Physicochemical properties of respirable-size lunar dust

Abstract We separated the respirable dust and other size fractions from Apollo 14 bulk sample 14003,96 in a dry nitrogen environment. While our toxicology team performed in vivo and in vitro experiments with the respirable fraction, we studied the size distribution and shape, chemistry, mineralogy, spectroscopy, iron content and magnetic resonance of various size fractions. These represent the finest-grained lunar samples ever measured for either FMR np-Fe 0 index or precise bulk chemistry, and are the first instance we know of in which SEM/TEM samples have been obtained without using liquids. The concentration of single-domain, nanophase metallic iron (np-Fe 0 ) increases as particle size diminishes to 2 µm, confirming previous extrapolations. Size-distribution studies disclosed that the most frequent particle size was in the 0.1–0.2 µm range suggesting a relatively high surface area and therefore higher potential toxicity. Lunar dust particles are insoluble in isopropanol but slightly soluble in distilled water (~0.2 wt%/3 days). The interaction between water and lunar fines, which results in both agglomeration and partial dissolution, is observable on a macro scale over time periods of less than an hour. Most of the respirable grains were smooth amorphous glass. This suggests less toxicity than if the grains were irregular, porous, or jagged, and may account for the fact that lunar dust is less toxic than ground quartz.

[1]  D. Ming,et al.  Dissolution kinetics of a lunar glass simulant at 25 degrees C: the effect of pH and organic acids. , 1996, Geochimica et cosmochimica acta.

[2]  James Papike,et al.  LUNAR MINERALS , 2012 .

[3]  B O Stuart,et al.  Deposition and clearance of inhaled particles. , 1976, Environmental health perspectives.

[4]  Carle M. Pieters,et al.  Optical effects of space weathering: The role of the finest fraction , 1993 .

[5]  E. Cloutis,et al.  Laboratory spectroscopic detection of hydration in pristine lunar regolith , 2014 .

[6]  I. B. Goldberg,et al.  Ferromagnetic resonance as a method of studying the micrometeorite bombardment history of the lunar surface , 1975 .

[7]  Carle M. Pieters,et al.  An experimental approach to understanding the optical effects of space weathering , 2007 .

[8]  D. Mckay,et al.  Apollo 14 soils: Size distribution and particle types , 1972 .

[9]  Michael E. Lipschutz,et al.  Lunar sourcebook: A user's guide to the moon , 1992 .

[10]  C. A. Pearse Photometry and polarimetry of the moon and their relationship to physical properties of the lunar surface , 1963 .

[11]  Bonnie L. Cooper,et al.  Lunar dust and lunar simulant activation and monitoring , 2008 .

[12]  The relationship of the lunar regolith less than 10 micrometer fraction and agglutinates. I - A model for agglutinate formation and some indirect supportive evidence , 1982 .

[13]  G. Guthrie,et al.  Mineral properties and their contributions to particle toxicity. , 1997, Environmental health perspectives.

[14]  R. Morris Origin and evolution of the grain-size dependence of the concentration of fine-grained metal in lunar soils - The maturation of lunar soils to a steady-state stage , 1977 .

[15]  J. Papike,et al.  The lunar regolith - Comparative chemistry of the Apollo sites , 1980 .

[16]  W. D. Carrier,et al.  Lunar soil grain size distribution , 1973 .

[17]  S. Taylor,et al.  Composition of the lunar uplands: chemistry of Apollo 14 samples for Fra Mauro , 1972 .

[18]  D. Mckay,et al.  Size Distribution of Fe0 Globules in Lunar Agglutinitic Glass , 2002 .

[19]  Terence Allen,et al.  Powder sampling and particle size measurement , 1997 .

[20]  D. Ming Lunar sourcebook. A user's guide to the moon , 1992 .

[21]  Richard V. Morris,et al.  The optical properties of the finest fraction of lunar soil: Implications for space weathering , 2001 .

