density measurement

The green relative densities, 0, of freeze-cast specimens vary from 38% to 43% (Fig. 3 (b)), depending on the slurry's water content.

NS5 specimens reach 58% to 70% density, depending on solution concentration. Additional cycles further raise *, and reach 67% to 82% after three cycles.

The density of the samples was measured using Archimedes principle.

Table 3 Minimum, bulk uncompressed, and maximum densities of LHS-1 and LMS-1 with 95% confidence intervals and ranges of each measure of density of lunar highlands and mare regolith.

The density of lunar soil and its change with depth is one of the most important and defining characteristics. The density average value of the lunar soil according to various measurements on the

The density of BP-1 once loaded was consistently 1.65 g cm 3 and independent of the total depth. Two levels of compression resulted in 1.82 and 1.90 g cm 3.

Specific properties that were tested included compression strength, hardness, density, magnetic properties, and the capability to drill and tap melted regolith.