川西地区低频率泥石流的特征
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水利部公益性行业科研专项经费“岷江上游滑坡泥石流溃坝洪水监测与防御”(200801032);国家自然科学基金项目“非集中固体物质补给的低频率泥石流形成机理研究”(40871054)


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

    泥石流按其暴发频率分为高频率(每年发生一次或多次)、中频率(数年至30a发生一次)和低频率(30a以上发生一次)泥石流3类。低频率泥石流具有暴发周期长,规模大,危害严重等基本特点。选取川西地区不同频率的泥石流沟道进行对比研究,结果表明,该区低频率泥石流还具有两个典型特征:低频率泥石流流域具有植被覆盖度高,不良地质现象数量少且规模小的特点;低频率泥石流在侵蚀过程中以沟床冲刷为主且侵蚀速度快,泥砂输移比高。关于低频率泥石流上述两点特征的研究,对泥石流的预防和治理有重要指导意义。

    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,2010,(1):227-230

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  • 收稿日期:2009-03-18
  • 最后修改日期:2009-07-21
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  • 在线发布日期: 2014-11-26
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