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Principal scientific results of the Surveyor 3 Mission

Jaffe, L. D. and Batterson, S. A. and Brown, W. E., Jr. and Christensen, E. M. and Gault, D. E. and Lucas, J. W. and Norton, R. H. and Scott, R. F. and Shoemaker, E. M. and Sutton, G. H. and Turkevich, A. L. (1968) Principal scientific results of the Surveyor 3 Mission. Journal of Geophysical Research, 73 (12). pp. 3983-3987. ISSN 0148-0227. https://resolver.caltech.edu/CaltechAUTHORS:20141107-140544174

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Abstract

The fine lunar surface material at the Surveyor 3 landing site has about 3 × 10^3-dyne/cm^2 cohesion, 35° angle of internal friction, 3 × 10^5-dyne/cm^2 static bearing capacity. A small rock withstood a local pressure of 2 × 10^7 dynes/cm^2. Soil strength and density increase significantly at depths of a few centimeters. Exposed surface has a considerably higher albedo than the material just below it. The photometric function changed when the surface was slightly compressed. Fine surface material appears to be gradually moving downslope.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/JB073i012p03983DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/JB073i012p03983/abstractPublisherArticle
Additional Information:Copyright 1968 by the American Geophysical Union. (Received January 23, 1968.)
Issue or Number:12
Record Number:CaltechAUTHORS:20141107-140544174
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20141107-140544174
Official Citation:Jaffe, L. D., et al. (1968), Principal scientific results of the Surveyor 3 Mission, J. Geophys. Res., 73(12), 3983–3987, doi:10.1029/JB073i012p03983.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:51452
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:07 Nov 2014 22:15
Last Modified:03 Oct 2019 07:33

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