概括
自1850年以来,大气中的沉积到偏远湖泊的数量增加了三倍,大气中的25%的从周围的土地出口到湖泊. 这表明存在广泛的源.
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:
- 偏远湖泊中的污染是一个越来越令人担忧的问题.
- 历史上的沉积率和陆地输入不太清楚.
- 大气中的沉积是主要的疑似来源.
研究的目的:
- 为了重建偏远湖泊中的沉积率.
- 为了量化大气中的出口到湖泊的陆地出口.
- 为了确定污染的来源.
主要方法:
- 来自明尼苏达州和威斯康星州七个河头湖泊的湖泊沉积物的分析.
- 沉积物核心的年代测定,以建立历史时间线.
- 计算整个盆地的流量.
主要成果:
- 自1850年以来,每年大气中的沉积量从3.7至12.5μg/m2增加.
- 大气中的25%的沉积在流域中被输送到湖中.
- 跨地点的类似沉积增加表明区域或全球来源.
结论:
- 自工业前时代以来,水银沉积到偏远湖泊的数量显著增加.
- 陆地生态系统是进入湖泊的重要途径.
- 区域或全球大气过程可能导致这些偏远湖泊的污染.
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