首页|2022年8月北黄海北部溶解甲烷分布、海-气交换通量及影响因素

2022年8月北黄海北部溶解甲烷分布、海-气交换通量及影响因素

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科学评估陆架边缘海溶解甲烷(CH4)的分布及海-气交换通量对于认识陆架边缘海CH4 的释放对大气CH4 的区域性贡献具有重要意义.基于 2022年 8月的现场调查数据和资料,研究北黄海北部海水溶解CH4 的分布、海-气交换通量及影响因素.结果表明:研究海域溶解CH4 浓度为 4.0~63.3 nmol/L,饱和度为 168%~2 360%,高值区位于鸭绿江口附近海域,随着离岸距离的增加表层海水溶解CH4 浓度迅速降低.鸭绿江等陆源冲淡水的输入耦合海水及沉积物有机质的降解致使近岸海域海水CH4 升高;陆源冲淡水与海水混合过程中海水CH4 的氧化消耗也是控制CH4 浓度和分布不容忽视的重要过程.离岸海域海水及沉积物有机质厌氧降解耦合黄海冷水团的作用使得底层海水溶解CH4 浓度高于表层海水.研究海域海-气CH4 交换通量为 18.4~578.8 μmol/(m2·d),是大气CH4 的源;鸭绿江口附近海域海-气CH4 交换通量高于离岸海域.由此可见,受陆源冲淡水输入的影响研究海域溶解CH4 浓度和海-气交换通量具有显著的区域性差异,且变幅高于世界其他海域;加强河口以及近海调查研究对于准确评估陆架边缘海CH4 的排放,明确CH4 排放源项的构成及制定CH4 减排的有效措施至关重要.
Distributions,Influencing Factors and Sea-Air Fluxes of Dissolved Methane in the Northern of North Yellow Sea in August 2022
Scientific assessment of the distribution and sea-air fluxes of dissolved methane(CH4)in the marginal sea is important for understanding the regional contribution of CH4 emission to the atmosphere.The distribution,influencing factors and sea-air fluxes of CH4 in the northern of the North Yellow Sea were studied based on a survey in August 2022.The results showed that the dissolved CH4 concentrations range were from 4.0 nmol/L to 63.3 nmol/L with saturations from 168%to 2 360%in the study area.High CH4 concentrations were observed in Yalu River estuary,and the dissolved CH4 concentrations in surface seawater decreased rapidly as the estuary extends to the sea,while the input of diluted water from terrestrial sources such as the Yalu River coupled with the degradation of seawater and sediment organic matter leaded to an increase in CH4 in inshore area.The oxidative consumption of CH4 in seawater mixing with the terrestrial diluted water was also an important process that could not be ignored in controlling CH4 concentration and distribution.The action of North Yellow Sea Cold Water Mass coupled with anaerobic degradation of sediment organic matter resulted in relatively high dissolved CH4 concentrations in bottom seawater than that in surface seawater in the offshore area.In the study area the sea-air CH4 fluxes were from 18.4 μmol/(m2·d)to 578.8 μmol/(m2·d),being the source of atmospheric CH4 and it was significantly higher in the inshore area than that of the offshore area.Therefore,the dissolved CH4 concentrations and sea-air fluxes in this area had significant differences due to the inputs of diluted water,and the variation amplitude was higher than that of other sea area in the world.It is crucial to strengthen the investigation and research in coastal areas such as estuary to accurately assess the CH4 emissions and emission source composition to formulate effective CH4 reduction measures.

the North Yellow Seadissolved methaneair-sea CH4 fluxinputs of diluted wateranaerobic degradation of organic matter

徐雪梅、王明丽、何宗财、韩建波、邢庆会、王心怡、陈虹

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国家海洋环境监测中心,辽宁大连 116023

山东省青岛生态环境监测中心,山东青岛 266003

大连海事大学环境科学与工程学院,辽宁大连 116026

北黄海 溶解甲烷 海-气CH4交换通量 冲淡水输入 有机质厌氧降解

国家自然科学基金项目国家自然科学基金项目大连市海洋碳汇重点实验室项目

4187612841206060

2024

海洋科学进展
中国海洋学会 国家海洋局第一海洋研究所

海洋科学进展

CSTPCD北大核心
影响因子:0.532
ISSN:1671-6647
年,卷(期):2024.42(4)