Yu Hao, Coffin Richard
Department of Physical and Environmental Sciences, Texas A&M University-Corpus Christi, 6300 Ocean Drive, Corpus Christi, TX 78412, USA.
Mar Pollut Bull. 2025 Oct;219:118320. doi: 10.1016/j.marpolbul.2025.118320. Epub 2025 Jun 19.
Coastal regions located in dynamic environments that are disturbed by extensive human activities have been recognized as long-term sources of atmospheric methane (CH). This study investigated dissolved CH concentrations, sea-air CH fluxes, and environmental factors in three urbanization-influenced subtropical estuaries in southern Texas, northwest of the Gulf of Mexico, from May 2018 to May 2021 to explore the interactions between natural processes and anthropogenic activities. The results revealed that high spatial-temporal variations in CH emissions occurred because of differences in the distributions of environmental features, hydrological conditions, and anthropogenic influences in each estuary. Elevated CH concentrations in channels were caused by waste discharge from maritime vessels and mechanical damage to seagrass meadows and sediment by dredging or boat grounding. Leakage from coastal oil and gas platforms was another anthropogenic source of atmospheric CH. Although sea-air CH fluxes were lowest in bay water, annual regional CH emissions evaluated using geometric mean sea-air CH fluxes were much higher than other environmental characteristics because of the larger areas of bay water, suggesting that the contribution of bay water to atmospheric CH cannot be ignored. Channels, as the primary anthropogenically disturbed areas, have not been found to input a significant amount of CH into the atmosphere; however, their high sea-air CH fluxes indicated a high risk of elevated CH emissions if the disturbance areas are not controlled. These findings emphasize the importance of monitoring anthropogenically related CH emissions from water to the atmosphere in the petroleum industry and maritime-influenced estuaries.
位于受广泛人类活动干扰的动态环境中的沿海地区,已被公认为大气甲烷(CH)的长期来源。本研究调查了2018年5月至2021年5月期间,位于墨西哥湾西北部得克萨斯州南部的三个受城市化影响的亚热带河口的溶解CH浓度、海气CH通量和环境因素,以探讨自然过程与人为活动之间的相互作用。结果表明,由于每个河口环境特征、水文条件和人为影响分布的差异,CH排放存在高时空变化。航道中CH浓度升高是由于海上船只的废物排放以及疏浚或船只搁浅对海草草甸和沉积物造成的机械破坏。沿海油气平台的泄漏是大气CH的另一个人为来源。尽管海湾水中的海气CH通量最低,但由于海湾水面积较大,使用几何平均海气CH通量评估的年度区域CH排放量远高于其他环境特征,这表明海湾水对大气CH的贡献不可忽视。航道作为主要的人为干扰区域,尚未发现向大气中输入大量的CH;然而,它们较高的海气CH通量表明,如果干扰区域得不到控制,CH排放增加的风险很高。这些发现强调了监测石油工业和受海洋影响的河口从水到大气的人为相关CH排放的重要性。