Kinetics of Fe(II)-Catalyzed Transformation of 6-line Ferrihydrite under Anaerobic Flow Conditions
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作者:
Yang, Li
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Yang, Li
[1
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Steefel, Carl I.
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Steefel, Carl I.
[1
]
Marcus, Matthew A.
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Univ Calif Berkeley, Lawrence Berkeley Lab, Adv Light Source, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Marcus, Matthew A.
[2
]
Bargar, John R.
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Stanford Synchrotron Radiat Lightsource, Menlo Pk, CA 94025 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Bargar, John R.
[3
]
机构:
[1] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
[2] Univ Calif Berkeley, Lawrence Berkeley Lab, Adv Light Source, Berkeley, CA 94720 USA
[3] Stanford Synchrotron Radiat Lightsource, Menlo Pk, CA 94025 USA
The readsorption of ferrous ions produced by the abiotic and microbially mediated reductive dissolution of iron oxy-hydroxides drives a series of transformations of the host minerals. To further understand the mechanisms by which these transformations occur and their kinetics within a microporous flow environment, flow-through experiments were conducted in which capillary tubes packed with ferrihydrite-coated glass spheres were injected with inorganic Fe(II) solutions under circumneutral pH conditions at 25 degrees C. Synchrotron X-ray diffraction was used to identify the secondary phase(s) formed and to provide data for quantitative kinetic analysis. At concentrations at and above 1.8 mM Fe(II) in the injection solution, magnetite was the only secondary phase formed (no intermediates were detected), with complete transformation following a nonlinear rate law requiring 28 and 150 h of reaction at 18 and 1.8 mM Fe(II), respectively. However, when the injection solution consisted of 0.36 mM Fe(II), goethite was the predominant reaction product and formed much more slowly according to a linear rate law, while only minor magnetite was formed. When the rates are normalized based on the time to react half of the ferrihydrite on a reduced time plot it is apparent that the 1.8 mM and 18 mM input Fe(II) experiments can be described by the same reaction mechanism, while the 0.36 input Fe(II) experiment is distinct. The analysis of the transformation kinetics suggests that the transformations involved an electron transfer reaction between the aqueous as well as sorbed Fe(II) and ferrihydrite acting as a semiconductor, rather than a simple dissolution and recrystallization mechanism. A transformation mechanism involving sorbed inner sphere Fe(II) alone is not supported, since the essentially equal coverage of sorption sites in the 18 mM and 1.8 mM Fe(II) injections cannot explain the difference in the transformation rates observed.
机构:
South China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R ChinaSouth China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R China
He, Feiqiang
Deng, Xianhe
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South China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R ChinaSouth China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R China
Deng, Xianhe
Chen, Min
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South China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R ChinaSouth China Univ Technol, Sch Chem & Chem Engn, Guangzhou 510640, Guangdong, Peoples R China
机构:
Harbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R China
Tongji Univ, Sch Environm Sci & Engn, State Key Lab Pollut Control & Resources Reuse, Shanghai, Peoples R ChinaHarbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R China
Guan, Xiaohong
Dong, Haoran
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Harbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R ChinaHarbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R China
Dong, Haoran
Ma, Jun
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Harbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R ChinaHarbin Inst Technol, State Key Lab Urban Water Resource & Environm, Harbin 150006, Peoples R China
机构:
Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Tang, Si-min
Xu, Ze-hao
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Ocean Univ China, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China
Ocean Univ China, Coll Chem & Chem Engn, Qingdao 266100, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Xu, Ze-hao
Liu, Ya-lei
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Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Liu, Ya-lei
Yang, Guang-feng
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Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Yang, Guang-feng
Mu, Jun
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Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Mu, Jun
Jin, Ren-cun
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Hangzhou Normal Univ, Coll Life & Environm Sci, Hangzhou 310036, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Jin, Ren-cun
Yang, Qiao
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Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China
Yang, Qiao
Zhang, Xiao-ling
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Zhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R ChinaZhejiang Ocean Univ, Coll Marine Sci, 1 Haida South Rd, Zhoushan 316022, Peoples R China