Until the landing of the Surveyor 1 spacecraft on the moon, it had been inferred from earth-based optical, thermal, radio, and radar observations that the surface f the moon consisted of material of low-bulk density (less than 1 g/cm^3) and high porosity. Recently, a change in this belief, at least with respect to the optical data, has occurred, although a low density continues to be postulated on the basis of radiometric data
International audienceNewly obtained gravity and topography data of the Moon, combined with a lithos...
From a soil mechanics point of view, the Moon is a relatively simple place. Without any water, organ...
The physical state of the lunar soil in the permanently shadowed craters of the moon is inferred fro...
Until the landing of the Surveyor 1 spacecraft on the moon, it had been inferred from earth-based op...
Mechanical, optical, thermal, and electrical properties of Surveyor I landing sit
The fine lunar surface material at the Surveyor 3 landing site has about 3 × 10^3-dyne/cm^2 cohesion...
The physical properties of the lunar regolith were originally inferred from remotely sensed data, fi...
This paper contains a review of the information that has been obtained about the mechanical properti...
The Apollo 14 lunar landing provided a greater amount of information on the mechanical properties of...
The landing dynamics of and soil penetration by Surveyor I indicated that the lunar soil has a poros...
Engineering telemetry data and lunar surface photographs by Surveyor 1 have been evaluated for infor...
During the sojourn of the second manned spacecraft on the moon in November 1969, the astronauts C. C...
The surface material at the Surveyor 5 site is granular and slightly cohesive. Spacecraft footpads p...
Accurate lunar rock densities are necessary for constructing gravity models of the Moon\u27s crust a...
The density of the Martian soil is evaluated at a depth up to one meter using the results of radar m...
International audienceNewly obtained gravity and topography data of the Moon, combined with a lithos...
From a soil mechanics point of view, the Moon is a relatively simple place. Without any water, organ...
The physical state of the lunar soil in the permanently shadowed craters of the moon is inferred fro...
Until the landing of the Surveyor 1 spacecraft on the moon, it had been inferred from earth-based op...
Mechanical, optical, thermal, and electrical properties of Surveyor I landing sit
The fine lunar surface material at the Surveyor 3 landing site has about 3 × 10^3-dyne/cm^2 cohesion...
The physical properties of the lunar regolith were originally inferred from remotely sensed data, fi...
This paper contains a review of the information that has been obtained about the mechanical properti...
The Apollo 14 lunar landing provided a greater amount of information on the mechanical properties of...
The landing dynamics of and soil penetration by Surveyor I indicated that the lunar soil has a poros...
Engineering telemetry data and lunar surface photographs by Surveyor 1 have been evaluated for infor...
During the sojourn of the second manned spacecraft on the moon in November 1969, the astronauts C. C...
The surface material at the Surveyor 5 site is granular and slightly cohesive. Spacecraft footpads p...
Accurate lunar rock densities are necessary for constructing gravity models of the Moon\u27s crust a...
The density of the Martian soil is evaluated at a depth up to one meter using the results of radar m...
International audienceNewly obtained gravity and topography data of the Moon, combined with a lithos...
From a soil mechanics point of view, the Moon is a relatively simple place. Without any water, organ...
The physical state of the lunar soil in the permanently shadowed craters of the moon is inferred fro...