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在新冠疫情封锁期间的寂静中捕捉伊斯基亚岛的热液低语。

Picking up the hydrothermal whisper at Ischia Island in the Covid-19 lockdown quiet.

作者信息

Falanga Mariarosaria, Cusano Paola, De Lauro Enza, Petrosino Simona

机构信息

Dipartimento Di Ingegneria Dell'Informazione Ed Elettrica E Matematica Applicata/DIEM, Università Degli Studi Di Salerno, Fisciano, Italy.

Istituto Nazionale Di Geofisica E Vulcanologia, Sezione Di Napoli - Osservatorio Vesuviano, Naples, Italy.

出版信息

Sci Rep. 2021 Apr 23;11(1):8871. doi: 10.1038/s41598-021-88266-9.

Abstract

In this paper, we analyse the seismic noise at Ischia Island (Italy) with the objective of detecting the hydrothermal source signals taking advantage of the Covid-19 quiescence due to lockdown (strong reduction of anthropogenic noise). We compare the characteristics of the background noise in pre-, during and post-lockdown in terms of spectral content, energy release (RMS) and statistical moments. The continuous noise is decomposed into two independent signals in the 1-2 Hz and 2-4 Hz frequency bands, becoming sharpened around 1 Hz and 3 Hz respectively in lockdown. We propose a conceptual model according to which a dendritic system of fluid-permeated fractures plays as neighbour closed organ pipes, for which the fundamental mode provides the persistent whisper and the first higher mode is activated in concomitance with energy increases. By assuming reasonable values for the sound speed in low vapor-liquid mass fraction for a two-phase fluid and considering temperatures and pressures of the shallow aquifer fed by sea, meteoric and deep hydrothermal fluids, we estimate pipe lengths in the range 200-300 m. In this scheme, Ischia organ-like system can play both continuous whisper and transients, depending on the energy variations sourced by pressure fluctuations in the hydrothermal fluids.

摘要

在本文中,我们分析了意大利伊斯基亚岛的地震噪声,目的是利用因封锁导致的新冠疫情期间的平静期(人为噪声大幅降低)来检测热液源信号。我们从频谱内容、能量释放(均方根)和统计矩方面比较了封锁前、封锁期间和封锁后的背景噪声特征。连续噪声在1 - 2赫兹和2 - 4赫兹频段被分解为两个独立信号,在封锁期间分别在1赫兹和3赫兹左右变得尖锐。我们提出了一个概念模型,根据该模型,充满流体的树枝状裂隙系统起到相邻封闭风琴管的作用,其基模产生持续的低语声,第一高阶模在能量增加时被激活。通过假设气液质量分数较低的两相流体中的声速合理值,并考虑由海水、大气降水和深部热液流体补给的浅层含水层的温度和压力,我们估计管长在200 - 300米范围内。在这个方案中,伊斯基亚岛类似风琴的系统可以产生持续的低语声和瞬态信号,这取决于热液流体中压力波动所引起的能量变化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5462/8065031/f389e16ff8e4/41598_2021_88266_Fig1_HTML.jpg

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