The spectral properties from 0.4 to 3μm of montmorillonite plus dark carbon grains (called opaques) of various sizes are studied as a function of the weight fraction of opaques present. The reflectance level and band depths of the 1.4-, 1.9-, 2.2-, and 2.8-μm water and/or OH absorption features are analyzed using derived empirical relationships and scattering theory. It is found that the absorption band depths and reflectance level are a very nonlinear function of the weight fraction of opaques present but can be predicted in many cases by simple scattering theory. The 2.8-μm bound water fundamental band is the most difficult absorption feature of suppress. The overtone absorptions are suppressed a greater amount than the fundamental but are still apparent even when 10-20 wt % opaques are present. Thus the band depth ratio of one overtone by the fundamental or other lower overtone varies as a function of the weight fraction of opaques present. The relationships observed and the simple scattering theory presented show that quantitative compositional remote sensing studies are feasible for surfaces containing complex mineral mixtures. The question of the uniqueness of quantitative remote sensing is discussed.