IEG 환경지질연구정보센터
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전체 글
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(4) . . . . Heavy Metal Retention by Secondary Minerals in Mine Waste Rocks at the Abandoned Seobo Mine Min-Ju Kang1, Pyeong-Koo Lee1*, Sang-Hoon Choi2 and Seong-Cheon Shin1 1. Geological and Environmental Hazards Department, KIGAM, Dept. of Earth and Environmental Sciences, Chungbuk National Univ.. 2. The main purposes of this study are to utilize mineralogical studies such as optical microscope, XRD and SEM/ EDS analyses to characterize the oxidation of sulfide minerals and the mechanisms controlling the movement of dissolved metals from waste rocks at the abandoned Seobo mine. Mineralogical research of the waste rocks confirms the presence of anglesite, covellite, goethite, native sulfur and nsutite as secondary minerals, suggesting that these phases control the dissolved concentrations of As, Cu, Fe, Mn, Pb and Zn. The dissolved metals are precipitated, adsorbed and/or coprecipitated with(or within) Fe(Mn)-hydroxides and Mn(Fe)-hydroxides. The main phases of secondary mineral, Fe-hydroxide, can be classified as amorphous or poorly crystalline and more crystallized phases(e.g. goethite) by crystallinity. Amorphous or poorly crystalline Fe-hydroxide has relatively high As contents(9-24 wt%). This poorly crystalline Fe-hydroxide changes toward more crystallized phase(e.g. goethite) which contains relatively low As(0.6-7.7 wt%). These results are mainly due to the progressive release of As with the crystallization evolution of the As-trapping poorly crystalline Fe-hydroxides. It is also attributed to the differences of specific surface areas between the poorly crystalline Fe-hydroxides and well crystallized phases. The dissolved metals from waste rocks at Seobo mine area are naturally attenuated by a series of precipitation(as Fe, Mn, Cu, Pb), coprecipitation(Fe, Mn) and adsorption(As, Cu, Pb, An) reactions. The results of mineralogical researches permit to assess the environmental impacts of mine waste rocks in the areas, and can be used as a useful data to lay available mine restoration plan.. Sulfide mineral, oxidation, secondary mineral, heavy metal retention, SEM/EDS.
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(102) EDS data(wt.%) of secondary minerals around arsenopyrite. Sample No.. O. S. Fe. Cu. As. As/Fe. SB10-1-7 SB10-1-8 SB10-1-9 SB10-1-3 SB10-1-10 SB10-1-11 SB10-1-12 SB10-1-13 SB10-1-14 SB10-1-15 SB10-1-16 min max mean. 22.49 21.52 22.16 21.33 21.90 20.47 21.62 21.59 19.63 20.98 20.45 19.63 22.49 21.29. 2.06 4.06 2.06 4.06 3.06. 50.11 50.85 48.36 51.36 52.64 52.44 50.91 53.92 45.24 53.35 52.05 45.24 53.92 51.02. 4.17 3.64 5.48 3.43 1.93 3.64 3.45 9.65 2.90 3.44 1.93 9.65 4.17. 23.23 23.98 21.94 23.87 23.53 23.45 24.02 24.48 21.43 22.78 24.06 21.43 24.48 23.34. 0.46 0.47 0.45 0.46 0.45 0.45 0.47 0.45 0.47 0.43 0.46 0.43 0.47 0.46.
