• 제목/요약/키워드: Water cluster ions

검색결과 18건 처리시간 0.017초

에어로솔 입자의 정밀입경분포 측정을 위한 물분자 클러스터 이온의 질량예측 (Mass Prediction of Various Water Cluster Ions for an Accurate Measurement of Aerosol Particle Size Distribution)

  • 정종환;이혜문;송동근;김태오
    • 한국대기환경학회지
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    • 제23권6호
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    • pp.752-759
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    • 2007
  • For an accurate measurement of aerosol particle size distribution using a differential mobility analyser (DMA), a new calculation process, capable of predicting the masses for the various kinds of water cluster ions generated from a bipolar ionizer, was prepared by improving the previous process. The masses for the 5 kinds of positive and negative water cluster ions produced from a SMAC ionizer were predicted by the improved calculation process. The aerosol particle charging ratios calculated by applying the predicted ion masses to particle charging equations were in good accordance with the experimentally measured ones, indicating that the improved calculation process are more reasonable than the previous one in a mass prediction of bipolar water cluster ions.

Generation of Water Droplet Ion Beam for ToF-SIMS Analysis

  • Myoung Choul Choi;Ji Young Baek;Aram Hong;Jae Yeong Eo;Chang Min Choi
    • Mass Spectrometry Letters
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    • 제14권4호
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    • pp.147-152
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    • 2023
  • The increasing demand for two-dimensional imaging analysis using optical or electronic microscopic techniques has led to an increase in the use of simple one-dimensional and two-dimensional mass spectrometry imaging. Among these imaging methods, secondary-ion mass spectrometry (SIMS) has the best spatial resolution using a primary ion beam with a relatively insignificant beam diameter. Until recently, SIMS, which uses high-energy primary ion beams, has not been used to analyze molecules. However, owing to the development of cluster ion beams, it has been actively used to analyze various organic molecules from the surface. Researchers and commercial SIMS companies are developing cluster ion beams to analyze biological samples, including amino acids, peptides, and proteins. In this study, a water droplet ion beam for surface analysis was realized. Water droplets ions were generated via electrospraying in a vacuum without desolvation. The generated ions were accelerated at an energy of 10 keV and collided with the target sample, and secondary ion mass spectra were obtained for the generated ions using ToF-SIMS. Thus, the proposed water droplet ion-beam device showed potential applicability as a primary ion beam in SIMS.

Chemical Reactivity of Ti+ within Water, Dimethyl Ether, and Methanol Clusters

  • Koo, Young-Mi;An, Hyung-Joon;Yoo, Seoung-Kyo;Jung, Kwang-Woo
    • Bulletin of the Korean Chemical Society
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    • 제24권2호
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    • pp.197-204
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    • 2003
  • The intracluster ion-molecule reactions of $Ti^+(H_2O)_n,\;Ti^+(CH_3OCH_3)_n,\;and\;Ti^+(CH_3OD)_n$ complexes produced by the mixing of the laser-vaporized plasma and the pulsed supersonic beam were studied using a reflectron time-of-flight mass spectrometer. The reactions of $Ti^+$ with water clusters were dominated by the dehydrogenation reaction, which produces $TiO^+(H_2O)_n$ clusters. The mass spectra resulting from the reactions of $Ti^+\;with\;CH_3OCH_3$ clusters exhibit a major sequence of $Ti^+(OCH_3)_m(CH_3OCH_3)_n$ cluster ions, which is attributed to the insertion of $Ti^+$ ion into C-O bond of $CH_3OCH_3$ followed by $CH_3$ elimination. The prevalence of $Ti^+(OCH_3)_m(CH_3OD)_n$ ions in the reaction of $Ti^+\;with\;CH_3OD$ clusters suggests that D elimination via O-D bond insertion is the preferred decomposition pathway. In addition, the results indicate that consecutive insertion reactions by the $Ti^+$ ion occur for up to three precursor molecules. Thus, examination of $Ti^+$ insertion into three different molecules establishes the reactivity order: O-H > C-O > C-H. The experiments additionally show that the chemical reactivity of heterocluster ions is greatly influenced by cluster size and argon stagnation pressure. The reaction energetics and formation mechanisms of the observed heterocluster ions are also discussed.

