International audienceDissolved gases are useful tools in hydrogeology. They inform us on physical and biogeochemical processes along the flow paths of groundwater (noble gases temperature, excess air, redox processes, groundwater ages,...). The sampling and measurement of dissolved gases are often complex and require sometimes long and costly analytical methods. Recently, field membrane inlet mass spectrometer (MIMS) technologies have been developed and optimized to environmental studies. We present here our "continuous flow" MIMS (CF-MIMS) for field measurements of dissolved gases: H2, He, Ne, Ar, N2, Kr, Xe, CH4, N2O, O2 and CO2. Calibration, optimization and limitations of the measurements are presented. The results of a gas tracer expe...
International audienceIdentification of biogeochemical reactions inaquifers and determining kinetics...
International audienceOver the last century, the Critical Zone faced remarkable climate and land use...
International audienceWater quality in rivers results from biogeochemical processes in contributing ...
International audienceDissolved gases are useful tools in hydrogeology. They inform us on physical a...
International audienceWe present an optimized Continuous Flow -Membrane Inlet Mass Spectrometer (CF-...
International audienceIn the perspective of a temporal and spatial exploration of aquatic environmen...
International audienceIn the perspective of a temporal and spatial exploration of aquatic ...
In the perspective of a temporal and spatial exploration of aquatic environments (surface and ground...
International audienceIn the perspective of a temporal and spatial exploration of the Critical Zone,...
We developed a stand-alone system based on a membrane inlet mass spectrometer (MIMS) for measuring d...
International audienceDissolved gases are particularly relevant tools for the investigation of envir...
In recent years, mass spectrometers with a membrane inlet separating gases from water for final anal...
A Membrane Inlet Mass Spectrometer (MIMS) is used to measure dissolved gas concentrations in environ...
Labeling groundwater by injecting an artificial tracer is a standard and widely used method to study...
International audienceIn natural waters, noble gas concentrations are governedby a diversity of rela...
International audienceIdentification of biogeochemical reactions inaquifers and determining kinetics...
International audienceOver the last century, the Critical Zone faced remarkable climate and land use...
International audienceWater quality in rivers results from biogeochemical processes in contributing ...
International audienceDissolved gases are useful tools in hydrogeology. They inform us on physical a...
International audienceWe present an optimized Continuous Flow -Membrane Inlet Mass Spectrometer (CF-...
International audienceIn the perspective of a temporal and spatial exploration of aquatic environmen...
International audienceIn the perspective of a temporal and spatial exploration of aquatic ...
In the perspective of a temporal and spatial exploration of aquatic environments (surface and ground...
International audienceIn the perspective of a temporal and spatial exploration of the Critical Zone,...
We developed a stand-alone system based on a membrane inlet mass spectrometer (MIMS) for measuring d...
International audienceDissolved gases are particularly relevant tools for the investigation of envir...
In recent years, mass spectrometers with a membrane inlet separating gases from water for final anal...
A Membrane Inlet Mass Spectrometer (MIMS) is used to measure dissolved gas concentrations in environ...
Labeling groundwater by injecting an artificial tracer is a standard and widely used method to study...
International audienceIn natural waters, noble gas concentrations are governedby a diversity of rela...
International audienceIdentification of biogeochemical reactions inaquifers and determining kinetics...
International audienceOver the last century, the Critical Zone faced remarkable climate and land use...
International audienceWater quality in rivers results from biogeochemical processes in contributing ...