海洋内部酸化在工业时代的进展
Jens D Müller1, Nicolas Gruber1
1Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, Zurich, Switzerland.
Science advances
|November 27, 2024
概括
由于人为二氧化碳 (CO2) 的吸收,海洋酸化在表面下变得越来越严重. 这项研究揭示了阿拉戈尼特和度 (Ωarag) 和pH值的显著下降,近几十年来迅速加速.
科学领域:
- 海洋化学 海洋化学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 由人为CO2吸收驱动的海洋酸化对海洋生态系统构成重大威胁.
- 了解海洋内部酸化的历史进展对于预测生态系统影响至关重要.
研究的目的:
- 为了重建工业时代海洋内部酸化的历史.
- 量化海洋上层的阿拉戈尼特和状态 (Ωarag) 和pH的变化.
主要方法:
- 利用基于观察的人类碳积累估计.
- 分析了从1800年到2014年的Ωarag和pH值在海洋顶部100米的变化.
主要成果:
- 自1800年以来,阿拉戈尼特和度 (Ωarag) 和pH分别下降了0.6和0.1以上,在前100米内.
- 近50%的酸性化发生在过去20年,在上热线上明显[H+]的最大增加.
- 阿拉戈尼特和地平线缩短了200多米,在某些地区,特别是南大洋,接近了euphotic区域.
结论:
- 自工业时代以来,海洋内部酸化已经取得了显著的进展,近几十年来,其速度正在加快.
- 潮的和地平线使更多的海洋生物暴露在腐蚀条件下,威胁到海洋生态系统.
- 需要进一步的研究来了解地下海洋酸化带来的全部生态后果.
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