[22]  R. Christoffersen,et al.  The Smallest Lunar Grains: Analytical TEM Characterization of the Sub-micron Size Fraction of a Mare Soil , 2010 .

[23]  G. Oberdörster,et al.  Nanotoxicology: An Emerging Discipline Evolving from Studies of Ultrafine Particles , 2005, Environmental health perspectives.

[24]  J. James,et al.  Estimate of safe human exposure levels for lunar dust based on comparative benchmark dose modeling , 2013, Inhalation toxicology.

[25]  D. Mckay,et al.  Discovery of Vapor Deposits in the Lunar Regolith , 1993, Science.

[26]  Richard V. Morris,et al.  Mineralogical and chemical characterization of lunar highland soils: Insights into the space weathering of soils on airless bodies , 2010 .

[27]  New Measurements of the Particle Size Distribution of Apollo 11 Lunar Soil 10084 , 2009 .

[28]  Richard V. Morris,et al.  Space weathering on the Moon: Patina on Apollo 17 samples 75075 and 76015 , 1999 .

[29]  David S. McKay,et al.  Grain size and the evolution of lunar soils. , 1977 .

[30]  A. Basu,et al.  Submillimeter grain‐size distribution of Apollo 11 soil 10084 , 2000 .

[31]  M. Lindstrom,et al.  A synthesis of lunar highlands compositional data , 1980 .

[32]  D. Mckay,et al.  The nature and origin of rims on lunar soil grains , 1997 .

[33]  L. Taylor,et al.  Nanophase iron-enhanced chemical reactivity of ground lunar soil , 2010 .

[34]  An experimental evaluation of mineral-specific comminution , 1992 .

[35]  J. Gaier The Effects of Lunar Dust on Eva Systems During the Apollo Missions , 2013 .

[36]  S. McLennan,et al.  Production of hydrogen peroxide in Martian and lunar soils , 2007 .

[37]  Bruce Hapke,et al.  Effects of vapor-phase deposition processes on the optical, chemical, and magnetic properties OE the lunar regolith , 1975 .

[38]  Hiroyuki Kawamoto,et al.  Extracting Respirable Particles from Lunar Regolith for Toxicology Studies , 2010 .

[39]  David S. McKay,et al.  Origin of small lunar particles and breccia from the Apollo 11 site , 1970 .

[40]  Mihaly Horanyi,et al.  The lunar dust environment , 2011 .

[41]  J. Goldstein,et al.  Metallic particles in the Apollo 14 lunar soil. , 1972 .

[42]  H. Rose,et al.  Compositional data for twenty-one Fra Mauro lunar materials. , 1972 .

[43]  C. M. Pieters,et al.  Strength of mineral absorption features in the transmitted component of near-infrared reflected light - First results from RELAB. [spectrogoniometer for planetary and lunar surface composition experiments] , 1983 .

[44]  R. Finkelman,et al.  Lunar Soil: Size Distribution and Mineralogical Constituents , 1970, Science.

[45]  F. J. Miller,et al.  Particle inhalability curves for humans and small laboratory animals. , 1995, The Annals of occupational hygiene.

[46]  Yang Liu,et al.  Dry separation of respirable lunar dust: Providing samples for the lunar airborne dust toxicity advisory group , 2008 .

[47]  J. James,et al.  Toxicity of lunar dust assessed in inhalation-exposed rats , 2013, Inhalation toxicology.

[48]  R. V. Morris,et al.  The surface exposure /maturity/ of lunar soils - Some concepts and I sub s/FeO compilation , 1978 .

[49]  Carle M. Pieters,et al.  Remote Determination of Exposure Degree and Iron Concentration of Lunar Soils Using VIS-NIR Spectroscopic Methods , 1994 .

[50]  Yang Liu,et al.  Characterization of Lunar Dust for Toxicological Studies. I: Particle Size Distribution , 2008 .