1985
DOI: 10.1080/09593338509384336
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Iron‐oxo‐hydroxides and their significance to the behaviour of heavy metals in estuaries

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Cited by 28 publications
(11 citation statements)
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“…The geochemical properties include, in the order of decreasing importance, Cs, Fe, Co, Rb and a small contribution for Sc, Ta and Li. Metals of this factor are related to the composition of fine-grained and clay-mineral-rich sediments because of the high correlation with kaolinite, chlorite and illite, similar to that with total Si, A1 and Fe, in accordance with the findings of Schoer (1985). The high correlation between Co-Hg (r --0.760), Co-W (r --0.838) and Co-Zn (r --0.730) is reflected in its contribution to factors 2 and 6 ( Table 3).…”
Section: Resultssupporting
confidence: 69%
“…The geochemical properties include, in the order of decreasing importance, Cs, Fe, Co, Rb and a small contribution for Sc, Ta and Li. Metals of this factor are related to the composition of fine-grained and clay-mineral-rich sediments because of the high correlation with kaolinite, chlorite and illite, similar to that with total Si, A1 and Fe, in accordance with the findings of Schoer (1985). The high correlation between Co-Hg (r --0.760), Co-W (r --0.838) and Co-Zn (r --0.730) is reflected in its contribution to factors 2 and 6 ( Table 3).…”
Section: Resultssupporting
confidence: 69%
“…Principal component Analysis (PCA) is used to understand the correlation structure of collected data and identify the most important factors contributing to the data structure (Schoer, 1985  2011, ALÖKI Kft., Budapest, Hungary used for statistical analyses, which were performed using SPSS 11.0 software. Eight environmental variables were reduced into three variable factors (PC1, PC2 and PC3) using the principal component analysis.…”
Section: Statistical Analysesmentioning
confidence: 99%
“…Ka or partition coefficient of the compound between sediment and water, K~ or the Kd corrected for the organic carbon content) (Schwarzenbach et al, 1993). For metals, the main processes are the co-precipitation and the co-reaction with oxides and hydroxides of manganese and iron, humic acids, sulfides and clays (Foerstner and Wittmann, 1981;Schoer, 1985;Belzile et al, 1989).…”
Section: Introductionmentioning
confidence: 99%