Vertical distributions of heavy metals of core sample sediments under 150 cm in abandoned mine tailings were examined. Core samples were analyzed by XRD and further examined by ICP-AES measurements after sequential extraction with 1 mol dm
-3 HC1, 10% HF, and conc. HNO
3. The XRD results showed that a-quartz was a main component in the core samples. Further, based on the sequential extraction results, the distributions of trace amounts of minerals, such as chlorite, sericite, rhodochrosite, pyrite and galena in core samples which were undistinguishable by XRD analysis, were estimated. Chlorite and rhodochrosite were relatively reactive and dissolved in HCl-extraction, a-quartz and sericite were dissolved in HF-extraction, and sulfides were dissolved in HNO
3-extraction. Under 40 cm-zone was relatively rich in clay minerals and carbonate where sulfate-reducing bacteria were active. Under 120 cm-zone contained pyrite-rich sediments. At present the function of sulfate-reducing bacteria is not so large to affect to the mineralogy in the sediment.
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