通过有机物质可用性的沿海沉积物中循环的超线性控制
Jing Sun1, Xiaotian Zhou1, Yuxuan Lin1
1Department of Ocean Science, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong SAR, PR China.
Water research
|May 30, 2025
概括
沿海沉积物 (P) 的回收复杂. 酸盐,而不仅仅是氧气,控制了有机丰富地区的P释放,影响了地球化学预算.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 海洋生物地质化学海洋生物地质化学
背景情况:
- 沉积物 (P) 循环对于水柱P可用性和生物地化学预算至关重要.
- 在沿海沉积物中量化P再生与固定是具有挑战性的,因为环境的变化.
- 现有的模型往往过于简化了P循环,主要关注氧气的作用.
研究的目的:
- 调查控制珍珠河河口沉积物P循环的因素.
- 为了确定氧气和酸盐在调节P释放中的相对重要性.
- 了解有机物重矿化和P efflux之间的关系.
主要方法:
- 在珍珠河河口的水深梯度 (9-63米) 上进行现场采样.
- 测量沉积物酸盐排放量和P回收效率.
- 对沉积物吸收氧气,有机物含量和营养度 (酸盐) 的分析.
主要成果:
- 观测到沉积物酸盐排放 (4.9-1190 μmol m−2 d−1) 中的显著变化.
- 发现酸盐的可用性,而不是氧气,在有机丰富,浅氧沉积物中主导了P的释放.
- 确定了有机物再矿化和河口和海上P流量之间的超线性 (权力法) 关系.
结论:
- 酸盐在保护P结合氧化铁中发挥着关键作用,抑制了上游地区的释放.
- 在富含铁的沿海系统中,有机物重矿化的高水平导致了不成比例的高P流量.
- 有机物对P循环的超线性控制需要纳入类似环境中的沉积物-水交换模型.
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