The flotation of quartz and magnetite was studied as a function of pH
when using N-alkyl-1, 3 diaminopropanes as collectors in the presence
of Ca(II). The alkyl chains of the diamines were 8, 12 and 16 carbons
in length. Two collector concentrations were used and flotation studie
d in the absence of additives and in the presence of CaCl2. All the am
ines are relatively stronger collectors for quartz than for magnetite
in both the absence and presence of CaCl2. The CaCl2, in the concentra
tion studied, 0.1 mol/dm3, functions as a depressant for the minerals.
Probable surface chemical phenomena giving rise to the observed exper
imental results are discussed.