Fates of water and salts in non-aqueous solvents for directional solvent extraction desalination: Effects of chemical structures of the solvents

  • Choi, Ohkyung;Kim, Minsup;Cho, Art E.;Choi, Young Chul;Kim, Gyu Dong;Kim, Dooil;Lee, Jae Woo
    • Membrane and Water Treatment
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    • 제10권3호
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    • pp.207-212
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    • 2019
  • Non-aqueous solvents (NASs) are generally known to be barely miscible, and reactive with polar compounds, such as water. However, water can interact with some NASs, which can be used as a new means for water recovery from saline water. This study explored the fate of water and salt in NAS, when saline water is mixed with NAS. Three amine solvents were selected as NAS. They had the same molecular formula, but were differentiated by their molecular structures, as follows: 1) NAS 'A' having the hydrophilic group ($NH_2$) at the end of the straight carbon chain, 2) NAS 'B' with symmetrical structure and having the hydrophilic group (NH) at the middle of the straight carbon chain, 3) NAS 'C' having the hydrophilic group ($NH_2$) at the end of the straight carbon chain but possessing a hydrophobic ethyl branch in the middle of the structure. In batch experiments, 0.5 M NaCl water was blended with NASs, and then water and salt content in the NAS were individually measured. Water absorption efficiencies by NAS 'B' and 'C' were 3.8 and 10.7%, respectively. However, salt rejection efficiency was 98.9% and 58.2%, respectively. NAS 'A' exhibited a higher water absorption efficiency of 35.6%, despite a worse salt rejection efficiency of 24.7%. Molecular dynamic (MD) simulation showed the different interactions of water and salts with each NAS. NAS 'A' formed lattice structured clusters, with the hydrophilic group located outside, and captured a large numbers of water molecules, together with salt ions, inside the cluster pockets. NAS 'B' formed a planar-shaped cluster, where only some water molecules, but no salt ions, migrated to the NAS cluster. NAS 'C', with an ethyl group branch, formed a cluster shaped similarly to that of 'B'; however, the boundary surface of the cluster looked higher than that of 'C', due to the branch structure in solvent. The MD simulation was helpful for understanding the experimental results for water absorption and salt rejection, by demonstrating the various interactions between water molecules and the salts, with the different NAS types.

Silver Ions in Zeolite A are Reduced by H$_2$ only at High Temperatures when 8-Rings are Blocked by Cs$^+$. Crystal Structures of Dehydrated $Ag_9Cs_3$-A Treated with H$_2$ at 23, 310, and 470${^{\circ}C}$

  • KIm, Yang;Seff, Karl
    • Bulletin of the Korean Chemical Society
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    • 제8권2호
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    • pp.69-72
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    • 1987
  • The structures of dehydrated $Ag_9Cs_3$-A treated with hydrogen gas at three different temperatures have been determined by single-crystal X-ray diffraction techniques. Their structures were solved and refined in the cubic space group Pm3m at 23(1) $^{\circ}C$. All crystals were ion exchanged in flowing streams of aqueous $AgNO_3$/$CsNO_3$ with a mole ratio 1:3.0 to achieve the desired crystal composition. The structures treated with hydrogen at $23^{\circ}C(a=12.288(1)\;{\AA})\;and\;310^{\circ}C(a=12.291(2)\;{\AA})$ refined to the final error indices R1 = 0.091 and R2 = 0.079, and 0.065 and 0.073, respectively, using the 216 and 227 reflections, respectively, for which I >3${\sigma}$(I). In both of these structures, eight $Ag^+$ ions are found nearly at 6-ring centers, and three $Cs^+$ ions lie at the centers of the 8-rings at sites of $D_{4h}$ symmetry. One $Ag^{\circ}atom$, presumably formed from the reduction of a $Ag^+$ ion by an oxide ion of a residual water molecule or of the zeolite framework during the dehydration process, is retained within the zeolite, perhaps in a cluster. In these two structures hydrogen gas could not enter the zeolite to reduce the $Ag^+$ ions because the large $Cs^+$ ions blocked all the 8-windows. However, hydrogen could slowly diffuse into the zeolite and was able to reach and to reduce about half of the $Ag^+$ ions in the structure only at high temperature ($470^{\circ}C$). The silver atoms produced migrated out of the zeolite framework, and the protons generated led to substantial crystal damage.

