人为二氧化碳对海洋中CaCO3系统的影响
Richard A Feely1, Christopher L Sabine, Kitack Lee
1Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, WA 98115-6349, USA. richard.a.feely@noaa.gov
概括
由于二氧化碳 (CO2) 的增加,海洋酸化增加了碳酸 (CaCO3) 的溶解. 全球海洋CaCO3溶解率估计为每年0.5百克的CaCO3-C,影响形成物种.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋化学 海洋化学
- 气候科学 气候科学
背景情况:
- 两个世纪以来,大气中二氧化碳 (CO2) 度的上升增加了海洋的二氧化碳吸收.
- 这一过程导致了海洋酸化,改变了有关碳酸 (CaCO3) 颗粒的和状态.
研究的目的:
- 在现场估计全球海洋中的CaCO3溶解速率.
- 讨论人类产生的二氧化碳对CaCO3形成物种的未来影响.
主要方法:
- 利用总度和化碳 (CFC) 数据来估计CaCO3的溶解速率.
- 分析数据以确定每公斤每年微摩尔的溶解率.
主要成果:
- 观察到CaCO3溶解速率在每公斤每年0.003至1.2微摩尔之间.
- 溶解开始于阿拉贡石和地平线附近.
- 全球海洋CaCO3溶解速度估计大约为每年0.5 +/- 0.2 五克的CaCO3-C.
结论:
- 估计的全球CaCO3溶解率占CaCO3.3出口总产量的45-65%.
- 海洋酸化对海洋生态系统,特别是形成贝的生物构成重大威胁.
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