Thermogravimetric analysis (TGA)

we compare profiles via simultaneous differential scanning calorimetry (DSC), thermogravimetric analysis (TGA), and evolved gas analysis (EGA) across a range of designated mare simulants, freshly

The outer portion of the reticulite is slightly more volatile-enriched. The CO2 signal is higher throughout, with a main degassing plateau between 375 C (coinciding with stronger oxidation) and 875 C

To approach this knowledge gap, a direct comparison of the reduction of pure ilmenite and the highland type lunar regolith simulant NU-LHT-2M was performed by means of thermogravimetric analysis (TGA)

Thermogravimetric analysis (TGA) was conducted in the temperature range of 30 1000 C with a heating rate of 10 C/min under an argon atmosphere.

Microstructural evolution and porosity characteristics were examined using thermogravimetric analysis (TGA), X-ray diffraction (XRD), nitrogen adsorption desorption (NAD), and scanning electron

Viscosity and glass formation behavior of lunar regolith simulants

The results of the thermogravimetric analyses (TGA) of EAC-1A and the fraction P < 100 m in the temperature range 40 1000 C, including the derivative thermogravimetry (DTG) curves, are shown in Fig. 3

Fig. 5 TGA curve for the JSC-1A lunar simulant.