• Title/Summary/Keyword: Lithium isotopes

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Chromatographic Enrichment of Lithium Isotopes by Hydrous Manganese(IV) Oxide

  • Kim, Dong Won
    • Bulletin of the Korean Chemical Society
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    • v.22 no.5
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    • pp.503-506
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    • 2001
  • Separation of lithium isotopes was investigated by chemical ion exchange with a hydrous manganese(IV) oxide ion exchanger using an elution chromatography. The capacity of manganese(IV) oxide ion exchanger was 0.5 meq/g. One molar CH3COO Na solution was used as an eluent. The heavier isotope of lithium was enriched in the solution phase, while the lighter isotope was enriched in the ion exchanger phase. The separation factor was calculated according to the method of Glueckauf from the elution curve and isotopic assays. The single stage separation factor of lithium isotope pair fractionation was 1.021.

Separation of Lithium Isotopes by Tetraazamacrocycles Tethered to Merrifield Peptide Resin

  • Jeon, Youn-Seok;Jang, Nak-Han;Kang, Byung-Moo;Jeon, Young-Shin;Kim, Chang-Suk;Choi, Ki-Young;Ryu, Hai-Il
    • Bulletin of the Korean Chemical Society
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    • v.28 no.3
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    • pp.451-456
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    • 2007
  • Tetraazamacrocyclic ion exchangers tethered to Merrifield peptide resin (DTDM, TTTM) were prepared and the ion exchange capacity of these was characterized. The isotope separation of lithium was determined using breakthrough method of column chromatography. The isotope separation coefficient was strongly dependent on the ligand structure by Glueckauf's theory. We found that the isotope separation coefficients were increased as the values of distribution coefficients were increased. In this experiment the lighter isotope, 6Li was enriched in the resin phase, while the heavier isotope, 7Li in the solution phase. The ion radius of lighter isotope, 6Li was shorter than the heavier isotope, 7Li. The hydration number of lithium ion with the same charge became small as mass number was decreased. Because 6Li was more strongly retained in the resin than 7Li, the isotopes of lithium were separated with subsequent enrichment in the resin phase.

Hydrogen isotope exchange behavior of protonated lithium metal compounds

  • Park, Chan Woo;Kim, Sung-Wook;Sihn, Youngho;Yang, Hee-Man;Kim, Ilgook;Lee, Kwang Se;Roh, Changhyun;Yoon, In-Ho
    • Nuclear Engineering and Technology
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    • v.53 no.8
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    • pp.2570-2575
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    • 2021
  • The exchange behaviors of hydrogen isotopes between protonated lithium metal compounds and deuterated water or tritiated water were investigated. The various protonated lithium metal compounds were prepared by acid treatment of lithium metal compounds with different crystal structures and metal compositions. The protonated lithium metal compounds could more effectively reduce the deuterium concentration in water compared with the corresponding pristine lithium metal compounds. The H+ in the protonated lithium metal compounds was speculated to be more readily exchangeable with hydrons in the aqueous solution compared with Li+ in the pristine lithium metal compounds, and the exchanged heavier isotopes were speculated to be more stably retained in the crystal structure compared with the light protons. When the tritiated water (157.7 kBq/kg) was reacted with the protonated lithium metal compounds, the protonated lithium manganese nickel cobalt oxide was found to adsorb and retain twice as much tritium (163.9 Bq/g) as the protonated lithium manganese oxide (69.9 Bq/g) and the protonated lithium cobalt oxide (75.1 Bq/g) in the equilibrium state.

Separation of Lithium Isotopes by Porous Sulfonated Styrene-Divinylbenzene Copolymer Ionexchanger (Porous Sulfonated Styrene-Divinylbenzene Copolymer Ionexchanger 에 의한 리튬 동위원소의 분리)

  • Dong Won Kim;Ki Suck Maeng;Hae Young Song;Hae Il Ryu
    • Journal of the Korean Chemical Society
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    • v.27 no.3
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    • pp.189-193
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    • 1983
  • The lithium isotopes separation experiments were carried out in hydrochloric acid with cation exchanger systerns. In these experiments were employed porous sulfonated styrene-divinylbenzene copolymer and Dowex 50w-x8 as cation exchanger. The contents of lithium of the fraction were determined with atomic absorption spectrophotometer. The relative mass of lithium isotopes of the fractions was analyzed on a mass spectrometer. The isotope separation factors of lithium were calculated from the isotope compositions of these eluted fractions. Separation factor for the system in hydrochloric acid and porous sulfonated styrene-divinylbenzene copolymer was found to be 1.0020, and for the case of system in hydrochloric acid and Dowex 50w-x8 was 1.0011${\om}$0.0002. From these results, we found that the separation factor for porous sulfonated styrene-divinylbenzene copolymer ionexchanger is larger than value of Dowex 50w-x8 ionexchanger.

