Methane and nitrous oxide emissions from a subtropical estuary (the Brisbane River estuary, Australia)

被引:74
作者
Musenze, Ronald S. [1 ]
Werner, Ursula [1 ]
Grinham, Alistair [1 ,2 ]
Udy, James [3 ]
Yuan, Zhiguo [1 ]
机构
[1] Univ Queensland, Adv Water Management Ctr, Brisbane, Qld 4072, Australia
[2] Univ Queensland, Sch Civil Engn, Brisbane, Qld 4072, Australia
[3] Hlth Waterways Ltd, Brisbane, Qld 4003, Australia
基金
澳大利亚研究理事会;
关键词
Greenhouse gas; Methane; Nitrous oxide; Estuary; Subtropical; Aquatic emissions; GAS TRANSFER VELOCITY; FRESH-WATER; HUDSON RIVER; RANDERS FJORD; N2O EMISSIONS; WIND-SPEED; EXCHANGE; MARINE; DENITRIFICATION; VARIABILITY;
D O I
10.1016/j.scitotenv.2013.11.085
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Methane (CH4) and nitrous oxide (N2O) are two key greenhouse gases. Their global atmospheric budgeting is, however, flout with challenges partly due to lack of adequate field studies determining the source strengths. Knowledge and data limitations exist for subtropical and tropical regions especially in the southern latitudes. Surface water methane and nitrous oxide concentrations were measured in a subtropical estuarine system in the southern latitudes in an extensive field study from 2010 to 2012 and water-air fluxes estimated using models considering the effects of both wind and flow induced turbulence. The estuary was found to be a strong net source of both CH4 and N2O all-year-round. Dissolved N2O concentrations ranged between 9.1 +/- 0.4 to 4.53 +/- 1.3 nM or 135 to 435% of atmospheric saturation level, while CH4 concentrations varied between 31.1 +/- 3.7 to 578.4 +/- 58.8 nM or 1210 to 26,430% of atmospheric saturation level. These results compare well with measurements from tropical estuarine systems. There was strong spatial variability with both CH4 and N2O concentrations increasing upstream the estuary. Strong temporal variability was also observed but there were no clear seasonal patterns. The degree of N2O saturation significantly increased with NOx concentrations (r(2) = 0.55). The estimated water-air fluxes varied between 0.1 and 3.4 mg N2O m(-2) d(-1) and 0.3 to 27.9 mg CH4 m(-2) d(-1). Total emissions (CO2-e) were N2O (64%) dominated, highlighting the need for reduced nitrogen inputs into the estuary. Choice of the model(s) for estimation of the gas transfer velocity had a big bearing on the estimated total emissions. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:719 / 729
页数:11
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