潜入Myojin-sho水下火山口

T. Ura, K. Nagahashi, A. Asada, K. Okamura, K. Tamaki, T. Sakamaki, K. Iizasa
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引用次数: 7

摘要

2005年8月,作为r - 2项目的成果之一,于2003年7月建造的AUV“r2D4”成功地以完全自主模式进入了Myojin-sho水下火山口。火山口位于东京以南约800公里处,直径8公里。在1952年多次喷发的火山口外缘东北部,有一座活跃的水下火山妙真寿。黑潮通常在火山口上流动,所以它周围的水流速度有时超过3节。可以说,在这种恶劣的环境下,载人车辆和遥控车辆潜入妙真寿火山口是非常危险的。干涉测量声纳捕获了陨石坑中央圆锥体的清晰图像,现场化学分析仪“GAMOS”检测到高浓度的锰离子,这表明陨石坑中存在热液活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dive into Myojin-sho Underwater Caldera
In August 2005, we succeeded in operating AUV "r2D4", which was constructed in July 2003 as one of fruits of R-Two project, into Myojin-sho underwater Caldera in full autonomous mode. The caldera is located about 800 km in the south of Tokyo, and 8 km in diameter. There is an active underwater volcano Myojin-sho at the Northeastern part of outer rim of caldera, which erupted repeatedly in 1952. The Kuroshio current is usually running over the Caldera, so that current speed around it is sometimes more than 3 knots. It can be said that the diving of human occupied vehicle and remotely operated vehicle into Myojin-sho Caldera is very dangerous due to such hostile environment. The interferometry SONAR captured a clear image of the central cone in the middle of crater, and the in-situ chemical analyzer "GAMOS" detected high concentration of manganese ion which indicates hydro-thermal activity in the crater.
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