3D near-surface P-wave velocity structure imaging with Distributed Acoustic Sensing and electric hammer source

• Published in: Earthquake research advances Vol. 4; no. 3; p. 100274
• Main Authors: Hong, Heting, Yin, Fu, Lei, Yuhang, Li, Yulan, Wang, Baoshan
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.07.2024; KeAi Communications Co. Ltd
• Subjects: Active source; Body wave; Distributed Acoustic Sensing (DAS); First-arrival travel time tomography; Near-surface structure; Near-surface structure; Active source; Distributed Acoustic Sensing (DAS); Body wave; First-arrival travel time tomography
• ISSN: 2772-4670; 2772-4670
• DOI: 10.1016/j.eqrea.2023.100274

Distributed Acoustic Sensing (DAS) is an emerging technique for ultra-dense seismic observation, which provides a new method for high-resolution sub-surface seismic imaging. Recently a large number of linear DAS arrays have been used for two-dimensional S-wave near-surface imaging in urban areas. In order to explore the feasibility of three-dimensional (3D) structure imaging using a DAS array, we carried out an active source experiment at the Beijing National Earth Observatory. We deployed a 1 ​km optical cable in a rectangular shape, and the optical cable was recast into 250 sensors with a channel spacing of 4 ​m. The DAS array clearly recorded the P, S and surface waves generated by a hammer source. The first-arrival P wave travel times were first picked with a Short-Term Average/Long-Term Average (STA/LTA) method and further manually checked. The P-wave signals recorded by the DAS are consistent with those recorded by the horizontal components of short-period seismometers. At shorter source-receiver distances, the picked P-wave arrivals from the DAS recording are consistent with vertical component recordings of seismometers, but they clearly lag behind the latter at greater distances. This is likely due to a combination of the signal-to-noise ratio and the polarization of the incoming wave. Then, we used the TomoDD software to invert the 3D P-wave velocity structure for the uppermost 50 ​m with a resolution of 10 ​m. The inverted P-wave velocity structures agree well with the S-wave velocity structure previously obtained through ambient noise tomography. Our study indicates the feasibility of 3D near-surface imaging with the active source and DAS array. However, the inverted absolute velocity values at large depths may be biased due to potential time shifts between the DAS recording and seismometer at large source-receiver distances.