气候变化领域集成服务门户(CCPortal): Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica

CCPortal

DOI	10.5194/tc-15-3443-2021
	Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica
	Brisbourne A.M.; Kendall M.; Kufner S.-K.; Hudson T.S.; Smith A.M.
发表日期	2021
ISSN	19940416
起始页码	3443
结束页码	3458
卷号	15 期号:7
英文摘要	Antarctic ice sheet history is imprinted in the structure and fabric of the ice column. At ice rises, the signature of ice flow history is preserved due to the low strain rates inherent at these independent ice flow centres. We present results from a distributed acoustic sensing (DAS) experiment at Skytrain Ice Rise in the Weddell Sea sector of West Antarctica, aimed at delineating the englacial fabric to improve our understanding of ice sheet history in the region. This pilot experiment demonstrates the feasibility of an innovative technique to delineate ice rise structure. Both direct and reflected P- and S-wave energy, as well as surface wave energy, are observed using a range of source offsets, i.e. a walkaway vertical seismic profile, recorded using fibre optic cable. Significant noise, which results from the cable hanging untethered in the borehole, is modelled and suppressed at the processing stage. At greater depth where the cable is suspended in drilling fluid, seismic interval velocities and attenuation are measured. Vertical P-wave velocities are high (VINTCombining double low line3984±218gmgs-1) and consistent with a strong vertical cluster fabric. Seismic attenuation is high (QINTCombining double low line75±12) and inconsistent with previous observations in ice sheets over this temperature range. The signal level is too low, and the noise level too high, to undertake analysis of englacial fabric variability. However, modelling of P- and S-wave travel times and amplitudes with a range of fabric geometries, combined with these measurements, demonstrates the capacity of the DAS method to discriminate englacial fabric distribution. From this pilot study we make a number of recommendations for future experiments aimed at quantifying englacial fabric to improve our understanding of recent ice sheet history. © 2021 Alex M. Brisbourne et al.
英文关键词	acoustic method; ice flow; ice sheet; P-wave; S-wave; seismic attenuation; surface wave; vertical seismic profile; wave energy; Antarctica; Southern Ocean; Weddell Sea; West Antarctica
语种	英语
来源期刊	Cryosphere
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/202286
作者单位	Idp, Nerc British Antarctic Survey, Cambridge, CB3 0ET, United Kingdom; Department of Earth Sciences, University of Oxford, Oxford, OX1 3AN, United Kingdom
推荐引用方式 GB/T 7714	Brisbourne A.M.,Kendall M.,Kufner S.-K.,et al. Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica[J],2021,15(7).
APA	Brisbourne A.M.,Kendall M.,Kufner S.-K.,Hudson T.S.,&Smith A.M..(2021).Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica.Cryosphere,15(7).
MLA	Brisbourne A.M.,et al."Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica".Cryosphere 15.7(2021).