• Title/Summary/Keyword: LiClO₄

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Enhanced Carboxymethylcellulase Production by a Newly Isolated Marine Bacterium, Cellulophaga lytica LBH-14, Using Rice Bran

  • Gao, Wa;Lee, Eun-Jung;Lee, Sang-Un;Li, Jianhong;Chung, Chung-Han;Lee, Jin-Woo
    • Journal of Microbiology and Biotechnology
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    • v.22 no.10
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    • pp.1412-1422
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    • 2012
  • The aim of this work was to establish the optimal conditions for production of carboxymethylcellulase (CMCase) by a newly isolated marine bacterium using response surface methodology (RSM). A microorganism producing CMCase, isolated from seawater, was identified as Cellulophaga lytica based 16S rDNA sequencing and the neighborjoining method. The optimal conditions of rice bran, ammonium chloride, and initial pH of the medium for cell growth were 100.0 g/l, 5.00 g/l, and 7.0, respectively, whereas those for production of CMCase were 79.9 g/l, 8.52 g/l, and 6.1. The optimal concentrations of $K_2HPO_4$, NaCl, $MgSO_4{\cdot}7H_2O$, and $(NH_4)_2SO_4$ for cell growth were 6.25, 0.62, 0.28, and 0.42 g/l, respectively, whereas those for production of CMCase were 3.72, 0.54, 0.70, and 0.34 g/l. The optimal temperature for cell growth and the CMCase production by C. lytica LBH-14 were $35^{\circ}C$ and $25^{\circ}C$, respectively. The maximal production of CMCase under optimized condition for 3 days was 110.8 U/ml, which was 5.3 times higher than that before optimization. In this study, rice bran and ammonium chloride were developed as carbon and nitrogen sources for the production of CMCase by C. lytica LBH-14. The time for production of CMCase by a newly isolated marine bacterium with submerged fermentations reduced to 3 days, which resulted in enhanced productivity of CMCase and a decrease in its production cost.

Syntheses and Characterization of PBO Precursors Containing Dimethylphenoxy and/or MPEG Pendant Groups (Dimethylphenoxy와 MPEG 팬던트 그룹을 갖는 폴리벤즈옥사졸 전구체의 합성 및 특성)

  • Yoon Doo-Soo;Choi Jae-Kon;Jo Byung-Wook
    • Polymer(Korea)
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    • v.29 no.5
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    • pp.493-500
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    • 2005
  • Polyhydroxyamides(PHAs) having poly(ethylene glycol)methyl ether (MPEG) and/or dimethylphenoxy pendant groups were synthesized by solution polycondensation at low temperature. The inherent viscosities of the PHAs measured at $35^{\circ}C$ in DMAC or DMAc/LiCl solution were in the range of $0.51\~2.31dL/g$. This precursor polymers were studied by FT-IR, $1H-NMR$, DSC, and TGA. Solubility of the precursors with higher MPEG unit was increased, especially the polymer having MPEG $(M_n=1100)$ was soluble or partially soluble in ethanol, methanol, and water as well as aprotic solvents, but the PBOs were nearly insoluble in a variety of solvents. PHAs were converted to polybenzoxazoles (PBOs) by thermal cyclization reaction with heat of endotherm. In case of the precursors having MPEG nit, the precursor polymers with a higher $M_n$ were fully cyclized at a lower temperature than one with a lower $M_n$.

Fluorine Distribution and Attenuation of Groundwater within Limestone and Granite from Keumsan-Wanju Fluorite Mineralized Zone (금산-완주지역 형석광화대내 석회암 및 화강암지역 지하수의 불소분포 특성 및 저감방안)

  • Hwang, Jeong
    • Economic and Environmental Geology
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    • v.34 no.1
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    • pp.105-117
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    • 2001
  • The characteristics of hydrogeochemistry and fluorine distribution in drinking groundwater from limestone and granite were studied in the Keumsan-Wanju area, where major important fluorite-deposits are distributed. The hydrochemical properties of groundwater from studied area arc commonly characterized as $Ca-HC0_3$ water type. However, some of the groundwater samples collected from Jurassic and Cretaceuus granites belong to $Ca-Na-HC0_3 and Na-HC0_3$ type, respectively. The contamination of drinking groundwater by minewater from the nearby fluorite deposits is not found yet. However, groundwater having high F contents up to 1].4 mgll, which is higher than the drinking water limit, is found from the wells located in Cretaceous granite. The tluorine contents in groundwater generally increase with increasing well depth. The concentrations of F in the groundwater show a positive relationship with the values of Na, $HC0_3, Cl. Si0_2$, pH, whereas a negative relationship with Ca. The positive correlation of F-concentrations to major elements ($Si0_2$, Na, CI) and trace elements (Li, B, Rb) may suggest that the groundwater come from the decomposition of tluoride-bearing silicate minerals within highly differentiated granitic rocks, Therefore, wells for drinking water should not be developed or should be drilled within shallow level in the Cretaceous granite region to reduce the F contents in the groundwater.

