the internal law of composite erosion, and guide the planning and design of soil and water conservation and the allocation of soil and water conservation measures. In this study, complex erosion indoor tests were carried out through the artificial rainfall-wind-freezing-thawing cycle solid model. The enrichment rate (ER), fractal dimension, and median diameter (d<sub>50</sub>) of soil particles were used to quantify the size distribution characteristics of sediment particles under different erosion dynamics. The coarse sediment was first transported in the process of soil erosion because of the special texture and terrain characteristics of Pisha sandstone soil. Moreover, the degree of heterogeneity of sediment under complex erosion was larger than that under water erosion. The effect of wind could aggravate the instability of the erosion dynamic system. Under the combined action of freezing-thawing, wind, and water, the particle size composition changed greatly, and the erosion energy was extremely unstable. The effect of complex erosion created conditions for the coarse sediment transportation. Under the freezing-thawing-wind-water combined action, the particle size of eroded sediment was the coarsest, and that of water erosion was the smallest. We concluded that the reason why the Pisha sandstone area has become the core area of the concentrated source of coarse sediment in the Yellow River is related not only to the special nature of the Pisha sandstone soil itself but also to the effect of complex erosion.</p>


2020 ◽  
Vol 5 (8(77)) ◽  
pp. 45-51
Author(s):  
Ulkar Zakir Akbarova

The factors causing water erosion have been investigated, an influence of erosion on soil fertility, agrophysical and agrochemical features, complications and economic losses, and also measures against erosion have been offered in this article. It was known that the last results of the erosion process was vividly shown in plants productivity. So, in areas where erosion is developing the plants productivity is 2-5 times lower in comparison with the areas where erosion isnꞌt observed and areas which are cultivated with the high agrotechnical rules. Thus, the agriculture suffers damage. During the research the raindrops and irrigation erosion were widely investigated. It was determined that as a result of the raindrops erosion the soil structure is obliterated, porosity decreases, penetration of water and air into the soil becomes difficult. To prevent from raindrops erosion it is recommended to determine rainfall quantity and intensity on seasons and to provide coverage of soil with the plant. It was determined that the zone slope, granulometric and structural composition, coverage percentage, not following the irrigation norms and rules caused formation and development of irrigation erosion. The research results show that while an amount of the muddy flow is 51,40 g/l in one liter of the flood water, this quantity is 43,50 g/l in the area, where the water consumption is 2,5 l/sec., it is 30,10 g/sec. in 2 l/sec. of water consumption.


2021 ◽  
Vol 51 (5) ◽  
Author(s):  
Guilherme Henrique Expedito Lense ◽  
Taya Cristo Parreiras ◽  
Velibor Spalevic ◽  
Junior Cesar Avanzi ◽  
Ronaldo Luiz Mincato

ABSTRACT: In the state of Rondônia, deforestation, and inadequate soil use and management have intensified the water erosion process, causing degradation of agricultural land. Modeling is a tool that can assist in the adoption of targeted and effective measures for soil and water conservation in the region. In this context, the objective of the research was to model soil losses due to water erosion in the state of Rondônia using the Revised Universal Soil Loss Equation (RUSLE). The parameters related to rain erosivity, relief, erodibility, and soil cover, as well as the conservation practices of the state of Rondônia, were considered. The modeling steps were performed with the aid of the Geographic Information System. Results were validated with data of total sediments transported with water discharge. The estimated total soil loss was about 605 million tons per year, corresponding to an average loss of 22.50 Mg ha-1 year-1. In 19% of the state, the erosion rate was higher than the soil loss tolerance(T), and these areas should be prioritized for adopting measures to mitigate the erosion process. The RUSLE underestimated the generation of sediments at 0.56 Mg ha-1 year-1, which corresponds to an error of 18.60%. Results obtained can assist in the development of different soil use and management scenarios and provide options for policymakers to encourage soil conservation in the state of Rondônia.


Revista EIA ◽  
2021 ◽  
Vol 18 (35) ◽  
Author(s):  
Ricardo Gutierrez Lopez ◽  
Juan José Muciño Porras ◽  
Jose Luis Arellano Monterrosas ◽  
Delva del Rocío Guichard Romero ◽  
Miguel Ángel Aguilar Suárez

Changes in land use and increased intensity of rainfall are factors of greater influence that accelerate the soil erosion process. The application of basin scale sedimentological models integrated to Geographic Information Systems (GIS), is a tool that allows the definition of critical zones, and of this the establishment of measures of control of processes of production and transport of sediments. This study evaluates the water erosion using the Universal Soil Loss Equation (USLE), five scenarios were studied: corresponding to the start of operations of the El Portillo II (1980) dam, and the before and after the two extreme events in the basin (September 1998 and October 2005). The transport of sediments was evaluated by regression, using full annually records (eight years) of flows of two gauging stations in the basin. Overall, variations in erosion rates were observed with changes in the vegetal coverage and statistical homogeneity in the gauging data, which allowed adjust them to a regression model, with correlation coefficient upper to 88%.


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