Abstract

Natural seepage of methane into the oceans is considerable, and plays a role in the global carbon cycle. Estimating the amount of this greenhouse gas entering the water column is important in order to understand their environmental impact. In addition, leakage from man-made structures such as gas pipelines may have environmental and economical consequences and should be promptly detected. Split beam echo sounders (SBES) detect hydroacoustic plumes due to the significant contrast in acoustic impedance between water and free gas. SBES are also powerful tools for plume characterization, with the ability to provide absolute acoustic measurements, estimate bubble trajectories, and capture the frequency dependent response of bubbles. However, under challenging conditions such as deep water and considerable background noise, it can be difficult to detect the presence of gas seepage from the acoustic imagery alone. The spatial coherence of the wavefield measured across the split beam sectors, quantified by the coherence factor (CF), is a computationally simple, easily available quantity which complements the acoustic imagery and may ease the ability to automatically or visually detect bubbles in the water column. We demonstrate the benefits of CF processing using SBES data from the Hudson Canyon, acquired using the Simrad EK80 SBES. We observe that hydroacoustic plumes appear more clearly defined and are easier to detect in the CF imagery than in the acoustic backscatter images.

Highlights

  • Detecting marine gas seeps using hydroacoustics started already in 1984, with many studies since aiming at mapping and monitoring marine seep sites [1,2,3,4,5]

  • multibeam echo sounders (MBES) data collected on the 2016 cruise showed evidence of seeps in the area identified by Weinstein et al [41]

  • While MBES are well suited for efficient mapping of large areas due to their wide transmit beam, calibrated split-beam echo sounders (SBES) add valuable information including absolute acoustic measurements which can be used to estimate bubble flux [23,27,38,54,55]

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Summary

Introduction

Detecting marine gas seeps using hydroacoustics started already in 1984, with many studies since aiming at mapping and monitoring marine seep sites [1,2,3,4,5]. Natural seepage of methane is common in many regions where geological structures such as pockmarks, mud-volcanoes, faults or salt domes allow this greenhouse gas to penetrate the seafloor and enter the water column [6]. Rising seawater temperatures may trigger the release of large amounts of gas currently trapped either in permafrost, or as gas hydrates stabilized by high pressure and low temperatures [7,8,9,10]. MBES are routinely used for seafloor mapping, Sensors 2018, 18, 2033; doi:10.3390/s18072033 www.mdpi.com/journal/sensors

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