在地震引发的山体滑坡后对河流沉积物疏散的控制:来自LiDAR时间序列的观测
Jon Tunnicliffe1, Jamie Howarth2, Chris Massey3
1School of Environment, University of Auckland, Auckland, New Zealand.
Science advances
|September 4, 2024
概括
在大地震之后,山地河流重新组织了它们的形状和沉积物运输. 滑坡碎片可以持续数年,大大延迟了河床侵蚀.
科学领域:
- 地质形态学 地质形态学
- 构造学 构造学 构造学 构造学
- 沉积物学的沉积物学
背景情况:
- 同地震滑坡导致山脉溪流中沉积物的灾难性过载.
- 这种沉积物输送从根本上重组了河流形态和沉积物运输.
研究的目的:
- 为了研究山地河流系统如何调节大地震后的沉积物输送.
- 分析滑坡碎片对河流系统的长期地形影响.
主要方法:
- 在5年内利用了13次空中LiDAR调查.
- 在新西兰哈普库河的高山支流中监测沉积物质量平衡的变化.
- 分析了山谷宽度对沉积物干扰传播的影响.
主要成果:
- 山地河流通过储存,道演化和床装甲来调节沉积物输送.
- 谷宽度的变化延迟和扩散了山体滑坡碎片的影响.
- 滑坡沉积物可以持续比触发地震的回归期更长时间.
结论:
- 地震诱导的沉积物脉冲显著改变了长时间的河流动态.
- 床岩切口明显减少,影响了活跃山区的侵蚀 - 构造学合.
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