The microped size distribution of erodible soils is one of the main fa
ctors controlling the emissions of mineral aerosol. To date, the micro
ped size distributions of desert soils in natural field conditions are
not well known and thus the existing dust source models cannot be app
lied to natural sites. Based on dry sieving and elemental analysis of
26 soil samples collected in arid and semiarid regions, it is shown th
at the microped size distributions of these desert soil samples involv
e a combination of four major mass size populations. These four size p
opulations correspond to salty soils, fine quartz sand, coarse dune sa
nd and aluminosilicate silt. We show that the microped size distributi
ons of the various desert soils, according to their mineralogical char
acteristics, can be calculated by a mixture involving two or three of
these four populations. The main held of application for this scheme i
s the characterization of the erodible soil size distributions for mod
elling the atmospheric dust cycle.