The behaviour of Co, Fe, Mn, and Ni was investigated in the mixing are
a of the Po fiver in six surveys over the period March 1992 to June 19
95 during low-to-medium solid load and flow conditions. The concentrat
ions (nM) of dissolved elements for the riverine and marine end-member
s respectively were in the ranges 0.09 to 0.93 and 0.24 to 0.98 for Co
, 10 to 53 and 5 to 20 for Ni, 12 to 87 and 5 to 33 for Fe, and 10 to
155 and 26 to 105 for Mn. Co and Mn behave non-conservatively in the P
o estuary: an addition to the dissolved phase occurred for these eleme
nts that was more marked in the summer period. The concentrations of d
issolved and particulate Ni decreased almost linearly with increase in
salinity, with more marked variations in dissolved Ni concentration i
n winter than summer. The concentrations of dissolved and particulate
Fe also varied conservatively with salinity. This unusual behaviour fo
r disserved Fe is attributed to the analytical procedure which exclude
d kinetically inert colloidal species.