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タイトル: Sorption-desorption column tests to evaluate the attenuation layer using soil amended with a stabilising agent
著者: Kato, Tomohiro  kyouindb  KAKEN_id  orcid https://orcid.org/0000-0003-3322-4791 (unconfirmed)
Gathuka, W., Lincoln
Okada, Takaomi
Takai, Atsushi  kyouindb  KAKEN_id  orcid https://orcid.org/0000-0003-3063-471X (unconfirmed)
Katsumi, Takeshi  kyouindb  KAKEN_id  orcid https://orcid.org/0000-0003-1936-275X (unconfirmed)
Imoto, Yukari
Morimoto, Kazuya
Nishikata, Miu
Yasutaka, Tetsuo
著者名の別形: 加藤, 智大
岡田, 雄臣
高井, 敦史
勝見, 武
キーワード: Fluoride
Geogenic contamination
Magnesium oxide
Partition coefficient
Advection-dispersion analysis
発行日: Aug-2021
出版者: Elsevier BV
誌名: Soils and Foundations
巻: 61
号: 4
開始ページ: 1112
終了ページ: 1122
抄録: Sorption-desorption column tests using acrylic columns (ϕ 5 cm × h 10 cm) were employed to evaluate the sorption performance of an attenuation layer against geogenic contamination. The attenuation layer material was silica sand amended with 1, 5, or 10% of a stabilising agent. The main component of the agent was magnesium oxide. The sorption behaviour of the materials was determined by a fluoride solution (C₀ = 80 mg/L F-), while the desorption behaviour was determined by distilled water. Breakthroughs (C/C₀ > 0.05) occurred after approximately 1, 20, and 50 PVF for stabilising agent contents of 1, 5, and 10%, respectively. The one-dimensional advection-dispersion equation modelled the breakthrough curves obtained from the tests. The predictions gave unrealistic estimates, especially for the breakthrough point where C/C₀ = 0.05. For the 1% agent content, approximately 20% of the sorbed mass, Ss, was desorbed, but the percentage of desorbed mass, Sd, was much smaller for the higher agent contents. The difference between the sorbed and desorbed masses was defined as the immobilised fraction, Ss - Sd. For the 5% agent content, Ss - Sd = 4.0 mg/g. The results suggest that when silica sand is amended with magnesium oxide as an agent, the mixture can immobilise the fluoride in the attenuation layer.
著作権等: © 2021 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society.
This is an open access article under the CC BY-NC-ND license
URI: http://hdl.handle.net/2433/276206
DOI(出版社版): 10.1016/j.sandf.2021.05.004
出現コレクション:学術雑誌掲載論文等

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