通过激光干扰复合体研究地层相互作用
Grigory Dolgikh1, Sergey Budrin1, Stanislav Dolgikh1
1V.I. Il'ichev Pacific Oceanological Institute, Far Eastern Branch Russian Academy of Sciences, 690041 Vladivostok, Russia.
Sensors (Basel, Switzerland)
|January 28, 2026
概括
这项研究使用先进的仪器监测地层波浪过程,揭示了地震事件,水层和大气压力中的模式. 这些发现突出了气压和地面变形之间的相互作用,以及区域海洋波浪特征.
科学领域:
- 地质物理学 地质物理学
- 环境科学 环境科学
- 海洋学 海洋学 海洋学
背景情况:
- 了解地球地层的波浪过程对于监测地震活动和环境变化至关重要.
- 以前的研究往往集中在个别领域,缺乏对相互连接的综合分析.
研究的目的:
- 监测和分析地层 (大气层,水层,岩层) 内的波浪过程.
- 识别地震事件,大气压力和水层变化之间的模式和相互作用.
- 区分自然和人为地震活动,描述海洋波动力学.
主要方法:
- 利用激光干扰仪器,气象站,地震计,纳米波谱仪,潮计和温度传感器进行现场数据收集.
- 使用激光压力计和地震计进行地震活动分析.
- 应用超灵敏探测器用于水球压力变化和潮计用于海浪分析.
主要成果:
- 在地震事件中确定了与水层和大气压力变化相关的一般模式.
- 通过使用激光压力计和地震计成功区分自然和人为地震活动.
- 使用激光纳米波图和张力计检测到巴罗变形相互作用.
- 通过分析压力,潮和温度数据,揭示了海洋波浪过程的区域特征.
结论:
- 地层波浪过程的综合监测提供了对地球系统动态的整体视图.
- 该研究证明了先进仪器在检测微妙的环境相互作用和活动方面的能力.
- 这些发现有助于更好地了解地震风险,大气影响和海洋动态.
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