The mineralogical, chemical and surface charge properties of Geric Ferralso
ls of New Caledonia were examined. These soils, which corresponded to two s
oil mantles formed either on ultramafic rocks or volcanic ejecta and ashes,
were respectively dominated by iron and aluminium oxides. The electric cha
rge characteristics were studied by measuring retention of Ca (2+) and Cl-
different pH values ranging from 3 to 7. The cation exchange capacity (CEC,
) increased with soil organic carbon and pH and varied from 0 to 35 cmol(c)
kg(-1) soil. The anion exchange capacity (AEC) reached 4.25 cmol(c) kg(-1)
soil in Bo horizons at pH 4. The magnitude of the CECT and AEC variations
was modelled according to CECT = 10(a1pH) * 10(B1) and AEC = - 10(a2pH) * 1
0(B2). Parameters a(1) and a(2) were low for samples with high organic carb
on (from 0.10 to 0.19 and from - 0.44 to - 0.66, respectively) and could in
crease to 1.25 and - 0.39, respectively, when organic carbon content decrea
sed. The parameters a(1) and a(2) could be also useful to regroup soil type
s according to the nature of the properties that can be manipulated for the
ir management. (C) 2001 Elsevier Science B.V. All rights reserved.