An open dynamic chamber for the continuous monitoring of diffusive and ebullitive fluxes of methane (CH4) in aquatic ecosystems was designed and developed. This method is based on a standard floating chamber in which a well-defined carrier gas flows. The concentration of CH4 is measured continuously at the outlet of the chamber, and the flux is determined from a mass balance equation. The method was carefully tested in a laboratory and was subsequently applied to two lakes, in Mexico, with contrasting trophic states. We show here that the method allows for the continuous quantification of CH4 diffusive flux higher than 25 × 10–6 g m–2 h–1, the determination of ebullitive flux, and the individual characterization of bubbles larger than 1.50–...
Methane is the main end product of anaerobic degradation in freshwater sediments. The flux of methan...
Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Enginee...
Three parameters must be known to use the thin boundary-layer model (or other bulk transfer models) ...
Processes driving the production, transformation and transport of methane (CH4) in wetland ecosystem...
Accurately quantifying total freshwater storage methane release to atmosphere requires the spatial-t...
Atmospheric methane (CH4) concentrations have more than doubled in the past ~ 250 yr, although the s...
Aquatic ecosystems are major sources of greenhouse gases (GHG). Representative measurements of GHG f...
In lakes and reservoirs with variable water level, gas ebullition can play a substantial role in met...
Methane (CH4) ebullition in northern peatlands is poorly quantified in part due to its high spatiote...
The closed chamber technique is widely used to measure the exchange of methane (CH4) and carbon diox...
Thesis: Ph. D. in Environmental Engineering, Massachusetts Institute of Technology, Department of Ci...
Uncertainties in wetland methane flux characteristics stem from complex spatial and temporal heterog...
We analyzed the processes affecting the methane (CH4) budget in Lake Kinneret, a deep subtropical la...
Estimations of methane (CH4) emissions are often based on point measurements using either flux chamb...
Methane is a non-toxic colourless gas created by decomposition of organic materials in anaerobic env...
Methane is the main end product of anaerobic degradation in freshwater sediments. The flux of methan...
Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Enginee...
Three parameters must be known to use the thin boundary-layer model (or other bulk transfer models) ...
Processes driving the production, transformation and transport of methane (CH4) in wetland ecosystem...
Accurately quantifying total freshwater storage methane release to atmosphere requires the spatial-t...
Atmospheric methane (CH4) concentrations have more than doubled in the past ~ 250 yr, although the s...
Aquatic ecosystems are major sources of greenhouse gases (GHG). Representative measurements of GHG f...
In lakes and reservoirs with variable water level, gas ebullition can play a substantial role in met...
Methane (CH4) ebullition in northern peatlands is poorly quantified in part due to its high spatiote...
The closed chamber technique is widely used to measure the exchange of methane (CH4) and carbon diox...
Thesis: Ph. D. in Environmental Engineering, Massachusetts Institute of Technology, Department of Ci...
Uncertainties in wetland methane flux characteristics stem from complex spatial and temporal heterog...
We analyzed the processes affecting the methane (CH4) budget in Lake Kinneret, a deep subtropical la...
Estimations of methane (CH4) emissions are often based on point measurements using either flux chamb...
Methane is a non-toxic colourless gas created by decomposition of organic materials in anaerobic env...
Methane is the main end product of anaerobic degradation in freshwater sediments. The flux of methan...
Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Enginee...
Three parameters must be known to use the thin boundary-layer model (or other bulk transfer models) ...