人間の活動が地球深部の地下流体の流れに強い影響を与えている(Human activities have an intense impact on Earth’s deep subsurface fluid flow)

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2024-04-23 アリゾナ大学

アリゾナ大学の水文学研究者は、人間の活動が地球の深部地下にどのように影響を与えているかを調査しました。この研究では、石油や天然ガスの抽出に伴う流体の生成速度が自然の水循環よりも大きいことが示されています。さらに、気候変動対策として提案されている地質的炭素隔離や地熱発電、リチウム抽出などの活動が将来的に増加すると予測されており、これらが深部地下の流体動態に大きな影響を与える可能性があります。地球の深部地下は通常意識されにくい領域ですが、環境への影響を考慮に入れた責任ある管理が重要であると強調されています。

<関連情報>

人新世における地下深部流体フラックスの加速 Acceleration of Deep Subsurface Fluid Fluxes in the Anthropocene

Grant Ferguson, Lydia R. Bailey, Ji-Hyun Kim, Magdalena R. Osburn, Peter W. Reiners, Henrik Drake, Bradley S. Stevenson, Jennifer C. McIntosh
Earth’s Future  Published: 05 April 2024
DOI:https://doi.org/10.1029/2024EF004496

人間の活動が地球深部の地下流体の流れに強い影響を与えている(Human activities have an intense impact on Earth’s deep subsurface fluid flow)

Abstract

The Anthropocene has been framed around humanity’s impact on atmospheric, biologic, and near-surface processes, such as land use and vegetation change, greenhouse gas emissions, and the above-ground hydrologic cycle. Groundwater extraction has lowered water tables in many key aquifers but comparatively little attention has been given to the impacts in the deeper subsurface. Here, we show that fluid fluxes from the extraction and injection of fluids associated with oil and gas production and inflow of water into mines likely exceed background flow rates in deep (>500 m) groundwater systems at a global scale. Projected carbon capture and sequestration (CCS), geothermal energy production, and lithium extraction to facilitate the energy transition will require fluid production rates exceeding current oil and co-produced water extraction. Natural analogs and geochemical modeling indicate that subsurface fluid manipulation in the Anthropocene will likely appear in the rock record. The magnitude and importance of these changes are unclear, due to a lack of understanding of how deep subsurface hydrologic and geochemical cycles and associated microbial life interact with the rest of the Earth system.

Key Points

  • Current anthropogenic fluid fluxes in the deep subsurface likely exceed background fluxes
  • Anthropogenic fluid fluxes in the deep subsurface are expected to accelerate with the energy transition
  • Injection and production of fluids from the deep subsurface is expected to leave a mark on the geologic record

Plain Language Summary

The Anthropocene is often framed in terms of changes in climate, ecosystems and land use. These have been accompanied by changes in the Earth’s water cycle, including depleted groundwater storage due to pumping in many regions. The scale of anthropogenic change in the subsurface at depths beyond typical water wells has received less attention. Fluid flow rates associated with oil and gas production likely exceed natural groundwater flow rates at depths greater than 500 m. Anthropogenic impacts to this deeper zone of the Earth’s subsurface are expected to increase dramatically as we look to store carbon, mine lithium from deep brines and produce geothermal energy as part of the ongoing energy transition.

1702地球物理及び地球化学
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