大気中の水銀堆積変化に対する生態系の応答を解明 (Unveiling ecosystem responses to changes in atmospheric mercury deposition)

2025-02-27 清華大学

清華大学環境学院の王書肖教授率いる研究チームは、全球の自然アーカイブ中の水銀(Hg)蓄積データと大気中のHg沈着モデルを統合し、環境中のHg動態を分析しました。1700年~2012年の氷、泥炭、湖底、海洋堆積物221のコアサンプルを調査し、過去300年間でHgフラックスが5~9倍に増加したことを確認。特に湖沼や泥炭地の堆積物は大気中のHg沈着変化と一致しましたが、氷や海洋堆積物では反応が鈍いことが判明しました。発展途上地域では石炭燃焼や金採掘によるHg蓄積が増加し、先進地域では1950年以降、環境政策の効果でHgフラックスが減少。この研究は生態系汚染の理解を深め、Hg汚染対策の政策立案に貢献するものです。

<関連情報>

水銀の自然記録から、大気沈着量の変化に対する生態系の応答が明らかになる Mercury records from natural archives reveal ecosystem responses to changing atmospheric deposition

Qinqin Chen, Qingru Wu, Yuying Cui, Shuxiao Wang
National Science Review  Published:19 November 2024
DOI:https://doi.org/10.1093/nsr/nwae417

(a) Spatial distributions of natural archive records of Hg. The numbers in brackets represent the number of cores from the respective natural archives compiled in the database. Note that some cores collected from the same or nearby locations are not fully visible in the figure; please refer to Dataset S1 for detailed core information. (b) A comparison between natural archive Hg fluxes and total (wet + dry) atmospheric Hg deposition fluxes modelled by GEOS-Chem at each coring site in the base year 1980—a year with the greatest number of cores. Larger circles indicate greater disparities in magnitude. Generally, lake-Hg, peat-Hg and marine-Hg fluxes are greater than the modelled total atmospheric Hg deposition fluxes, while ice-Hg fluxes are smaller. A total of 42% of the cores show good agreement with the modelled values, indicated by a difference within 1-fold. However, 12% of the cores exhibit differences of >10-fold, mostly marine and ice cores.

ABSTRACT

Global ecosystems face mercury contamination, yet long-term data are scarce, hindering understanding of ecosystem responses to atmospheric Hg input changes. To bridge the data gap and assess ecosystem responses, we compiled and compared a mercury accumulation database from peat, lake, ice and marine deposits worldwide with atmospheric mercury deposition modelled by GEOS-Chem, focusing on trends, magnitudes, spatial–temporal distributions and impact factors. The mercury fluxes in all four deposits showed a 5- to 9-fold increase over 1700–2012, with lake and peat mercury fluxes that generally mirrored atmospheric deposition trends. Significant decreases in lake and peat mercury fluxes post-1950 in Europe evidenced effective environmental policies, whereas rises in East Asia, Africa and Oceania highlighted coal-use impacts, inter alia. Conversely, mercury fluxes in marine and high-altitude ecosystems did not align well with atmospheric deposition, emphasizing natural influences over anthropogenic impacts. Our study underscores the importance of these key regions and ecosystems for future mercury management.

1904環境影響評価
ad
ad
Follow
ad
タイトルとURLをコピーしました