International audienceUnderstanding the slow densification process of polar firn into ice is essential in order to constrain the age difference between the ice matrix and entrapped gases. The progressive microstructure evolution of the firn column with depth leads to pore closure and gas entrapment. Air transport models in the firn usually include a closed porosity profile based on available data. Pycnometry or melting–refreezing techniques have been used to obtain the ratio of closed to total porosity and air content in closed pores, respectively. X-ray-computed tomography is complementary to these methods , as it enables one to obtain the full pore network in 3-D. This study takes advantage of this nondestructive technique to discuss the ...
International audienceInterpretation of greenhouse gas records in polar ice cores requires a good un...
The firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomo...
The air trapped in polar ice cores is not a direct record of past atmospheric composition but is str...
International audienceUnderstanding the slow densification process of polar firn into ice is essenti...
Very recently it has been observed, that in contradiction to former beliefs polar firn exhibits almo...
Air is enclosed during the firn-ice transition and stored in polar ice, forming a reliable archive f...
In order to interpret the paleoclimatic record stored in the air enclosed in polar ice cores, it is ...
Investigations into the physical characteristics of deep firn near the lock-in zone through pore clo...
International audienceIn the 1990s, closed and open porosity volumes of firn samples were measured b...
The transformation of snow and firn to ice is defined by the acquisition of "zero permeability" and ...
International audienceWe study a firn and ice core drilled at the new "Lock-In" site in East Antarct...
In order to interpret the paleoclimatic record stored in the air enclosed in polar ice cores, it is...
International audienceInterpretation of greenhouse gas records in polar ice cores requires a good un...
The firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomo...
The air trapped in polar ice cores is not a direct record of past atmospheric composition but is str...
International audienceUnderstanding the slow densification process of polar firn into ice is essenti...
Very recently it has been observed, that in contradiction to former beliefs polar firn exhibits almo...
Air is enclosed during the firn-ice transition and stored in polar ice, forming a reliable archive f...
In order to interpret the paleoclimatic record stored in the air enclosed in polar ice cores, it is ...
Investigations into the physical characteristics of deep firn near the lock-in zone through pore clo...
International audienceIn the 1990s, closed and open porosity volumes of firn samples were measured b...
The transformation of snow and firn to ice is defined by the acquisition of "zero permeability" and ...
International audienceWe study a firn and ice core drilled at the new "Lock-In" site in East Antarct...
In order to interpret the paleoclimatic record stored in the air enclosed in polar ice cores, it is...
International audienceInterpretation of greenhouse gas records in polar ice cores requires a good un...
The firnificaton of dry polar firn has been investigated with the means of X-ray micro-computer tomo...
The air trapped in polar ice cores is not a direct record of past atmospheric composition but is str...