Distribution of dissolved methane concentration and its flux in early autumn in the Yangtze Estuary-Hangzhou Bay
Abstract
基于2022年9月长江口−杭州湾海洋污染基线试点调查航次,本文开展了溶解甲烷浓度和海−气交换通量及主要调控因子的观测研究。结果显示,观测海域表层海水中溶解甲烷浓度范围为(6.89~43.41)nmol/L,平均值为(18.58 ± 8.88)nmol/L,底层海水中溶解甲烷浓度范围为(8.88~36.15)nmol/L,平均值为(8.25 ± 89.34)nmol/L。溶解甲烷浓度总体呈长江口和杭州湾内较高、离岸外海较低的分布特征,显示陆源河流输入和沉积物释放是观测海域溶解甲烷的主要来源。观测海域表层海水中溶解甲烷平均饱和度达(275.10 ± 6.70)%,海−气甲烷交换通量平均值为(157.40 ± 145.68)μmol/(m2·d),是大气甲烷的源。初步估算该海域甲烷年释放量约为1.78 ×109 mol,约占全球海洋年释放量的0.16%,可直接导致观测海域海表大气甲烷摩尔分数抬升约3.2 nmol/mol。
Fields of Study & Subjects
Methane Hydrates and Related Phenomena
Atmospheric and Environmental Gas Dynamics
Marine and coastal ecosystems
Publication details
- Journal / source
- Marine Environmental Science
- Publication date
- 1 January 2026
- Language
- EN