東テキサスの液体注入による表面上昇と時間依存の地震リスク
Manoochehr Shirzaei1, William L Ellsworth2, Kristy F Tiampo3
1School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA. shirzaei@asu.edu.
まとめ
東テキサスの排水は 低圧縮性の岩石の孔圧を増加させ 地面の上昇を引き起こします この研究は地震活動と 流体注入を 関連付けています
科学分野:
- 地理学
- 地震科学
- 環境地質学
背景:
- 排水の注入と地震性の間の直接的なリンクはよく確立されていません.
- 地下流体注入作業の管理には,誘発性地震性の理解が不可欠です.
研究 の 目的:
- テキサス州東部の 排水と地震の因果関係を証明する
- 液体の注入が地殻の張力や毛穴の圧力に及ぼす影響を定量化する.
主な方法:
- 地面上昇を検出するためにレーダーインターフェロメトリックデータを利用した.
- 報告された注射データと統合された上昇測定.
- 皮質の張力と毛穴圧力を計算するために,ポロ弾性モデルを使用した.
主要な成果:
- 井戸から8km以上で検出可能な排水インジケートされた土壌上昇.
- 低圧縮性の岩石では 1 メガパスカルを超える孔圧増加が地震を引き起こした.
- 孔圧拡散による注射率の低下にも関わらず,地震活動は継続した.
結論:
- 汚染水の注入は 東テキサスで発生した地震の 直接的な原因です
- 孔圧拡散は地震のタイミングと持続に重要な役割を果たします.
- 孔圧の伝播を防ぐ地質学的構造は,誘発された地震性を抑制することができます.
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