Crystallographic Evidence for the Reduction of CO in Partially Dehydrated Silver Zeolite A

  • Kim, Yang;Song, Seong-Hwan;Seff, Karl
    • Bulletin of the Korean Chemical Society
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    • 제10권3호
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    • pp.230-234
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    • 1989
  • The crystal structure of $Ag^+$-exchanged zeolite A vacuum-dehydrated at $370^{\circ}C$ and then treated with carbon monoxide at $$23^{\circ}C$ has been determined by single crystal x-ray diffraction methods in the cubic space group Pm3m at $23^(1){\circ}C$ ; a = 12.116 (2)${\AA}$. The structure was refined to the final error indices $R_1\;=\;0.061\;and\;R_2$(weighted) = 0.068 using 349 independent reflections for which I > 3${\sigma}(I).\;3.6\;Ag_+-CO$ complexes, where -CO may represent -CHO or -$CH_2OH$, were found in each large cavity. By coordination to silver atoms followed by reaction with $Ag^{\circ}and\;H^+$ within the zeolite, carbon monoxide has been partially reduced. In about 28% of the sodalite units, a $Ag_6(Ag^+)_2$ cluster may be present. In about 37% of the sodalite units, three $Ag^+$ ions are found on threefold axes where they may be bridged by three water molecules. The remaining 35% of the sodalite units are empty of silver species. Two $Ag^+$ ions per unit cell are associated with 8-ring oxygens. The remaining ca $$3Ag^+$ ions per unit cell have been reduced during the synthesis and have migrated to form small silver crystallities on the surface of the zeolite single crystal.

지구통계 기법을 활용한 울진 지역 천부 지하수의 수질 및 수리지구화학 특성 해석 (Geostatistical Interpretation of Water Quality and Hydrogeochemistry of shallow Groundwater in the Uljin Area, Korea)

  • 김남진;윤성택;김형수;정경문;김규범
    • 자원환경지질
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    • 제34권2호
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    • pp.175-192
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    • 2001
  • 동해안 울진 지역 천부 지하수의 수리지구화학 자료에 대하여 지구통계 분석(이원배치 분산 분석, 군집 분석, 요인 분석)을 수행함으로써, 수질 자료와 오염 특성의 시간적.공간적 변화 양상을 규명하고 대수층에서 일어나는 주요 반응을 고찰하였다. 이원배치 분산 분석 결과, 광역적 수질 특성은 8개 수계분지를 따라 유의한 공간적 변화를 보여주지 않았으나, Ca, HCO$_3$,SO$_4$등 일부 이온종은 수계분지별로 의미 있는 변화를 나타내었다. 시료 채취시기에 따른 계절 변화는 SO$_4$를 제외하고는 인지되지 않았다. 그러나 군집 분석 결과, 수리지구화학 특성의 변화는 해안으로부터의 거리에 따라 아주 잘 설명될 수 있음을 지시하였다. 요인 분석 결과, 연구 지역 천부 지하수의 수리지구화학 특성은 다양한 요인에 의해 지배됨을 확인하였다. 중요 순서로 그 요인을 나열하면, 1) 물-암석 반응(주로 탄산염 광물의 용해), 2) 바다에서 기원한 해염의 혼입, 3) 비료와 각종 농화학 약품에 의한 오염으로 밝혀졌다.

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제올라이트 A 동공 내 비골격 ZrI6Tl119+ 양이온 클러스터의 합성과 구조 연구 (Synthesis and Structural Study of Extraframework ZrI6Tl119+ Cationic Cluster in Zeolite A)