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(105) EDS data(wt.%) of Fe(Mn)-hydroxide and Mn(Fe)-hydroxide. Sample No.. O. Fe. As. Zn. Mn. Pb. Ca. Cu. K. As/Fe. Zn/Mn. SB2-2 SB2-3 SB2-5 SB2-8 SB2-10 SB2-12 SB2-14 SB2-16 SB2-17 SB2-18 SB2-19 min max mean. 15.08 15.12 12.64 14.59 13.42 13.62 14.27 13.99 13.35 13.38 13.52 12.64 15.74 14.06. 59.22 11.40 0.00 9.97 16.39 0.00 0.00 0.00 0.00 22.69 0.00 0.00 59.22 10.88. 6.66 0.00 0.74 0.00 0.85 0.00 0.00 0.00 0.00 0.87 0.00 0.00 6.66 0.83. 0.00 2.66 3.51 2.05 2.00 3.30 1.29 0.62 2.10 1.63 0.80 0.00 3.51 1.81. 17.78 70.15 76.81 71.85 64.14 80.47 82.67 84.46 83.25 58.29 85.18 17.78 85.18 70.46. 0.00 0.00 5.50 0.00 2.30 0.00 0.00 0.00 0.00 2.36 0.00 0.00 5.50 0.92. 1.26 0.68 0.79 1.29 0.89 0.96 0.38 0.30 0.62 0.63 0.27 0.27 1.29 0.73. 0.00 0.00 0.00 0.00 0.00 0.78 0.00 0.00 0.00 0.00 0.00 0.78 0.78 0.07. 0.00 0.00 0.00 0.26 0.00 0.87 0.47 0.62 0.19 0.15 0.22 0.00 0.87 0.25. 0.112 0.000 0.000 0.000 0.052 0.000 0.000 0.000 0.000 0.038 0.000 0.000 0.112 0.018. 0.000 0.038 0.046 0.029 0.031 0.041 0.016 0.007 0.025 0.028 0.009 0.000 0.046 0.025. # ^" ÓÔC# c 7³þ; !.7 ¥ Ù(w #,-I Ý" 0" ÓÔ C # ´](w c 7P O4 0 ¹$ \]/ # mÄ [ " 8 êê C# òóé; ô K ;³4 9b8 \]/ C#$%) ?F ù7³V¥ ? >" > ¹#F :" DV ! ./4 ; C# ©J >$ YZ/ ? >B K h? $% h Eñ V% $ YZ/ Eñ ?>" ;³4 0I c [) ÓÔ C# ÓÔ C# G ÓÔC# ; % _ '2KB ;u O4 8 ;@ [$) ?< ; YZ7P OV¥ ÓÔ C#$) ¨:V ?F R(w YZ7u ÓÔ C# ^" ÓÔC#$ ) ; R(w YZ7u Oþ; !./4 ; ) ÓÔ C# ÓÔ C# / \] 23/ DV
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(126) EDS data(wt.%) of amorphous or poorly crystallized Fe-(oxy)hydroxide. Sample No. SB10-2-5 SB10-2-6 SB10-2-7 SB10-2-8 SB10-2-9 min max mean. O 17.89 21.37 19.55 20.95 21.32 17.89 21.37 20.216. S 1.19 1.17 1.17 1.19 1.18. Fe 70.13 56.51 65.68 55.17 55.36 55.17 70.13 60.57. Cu 1.53 1.53 1.53 1.53. As 9.26 22.13 13.6 23.89 23.32 9.26 23.89 18.44. As/Fe 0.132 0.392 0.207 0.433 0.421 0.132 0.433 0.317.
(127) EDS data(wt.%) of well crystallized Fe-(oxy)hydroxide. Sample No.. O. S. Fe. Cu. As. SB10-2-1 SB10-2-2 SB10-2-3 SB10-2-4 min max mean. 15.34 16.14 16.77 15.98 15.34 16.77 16.06. 1.05 1.04 1.25 1.04 1.25 1.11. 81.93 75.33 79.60 76.28 75.33 81.93 78.29. 0.63 7.49 2.38 7.74 0.63 7.74 4.56. 0.008 0.099 0.030 0.101 0.008 0.101 0.060.
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관련 문서
따라서 판상형의 캐올리나이트는 반응 초기에 형성된 막대형의 뵈마이트 구조를 기본으 로 하여 반응시간의 증가에 따라 반응용액에 용해 되어 있는 비정질 실리카와