This article presents the amounts of heavy metals bound to the sediment mat
rices (carbonates, Fe-oxides, Mn-oxides, and organic matter), the correlati
ons between any two heavy-metal binding fractions, and the correlations bet
ween sediment matrices and their heavy-metal binding fractions. Data consis
ted of 313 sets obtained from five main rivers (located in southern Taiwan)
were analyzed by statistical methods. Among six heavy metals analyzed (Zn,
Cu, Pb, Ni, Cr, and Co), the statistical results show that Zn is primarily
bound to organic matter, and Cr is primarily bound to Fe-oxides. Principal
component analysis (PCA) and correlation analysis (CA) result in significa
nt correlations between carbonates bound Ni and carbonates bound Cr, Fe-oxi
des bound Ni and Fe-oxides bound Cr, and Mn-oxides bound Cu and Mn-oxides b
ound Cr. From linear regression results, the levels of the six heavy metals
bound to either organic matter or Fe-oxides is moderately dependent on the
contents of organic matter or Fe-oxides, especially true for Cr and Pb. Ac
cording to slope values of linear regression, Cu and Cr have the highest sp
ecific binding amounts (SBA) to organic matter and Fe-oxides, respectively.
A significant correlation between organic matter and organically bound hea
vy metals implied that organic matter contained in the sediments of the Pot
zu river and the Yenshui river can be adequately used as a normalizing agen
t. However, the six heavy metals bound to either carbonates or Mn-oxides do
not correlate with carbonates or Mn-oxides. The obtained results also impl
y that competitions of various sediment phases in association with heavy me
tals occur, and organic matter and Fe-oxides are more accessible to heavy m
etals than other sediment phases. (C) 2001 Elsevier Science Ltd. All rights
reserved.