Em. Fischer et Cm. Pieters, REMOTE DETERMINATION OF EXPOSURE DEGREE AND IRON CONCENTRATION OF LUNAR SOILS USING VIS-NIR SPECTROSCOPIC METHODS, Icarus, 111(2), 1994, pp. 475-488
On the Moon, space weathering processes such as micrometeorite bombard
ment alter the optical properties of lunar soils. As a consequence, lu
nar soil optical properties are a function not only of composition, bu
t of degree of exposure on the lunar surface as well. In order to accu
rately assess the compositional properties of the lunar surface using
remotely acquired visible and near-infrared spectroscopic data, it is
thus necessary either (1) to compare optical properties only of soils
characterized by similar degrees of exposure or (2) to otherwise norma
lize or remove the optical effects due to exposure. Laboratory spectro
scopic data for lunar soils are used to develop and test remote spectr
oscopic methods for determining degree of exposure and for distinguish
ing between the optical effects due to exposure and those due to compo
sition. A method employing a ratio between reflectances within and out
side of the 1 mu m Fe2+ crystal field absorption band was developed fo
r remotely identifying highland soils that have reached a steady-state
maturity. The relative optical properties of these soils are a functi
on solely of composition and as such can be directly compared. Spectro
scopic techniques for accurate quantitative determination of iron cont
ent for lunar highland soils are investigated as well. It is shown tha
t approximations of the 1 mu m Fe2+ absorption band depth using few to
several channel. multispectral data or spectroscopic data of inadequa
te spectral range cannot be used with confidence for compositional ana
lysis. However, band depth measurements derived from continuum-removed
high spectral resolution data can be used to calculate the weight per
cent FeO and relative proportion of iron-bearing silicates in mature l
unar highland and mare/highland mixture soils. A preliminary effort to
calibrate telescopic band depth to laboratory soil measurements is de
scribed. (C) 1994 Academic Press, Inc.