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Electrochemical Reduction Process for Pyroprocessing (파이로프로세싱을 위한 전해환원 공정기술 개발)

  • Choi, Eun-Young;Hong, Sun-Seok;Park, Wooshin;Im, Hun Suk;Oh, Seung-Chul;Won, Chan Yeon;Cha, Ju-Sun;Hur, Jin-Mok
    • Korean Chemical Engineering Research
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    • v.52 no.3
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    • pp.279-288
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    • 2014
  • Nuclear energy is expected to meet the growing energy demand while avoiding CO2 emission. However, the problem of accumulating spent fuel from current nuclear power plants which is mainly composed of uranium oxides should be addressed. One of the most practical solutions is to reduce the spent oxide fuel and recycle it. Next-generation fuel cycles demand innovative features such as a reduction of the environmental load, improved safety, efficient recycling of resources, and feasible economics. Pyroprocessing based on molten salt electrolysis is one of the key technologies for reducing the amount of spent nuclear fuel and destroying toxic waste products, such as the long-life fission products. The oxide reduction process based on the electrochemical reduction in a LiCl-$Li_2O$ electrolyte has been developed for the volume reduction of PWR (Pressurized Water Reactor) spent fuels and for providing metal feeds for the electrorefining process. To speed up the electrochemical reduction process, the influences of the feed form for the cathode and the type of anode shroud on the reduction rate were investigated.

Janggunite, a New Mineral from the Janggun Mine, Bonghwa, Korea (경북(慶北) 봉화군(奉化郡) 장군광산산(將軍鑛山産) 신종광물(新種鑛物) 장군석(將軍石)에 대(對)한 광물학적(鑛物學的) 연구(硏究))

  • Kim, Soo Jin
    • Economic and Environmental Geology
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    • v.8 no.3
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    • pp.117-124
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    • 1975
  • Wet chemical analysis (for $MnO_2$, MnO, and $H_2O$(+)) and electron microprobe analysis (for $Fe_2O_3$ and PbO) give $MnO_2$ 74.91, MnO 11.33, $Fe_2O_3$ (total Fe) 4.19, PbO 0.03, $H_2O$ (+) 9.46, sum 99.92%. 'Available oxygen determined by oxalate titration method is allotted to $MnO_2$ from total Mn, and the remaining Mn is calculated as MnO. Traces of Ba, Ca, Mg, K, Cu, Zn, and Al were found. Li and Na were not found. The existence of (OH) is verified from the infrared absorption spectra. The analysis corresponds to the formula $Mn^{4+}{_{4.85}}(Mn^{2+}{_{0.90}}Fe^{3+}{_{0.30}})_{1.20}O_{8.09}(OH)_{5.91}$, on the basis of O=14, 'or ideally $Mn^{4+}{_{5-x}}(Mn^{2+},Fe^{3+})_{1+x}O_{8}(OH)_{6}$ ($x{\approx}0.2$). X-ray single crystal study could not be made because of the distortion of single crystals. But the x-ray powder pattern is satisfactorily indexed by an orthorhombic cell with a 9.324, b 14.05, c $7.956{\AA}$., Z=4. The indexed powder diffraction lines are 9.34(s) (100), 7.09(s) (020), 4.62(m) (200, 121), 4.17(m) (130), 3.547(s) (112), 3.212(vw) (041), 3.101(s) (300), 2.597(w) (013), 2.469(m) (331), 2.214(vw)(420), 2.098(vw) (260), 2.014 (vw) (402), 1.863(w) (500), 1.664(w) (314), 1.554(vw) (600), 1.525(m) (601), 1.405(m) (0.10.0). DTA curve shows the endothermic peaks at $250-370^{\circ}C$ and $955^{\circ}C$. The former is due to the dehydration: and oxidation forming$(Mn,\;Fe)_2O_3$(cubic, a $9.417{\AA}$), and the latter is interpreted as the formation of a hausmannite-type oxide (tetragonal, a 5.76, c $9.51{\AA}$) from $(Mn,\;Fe)_2O_3$. Infrared absorption spectral curve shows Mn-O stretching vibrations at $515cm^{-1}$ and $545cm^{-1}$, O-H bending vibration at $1025cm^{-1}$ and O-H stretching vibration at $3225cm^{-1}$. Opaque. Reflectance 13-15%. Bireflectance distinct in air and strong in oil. Reflection pleochroism changes from whitish to light grey. Between crossed nicols, color changes from yellowish brown with bluish tint to grey in air and yellowish brown to grey through bluish brown in oil. No internal reflections. Etching reactions: HCl(conc.) and $H_2SO_4+H_2O_2$-grey tarnish; $SnCl_2$(sat.)-dark color; $HNO_3$(conc.)-grey color; $H_2O_2$-tarnish with effervescence. It is black in color. Luster dull. Cleavage one direction perfect. Streak brownish black to dark brown. H. (Mohs) 2-3, very fragile. Specific gravity 3.59(obs.), 3.57(calc.). It occurs as radiating groups of flakes, flower-like aggregates, colloform bands, dendritic or arborescent masses composed of fine grains in the cementation zone of the supergene manganese oxide deposits of the Janggun mine, Bonghwa-gun, southeastern Korea. Associated minerals are calcite, nsutite, todorokite, and some undetermined manganese dioxide minerals. The name is for the mine, the first locality. The mineral and name were approved before publication by the Commission on New Minerals and Mineral Names, I.M.A.

