Characteristics of Low-frequency Debris Flow in Mountain Area of Western Sichuan Province
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    Abstract:

    Debris flow can be divided into three types according to its outbreak frequency:high-frequency( one or many times in a year),medium-frequency(one time in several to 30 years),and low-frequency(one time in more than 30 years).Low-frequency debris flow often burst fiercely without any anticipation and cause serious harm.Based on the analysis of the data from debris flow gullies with different outbreak frequencies,the characteristics of low-frequency debris flow are summarized.Watersheds with Low-frequency debris flow are characterized by high vegetation coverage and a small number and small-scale of adverse geological phenomena.The groove bed scour of low-frequency debris flow is dominant and erosion rate and sediment transport capacity are high.Understanding the characteristics of low-frequency debris flow has important significance in guiding debris flow prevention.

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林明安,王士革,范晓岭,卢铖昀.川西地区低频率泥石流的特征[J].水土保持通报英文版,2010,(1):227-230

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History
  • Received:March 18,2009
  • Revised:July 21,2009
  • Adopted:
  • Online: November 26,2014
  • Published: