研究报告

  • 漆梦婷,罗柳,洪晓静,钱伟,仝川,李小飞.闽江河口表层水体氧化亚氮释放时空变化特征及其影响因素[J].环境科学学报,2022,42(7):489-500

  • 闽江河口表层水体氧化亚氮释放时空变化特征及其影响因素
  • Spatial and temporal variations and influencing factors of nitrous oxide emissions from surface water in Min River Estuary
  • 基金项目:国家自然科学基金(No.42071130,41701548);福建省自然科学基金(No.2020J01184)
  • 作者
  • 单位
  • 漆梦婷
  • 福建师范大学地理科学学院,福州 350007
  • 罗柳
  • 福建师范大学地理科学学院,福州 350007
  • 洪晓静
  • 福建师范大学地理科学学院,福州 350007
  • 钱伟
  • 福建师范大学地理科学学院,福州 350007;福建师范大学湿润亚热带生态-地理过程教育部重点实验室,福州 350007
  • 仝川
  • 福建师范大学地理科学学院,福州 350007;福建师范大学湿润亚热带生态-地理过程教育部重点实验室,福州 350007
  • 李小飞
  • 福建师范大学地理科学学院,福州 350007;福建师范大学湿润亚热带生态-地理过程教育部重点实验室,福州 350007
  • 摘要:以闽江口水体为研究对象,研究了闽江河口上段(城市河口段)、河口中段和河口下段(口外海滨段)不同季节水体N2O的溶存浓度、水-气界面通量及其环境影响因子.结果表明,闽江口水体N2O溶存浓度为0.99~55.92 nmol·L-1,N2O饱和度为8.0%~396%,水-气界面N2O释放通量为-5.21~7.91 μg·m-2·h-1.从季节差异看,7月(夏季)、9月(秋季)和12月(冬季)水体中N2O过饱和,表现为N2O的排放“源”;4月(春季)水体中N2O不饱和,表现为N2O“汇”.水-气界面N2O释放通量呈夏、秋和冬季高,春季低的季节变化规律.在空间变化上,水-气界面N2O释放通量从 河口上段到下段降低,与氮含量变化趋势一致.N2O间接性释放因子为0.004%~0.128%,低于IPCC推荐值(0.25%).温度、盐度、pH、NO3-、DO、 悬浮颗粒物浓度是影响N2O溶存浓度与释放通量的主要影响因素.因此,季节性变化和人类活动导致河口N2O释放存在较大的时空差异性,从而增加了河口N2O排放评估的不确定性.
  • Abstract:In this study, seasonal variability of N2O concentrations and fluxes and associated environmental factors were investigated in the upper section (urban estuary), the middle section and the lower section (coastal section outside the estuary) of Min River Estuary. The results indicated that N2O concentrations, N2O saturations and N2O fluxes were in a range of 0.99~55.92 nmol·L-1, 8.0%~396%, and -5.21~7.91 μg·m-2·h-1. Water N2O was supersaturated in July (summer), September (autumn) and December (winter), representing the "source" of N2O emission. However, N2O emissions exhibited the "sink" in April (spring). N2O fluxes were significantly higher in summer, autumn and winter than in spring, and decreased from the upper to lower estuary. Indirect N2O emission factors ranged from 0.004% to 0.128%, which was significantly lower than the IPCC default value (0.25%). Temperature, salinity, pH, NO3-, DO and suspended particulate matter were the crucial factors affecting dissolved N2O concentrations and fluxes. Therefore, seasonal changes and human activities can trigger the large variability of N2O emissions, leading to the increasing uncertainty of N2O projections.

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