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北部硬水湖的二氧化碳排放量减少,随着大气变暖的增加
Kerri Finlay1, Richard J Vogt1, Matthew J Bogard1
1Limnology Laboratory, Department of Biology, University of Regina, Regina, Saskatchewan, Canada S4S 0A2.
Nature
|March 4, 2015
概括
大气变暖可能会通过减少冰盖来减少硬水湖的二氧化碳 (CO2) 排放. 这种转变表明,温度上升并不总是增加水生生态系统的二氧化碳排放.
科学领域:
- 环境科学 环境科学
- 临界技术 临界技术
- 生物地质化学生物地质化学
背景情况:
- 玻里亚湖是重要的生物地化学热点,影响全球碳循环.
- 稀释的北极湖泊释放大量的二氧化碳 (CO2) 和甲,由于气候变化而可能增加.
- 碳酸盐丰富的硬水和盐湖中的碳流动动力学仍然不太了解.
研究的目的:
- 为了研究大气变暖对硬水湖中的碳流的影响.
- 分析湖泊pH和二氧化碳交换的十年趋势,以应对气候变化.
- 了解推动水生碳循环变化的机制.
主要方法:
- 对气象数据,二氧化碳流量和水化学的十年记录的分析.
- 在不同湖泊类型中研究pH和碳交换的变化.
- 利用统计分析将气候变量与湖泊生物地化学过程联系起来.
主要成果:
- 硬水湖在20世纪90年代中期至2010年间从二氧化碳来源转变为二氧化碳沉.
- 观察到这些湖泊每年平均pH值的持续增加.
- 大气变暖引起的春季冰层减少与二氧化碳积累减少和二氧化碳吸收增加有关.
结论:
- 大气变暖可以减少硬水湖的二氧化碳排放,这与普遍的预期相反.
- 冰盖持续时间的变化显著影响湖泊的pH值和碳捕获.
- 水生生态系统可能会对气候变化表现出复杂的反应,而不是均地增加碳排放.
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