J. Sutherland, K.-U. Hess, T. Bissbort, S. Stapperfend, A. Müller, T. C. Hansen, A. Rack, D. B. Dingwell | 2025 | Chemical Geology
DOI 10.1016/j.chemgeo.2025.123115Review state
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This paper evaluates volatile loss during heating of lunar mare simulants and related compositions using DSC, TGA, and EGA. JSC-1A simulant shows overlap with fresh volcanic material. Etna ash is noted as a close match for water loss differences. Neutron powder diffraction indicates prolonged volatile fluxing effects beyond major degassing. This study investigates the thermal properties of lunar regolith simulants using a combination of experimental techniques and data analysis. The research focuses on understanding the behavior of these simulants under various thermal conditions, which is crucial for applications in space exploration and planetary science. The study highlights the importance of accurate thermal modeling and the role of different mineralogical components in influencing thermal properties. The findings contribute to the broader understanding of lunar regolith and its potential use in future space missions. The provided text appears to be a mix of metadata and possibly partial content from a scientific or technical paper, likely related to mineralogy or geochemistry. It includes references to figures, image types (thumbnail, downscaled, high-resolution), and URLs poi
These are the records this paper contributes to the simulant, returned sample, method, and property browsers.
Chang'e-5 | measured
Apollo | measured
Apollo 12 sample 12070 | Apollo 12 | Apollo 12 | measured
TGA-DSC
Thermogravimetric Analysis - Differential Scanning Calorimetry
EGA
Evolved Gas Analysis
NPD
Neutron Powder Diffraction
Differential scanning calorimetry (DSC)
thermal analysis
Thermogravimetric analysis (TGA)
thermal analysis
Evolved gas analysis (EGA)
thermal analysis
Neutron powder diffraction (NPD)
structural analysis
Thermogravimetric and heat flow data collection
thermogravimetric analysis
thermal
thermal stability
thermal
thermal decomposition
thermal
thermal expansion
melting onset
determined by DSC and NPD
decomposition reactions
attributed to thermal analysis
solidus temperature
apparent due to heating rate
liquidus temperature
apparent due to heating rate
thermal equilibrium
not fully achieved at 15 C/min