Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching
The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescen...
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| Autor*in: |
Shao, Lixiong [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Anmerkung: |
© The Minerals, Metals & Materials Society 2021 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of sustainable metallurgy - Berlin : Springer, 2015, 7(2021), 4 vom: 09. Nov., Seite 1790-1804 |
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| Übergeordnetes Werk: |
volume:7 ; year:2021 ; number:4 ; day:09 ; month:11 ; pages:1790-1804 |
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| DOI / URN: |
10.1007/s40831-021-00454-z |
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| Katalog-ID: |
SPR045793263 |
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| 520 | |a The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. | ||
| 650 | 4 | |a Dissolution |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tellurium–bismuth ore |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Oxidic–acidic leaching |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Minerals |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Diao, Jiang |4 aut | |
| 700 | 1 | |a Hu, Ruixin |4 aut | |
| 700 | 1 | |a Ji, Chengqing |4 aut | |
| 700 | 1 | |a Tan, Wenfeng |4 aut | |
| 700 | 1 | |a Li, Hongyi |4 aut | |
| 700 | 1 | |a Xie, Bing |4 aut | |
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10.1007/s40831-021-00454-z doi (DE-627)SPR045793263 (SPR)s40831-021-00454-z-e DE-627 ger DE-627 rakwb eng Shao, Lixiong verfasserin aut Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Minerals, Metals & Materials Society 2021 The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 Diao, Jiang aut Hu, Ruixin aut Ji, Chengqing aut Tan, Wenfeng aut Li, Hongyi aut Xie, Bing aut Enthalten in Journal of sustainable metallurgy Berlin : Springer, 2015 7(2021), 4 vom: 09. Nov., Seite 1790-1804 (DE-627)817362541 (DE-600)2808817-7 2199-3831 nnns volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 https://dx.doi.org/10.1007/s40831-021-00454-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 7 2021 4 09 11 1790-1804 |
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10.1007/s40831-021-00454-z doi (DE-627)SPR045793263 (SPR)s40831-021-00454-z-e DE-627 ger DE-627 rakwb eng Shao, Lixiong verfasserin aut Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Minerals, Metals & Materials Society 2021 The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 Diao, Jiang aut Hu, Ruixin aut Ji, Chengqing aut Tan, Wenfeng aut Li, Hongyi aut Xie, Bing aut Enthalten in Journal of sustainable metallurgy Berlin : Springer, 2015 7(2021), 4 vom: 09. Nov., Seite 1790-1804 (DE-627)817362541 (DE-600)2808817-7 2199-3831 nnns volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 https://dx.doi.org/10.1007/s40831-021-00454-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 7 2021 4 09 11 1790-1804 |
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10.1007/s40831-021-00454-z doi (DE-627)SPR045793263 (SPR)s40831-021-00454-z-e DE-627 ger DE-627 rakwb eng Shao, Lixiong verfasserin aut Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Minerals, Metals & Materials Society 2021 The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 Diao, Jiang aut Hu, Ruixin aut Ji, Chengqing aut Tan, Wenfeng aut Li, Hongyi aut Xie, Bing aut Enthalten in Journal of sustainable metallurgy Berlin : Springer, 2015 7(2021), 4 vom: 09. Nov., Seite 1790-1804 (DE-627)817362541 (DE-600)2808817-7 2199-3831 nnns volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 https://dx.doi.org/10.1007/s40831-021-00454-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 7 2021 4 09 11 1790-1804 |
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10.1007/s40831-021-00454-z doi (DE-627)SPR045793263 (SPR)s40831-021-00454-z-e DE-627 ger DE-627 rakwb eng Shao, Lixiong verfasserin aut Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Minerals, Metals & Materials Society 2021 The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 Diao, Jiang aut Hu, Ruixin aut Ji, Chengqing aut Tan, Wenfeng aut Li, Hongyi aut Xie, Bing aut Enthalten in Journal of sustainable metallurgy Berlin : Springer, 2015 7(2021), 4 vom: 09. Nov., Seite 1790-1804 (DE-627)817362541 (DE-600)2808817-7 2199-3831 nnns volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 https://dx.doi.org/10.1007/s40831-021-00454-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 7 2021 4 09 11 1790-1804 |
