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对希腊科林斯湾土壤氡浓度与压力相关变化的观测。

Observations on the stress related variations of soil radon concentration in the Gulf of Corinth, Greece.

机构信息

Institute of Geodynamics, National Observatory of Athens, Athens, Greece.

Schmid College of Science and Technology, Chapman University, Orange, California, USA.

出版信息

Sci Rep. 2022 Mar 31;12(1):5442. doi: 10.1038/s41598-022-09441-0.

Abstract

Our observations indicate a characteristic pattern in the long-term variation of soil radon concentrations, which seems to be consistent with the expected variation of regional stress in relation to seismicity. However, it seems that the major changes in radon level begin before the rock rapture, i.e. before the earthquake occurs. These conclusions have emerged after long-term observations with continuous and thorough real-time gamma-radiation monitoring in the seismically active area of the Gulf of Corinth, Greece. The recordings acquired close to a hot spring were of very high quality, implying that the deep hydraulic flow can possibly play a key role in the pre-earthquake variation of radon level. We were able to observe outstanding examples of radon level variations before significant seismic events in the Gulf of Corinth that cannot be attributed to other external factors such as atmospheric phenomena.

摘要

我们的观察表明,土壤氡浓度的长期变化呈现出一种特征模式,这似乎与地震活动相关的区域应力的预期变化一致。然而,氡水平的主要变化似乎在岩石破裂之前开始,即在地震发生之前。这些结论是在对希腊科林斯湾地震活跃地区进行长期连续和彻底的实时伽马辐射监测后得出的。在温泉附近采集的记录质量非常高,这意味着深部水力流动可能在氡水平的地震前变化中发挥关键作用。我们能够观察到科林斯湾在重大地震事件之前的氡水平变化的突出例子,这些变化不能归因于大气现象等其他外部因素。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ec6d/8971420/a1ae0a03dd45/41598_2022_9441_Fig1_HTML.jpg

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