Measuring in situ soil fluxes of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) continuously at high frequency requires appropriate technology. We tested the combination of a commercial automated soil CO2 flux chamber system (LI-8100A) with a CH4 and N2O analyzer (Picarro G2308) in a tropical rainforest for 4 months. A chamber closure time of 2 min was sufficient for a reliable estimation of CO2 and CH4 fluxes (100% and 98.5% of fluxes were above minimum detectable flux - MDF, respectively). This closure time was generally not suitable for a reliable estimation of the low N2O fluxes in this ecosystem but was sufficient for detecting rare major peak events. A closure time of 25 min was more appropriate for reliable estimation o...
Here we present novel method development and instruction in the construction and use of Field Portab...
Chamber measurements of trace gas fluxes between the land surface and the atmosphere have been condu...
Soil methane (CH4) and nitrous oxide (N2O) fluxes are difficult to predict from soil temperature and...
International audienceMeasuring in situ soil fluxes of carbon dioxide (CO2), methane (CH4), and nitr...
International audienceTree stems and soils can act as sources and sinks for the greenhouse gases (GH...
International audienceTree stems and soils can act as sources and sinks for the greenhouse gases (GH...
Recent technological advances have enabled the wider application of automated chambers for soil gree...
As soil–atmosphere fluxes of greenhouse gases are characterized by high temporal fluctuations, frequ...
Ten sites covering six different ecosystems were selected for detailed situ N2O and CH4 exchange mea...
Measurements of greenhouse gas (GHG) fluxes, particularly methane (CH4) and nitrous oxide (N2O) in m...
The closed chamber technique is widely used to measure the exchange of methane (CH4) and carbon diox...
An automated transient-state closed-system canopy-chamber for gas-exchange determinations of field-c...
Methods and techniques are described for automated measurements of greenhouse gases (GHGs) in both t...
Carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) are the greenhouse gases largely respon...
This protocol addresses the measurement of greenhouse gases (GHGs) soil ef\ufb02 ux by soil chamber...
Here we present novel method development and instruction in the construction and use of Field Portab...
Chamber measurements of trace gas fluxes between the land surface and the atmosphere have been condu...
Soil methane (CH4) and nitrous oxide (N2O) fluxes are difficult to predict from soil temperature and...
International audienceMeasuring in situ soil fluxes of carbon dioxide (CO2), methane (CH4), and nitr...
International audienceTree stems and soils can act as sources and sinks for the greenhouse gases (GH...
International audienceTree stems and soils can act as sources and sinks for the greenhouse gases (GH...
Recent technological advances have enabled the wider application of automated chambers for soil gree...
As soil–atmosphere fluxes of greenhouse gases are characterized by high temporal fluctuations, frequ...
Ten sites covering six different ecosystems were selected for detailed situ N2O and CH4 exchange mea...
Measurements of greenhouse gas (GHG) fluxes, particularly methane (CH4) and nitrous oxide (N2O) in m...
The closed chamber technique is widely used to measure the exchange of methane (CH4) and carbon diox...
An automated transient-state closed-system canopy-chamber for gas-exchange determinations of field-c...
Methods and techniques are described for automated measurements of greenhouse gases (GHGs) in both t...
Carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) are the greenhouse gases largely respon...
This protocol addresses the measurement of greenhouse gases (GHGs) soil ef\ufb02 ux by soil chamber...
Here we present novel method development and instruction in the construction and use of Field Portab...
Chamber measurements of trace gas fluxes between the land surface and the atmosphere have been condu...
Soil methane (CH4) and nitrous oxide (N2O) fluxes are difficult to predict from soil temperature and...