자연기원 불소축적토양 정화를 위한 화학적 세척 및 부유선별 공법의 적용성 평가Feasibility of Chemical Washing and Froth-flotation Separation Processes for the Remediation of Natural Origin Fluorine-enriched Soil
- Other Titles
- Feasibility of Chemical Washing and Froth-flotation Separation Processes for the Remediation of Natural Origin Fluorine-enriched Soil
- Authors
- 조정환; 백동준; 문영; 안진성
- Issue Date
- Apr-2021
- Publisher
- 한국지하수토양환경학회
- Keywords
- Natural sources; Fluorine-enriched soil; Soil remediation; Froth-flotation separation; Chemical washing
- Citation
- 지하수토양환경, v.26, no.2, pp 28 - 34
- Pages
- 7
- Indexed
- KCI
- Journal Title
- 지하수토양환경
- Volume
- 26
- Number
- 2
- Start Page
- 28
- End Page
- 34
- URI
- https://scholarworks.bwise.kr/erica/handle/2021.sw.erica/113770
- DOI
- 10.7857/JSGE.2021.26.2.028
- ISSN
- 1598-6438
2287-8831
- Abstract
- This study evaluated the feasibility of chemical washing and froth-flotation separation methods for remediating naturally occurring fluorine (F)-enriched soil due to mica weathering. The F concentration of the target soil was analyzed to be 472 ± 40.4 mg/kg. In the chemical washing experiment performed with HCl concentrations of 1, 2, and 2.5 M to remediate the soil enriched with F, only a maximum removal efficiency of up to less than 1% was achieved. As a result of sequential extraction, the residual fraction of F amounted to 99.6%, indicating that most of the F originating from weathered mica minerals was present in the soil in a chemically stable form. Thus, the chemical washing method was found to be infeasible. The froth-flotation separation was adopted by varying the collector amount, the particle size of the sample, and the pulp concentration. Consequently, a maximum removal efficiency of 62.4% (F concentration after remediation = 248 ± 29 mg/kg) was achieved, satisfying the Korean worrisome level of soil contamination (400 mg/kg). In this study, it was demonstrated that physical separation techniques, such as flotation, can be an effective measure for the active remediation (concentration reduction) of soil with accumulated F originating from F-containing mica weathering.
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