REGOLITH BUFFER SYSTEMS
1.NEED STATEMENT
1.1LUNAR SOIL ANALYSIS
1.2PARTICLE COMPOSITION
1.3TECHNOLOGIES AVAILABLE
1.4COMPARATIVE STUDY 2.1LUNAR SOIL PROFILE
2.2CAUSING FACTORS
2.3PHYSICAL AND CHEMICAL PROPERTIES OF REGOLITH 3.1PRESENT TECHNOLOGY IS SUFFICIENT?
LAYER | RANGE | NAME |
FIRST LAYER | 0- ~10 m | REGOLITH |
SECOND LAYER | ~10 m – 2 km | LARGE SCALE EJECTA |
THIRD LAYER | ~2 km – 10 km | STRUCTURALLY DISTURBED CRUST |
FOURTH LAYER | ~10 km – 25 km | FRACTURED CRUST |
FIFTH LAYER | ~25 km - >œ ~(km) | INTACT LUNAR CRUST |
SOLUTION #1
•RADIATION
VS RADIATION •But it’s not possible to create another solar wind! Or Galactic Wind at the required time.
SOLUTION #2
•COMPLEX GEOMETRY VS COMPLEX GEOMETRY
•The Complex structure of nature has high entropy thus they are thermodynamic ally non settle substances
•Cost effectiveness will reduce but it’s a working solution
SOLUTION #3
•SILICON IS BEHAVING LIKE GRAPHITE LAYERS
TESTING OF THE PROTOTYPE
•The structural behavior due to dielectric provided the pyroxene and olivine to channel through the valley gaps of the structures.
REFERENCE
•SAMPLE INDEX* •12001 291, 292, 300, 320, 344, 346, 347, 349, 404, 414, 478, 497, 502, 504, 505, 570, 575, 577, 579 12002 172, 175, 191, 193, 203, 204, 207, 208, 261, 262, 482, 502, 532, 549, 550, 581 12003 320,344 12004 179, 180, 199 12005 199, 616 12008 616 12009 166, 175, 194, 199, 204, 208 12011 616 12012 616 12013 132, 134, 135, 169, 181, 232, 368, 381, 610, 616 12015 616 •14003 346, 478, 571, 581 14047 230,231,276 14053 147, 151, 159, 163, 172, 175, 195, 261, 263, 619 14055 619 14063 234, 242, 244, 277, 619 14064 244, 278, 619 14066 243, 250, 280, 281 14068 243, 252, 280, 281 14072 147, 151, 175, 207 14073 150, 175
•Abbas, M.M., D. Tankosic, P.D. Craven, J.F. Spann, A. LeClair, E.A. West, 2007. Lunar dust charging by photoelectric emissions. Planetary and Space Science, vol. 55, issues 7-8, p. 953- 965.
•Agrell, S. O., Scoon, J. H., Muir, I. D., Long, J. V., McConnell, J. D., Peckett, A., 1970. Mineralogy and petrology of some lunar samples, science 30, vol. 167. no. 3918, p. 583-586.
•Fubini, B., Hubbard, A., 2003. Reactive oxygen species (ros) and reactive nitrogen species (rns) generation by silica in inflammation and fibrosis. Free Radical Biology & Medicine, vol. 34, no. 12, p. 1507–1516.
Grossman, J. J., Ryan, J. A., Mukherjee, N. R., and Wegner, M. W., 1970. Surface properties of lunar samples, Science 30, vol. 167. no. 3918, p. 743-745
•Hapke B. W., Cohen, A. J., Cassidy, W. A., and Wells, E. N., 1970. Solar Radiation Effects in Lunar Samples. Science 30, Vol. 167. no. 3918, pp. 745 – 747. •Shoemaker, D.A., Pretty, J.R., Ramsey, D.M., McLaurin, J.L., Khan, A., Teass, A.W., Castranova, V., Pailes, W.H., Dalal, N.S., Miles, P.R., et al., 1995. Particle activity and in vivo pulmonary response to freshly milled and aged alpha-quartz. Scand J Work Environ Health, 21 Suppl 2:15-8. Press, New York.
•Wentworth, S.J., Keller, L.P, McKay, D.S., Morris, R.V., 1999. Space weathering on the moon: patina on Apollo 17 samples 75075 and 76015, Meteor Planet Sci, 34,593-603.
VOTE OF THANKS
•NASA GLEN RESEARCH CENTRE •NASA AMES RESEARCH CENTRE
•JAXA PROPULSION LAB
•ISRO - CHANDRAYAAN 1, CHANDRAYAAN 2