首页> 外文会议>Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment >Calibration of infrasound monitoring system and acoustic characteristics of debris-flow movement by field studies
【24h】

Calibration of infrasound monitoring system and acoustic characteristics of debris-flow movement by field studies

机译:次声监测系统的标定和泥石流运动的声学特性,通过实地研究

获取原文

摘要

Naturally occurring infrasounds produced by debris flows are explored in this study by examining the field data both in Jiangjia Gully, Yunnan and Houyenshan, Taiwan, respectively. Infrasound propagates to long distance in the atmosphere at the speed of sound for the low adsorption in the air and the high reflectivity of the ground. The infrasonic signals induced by debris flows are related to the magnitude and composition of the failure zone as well as the slope areas. In Jiangjia Gullies, the peak frequency of infrasounds is about 6 Hz when debris flow discharges are less than 500 m3/s. While the peak frequency decreases with the increasing discharge of debris flows. The stony debris flows occur in Houyenshan with the peak frequencies between 5-15 Hz during the surges. Non-stationary acoustic signals of the debris flows are analyzed by adopting the HHT approach.
机译:通过研究分别位于云南江家沟和台湾后燕山的现场数据,探索了由泥石流产生的自然发生的次声。次声以声音的速度在大气中传播到很远的距离,这是因为空气中的低吸附性和地面的高反射率。泥石流引起的次声信号与破坏区的大小和组成以及坡度有关。在江家沟壑区,当泥石流流量小于500 m3 / s时,次声的峰值频率约为6 Hz。而峰值频率随着碎屑流排放的增加而降低。石质泥石流发生在后缘山,浪涌期间的峰值频率在5-15 Hz之间。采用HHT方法分析了泥石流的非平稳声信号。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号