2007
DOI: 10.1016/j.still.2006.06.007
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Morphology parameters of ephemeral gully in characteristics hillslopes on the Loess Plateau of China

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Cited by 75 publications
(42 citation statements)
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“…Furthermore, ephemeral gullies can accelerate interrill and rill erosions via increasing the local slope gradient after several void-filling cycles Poesen et al, 2003). On the Chinese Loess Plateau, especially on steep slopes, ephemeral gullies approximately contribute to 35-70% of the slope soil loss (Cheng et al, 2007;Gong et al, 2011). A better understanding of ephemeral gully erosion processes and their potential effect is of paramount importance to identify the innate characteristics of soil erosion on the Loess Plateau.…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, ephemeral gullies can accelerate interrill and rill erosions via increasing the local slope gradient after several void-filling cycles Poesen et al, 2003). On the Chinese Loess Plateau, especially on steep slopes, ephemeral gullies approximately contribute to 35-70% of the slope soil loss (Cheng et al, 2007;Gong et al, 2011). A better understanding of ephemeral gully erosion processes and their potential effect is of paramount importance to identify the innate characteristics of soil erosion on the Loess Plateau.…”
Section: Introductionmentioning
confidence: 99%
“…In the last decades, the importance of gully erosion has been widely recognized (Capra et al, 2009;Cheng et al, 2007;Daggupati et al, 2014;Nachtergaele et al, 2001;Stefano et al, 2013;Woodward, 1999). Poesen et al (2003) distinguished ephemeral gullies from rills by a critical cross-sectional area of 929 cm 2 (1 ft 2 ), while others defined it with a critical width, such as 0.3 m (Brice, 1966) or 0.5 m (Imeson and Kwaad, 1980).…”
Section: Introductionmentioning
confidence: 99%
“…Since the 1950s, much attention has been paid to loess landforms from geological and geomorphological viewpoints. Some scholars investigated the regional variation of soil erosion and the stages of geomorphological developmental of landforms in the Loess Plateau (Stolte et al, 2003;Xu et al, 2004;Cheng et al, 2007;Chen et al, 2008;Zheng et al, 2008;Chen et al, 2010;Hughes et al, 2010;Liu and Liu, 2010;Fu et al, 2011;Zhu, 2012;Xiong et al, 2013). Liu (1985) investigated profiles of loess deposits for the three typical landforms in the Loess Plateau (hill, ridge, and tableland), and found that the sedimentary environment of loess deposits, including the underlying bedrock paleotopography, has been related to climate change.…”
Section: Introductionmentioning
confidence: 99%