控制季节性大气-生态系统二氧化碳交换在温带盐沼地区的控制
Jesus Ruiz-Plancarte1,2, Jose D Fuentes1, Karen J McGlathery3
1Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, Pennsylvania, USA.
Global change biology
|February 12, 2026
概括
盐沼对于沿海碳循环至关重要. 潮和光线质量显著影响二氧化碳 (CO2) 交换,影响沼泽生物地质化学,特别是随着海平面的变化和温度的升温.
科学领域:
- 沿海生物地质化学
- 生态系统的碳循环循环.
- 盐沼生态学盐沼生态学
背景情况:
- 盐沼对于沿海生物地质化学至关重要.
- 对二氧化碳交换的生物物理控制 (净生态系统交换 - NEE) 量化不足.
- 斯巴尔蒂纳 (Spartina alterniflora) 盐沼是重要的碳汇.
研究的目的:
- 为了研究在Spartina alterniflora盐沼泽中对NEE的生物物理控制.
- 量化潮洪水和光质对二氧化碳交换的影响.
- 为改善潮沼泽生物地球化学模型提供数据.
主要方法:
- 埃迪-协方差法用于估计每半小时的NEE.
- 从2016年3月到2017年2月,持续监测二氧化碳交换情况.
- 与潮淹没和光合作用活性辐射 (PAR) 相关的NEE分析.
主要成果:
- 最大的二氧化碳交换发生在6月和7月,NEE达到-10.0 ± 2.5μmol二氧化碳m−2s−1.1.
- 潮淹没 (0.7米) 减少了二氧化碳的吸收和释放.
- 与直接光相比,分散光条件提高了生态系统量子利用效率 (α) 三倍,增加了30%的二氧化碳同化.
结论:
- 潮淹没和光质是潮沼泽中碳循环的关键调节因素.
- 这些因素必须纳入潮沼泽生物地球化学模型.
- 鉴于海平面上升和大气变暖,了解这些控制非常重要.
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