Soil 10084 is the only representative soil sample from Apollo 11 and arguab
ly one of the purest mare soils in the Apollo collection. It was wet sieved
in 1970 and dry sieved in 1971 with different results. Therefore, some dou
bt about its grain-size distribution persists. We consider allocation inhom
ogeneity, if any, to be a minor cause for the discrepancy. Rather, the diff
erence in methodology is likely to be the major cause for different results
. We report the results of a new analysis of an allocation of 0.99 g using
the contemporary method of wet sieving at Johnson Space Center; this method
uses water instead of freon. Our results show that the mean grain size and
sorting of the submillimeter fraction of soil 10084 are 4.28 phi (= 51 mum
) and 2.23 phi (= 213 mum), respectively. A significant proportion (14.2%)
of the soil is in the <10 <mu>m size range, which contrasts to previous det
erminations of 6.4% and 9.8%, respectively. The newly determined grain-size
distribution is skewed towards the finest grain sizes. This result is more
compatible with the high maturity of this soil than the results of previou
s determinations.