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Chromatographic Separation of Lithum Isotopes by Hydrous Managanese(Ⅳ) Oxide (가수된 산화 망간(Ⅳ)에 의한 리튬 동위원소의 크로마토그래피적 분리)

  • Kim, Dong Won
    • Journal of the Korean Chemical Society
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    • v.45 no.3
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    • pp.219-222
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    • 2001
  • Separation of lithium isotopes was investigated by chemical ion exchange with a hydrous manganese(IV) oxide ion exchanger using an elution chromatography. The capacity of manganese(IV) oxide ion exchanger was 0.5 meq/g. The heavier lithium isotope was enriched in the solution phase, while the lighter isotope was enriched in the ion exchanger phase. The separation factor was determined according to the method of Glueckauf from the elution curve and isotopic assays. The separation factor of $^6Li^+$-$^7Li^+$ isotope pair fractionation was 1.018.

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Enrichment of Lithium Isotopes by Cation Exchange Chromatography (양이온 교환 크로마토그래피에 의한 리튬 동위원소의 농축)

  • Kim, Dong Won;Kim, Chang Suck;Choi, Ki Young;Jeon, Young Shin;Jeong, Young Kyu;Park, Sung Up
    • Analytical Science and Technology
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    • v.7 no.2
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    • pp.201-204
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    • 1994
  • Cation exchange column chromatography of lithium was carried out to investigate the lithium isotope separation in aqueous ion exchange system. A Pyrex glass column of $50cm{\times}6mm$ inner radius with a water jacket was used as the separation column in experiment. Upon column chromatography using hydrochloric and succinic acid mixtures as an elunent, single separation factor, ${\alpha}$, 1.0068 was obtained. From the experiment, it was found that $^6Li$ was enriched in the resin phase and $^7Li$ in the solution phase.

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A Suitability Study on the Indicator Isotopes for Graphite Isotope Ratio Method (GIRM) (흑연 동위원소 비율법의 지표 동위 원소 적합성 연구)

  • Han, Jinseok;Jang, Junkyung;Lee, Hyun Chul
    • Journal of Nuclear Fuel Cycle and Waste Technology(JNFCWT)
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    • v.18 no.1
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    • pp.83-90
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    • 2020
  • The Graphite Isotope Ratio Method (GIRM) can verify non-proliferation of nuclear weapon by estimating the total plutonium production in a graphite-moderated reactor. Using the reactor, plutonium is generated and accumulated through the 238U neutron capture reaction, and impurities in the graphite are converted to nuclides due to the nuclear reaction. Therefore, the amount of plutonium production and concentration of the impurities are correlated. However, the plutonium production cannot be predicted using only the absolute concentration of the impurities. It can only be predicted when the initial concentration of the impurities is obtained because the concentration, at a certain time, depends on it. Nevertheless, the ratios of the isotopes in an element are known regardless of the impurity of an element in the graphite moderator. Thus, the correlation between the isotope ratio and amount of plutonium produced helps predict plutonium production in a graphite-moderated reactor. Boron, Lithium, Chlorine, Titanium, and Uranium are known as indicator elements in the GIRM. To assess whether the correlation between the indicator isotope and amount of plutonium produced is independent of the initial concentration of the impurities, four different impurity compositions of graphite were used. 10B/11B, 36Cl/35Cl, 48Ti/49Ti, and 235U/238U had a consistent correlation with the cumulative plutonium production, regardless of the initial impurity concentration of the graphite, because these isotopes were not generated through the nuclear reaction of other elements. On the other hand, the correlation between 6Li/7Li and plutonium production depended on the initial concentration of the impurities in graphite. Although 7Li can be produced through the neutron capture reaction of 6Li, the (n, α) reaction of 10B was the major source of 7Li. Therefore, the initial concentration of 10B affected the production of 7Li, making Li unsuitable as an indicator element for the GIRM.