Correlation analyses on binding behavior of heavy metals with sediment matrices

Citation
Kc. Yu et al., Correlation analyses on binding behavior of heavy metals with sediment matrices, WATER RES, 35(10), 2001, pp. 2417-2428
Citations number
31
Categorie Soggetti
Environment/Ecology
Journal title
WATER RESEARCH
ISSN journal
00431354 → ACNP
Volume
35
Issue
10
Year of publication
2001
Pages
2417 - 2428
Database
ISI
SICI code
0043-1354(200107)35:10<2417:CAOBBO>2.0.ZU;2-4
Abstract
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.