マウントの上昇,崩壊,圧縮 2017年9月3日の北朝鮮の核実験のマンタップ
Teng Wang1, Qibin Shi2,3, Mehdi Nikkhoo4
1Earth Observatory of Singapore, Nanyang Technological University, Singapore. wang.teng@ntu.edu.sg shjwei@ntu.edu.sg dreger@seismo.berkeley.edu.
まとめ
衛星レーダーによる監視は 北朝鮮最大の核実験で 地面が大きく変形したことを明らかにしました この地質学的遠隔検知アプローチは,地下核爆発とその出力を特徴づけるのに役立ちます.
科学分野:
- 地理学
- リモートセンシング
- 核実験の監視
背景:
- 世界的な地震ネットワークは 秘密の核実験の監視のための主要なツールです
- この目的のために,特に衛星レーダーを使用する宇宙での監視能力は,未充分に活用されています.
研究 の 目的:
- 地下核実験の特徴化のための衛星レーダー画像の有用性を評価する.
- 北朝鮮の最大の核爆発と関連した 表面の移動を定量化するために
主な方法:
- 衛星レーダー画像を用いて 完全な地表移位を導き出した.
- 地質学と地震学を組み合わせた遠隔感知技術
- 水平運動と沈み込みを含む変形パターンを分析した.
主要な成果:
- 3.5メートルの水平移動と 0.5メートルの沈下を検出しました
- 地下崩壊と破損した岩石の非地震的圧縮が確認された.
- 爆発力はTNTの191キロトンで 450メートルの深さです
結論:
- 宇宙での遠隔検知は 地下での大規模な核実験を 特徴づけるのに適したツールです
- 地質学的遠隔検知は 核爆発後の物理的なプロセスに 価値ある洞察を与えてくれます
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