  • 임현승;박종삼;김철웅;임우택
    • 광물과 암석
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    • 제35권4호
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    • pp.447-455
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    • 2022
  • Tl+ 이온으로 교환된 제올라이트 A (|Tl12|[Si12Al12O48]-LTA, Tl12-A) 단결정을 진공 탈수시킨 후, 623 K에서 72시간 동안 ZrI4 (g, 6.0 × 103 Pa) 와 반응시켜, Zr,I,Tl-A (|Zr0.25I1.5Tl12|[Si12Al12O48]-LTA)를 제조하였다. 제조된 단결정의 구조는 294 K에서 단결정 X-선 회절 기술을 이용하여 Pm3m (a = 12.337(2) Å) 입방 공간군에 속함을 확인 하였고, Fo> 4σ(Fo)를 사용하여 최종 오차 인자를 R1/wR2= 0.055/0.189로 정밀화 하였다. 이 구조에서 Tl+ 이온은 6-ring 맞은편의 3-fold 축상의 서로 다른 3개의 결정학적 위치에서 단위세포당 7.5개가 발견되었고, 모든 8-ring 근처(단위세포당 3개)에서 3개의 결정학적 위치로 채워졌다. 그리고 단위세포당 1.5개의 Tl+ 이온은 ZrI4(g)와 반응 후 sodalite cavity 안에서 3-fold 축상을 벗어난 자리에서 골격산소 O2 및 O3와 결합하면서 발견되었다. Zr4+ 이온은 6개의 I- 이온과 함께 8면체의 ZrI62- 형태로 large cavity 정중앙에 존재하였고, 이들은 8-ring 및 6-ring 근처에 존재하고 있던 Tl+ 양이온과 3차원적으로 연결하면서 ZrI6Tl119+ cationic cluster을 형성하였다. 이러한 cationic cluster은 Zr,I,Tl-A의 large cavity 중에서 약 25%에만 존재하였다.

Crystal Structure of Fully Dehydrated Partially Ag$^+$-Exchanged Zeolite 4A, $Ag_{7.6}Na_{4.4}$-A. Ag$^+$ Ions Prefer 6-Ring Sites. One Ag$^+$ Ion is Reduced

  • Kim, Yang;Han, Young-Wook;Seff, Karl
    • Bulletin of the Korean Chemical Society
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    • 제7권3호
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    • pp.190-193
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    • 1986
  • The structure of partially $Ag^+$-exchanged zeolite 4A, $Ag_{7.6}Na_{4.4}-A$, vacuum dehydrated at $370^{\circ}C$, has been determined by single-crystal x-ray diffraction techniques in the cubic space group, Pm3m (a = 12.311(1)${\AA}$) at $24(1)^{\circ}}C$. The structure was refined to the final error indices $R_1$ = $R_2$ (weighted) = 0.064 using 266 independent reflections for which $I_0$>$3{\sigma}(I_0)$. Three $Na^+$ ions occupy the 3 8-ring sites, and the remaining ions, 1.4 $Na^+$ and 6.6 $Ag^+$, fill the 8 6-ring sites; each $Ag^+$ ion is nearly in the [111] plane of its 3 O(3) ligands, and each $Na^+$ ion is 0.9${\AA}$ from its corresponding plane, on the large-cavity side. One reduced silver atom per unit cell was found inside the sodalite unit. It was presumably formed from the reduction of a $Ag^+$ ion by an oxide ion of a residual water molecule or of the zeolite framework. It may be present as a hexasilver cluster in 1/6 of the sodalite units, or, most attractively among several alternatives, as an isolated Ag atom coordinated to 4 Ag ions in each sodalite unit to give $(Ag_5)^{4+}$, symmetry 4mm.

Theoretical Studies on Selectivity of Dibenzo-18-Crown-6-Ether for Alkaline Earth Divalent Cations

  • Heo, Ji-Young
    • Bulletin of the Korean Chemical Society
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    • 제33권8호
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    • pp.2669-2674
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    • 2012
  • Crown ether is one of well-known host molecules and able to selectively sequester metal cation. We employed M06-2X density functional theory with IEFPCM and SMD continuum solvation models to study selectivity of dibenzo-18-crown-6-ether (DB18C6) for alkaline earth dications, $Ba^{2+}$, $Sr^{2+}$, $Ca^{2+}$, and $Mg^{2+}$ in the gas phase and in aqueous solution. $Mg^{2+}$ showed predominantly strong binding affinity in the gas phase because of strong polarization of CO bonds by cation. In aqueous solution, binding free energy differences became smaller among these dications. However, $Mg^{2+}$ had the best binding, being incompatible with experimental observations in aqueous solution. The enthalpies of the dication exchange reaction between DB18C6 and water cluster molecules were computed as another estimation of selectivity in aqueous solution. These results also demonstrated that $Mg^{2+}$ bound to DB18C6 better than $Ba^{2+}$. We speculated that the species determining selectivity in water could be 2:1 complexes of two DB18C6s and one dication.