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岩石记录中洪水变化的定量约束
Jonah S McLeod1, James Wood2, Sinéad J Lyster2,3
1Department of Earth Science and Engineering, Imperial College London, London, SW7 2BX, UK. jonah.mcleod18@imperial.ac.uk.
Nature communications
|June 8, 2023
概括
现在可以从地质记录中量化过去的河流洪水. 这项研究揭示了多年生河流易发生短时间,强烈 (4-16小时) 突发性洪水,使用石灰岩阶层结构学.
科学领域:
- 地质地质地质地质地质地
- 沉积物学的沉积物学
- 古水文学的古水文学.
背景情况:
- 了解河流的行为和排放变化对于评估景观对环境变化的敏感性至关重要.
- 从地质层测量过去的洪水事件的量化测量是有限的,这阻碍了我们重建历史水文动态的能力.
研究的目的:
- 开发和应用一种方法来量化地质过去的风暴驱动的河流洪水,使用沉积物层学.
- 重建古代河流系统中流量变化的大小和持续时间.
主要方法:
- 在碳岩层 (南威尔士的Pennant形成) 中分析沙丘交叉集几何,以确定排放驱动的不平衡动态.
- 床形保存理论的应用,以量化沙丘周转时间尺度,推断流动变化.
- 与基于面部的洪水标记物的相关性,例如大规模保存的木质碎片.
主要成果:
- 布形成的河流沉积是由不平衡动力学主导的.
- 量化洪水事件表明多年生河流经历了持续4-16小时的闪闪发光的洪水.
- 这种不平衡的床形保护和闪闪发光的洪水模式在400万年的平流学中是一致的.
结论:
- 现在可以量化气候驱动的沉积事件,并从岩石记录中重建每日时间尺度的排放变化.
- 形形成代表着一个由多年河流系统内闪闪发光的洪水主导的地质记录.
- 这种方法为过去的水文制度和景观对环境变化的反应提供了一个新的窗口.
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