Arid
DOI10.2489/jswc.73.3.353
Hydrological and erosive response of soil surfaces to rainfall intensity as affected by gravel fragment coverage
Sun, J.1,2; Yu, X.1; Fan, D.1; Huang, C.2
通讯作者Yu, X.
来源期刊JOURNAL OF SOIL AND WATER CONSERVATION
ISSN0022-4561
EISSN1941-3300
出版年2018
卷号73期号:3页码:353-362
英文摘要

Gravel fragment cover is an important factor in determining soil erosion rate, particularly in arid and semiarid lands where vegetation coverage is very low. For example, in North China, soil is a shallow gravelly loam with 30% coarse fraction, and gravels affect local agriculture and forestry dramatically. This study was conducted to quantify the effects of gravel fragment coverage on slope erosion. Three rainfall intensities (30, 60, and 90 mm h(-1)) were conducted on five gravel fragment coverages (0%, 10%, 20%, 30%, and 40%) by simulated rainfall. The results showed that both runoff and sediment yield rates decreased significantly with the increase of gravel fragment coverage, and they were negatively correlated with rainfall intensity. Gravel fragment cover reduced cinnamon soil (Haplustalfs) loss from slopes. Equations were established to quantify the effects of rainfall intensity and gravel fragment coverage on runoff and sediment yield. Mean runoff velocity, Reynolds number, and Froude number of gravel fragment-covered slopes varied from 0.88 to 3.17 cm s(-1), 8.35 to 46.21, and 0.21 to 0.59, respectively. They generally increased with increasing rainfall intensity and decreased with increasing gravel fragment coverage. Sediment yield rate was in a logarithmic function with resistance coefficient. Mean shear stress (tau), runoff power (omega) and unit runoff power (P) of gravel fragment-covered slopes ranged from 0.836 to 1.548 Pa, 0.013 to 0.072 N m(-1) s(-1), and 0.003 to 0.009 m s(-1), respectively. Relationships between runoff shear stress and sediment yield rate, and runoff power and sediment yield rate were both linear. The critical shear stress of the bare slope was 0.48 Pa, which was increased by 0.30 to 0.82 Pa in fragment-covered slopes. The critical runoff power of the bare slope was 0.0003 N m(-1) s(-1), and gravel fragment cover increased runoff power by 0.0112 to 0.0187 N m(-1) s(-1). The results of Pearson analysis indicated that Reynolds number was the most sensitive parameter to estimate runoff hydraulic characteristics. In conclusion, gravel cover resulted an effective conservation measure to prevent erosion and conserve rainwater.


英文关键词erosion gravel rainfall intensity runoff
类型Article
语种英语
国家Peoples R China ; USA
收录类别SCI-E
WOS记录号WOS:000437987000016
WOS关键词ROCK FRAGMENTS ; STONE-COVER ; SIMULATED RAINFALL ; SEDIMENT YIELD ; LOESS PLATEAU ; RILL EROSION ; WATER ; INFILTRATION ; RUNOFF ; HYDRAULICS
WOS类目Ecology ; Soil Science ; Water Resources
WOS研究方向Environmental Sciences & Ecology ; Agriculture ; Water Resources
来源机构北京林业大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/211286
作者单位1.Beijing Forestry Univ, Minist Educ, Key Lab Soil & Water Conservat & Desertificat Com, Beijing, Peoples R China;
2.ARS, USDA, Natl Soil Eros Res Lab, W Lafayette, IN USA
推荐引用方式
GB/T 7714
Sun, J.,Yu, X.,Fan, D.,et al. Hydrological and erosive response of soil surfaces to rainfall intensity as affected by gravel fragment coverage[J]. 北京林业大学,2018,73(3):353-362.
APA Sun, J.,Yu, X.,Fan, D.,&Huang, C..(2018).Hydrological and erosive response of soil surfaces to rainfall intensity as affected by gravel fragment coverage.JOURNAL OF SOIL AND WATER CONSERVATION,73(3),353-362.
MLA Sun, J.,et al."Hydrological and erosive response of soil surfaces to rainfall intensity as affected by gravel fragment coverage".JOURNAL OF SOIL AND WATER CONSERVATION 73.3(2018):353-362.
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