尉建功, 杨胜雄, 梁金强, 陆敬安, 刘胜旋, 张伟. 海洋钻探对甲烷渗漏的影响:以南海北部天然气水合物钻探GMGS2-16站位为例[J]. 海洋地质与第四纪地质, 2018, 38(5): 63-70. DOI: 10.16562/j.cnki.0256-1492.2018.05.006
引用本文: 尉建功, 杨胜雄, 梁金强, 陆敬安, 刘胜旋, 张伟. 海洋钻探对甲烷渗漏的影响:以南海北部天然气水合物钻探GMGS2-16站位为例[J]. 海洋地质与第四纪地质, 2018, 38(5): 63-70. DOI: 10.16562/j.cnki.0256-1492.2018.05.006
WEI Jiangong, YANG Shengxiong, LIANG Jinqiang, LU Jingan, LIU Shengxuan, ZHANG Wei. Impact of seafloor drilling on methane seepage—enlightenments from natural gas hydrate drilling site GMGS2-16, northern South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(5): 63-70. DOI: 10.16562/j.cnki.0256-1492.2018.05.006
Citation: WEI Jiangong, YANG Shengxiong, LIANG Jinqiang, LU Jingan, LIU Shengxuan, ZHANG Wei. Impact of seafloor drilling on methane seepage—enlightenments from natural gas hydrate drilling site GMGS2-16, northern South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(5): 63-70. DOI: 10.16562/j.cnki.0256-1492.2018.05.006

海洋钻探对甲烷渗漏的影响:以南海北部天然气水合物钻探GMGS2-16站位为例

Impact of seafloor drilling on methane seepage—enlightenments from natural gas hydrate drilling site GMGS2-16, northern South China Sea

  • 摘要: 目前世界上许多国家对海洋天然气水合物开展了调查和试开采,但是对水合物开发与海底甲烷渗漏之间的关系缺乏了解。本文依托我国第二次天然气水合物钻探航次(GMGS2),对GMGS2-16钻孔开展了两次钻后甲烷渗漏调查。第一次使用水下机器人(ROV)在该孔开钻之前、钻探过程中及完钻67天内进行了4次海底观察,其中开钻之前未发现海底甲烷渗漏,而在完钻后的两次海底观察中,发现大量气泡从废弃井口冒出。第二次使用船载多波束在该孔完钻18个月后开展水体调查,发现水体中存在火焰状的高回波强度,表明水体中存在气体羽状流,指示海底发生了甲烷渗漏。地震剖面显示该站位水合物赋存层下伏游离气,甲烷渗漏可能是由于钻探打通了海底与该游离气层,形成了甲烷气体运移的优势通道,造成海底甲烷渗漏。多波束水体数据显示甲烷气泡从海底溢出,在海面以下约650m处消失,表明甲烷气体在通过水体的过程中被完全溶解,因此,钻探导致的甲烷渗漏对大气的影响较小。未来随着井壁的坍塌以及水合物在井内的形成,气体运移的优势通道将会完全关闭,甲烷渗漏终止。

     

    Abstract: There are a few countries in the world, which have conducted gas hydrate exploration and test production. However, the knowledge about the impact of seafloor drilling on methane seepage is limited. This study conducted two post seafloor investigations on the GMGS2-16 drilling site of the second gas hydrate drilling expedition (GMGS2). The first investigation consisted of four ROV dives, including one dive before drilling, one dive during drilling and two dives after drilling. The first dive did not find any seafloor gas emission. However, during the last two dives, massive gas bubble emission was observed from the abandoned well. The second investigation was conducted with multibeam echosounder 18 months after the well GMGS2-16A was completed. Flare-shaped high amplitude backscatter was observed in the water column, indicating methane leakage from the seafloor. The seismic profile showed that the free gas was distributed beneath the hydrate-bearing sediment. The seafloor drilling penetrated the hydrate-bearing sediment layer and built up the pathway between seafloor and free gas reservoir, which led to seafloor methane seepage. The water column multibeam data shows that gas flares disappeared at around 650 mbsl, indicating that methane gas was totally dissolved in the seawater. The impact of drilling-induced methane seepage on the atmosphere is quite limited. The methane leakage will stop when the pathways are closed by wall collapse and hydrate deposited later.

     

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