首页|泥石流承灾体群体效应特征反演——以7·12四川平武县黑水沟泥石流为例

泥石流承灾体群体效应特征反演——以7·12四川平武县黑水沟泥石流为例

扫码查看
群体建筑结构的分布格局、结构形式等因素影响泥石流冲击过程和致灾表现.泥石流冲击存在绕流现象、放大作用和遮蔽效应,泥石流与建筑群之间存在复杂的流固耦合模态,但针对这类泥石流承灾体群体效应的过程与机制仍不清晰.本研究通过野外调查、物理实验和数值模拟等方法,调查泥石流承灾体群体效应特征,反演泥石流冲击流场分布和建筑损伤过程,提出了一套建筑群对泥石流的承灾动力响应特征分析方法.研究结果表明:(1)泥石流流场存在放大作用.面对泥石流冲击,建筑群的破坏导致沟道区域流速增加20%,建筑群区域流速增加46%.(2)泥石流流场存在绕流现象.建筑群阻碍泥石流直进输运,导致建筑拐角之间存在局部压力高度集中现象.(3)在建筑群中存在明显的遮蔽效应.失去建筑的上游遮蔽保护可使下游建筑受到的泥石流冲击强度增加120%.(4)泥石流致灾过程中,建筑群周边与内部的泥石流冲击特征差异明显.在建筑群外围,受前排建筑破坏的影响,泥石流流线后排建筑受泥石流冲击时刻提前10 s,泥石流冲击强度增加速率达2.1倍;(5)泥石流对建筑群内建筑冲击强度分为冲击力急剧增加—缓慢增加—逐渐稳定三个阶段,对应泥石流流深增高、缓慢淤积过程.研究结果可以为泥石流易发区村落城镇的建筑规划布局和防灾减灾措施提供科学参考.
Collective Effects of Debris Flow Striking on Structure Clusters Downstream:A Case Study of the Heishui Gully Debris Flow on July 12th in Pingwu County,Sichuan Province,China
The destructive consequence of debris flow striking on structure clusters are subject to the placement of each structure downstream at gully mouth and their structural types.In the process of debris flows running through structure clusters,it exhibits several observable phenomena,such as flow diversion,amplification effect,and shielding action,which are resultants of complex fluid-solid coupling mechanism;unfortunately,there was big unknown to the processes and mechanisms of the collective effects of debris flow on grouped structures.In this study,it introduced an approach to mathematically describing the collective responses of structure clusters under striking of debris flows.It conducted field investigation,indoor experiments,and numerical simulation,then fluid stress field of debris flow was obtained for a proper interpretation of the complex process of structure damages.(1)There was an amplification effect for debris flow running through grouped structures.Under debris flow attacking,damaging structure clusters leaded to an increase of 20%in flow velocity in debris flow channel and a 46%increase inside the structures.(2)There was a flow diverging phenomenon for debris flow running through grouped structures.As debris flow traversing a structure cluster was impeded,it immediately diverged around the block in a circular pattern,leading to a localized pressure concentration at the corners of structures.(3)There was a noticeable shielding action occurred in structure cluster during debris flow running through grouped structure.Without shelter protection from upstream structures,downstream structures experienced a heavy hit of debris flow at a maximum of 120%increase in impact strength.(4)There were noticeable differences in responses of a structure cluster to debris flow striking at the positions of its periphery and interior.At the periphery of a structure cluster,affected by upstream structure ruined by debris flow striking,the immediately downstream structure had a 10 seconds earlier time of being attacked by debris flow,with an impact strength of increasing by 2.1 times.(5)The impact strength of debris flow on a structure cluster could be divided into three stages:rapid increase phase,slow increase phase,and gradual stabilization phase,which corresponded to the process of increasing debris flow depth and slow siltation.The research provide scientific references for construction layout planning and geo-disaster prevention in debris flow-prone areas of mountain villages.

structure clustersthe Heishui gullydebris flowcollective effect

姚鸿坤、邹强、蒋虎、周文韬、陈思谕、周斌

展开 >

中国科学院、水利部成都山地灾害与环境研究所山地自然灾害与工程安全全国重点实验室,成都 610299

中国科学院大学,北京 100049

西南科技大学环境与资源学院,四川绵阳 621010

建筑群 黑水沟 泥石流 承灾动力响应

国家自然科学基金"西部之光"人才培养计划四川省科技厅项目

42171085xbzgzdsys-2021042023YFS0434

2024

山地学报
中科院水利部成都山地灾害与环境研究所 中国地理学会

山地学报

CSTPCD北大核心
影响因子:1.275
ISSN:1008-2786
年,卷(期):2024.42(1)
  • 41