2014
DOI: 10.1016/j.scitotenv.2014.03.140
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Rich soil carbon and nitrogen but low atmospheric greenhouse gas fluxes from North Sulawesi mangrove swamps in Indonesia

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Cited by 76 publications
(26 citation statements)
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“…Nitrate concentrations were also lower at all study sites (0.37-2.23 mg kg −1 ) as compared to swamps at North Sulawesi (1.54-13.68 mg kg −1 ; Chen et al 2014), Mai Po (0.31-5.29 mg kg −1 ; Chen et al 2012), and South East Queensland (1-25 mg kg −1 ; Allen et al 2007). Despite similarities in nitrate concentrations, the Pear River Estuary in China showed much higher N 2 O fluxes (1.48-251.6 g ha −1 day −1 ) than those reported in this study (Chen et al 2010).…”
Section: Annual Ghg Fluxes and Comparison With Other Studiesmentioning
confidence: 72%
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“…Nitrate concentrations were also lower at all study sites (0.37-2.23 mg kg −1 ) as compared to swamps at North Sulawesi (1.54-13.68 mg kg −1 ; Chen et al 2014), Mai Po (0.31-5.29 mg kg −1 ; Chen et al 2012), and South East Queensland (1-25 mg kg −1 ; Allen et al 2007). Despite similarities in nitrate concentrations, the Pear River Estuary in China showed much higher N 2 O fluxes (1.48-251.6 g ha −1 day −1 ) than those reported in this study (Chen et al 2010).…”
Section: Annual Ghg Fluxes and Comparison With Other Studiesmentioning
confidence: 72%
“…However, higher CH 4 emissions have been reported in other mangroves, e.g., the fluxes reported for mangrove swamps at Guangdong, China (0.005 to 19.9 kg ha −1 day −1 ) and South East Queensland, Australia (0.001 to 4.18 kg ha −1 day −1 ) are similar to those recorded in the present study (Table 4). In North Sulawesi, Chen et al (2014) showed that despite low CH 4 emissions, sulfate reduction was unlikely to occur as little or no sulfate reduction occurs with a redox potential over −150 mV. Low sulfate reduction rates were also reported at the tropical Ao Nam Bor mangrove in Thailand (Kristensen et al 1994).…”
Section: Annual Ghg Fluxes and Comparison With Other Studiesmentioning
confidence: 99%
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“…The major sources of methane include wetlands (Belger et al 2011), rivers (Sawakuchi et al 2014), swamps (Chen et al 2014), rice paddies (Bhatia et al 2011;Liu et al 2012b), and ruminant livestock (Moraes et al 2014). The major sinks of methane are photochemical oxidation by the hydroxyl radical (OH) in the atmosphere (Cicerone and Oremland 1988) and biological oxidation by the methanotrophs in the aerobic soil (Curry 2007).…”
Section: Introductionmentioning
confidence: 99%