Te. Madey et al., DESORPTION OF ALKALI ATOMS AND IONS FROM OXIDE SURFACES - RELEVANCE TO ORIGINS OF NA AND K IN ATMOSPHERES OF MERCURY AND THE MOON, J GEO R-PLA, 103(E3), 1998, pp. 5873-5887
This paper begins with a brief survey of the literature dealing with t
he adsorption and desorption of alkalis on oxide surfaces. Emphasis is
on desorption phenomena: thermal desorption, electron- and photon-sti
mulated desorption, and ion-induced desorption (sputtering). Then the
relevance of these data to the desorption of alkalis from mineral surf
aces and to the origins of alkali vapors in tenuous planetary atmosphe
res is discussed. The data presented for Na and K indicate that desorp
tion processes initiated by thermal or electronic excitations do not d
epend strongly on whether the Na returns to the surface or diffuses up
through the regolith, and that neutral yields dominate ion yields in
all cases. Although the desorbed neutral energy distributions are not
well approximated by Maxwell-Boltzmann distributions, the mean energie
s of the desorbed neutral Na and K are seen to be consistent with the
temperatures extracted for the ''hot'' component of the lunar atmosphe
re. This suggests that the ''hot'' component may be produced by electr
onically stimulated desorption (e.g., electron-stimulated desorption a
nd/or photon-stimulated desorption). If this is the case, a possible '
'size effect'' may be operative, in which desorbed neutral K atoms are
somewhat more energetic than desorbed Na. In such desorption processe
s a low-energy component may be generated by scattering of desorbing a
toms in the porous regolith; thermal desorption can also generate low-
energy atoms. The data further indicate that thermal desorption should
be rapid in the equatorial regions of Mercury, possibly depleting thi
s region of alkalis, whereas thermal desorption should be less efficie
nt on the Moan. Surface charging may be important at the surface of th
e Moon, by accelerating the solar electrons to energies above the thre
shold for initiating alkali desorption. Suggestions are made for futur
e laboratory work.