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定量揭示沿海湿地在调节富营养化和提高水环境保护能力方面的作用。

Quantitatively unveiling the role of coastal wetlands in regulating eutrophication and enhancing water environmental capacity.

机构信息

School of Ecology, Hainan University, Haikou, 570228, China; State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian, 116024, China.

State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian, 116024, China.

出版信息

Mar Environ Res. 2024 Nov;202:106787. doi: 10.1016/j.marenvres.2024.106787. Epub 2024 Oct 12.

DOI:10.1016/j.marenvres.2024.106787
PMID:39406170
Abstract

Human activities have intensified the global challenge of coastal eutrophication. Recently, water resource managers have encountered difficulties in formulating precise pollutant reduction strategies to mitigate coastal eutrophication. Despite the recognized importance of coastal wetlands and pollution sources in influencing coastal nutrient levels, accurately quantifying their impact remains difficult. To address this challenge, this study introduces a novel approach for optimizing water environmental capacity. A coupled model integrating hydrodynamics, water quality, and wetland nutrient mechanisms was developed to simulate the spatio-seasonal distribution of water, sediment, and vegetation nutrients in a semi-enclosed bay (Liaodong Bay, China) and a large-scale coastal wetland (Liaohe estuary wetland, China). Model parameters and simulation results were calibrated and validated using extensive long-term field investigations and laboratory experiments. The average root mean square errors between simulated and observed values for all validation points were as follows: 0.80 mg L, 0.53 mg L, 0.08 mg L, 6.70 μg L, and 0.50 μg L for dissolved oxygen, chemical oxygen demand, dissolved inorganic nitrogen, dissolved inorganic phosphorus, and chlorophyll-a, respectively. The total nitrogen (TN) and total phosphorus (TP) in the sediment were 0.10 g kg and 0.05 g kg, respectively. For Suaeda salsa, the TN and TP were 2.91 g kg and 0.08 g kg , respectively. For Phragmites australis, the TN and TP were 114.22 g kg and 6.21 g kg , respectively. The results suggest that excessive river discharge and a stable residual circulation structure contribute to the persistent eutrophication in Liaodong Bay. The Liaohe estuary wetland enhances the environmental capacity of dissolved inorganic nitrogen and dissolved inorganic phosphorus in Liaodong Bay to 271 ± 31 t yr and 8 ± 1 t yr, respectively, accounting for 1.8 ± 0.2% and 1.3 ± 0.2% of their respective environmental capacities. The reduction in dissolved inorganic nitrogen concentration is significant, with a maximum decrease of 0.17 mg L. The maximum contributions of atmospheric deposition and aquaculture wastewater to dissolved inorganic nitrogen concentration are 0.08 mg L and 0.03 mg L, respectively, with higher contributions in spring and summer than in fall and winter. These findings highlight the critical role of coastal wetlands in mitigating eutrophication and underscore the need for spatio-seasonal water management programs. This work serves as a model for effectively reducing global coastal pollution emissions.

摘要

人类活动加剧了沿海富营养化的全球性挑战。最近,水资源管理者在制定精确的污染物减排策略以减轻沿海富营养化方面遇到了困难。尽管沿海湿地和污染源对影响沿海营养水平的重要性得到了认可,但准确量化它们的影响仍然很困难。为了解决这一挑战,本研究引入了一种优化水环境保护容量的新方法。开发了一个将水动力、水质和湿地营养机制相结合的耦合模型,以模拟半封闭海湾(中国辽东湾)和大型沿海湿地(中国辽河河口湿地)的水、沉积物和植被营养物质的时空分布。使用广泛的长期现场调查和实验室实验对模型参数和模拟结果进行了校准和验证。所有验证点模拟值与实测值的平均均方根误差分别为:溶解氧为 0.80mg/L,化学需氧量为 0.53mg/L,溶解无机氮为 0.08mg/L,溶解无机磷为 6.70μg/L,叶绿素 a 为 0.50μg/L。沉积物中的总氮(TN)和总磷(TP)分别为 0.10g/kg 和 0.05g/kg。对于盐地碱蓬,TN 和 TP 分别为 2.91g/kg 和 0.08g/kg。对于芦苇,TN 和 TP 分别为 114.22g/kg 和 6.21g/kg。结果表明,过量的河流排放和稳定的残余环流结构导致辽东湾持续富营养化。辽河河口湿地将辽东湾的溶解无机氮和溶解无机磷的环境容量分别提高到 271±31t/yr 和 8±1t/yr,分别占各自环境容量的 1.8±0.2%和 1.3±0.2%。溶解无机氮浓度的降低幅度显著,最大降低幅度为 0.17mg/L。大气沉降和水产养殖废水对溶解无机氮浓度的最大贡献分别为 0.08mg/L 和 0.03mg/L,春季和夏季的贡献高于秋季和冬季。这些发现强调了沿海湿地在减轻富营养化方面的关键作用,并强调了需要制定时空水资源管理计划。这项工作为有效减少全球沿海污染排放提供了一个模型。

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