使用酸盐的双同位素解密和量化黄海中部的酸盐来源和过程
Xiaosong Zhong1, Xiangbin Ran2
1Marine Ecology Research Center, The First Institute of Oceanology, Ministry of Natural Resources, Qingdao 266061, China.
Water research
|June 27, 2024
概括
黄海的酸盐来源是使用双同位素识别的. 大气沉积是关键的表面酸盐来源,而同化和有机物质驱动深水中的积累.
科学领域:
- 海洋生物地质化学海洋生物地质化学
- 同位素地球化学 同位素地球化学
- 沿海海洋学 沿海海洋学
背景情况:
- 人类活动导致沿海地区的积.
- 确定酸盐来源对于管理沿海污染至关重要.
- 像黄海这样的边缘海面临着重大的气挑战.
研究的目的:
- 通过使用双同位素,研究酸盐 (NO3-) 的来源和黄海中部的循环.
- 了解不同水体中酸盐度的空间变化.
- 评估分层对营养物质运输和来源的影响.
主要方法:
- 对双酸盐 (NO3-) 同位素 (δ15N-NO3-和 δ18O-NO3-) 的分析.
- 调查不同水体中的酸盐度:黄海表面水 (YSSW),长江稀释水 (CDW),黄海冷水体 (YSCWM) 和台湾暖流水 (TWCW).
- 评估分层对垂直营养物质运输的影响.
主要成果:
- 在水体中观察到酸盐度的显著空间变化.
- 大气沉积被确定为表面酸盐的主要来源 (在YSSW中约为30%).
- 在CDW中表明酸盐同化不完全,而有机物矿化和分层导致YSCWM和TWCW中酸盐积累.
结论:
- 双化物同位素分析对于追踪沿海海域的源是有效的.
- 沿海酸盐供应是海洋,陆地和大气过程的复杂相互作用.
- 了解这些动态对于减轻人为营养污染至关重要.
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