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10.1007/s40831-021-00454-z doi (DE-627)SPR045793263 (SPR)s40831-021-00454-z-e DE-627 ger DE-627 rakwb eng Shao, Lixiong verfasserin aut Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Minerals, Metals & Materials Society 2021 The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 Diao, Jiang aut Hu, Ruixin aut Ji, Chengqing aut Tan, Wenfeng aut Li, Hongyi aut Xie, Bing aut Enthalten in Journal of sustainable metallurgy Berlin : Springer, 2015 7(2021), 4 vom: 09. Nov., Seite 1790-1804 (DE-627)817362541 (DE-600)2808817-7 2199-3831 nnns volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 https://dx.doi.org/10.1007/s40831-021-00454-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 7 2021 4 09 11 1790-1804 |
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English |
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Enthalten in Journal of sustainable metallurgy 7(2021), 4 vom: 09. Nov., Seite 1790-1804 volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 |
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Enthalten in Journal of sustainable metallurgy 7(2021), 4 vom: 09. Nov., Seite 1790-1804 volume:7 year:2021 number:4 day:09 month:11 pages:1790-1804 |
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Dissolution Tellurium–bismuth ore Oxidic–acidic leaching Minerals |
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Journal of sustainable metallurgy |
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Shao, Lixiong @@aut@@ Diao, Jiang @@aut@@ Hu, Ruixin @@aut@@ Ji, Chengqing @@aut@@ Tan, Wenfeng @@aut@@ Li, Hongyi @@aut@@ Xie, Bing @@aut@@ |
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The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. 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Shao, Lixiong |
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Shao, Lixiong misc Dissolution misc Tellurium–bismuth ore misc Oxidic–acidic leaching misc Minerals Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching |
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Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching Dissolution (dpeaa)DE-He213 Tellurium–bismuth ore (dpeaa)DE-He213 Oxidic–acidic leaching (dpeaa)DE-He213 Minerals (dpeaa)DE-He213 |
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dissolution behaviors of minerals in tellurium–bismuth ore during oxidic–acidic leaching |
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Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching |
| abstract |
The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. © The Minerals, Metals & Materials Society 2021 |
| abstractGer |
The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. © The Minerals, Metals & Materials Society 2021 |
| abstract_unstemmed |
The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically in this work. The Te–Bi phase in the ore distributes in network shape, triangular shape, tree shape, strip shape, bulk shape, sparse granule, flake shape, crescent, etc., which are closely intercalated with FeS, $ FeS_{2} $, and $ CaCO_{3} $·(Mg,Fe,Mn)$ CO_{3} $. Under suitable conditions, 95.61% Te and 95.77% Bi can be recovered. Within 20 min of the initial leaching, most of dolomite and Te–Bi phase dissolve rapidly. With the extension of leaching time, a large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. The (Mg,Fe,Al)(Si,Al)$ O_{x} $(OH)y phase dissolves mainly within 60 min. Fe–S phase can be corroded but cannot dissolve completely. $ SiO_{2} $ cannot dissolve at all. Besides, $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. Without $ Fe^{3+} $ or $ H_{2} %$ SO_{4} $ in immersion liquid, Te and Bi are difficult to be leached into the lixivium from the tellurium–bismuth ore. As $ H_{2} %$ SO_{4} $ concentration and $ Fe^{3+} $ concentration increase, Te–Bi phase and Fe–Mg–Al–Si–O phase gradually dissolve, the Fe–S phase can be corroded obviously but cannot dissolve, and the Si–O phase has no change. The dissolution of dolomite is mainly controlled by $ H_{2} %$ SO_{4} $. Graphical Abstract The dissolution behaviors of various minerals in the tellurium–bismuth ore during oxidic–acidic leaching were investigated systematically. Most of dolomite and Te–Bi phase dissolve rapidly. A large amount of rod-shape $ CaSO_{4} $ particles form, attach on the surface of the tellurium–bismuth ore particles, and then grow and coarsen. $ H_{2} %$ SO_{4} $ and $ Fe^{3+} $ play a significant role on the dissolution of various minerals in the ore. © The Minerals, Metals & Materials Society 2021 |
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| title_short |
Dissolution Behaviors of Minerals in Tellurium–Bismuth Ore During Oxidic–Acidic Leaching |
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https://dx.doi.org/10.1007/s40831-021-00454-z |
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Diao, Jiang Hu, Ruixin Ji, Chengqing Tan, Wenfeng Li, Hongyi Xie, Bing |
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Diao, Jiang Hu, Ruixin Ji, Chengqing Tan, Wenfeng Li, Hongyi Xie, Bing |
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2024-07-03T18:19:48.674Z |
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| score |
7.4007587 |