Author:
Cao Chen,Ge Yongqiang,Chen Jiawang,Wang Hao,Ge Han,Zhou Peng,Gao Feng,Sheng Yan,Tian Lieyu,Huang Yifan
Abstract
Abstract As an important green energy source for the future, deep-sea natural gas hydrate has attracted worldwide attention in recent years, and several trial exploitations have been carried out. Hydrates are prone to decomposition leading to terrain subsidence; hence, there
is an urgent need to monitor terrain change during the exploration. In this study, a monitoring device based on six-axis Micro-Electro-Mechanical System array is developed to monitor the terrain subsidence during production of gas hydrate. The liability of the device has been tested both by
lab experiments and a sea trial in the “Shenhu” area of the South China Sea with water-depth of 1,203 m. The device performed in-situ monitoring for 193 consecutive days; the deformation of the seafloor terrain has been successfully measured, and the seafloor topography has been
obtained and reconstructed, showing that the overall average uplift of the seafloor terrain is 0.82 cm, with a maximum uplift of 5.98 cm and a maximum subsidence of 3.21 cm. The result shows that the geological conditions in the “Shenhu” area are stable, which provide a reference
for the development of hydrates.
Publisher
Marine Technology Society
Subject
Ocean Engineering,Oceanography
Cited by
1 articles.
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