09:45 〜 10:00
[SCG44-15] Recent developments on distributed fiber-optic sensing for long-term geophysical monitoring
★Invited Papers
キーワード:distributed fiber optic sensing, Earthquake monitoring, long-term strain monitoring
Optical Time Domain Reflectometer based Distributed Fiber-Optic Sensing (DFOS) technology converts a regular telecommunications fiber into a dense sensor array. As a subset of DFOS, Distributed Acoustic Sensing (DAS) and Distributed Strain Sensing (DSS) technologies can measure strain distribution along a fiber with high spatial and temporal resolutions. DFOS-based strain measurements have a very broad frequency spectrum. Depending on measuring methods, DFOS can be used to monitor long-term (days to months) deformation as well as strain changes induced by thousands of Hertz vibrations. It also enjoys sub-micro strain sensitivities thanks to recent improvements in instrument designs.
This presentation introduces measuring principles and geophysics applications of different types of DFOS-based strain measurements, including DAS and two types of long-term DSS. First, I will showcase the recent developments on DAS-based earthquake and microseismic monitoring, and discuss the advantages and disadvantages of DAS-based seismic monitoring systems. I will then review long-term DSS monitoring, including hydraulic fracture geomechanical monitoring and landslide monitoring. I will conclude the presentation by discussing the opportunities of using DFOS measurements to monitor slow and fast earthquakes.
This presentation introduces measuring principles and geophysics applications of different types of DFOS-based strain measurements, including DAS and two types of long-term DSS. First, I will showcase the recent developments on DAS-based earthquake and microseismic monitoring, and discuss the advantages and disadvantages of DAS-based seismic monitoring systems. I will then review long-term DSS monitoring, including hydraulic fracture geomechanical monitoring and landslide monitoring. I will conclude the presentation by discussing the opportunities of using DFOS measurements to monitor slow and fast earthquakes.