Against the background of the great similarity of the general properti
es and mineralogical composition of Serozems and Gray-Cinnamon Brown s
oils of Kashmir, soils which are favorable for growing saffron are dis
tinguished by the least weathered material with high totals and simila
r reserves of potassium and magnesium. Such soils are identified by a
linear discriminant function which includes four properties of only th
e upper horizons (0-20 cm): pH, dithionite-soluble iron, sodium, and p
otassium in Maslova extract.