%T Continued investigation of LDEF's Structural Frame and Thermal Blankets by the Meteoroid & Debris Special Investigation Group %A Thomas H. See %A Kimberly S. Mack %A Jack L. Warren %A Michael E. Zolensky %A Herbert A. Zook %B 69 Months in Space - Second LDEF Post-Retrieval Symposium %R NASA CP-3194, Part 2 %D April, 1993 %P 313-324 %E Arlene S. Levine %I Langley Research Center Hampton, VA 23681-0001 %U http://setas-www.larc.nasa.gov/setas/PUBS/LDEF/cp3194-93-p313.ps.Z %X Since the return of the Long Duration Exposure Facility (LDEF) in January, 1990, the Meteoroid and Debris Special Investigation Group (M&D SIG) has been examining LDEF hardware (i.e., experiment trays and structural components) in an effort to define the low-Earth orbit (LEO) particulate environment as witnessed by the spacecraft during its 5.7 year stay in orbit. Last year we reported (ref. 1) on the frequency of larger features as determined from data acquired by the M&D SIG's Analysis Team (A-Team) during LDEF deintegration. At that time the A-Team examined every square millimeter of the spacecraft locating and documenting the presence of all impact craters >=500 micrometers in diameter and all penetration holes >=300 micrometers in diameter (ref. 2). Over the past year M&D SIG members and Lockheed Engineering & Sciences Co. personnel at the Johnson Space Center (JSC) in Houston, Texas have been examining selected LDEF structural frame components (i.e., intercostals) in much greater detail in order to augment this large-particle data with that from smaller particles.

In all, LDEF exposed ~130 m2 of surface area to the LEO particulate environment, ~15.4 m2 of which was occupied by structural frame components of the spacecraft. This report focuses on the data acquired by detailed examination of LDEF intercostals, 68 of which are now in possession of the M&D SIG at JSC (Figure 1). In addition, limited data will be presented for several small sections from A0178 thermal control blankets that were examined/counted prior to being shipped to Principal Investigators (PI's) for scientific study. As was the case in Ref. 1, the data presented here are limited to measurements of crater and penetration-hole diameters and their frequency of occurrence which permits, yet also constrains, more model-dependent, interpretative efforts. Such efforts will focus on the conversion of crater and penetration-hole sizes to projectile diameters (and masses), on absolute particle fluxes, and on the distribution of particle-encounter velocities. These are all complex issues (refs. 3, 4, 5, 6, 7, 8) that presently cannot be pursued without making various assumptions which relate, in part, to crater-scaling relationships, and to assumed trajectories of natural and man-made particle populations in LEO that control the initial impact conditions.