The dynamic response of splash erosion to aggregate mechanical breakdown through rainfall simulation events in Ultisols (subtropical China)

CATENA ◽  
2014 ◽  
Vol 121 ◽  
pp. 279-287 ◽  
Author(s):  
Ren-Ming Ma ◽  
Zhao-Xia Li ◽  
Chong-Fa Cai ◽  
Jun-Guang Wang
Water ◽  
2019 ◽  
Vol 11 (6) ◽  
pp. 1228 ◽  
Author(s):  
María Fernández-Raga ◽  
Julián Campo ◽  
Jesús Rodrigo-Comino ◽  
Saskia D. Keesstra

For the study of soil erosion it is important to set up the experiments well. In the experimental design one of the key factors is the choice of the measurement device. This is especially important when one part of the erosion process needs to be isolated, such as for splash erosion. Therefore, the main aim of this research is to list the general characteristics of the commonly used splash erosion devices and to discuss the performance, to be able to relate them, and make suggestions regarding their use. The devices we selected for this comparative comparison were: the splash cup, funnel, Morgan tray, Tübingen cup, tower, and the gutter. The devices were tested under the same conditions (rainfall characteristics, slope, and soil type) to assess their hydrological response under different intensities of simulated rainfall. All devices were installed on a sloping plot (10°) with sandy soil, and were exposed to 10 min. of simulated rain with intensities ranging from 60 to 172 mm/h to measure the splashed sediment, and to describe problems and differences among them. The results showed that the Tübingen cup was the best performing device to measure kinetic energy of the rain, but, because of its design, it is not possible to measure the detached splashed sediment under natural (field) conditions. On the other hand, the funnel device showed a significant relation with rain intensity because it loses little sediment to washing. In addition, the device is easy to use and cheap. Therefore, this device is highly recommended to estimated splash erosion. to the good performance measuring the actual splash erosion, because it loses little sediment by washing. The device is also cheap and easy to install and manage.


2010 ◽  
Vol 16 (3) ◽  
pp. 1107-1121 ◽  
Author(s):  
HAO SHENG ◽  
YUSHENG YANG ◽  
ZHIJIE YANG ◽  
GUANGSHUI CHEN ◽  
JINSHENG XIE ◽  
...  

2017 ◽  
Vol 68 (6) ◽  
pp. 797-805 ◽  
Author(s):  
H. Xiao ◽  
G. Liu ◽  
M. A. M. Abd-Elbasit ◽  
X. C. Zhang ◽  
P. L. Liu ◽  
...  

Water ◽  
2020 ◽  
Vol 12 (9) ◽  
pp. 2318
Author(s):  
Yanjun Wang ◽  
Fan Yang ◽  
Shenglin Qi ◽  
Jinhua Cheng

Splash erosion is an important soil erosion process in sloping lands. This study aims to improve the model of rain splash transport based on the results of previous studies and field experiments involving rainfall simulation. A field study was conducted to examine the effects of rainfall properties, herbaceous cover and surface flow on splash processes on hillslopes in northern China. On the basis of the experimental results, a comprehensive model of rain splash was established through the quantitative analysis of the interactive effects of rainfall kinetic energy, vegetation coverage and overland runoff depth on splash erosion rate and the probability density of splashed particles and maximum splash distance. The results showed that the estimated and observed values of splash transport exhibit high consistency and adaptability. However, several discrepancies were observed between the estimated and observed values for events with high vegetation coverage. These differences can be ascribed to the variation in overland runoff connectivity and the differences in soil surface cohesion at various wetness degrees. The proposed model provides insights into splash erosion characteristics and suggestions for erosion control practices on hillslopes.


Author(s):  
Edward Seckel ◽  
Ian A. M. Hall ◽  
Duane T. McRuer ◽  
David H. Weir
Keyword(s):  

1991 ◽  
Vol 1 (1) ◽  
pp. 63-77 ◽  
Author(s):  
M. Nifle ◽  
H. J. Hilhorst

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