纳拉甘塞特湾缺氧的现代历史:地化学记录
Warren S Boothman1, Laura Coiro1
1U.S. Environmental Protection Agency, Office of Research and Development, Center for Environmental Measurement and Modeling, Atlantic Coastal Environmental Sciences Division, 27 Tarzwell Drive, Narragansett, RI 02882, USA.
The Science of the total environment
|September 5, 2024
概括
历史沉积物核心显示,人类活动增加的污染加剧了纳拉甘塞特湾的缺氧. 污水处理设施的性能直接影响这些有害的低氧事件的严重程度和持续时间.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 生态生态学 生态生态学
背景情况:
- 河口生态系统因农业和城市化增加的气而面临水质退化.
- 低氧 (低氧) 事件在沿海系统中变得越来越频繁和严重.
- 河口中缺氧的历史记录是不太了解的.
研究的目的:
- 为了重建Narragansett湾上部缺氧的历史记录.
- 为了将缺氧趋势与人口变化和人为投入相关联.
- 评估废水处理设施 (WWTF) 对河口低氧的影响.
主要方法:
- 在沉积物核心中分析地质化学标记物 (自生,碳,,同位素).
- 沉积物核心的垂直分析,以确定历史环境条件.
- 地化学数据与历史人口和WWTF数据的相关性.
主要成果:
- 甲基度表明与人口增长和WWTFs相关的低氧的频率和持续时间增加.
- 上纳拉甘塞特湾在20世纪经历了长时间的缺氧,受到WWTF表现的影响.
- 格林尼治湾的低氧水平大幅增加,与郊区人口增长和WWTF运营相关.
- 沉积性碳和同位素证实了20世纪下半叶缩和生产率的增加.
结论:
- 社会活动,特别是投入和WWTF的有效性,显著推动了纳拉甘塞特湾的历史低氧趋势.
- 了解过去的缺氧动态对于管理城市化河口当前的水质问题至关重要.
- 沉积地质化学标记为重建河口低氧史提供了宝贵的工具.
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