Potassium-Bicarbonate-Induced Mineralized Acid Mine Drainage into Iron Hydroxyl Sulfate Minerals for Better Water Remediation and Resource Reuse
Xin He,
Honghao Wang,
Chunlei Tang,
Hong Yan () and
Hua Jin ()
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Xin He: College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
Honghao Wang: College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
Chunlei Tang: Key Laboratory of Karst Dynamics, Ministry of Land and Resources, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China
Hong Yan: College of Materials Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
Hua Jin: College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
Sustainability, 2024, vol. 16, issue 2, 1-13
Abstract:
Iron hydroxyl sulfate minerals (IHSMs, including schwertmannite and jarosite) are a promising material for environmental applications with excellent adsorption of metal oxygen anions. The acid mine drainage (AMD) abundant in iron and sulfate ions holds potential for the production of valuable IHSMs, thereby achieving resource recycling whilst simultaneously mitigating water contamination, which is important for the sustainable remediation of AMD. Conventional mineralization, which promotes the generation of minerals from Fe 3+ and SO 4 2− through the energy provided by chemical or biological oxidation, can only partially mineralize iron in AMD containing substantial quantities of Fe 2+ . In this study, an improved method for mineralizing AMD containing iron of a different valence into IHSMs under the induction of KHCO 3 was proposed. For AMD containing Fe 2+ , the combination of KHCO 3 and H 2 O 2 was used to promote the hydrolysis of iron (92.7%) and sulfate (11.1%) into IHK minerals, which resulted in a significant increase in iron removal of 75.2% and a minor increase in sulfate removal of 4.9%, compared with the formation of schwertmannite from oxidation solely involving H 2 O 2 . For the AMD containing Fe 3+ , the energy generated by the acid–base reaction in water could also directly promote the formation of IK minerals from 97.2% iron and 6.9% sulfate. XRD and FTIR analyses confirmed the identification of the IHK and IK minerals as IHSMs transitioning from schwertmannite to jarosite. SEM and elemental analyses indicated that the mineral exhibited denser aggregate spheres with the incorporation of KHCO 3 in mineralization yet displayed enhanced mineralization abilities for the contaminant ions in AMD. Moreover, despite the SSA of the modified minerals being diminished (2.02, 1.83 and 1.83 m 2 /g for IH, IHK and IK, respectively), the presence of more sulfate in the mineral enhanced the adsorption capacity of Cr(VI). Furthermore, the water quality results also illustrated that the removal ratios of iron and sulfate in AMD notably increased with the involvement of KHCO 3 in mineralization. In conclusion, the KHCO 3 -induced mineralization of iron-containing (either divalent or trivalent) AMD into IHSMs not only improved the mineralization ratios and contaminant removal ratios for better remediation of AMD but also obtained mineral resources with better adsorption of Cr(VI), thereby fostering the sustainable advancement of the remediation of AMD. Therefore, this innovative strategy employing KHCO 3 -assisted chemical mineralization to form IHSMs holds ample potential and promises to be an efficacious methodology for the sustainable remediation of iron-rich AMD.
Keywords: adsorption properties; chromium; schwertmannite; induced mineralization; acid mine drainage (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2024
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