Development of rill erosion on bare sloping farmland under natural rainfall conditions

Rill erosion plays an important role in soil erosion, and studying this process can provide a basis for controlling soil loss on sloping farmland. The objectives of this study were to observe runoff and sediment transport processes during two continuous and two intermittent natural rainfall events a...

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Bibliographic Details
Main Authors: Huang, D. (Author), Zhang, J. (Author), Zhou, L. (Author)
Format: Article
Language:English
Published: Springer Science and Business Media Deutschland GmbH 2022
Subjects:
Online Access:View Fulltext in Publisher
LEADER 02902nam a2200409Ia 4500
001 10.1007-s12665-022-10383-z
008 220510s2022 CNT 000 0 und d
020 |a 18666280 (ISSN) 
245 1 0 |a Development of rill erosion on bare sloping farmland under natural rainfall conditions 
260 0 |b Springer Science and Business Media Deutschland GmbH  |c 2022 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1007/s12665-022-10383-z 
520 3 |a Rill erosion plays an important role in soil erosion, and studying this process can provide a basis for controlling soil loss on sloping farmland. The objectives of this study were to observe runoff and sediment transport processes during two continuous and two intermittent natural rainfall events and to monitor the changing morphological characteristics of rills within a standard runoff plot of bare soil (20 m length, 5 m width, and slope of 10°) at five successive observation times. We found that the processes of runoff and sediment transport presented a pattern with multiple peaks during continuous rainfall events and with a single or two peaks during intermittent rainfall events. The peak runoff and sediment yield rates exhibited a time-lag phenomenon of 1‒12 min compared with instantaneous rainfall intensity. Rills occurred as strip-shapes, V-shapes, and with a tree-branch-like distribution; their widths were mainly 5–20 cm and their depths 0–10 cm. Compared to our initial rill observation, the mean rill length, width, and depth increased by 227%, 26%, and 6%, respectively, after four subsequent rill observations over a period of almost one month. Side-wall collapse erosion was greater than downcutting erosion on the middle slope (section II; 6.67–13.34 m), while rill depth reached a minimum value on the lower slope (section III; 13.34–20 m). These findings help us to understand bare slope runoff and erosion mechanisms and provide a scientific basis for soil erosion modeling of sloping farmland. © 2022, The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature. 
650 0 4 |a Continuous natural rainfall 
650 0 4 |a Continuous natural rainfall 
650 0 4 |a Erosion 
650 0 4 |a Farms 
650 0 4 |a Intermittent natural rainfall 
650 0 4 |a Intermittent natural rainfall 
650 0 4 |a Morphology 
650 0 4 |a Natural rainfalls 
650 0 4 |a Rain 
650 0 4 |a Rainfall condition 
650 0 4 |a Rainfall event 
650 0 4 |a Rill erosion 
650 0 4 |a Rill morphology 
650 0 4 |a Rill morphology 
650 0 4 |a Runoff 
650 0 4 |a Runoff process 
650 0 4 |a Runoff processes 
650 0 4 |a Sediment transport 
650 0 4 |a Sedimentation 
650 0 4 |a Sloping farmlands 
650 0 4 |a Soils 
700 1 |a Huang, D.  |e author 
700 1 |a Zhang, J.  |e author 
700 1 |a Zhou, L.  |e author 
773 |t Environmental Earth Sciences