Li Tiegang, Feng Aiping, Liu Yanxiong, Li Zhenhong, Guo Kai, Jiang Wenzheng, Du Jun, Tian Ziwen, Xu Wenxue, Liu Yang, Wang Yanru
The First Institute of Oceanography (FIO), State Oceanic Administration (SOA), Qingdao, 266061, China.
School of Engineering, Newcastle University, Newcastle upon Tyne, NE1 7RU, UK.
Sci Rep. 2018 Nov 20;8(1):17122. doi: 10.1038/s41598-018-35220-x.
The Sansha Yongle Blue Hole (SYBH) is the deepest blue hole found anywhere to date. Study of the SYBH can provide insight into the interactions between hole wall morphology and many geological/hydrological mechanisms. A comprehensive investigation of the SYBH was carried out for the first time in 2017 using a professional-grade underwater remotely operated vehicle (ROV) to obtain accurate depth and three-dimensional (3D) topographic data. The SYBH resembles a ballet dancer's shoe and has a volume of ~499609 m. The observed deepest portion of the SYBH is at 301.19 m below the local 10-year mean sea level. The cave bottom laterally deviates from its entrance by 118 m at an azimuth of 219 degrees. The cave entrance is shaped like a comma and has an average width of 130 m; the widest part is 162.3 m wide, while the narrowest part is 26.2 m wide and is at 279 mbsl (meters below sea level). The 3D topography of the SYBH and underwater photography revealed two large transitions at ~76 to 78 mbsl and at 158 mbsl, indicating that the initiation of the blue hole was likely a step wise process and that the hole wall morphology was subsequently remolded through a paleo-sea level stillstand (at or near Younger Dryas). The topographic data also indicated that the blue hole is situated within an isolated environment with no water or material exchange with the outside open sea.
三沙永乐龙洞是迄今为止发现的最深的蓝洞。对三沙永乐龙洞的研究有助于深入了解洞壁形态与多种地质/水文机制之间的相互作用。2017年首次使用专业级水下遥控潜水器(ROV)对三沙永乐龙洞进行了全面调查,以获取精确的深度和三维(3D)地形数据。三沙永乐龙洞形似芭蕾舞鞋,容积约为499609立方米。观测到的三沙永乐龙洞最深部分位于当地10年平均海平面以下301.19米处。洞穴底部在方位角219度处横向偏离洞口118米。洞口呈逗号状,平均宽度为130米;最宽处为162.3米,最窄处为26.2米,位于海平面以下279米处。三沙永乐龙洞的三维地形和水下摄影显示,在海平面以下约76至78米和158米处有两个大的转折,这表明蓝洞的形成可能是一个逐步的过程,并且洞壁形态随后通过古海平面停滞期(在新仙女木期或接近新仙女木期)进行了重塑。地形数据还表明,该蓝洞位于一个孤立的环境中,与外部公海没有水或物质交换。