Dissolved methane concentrations and fluxes to the atmosphere from a tropical floodplain lake

2020 ◽  
Vol 148 (2) ◽  
pp. 129-151 ◽  
Author(s):  
Pedro M. Barbosa ◽  
John M. Melack ◽  
João H. F. Amaral ◽  
Sally MacIntyre ◽  
Daniele Kasper ◽  
...  
2013 ◽  
Vol 36 (4) ◽  
pp. 257-266 ◽  
Author(s):  
Bárbara Dunck ◽  
Jascieli Carla Bortolini ◽  
Liliana Rodrigues ◽  
Luzia Cleide Rodrigues ◽  
Susicley Jati ◽  
...  

PLoS ONE ◽  
2015 ◽  
Vol 10 (4) ◽  
pp. e0123319 ◽  
Author(s):  
Roberta B. Peixoto ◽  
Fausto Machado-Silva ◽  
Humberto Marotta ◽  
Alex Enrich-Prast ◽  
David Bastviken

Author(s):  
Laura Lapham ◽  
Kathleen Marshall ◽  
Cédric Magen ◽  
Viacheslav Lyubchich ◽  
Lee W. Cooper ◽  
...  

2009 ◽  
Vol 60 (11) ◽  
pp. 2963-2971 ◽  
Author(s):  
Jeff Foley ◽  
Zhiguo Yuan ◽  
Paul Lant

At present, the potential generation of methane in wastewater collection systems is ignored under international greenhouse gas (GHG) accounting protocols, despite recent reports of substantial dissolved methane formation in sewers. This suggests that the current national GHG inventories for wastewater handling systems are likely to be underestimated for some situations. This study presents a new catalogue of field data on methane formation in rising main sewerage systems and proposes an empirically-fitted, theoretical model to predict dissolved methane concentrations, based upon the independent variables of pipeline geometry (i.e. surface area to volume ratio, A/V) and hydraulic retention time (HRT). Systems with longer HRT and/or larger A/V ratios are shown to have higher dissolved methane concentrations. This simple predictive model provides a means for water authorities to estimate the methane emissions from other pressurised sewerage systems of similar characteristics.


2011 ◽  
Vol 38 (8) ◽  
pp. n/a-n/a ◽  
Author(s):  
Xin Zhang ◽  
Keith C. Hester ◽  
William Ussler ◽  
Peter M. Walz ◽  
Edward T. Peltzer ◽  
...  

2013 ◽  
Vol 47 (3) ◽  
pp. 27-36 ◽  
Author(s):  
Mark Schmidt ◽  
Peter Linke ◽  
Daniel Esser

AbstractRecently developed methane sensors, based on infrared (IR) absorption technology, were successfully utilized for subsea methane release measurements. Long-term investigation of methane emissions (fluid flux determination) from natural methane seeps in the Hikurangi Margin offshore New Zealand were performed by using seafloor lander technology. Small centimeter-sized seep areas could be sampled at the seafloor by video-guided lander deployment. In situ sensor measurements of dissolved methane in seawater could be correlated with methane concentrations measured in discrete water samples after lander recovery. High backscatter flares determined by lander-based Acoustic Doppler Current Profiler (ADCP) measurement indicate bubble release from the seafloor. Highest methane concentrations determined by the IR sensor coincided with periods of high ADCP backscatter signals. The high fluid release cannot be correlated with tidal changes only. However, this correlation is possible with variability in spatial bubble release, sudden outbursts, and tidal changes in more quiescent seepage phases.A recently developed IR sensor (2,000 m depth-rated) with a detection limit for methane of about 1 ppm showed good linearity in the tested concentration range and an acceptable equilibration time of 10 min. The sensor was successfully operated offshore Santa Barbara by a small work-class ROV at a natural methane seep (Farrar Seep). High background methane concentration of 50 nmol L−1 was observed in the coastal water, which increases up to 560 nmol L−1 in dissolved methane plumes south of the seepage area. ROV- and lander-based sensor deployments have proven the applicability of IR sensor technology for the determination of subsea methane release rates and plume distribution. The wide concentration range, low detection limit, and its robust detection unit enable this technology for both subsea leak detection and oceanographic trace gas investigations.


2015 ◽  
Vol 12 (18) ◽  
pp. 5261-5276 ◽  
Author(s):  
S. Mau ◽  
T. Gentz ◽  
J.-H. Körber ◽  
M. E. Torres ◽  
M. Römer ◽  
...  

Abstract. We investigated dissolved methane distributions along a 6 km transect crossing active seep sites at 40 m water depth in the central North Sea. These investigations were done under conditions of thermal stratification in summer (July 2013) and homogenous water column in winter (January 2014). Dissolved methane accumulated below the seasonal thermocline in summer with a median concentration of 390 nM, whereas during winter, methane concentrations were typically much lower (median concentration of 22 nM). High-resolution methane analysis using an underwater mass-spectrometer confirmed our summer results and was used to document prevailing stratification over the tidal cycle. We contrast estimates of methane oxidation rates (from 0.1 to 4.0 nM day−1) using the traditional approach scaled to methane concentrations with microbial turnover time values and suggest that the scaling to concentration may obscure the ecosystem microbial activity when comparing systems with different methane concentrations. Our measured and averaged rate constants (k') were on the order of 0.01 day−1, equivalent to a turnover time of 100 days, even when summer stratification led to enhanced methane concentrations in the bottom water. Consistent with these observations, we could not detect known methanotrophs and pmoA genes in water samples collected during both seasons. Estimated methane fluxes indicate that horizontal transport is the dominant process dispersing the methane plume. During periods of high wind speed (winter), more methane is lost to the atmosphere than oxidized in the water. Microbial oxidation seems of minor importance throughout the year.


Sign in / Sign up

Export Citation Format

Share Document