Abstract

In recent years, discoveries of methane plumes (also called methane flares) have been reported in various sea areas around the world. Clusters of naturally seeping methane bubbles rising from the seafloor are visualized as methane plumes on the echograms of quantitative echo sounders and multibeam sonars. In order to determine if seeping methane can be used as energy resources and its environmental impact, it is necessary to estimate the amount of naturally seeping methane. From April, 2020, a 3-year project is being conducted in Japan to evaluate the amount of methane seepage from methane plumes. The authors propose the following steps to quantify the amount of methane seepage accurately. First of all, methane plumes in the Exclusive Economic Zone (EEZ) of Japan are mapped out using acoustic devices such as quantitative echo sounders and multibeam sonars. Secondly, methane bubbles of a few millimeters in diameter from methane seeps at seafloor are collected and sampled using a cone-shaped collector with 20 cm in diameter, operated by Remotely Operated Vehicle (ROV). If we can identify the number of seep mouths that form into one single plume, we will be able to quantify the methane seepage from one plume. Based on this result, calibration of the mean backscattering strength and the amount of seeping methane from methane plumes becomes possible and will be applied to the mapped plumes in order to estimate the methane seepage in the EEZ of Japan. Once this calibration is established, it can be applied to the methane plumes observed worldwide, and methane seepage can be quantified simply by acoustic observations of methane plumes. In this study, a method to verify the correlation between methane plumes and methane seeps is introduced, as well as a method to locate methane seeps effectively using the Target Position function of a quantitative echo sounder. The authors intend to use this as the basic data for establishing a method to estimate the amount of methane released from a methane plume by observing the methane plume acoustically.

Highlights

  • Recent offshore seismic surveys and logging have confirmed a wide distribution of methane hydrate in deep sea deposits (Shipley and Houston, 1979; Shipley and Didyk, 1982; Matsumoto, 2001)

  • Shallow type methane hydrate refers to methane hydrate that is, generated and observed near seafloor surface in various forms such as plates, veins, and clumps (Ministry of Economy, Trade and Industry, 2016) on the seafloor surface in waters deeper than 500 m, and at about 100 m below seafloor in the sea area of Joetsu, Sea of Japan

  • Called methane flares, are bubbles seeping from the seafloor which can be observed on the monitors of quantitative echo sounders and echogram of multibeam sonars onboard (Aoyama et al, 2009)

Read more

Summary

INTRODUCTION

Recent offshore seismic surveys and logging have confirmed a wide distribution of methane hydrate in deep sea deposits (Shipley and Houston, 1979; Shipley and Didyk, 1982; Matsumoto, 2001). Investigations such as drilling and diving surveys are being conducted in methane hydrate bearing sea areas (Aoyama and Matsumoto, 2009). Shallow type methane hydrate in the Sea of Japan is mostly confirmed in muddy sediments at 500–1,500 m depths, shallower than about 100 m below seafloor (National Institute of Advanced Industrial Science and Technology, 2021)

METHANE PLUME
QUANTIFICATION OF METHANE PLUME SEEPAGE
Methane Plume Mapping
Quantification of Methane Seepage From Seafloor
CONCLUSION
DATA AVAILABILITY STATEMENT
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call