Feasibility study on calculating the Q value of shallow media by using a dense seismic array and a large-volume airgun source

被引:1
|
作者
Du, Shen [1 ]
Yu, YanXiang [1 ]
Xiao, Liang [1 ]
机构
[1] China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
来源
EARTH PLANETS AND SPACE | 2022年 / 74卷 / 01期
关键词
Airgun seismic source; Dense array; Q value; Amplitude-distance attenuation; Coda normalization; FREQUENCY-DEPENDENT ATTENUATION; S-WAVE ATTENUATION; SHEAR-WAVES; CODA WAVES; P-WAVES; REGION; EARTHQUAKES; SEDIMENTS; VOLCANO; EVENTS;
D O I
10.1186/s40623-022-01625-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The feasibility of using a dense seismic array with an airgun source to study the quality factors of shallow media is verified. Data were obtained from 37 stations in the dense seismic array located in Binchuan, Yunnan Province, China, and the amplitude-distance attenuation method and the coda normalization method were applied to calculate the S-wave quality factors in the area. The amplitude-distance attenuation method yielded Q(s)(-1) =0.0260 +/- 0.0103, and the frequency-dependent Q(s)(-1) calculated by the coda normalization method can be expressed by the power law Q(s)(-1)(f) congruent to 0.0554f(-0.5643). The consistency between the results of these two methods shows that a dense seismic array with an airgun source can be used to study the attenuation characteristics of shallow media. The amplitudes at some points deviate substantially from the fitted curve and thus have a certain influence on the fitting results; hence, we must select high-precision data for the calculation. Given the topography, we speculate that the anomalous stations located on the edge of the Binchuan Basin and in the western hilly area are due to the edge effect of the basin and the weak attenuation of the hilly area and that the anomalous station located in the northern Binchuan depocenter is attributable to local site factors. Compared with the Q(s)(-1) estimated by previous studies, the Q(s)(-l) in the Binchuan area is found to lie between those of the hard soil and sedimentary rock and is similar to the Q(s)(-l) in the North China Basin, corresponding to the shallow velocity structure in this area.
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页数:19
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