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After the 2008 Wenchuan earthquake, a large amount of loose landslide deposits was left in the stricken region. A heavy storm in 2010 turned numerous deposits into debris flows. After 2010, vegetation gradually recovered on the remnant soil deposits. During the wet seasons in 2013 and 2015, the number of debris flows decreased significantly compared with that in 2010. This paper investigates the role...
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