The bottom environment of Osaka Bay was assessed by comparing organometal composition of sediments from inner part of the bay (along shore from Kobe City to Osaka City) with those in coasts along Awaji Island. The organometals designated in this study are those extracted by toluene-methanol mixed solvent. The result showed that human effects seem to be stronger in the inner bay than in the area along Awaji Island; the former shows higher concentrations of Mg, Cr, As, Ni, Se, Sn, Hg, Pb, Co, Cu and Zn. The main results obtained in this study are;
1. The concentration of organomagnesium is apparently higher by 2-3 orders of magnitude in comparison with other organometals, suggesting the large contribution of chlorophyll contained in phytoplankton. The higher concentration of organomagnesium in sediments from the inner bay suggests that human-supplied nutrients may cause higher production of phytoplankton. The positive correlation of organomagnesium with organoarsenic and organolead suggests the possibility that arsenic and lead are also concentrated by phytoplankton.
2. Sediments from the mouth of Shin-Yodo River are enriched in organic forms of Co, Cu, Hg, Ni, Zn, Sn, Se, and Pb and those from the mouth of Muko River are enriched in organic forms of Co, Cu, Zn, Sn, As, Se, and Pb. Those metals may orginate as pollutants from the river. However, all these organometals are not necessarily human-derived, because some may originate from other processes such as absorption of inorganic metals onto terrigenous highmolecular weight organic matter and from biological activity.
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