Sol88
Philosopher
- Joined
- Mar 23, 2009
- Messages
- 8,437
Are you implying all those PEER REVIEWED MAINSTREAM PAPERS are wrong? Or just misusing words ‘cos it’s easier to say rock than we’ll consolidated refractory material?
Looks like it to this LIAR!
And a cherry pick
Ouch!
4Mpa lower limit for 67P?
Looks like it to this LIAR!
The Deep Impact experiment on comet Tempel-1 yielded initially an extremely low (“effective”) strength (<65 Pa) (7), raising questions as to whether a comet lander could land on such weak material. Experimental work on the aerodynamic (i.e., tensile?) strength of meteoroids (5), as well as particles collected by Stardust in the coma of comet 81P/Wild 2 (6), also indicated a strength range of 3 to 80 kPa on the submillimeter-to-centimeter scale. The landings of Philae, despite not proceeding as planned, provide direct observations of the surface mechanical properties and thus a baseline for comparison with these previous studies.
And a cherry pick
The two sites Agilkia and Abydos are situated in two different morphological regions: very likely in Ma’at and Bastet. Whereas the Ma’at region appears to be covered by a smooth “dust” layer (15, 23) with a brittle underlayer, Bastet is described as an exposed consolidated surface with minimal bouldering, possibly part of the basal unit. The size distribution of the regolith at Ma’at is now constrained by ROLIS data as still granular at 0.9 cm/pixel and is interpreted as “airfall” (15). Both morphological descriptions are consistent with our observations.
Ouch!
4Mpa lower limit for 67P?
Last edited:
.