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Molecular Structure of PCP Pincer Complexes: Poisoning Catalyst on the Dehydrogenation of Alkanes (알칸의 탈수소화반응에서의 촉매독 화합물의 분자구조)

  • Lee Ji Hyun;Chun Sang Jin;Kwon Ki Hyeok;Lee Do Weon
    • Korean Journal of Crystallography
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    • v.16 no.1
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    • pp.43-53
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    • 2005
  • The dihydrido P-C-P pincer complex, $IrH_2{C_6H_3-2,6-(CH_2PBu_2^t)_2}$ (1), was successfully prepared from the reaction of the hydrochloride complex, $IrClH (C_6H_3-2,6-(CH_2PBu_2^t)_2}$, and super acid $(LiBEt_3H)$ under 1 atm of hydrogen in pentane solution at room temperature and followed by Heating at $130^{\circ}C$ in vacuo. Jensen recently found that the dihydrido P-C-P pincer complex 1 is a highly active homogeneous catalyst for the transfer dehydrogenation of alkanes with unusual longterm stability at temperatures as high as $200^{\circ}C$. The treatment of dihydrido complex 1 with nitrogen, water, carbon dioxide, and carbon monoxide in presence of tert-butylethylene (the) at room temperature in an appropriate solution gave the dinitrogen complex, $[Ir{C-6H_3-2,6-(CH_2PBu_2^t)_2}]_2({\mu}-N_2)$ (2), the hydrido hydroxyl complex, $IrH(OH){C_6H_3-2,6-(CH_2PBu_2^t)_2}$ (3), the carbon dioxide complex, $Ir({\eta}^2-CO_2) {C_6H_3-2,6-(CH_2PBu_2^t)_2}$ (including the bicarbonate complex, $IrH({\kappa}^2-O_2COH){C_6H_3-2,6-(CH_2PBu_2^t)_2}\;(4))$, and the carbonyl complex, $Ir(CO) {C_6H_3-2,6-(CH_2PBu_2^t)_2}\;(5)$ (including the carboxyl complex, $IrH(C(O)OH) {C_6H_3-2,6-(CH_2PBu_2^t)_2}\;(6))$, in good yield, respectively. These P-C-P iridium complexes were isolated and characterized by $^1H,\;^{13}C,\;^{31}P\; NMR$, and IR spectroscopy. In addition, the complexes (1-6) were characterized by a single crystal X-ray crystallography. These complexes account for these small molecules' inhibition of dehydrogenation of alkanes catalyzed by the dihydrido complex 1.

Enhanced Production of Cellobiase by a Marine Bacterium, Cellulophaga lytica LBH-14, in Pilot-Scaled Bioreactor Using Rice Bran (파이롯트 규모에서 미강을 이용한 해양미생물 Cellulophaga lytica LBH-14 유래의 cellobiase 생산)

  • Cao, Wa;Kim, Hung-Woo;Li, Jianhong;Lee, Jin-Woo
    • Journal of Life Science
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    • v.23 no.4
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    • pp.542-553
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    • 2013
  • The aim of this work was to establish the optimal conditions for the production of cellobiase by a marine bacterium, Cellulophaga lytica LBH-14, using response-surface methodology (RSM). The optimal conditions of rice bran, ammonium chloride, and the initial pH of the medium for cell growth were 100.0 g/l, 5.00 g/l, and 7.0, respectively, whereas those for the production of cellobiase were 91.1 g/l, 9.02 g/l, and 6.6, respectively. The optimal concentrations of $K_2HPO_4$, NaCl, $MgSO_4{\cdot}_{7H2}O$, and $(NH_4)_2SO_4$ for cell growth were 6.25, 0.62, 0.28, and 0.42 g/l, respectively, whereas those for the production of cellobiase were 4.46, 0.36, 0.27, and 0.73 g/l, respectively. The optimal temperatures for cell growth and for the production of cellobiase by C. lytica LBH-14 were 35 and $25^{\circ}C$, respectively. The maximal production of cellobiase in a 100 L bioreactor under optimized conditions in this study was 92.3 U/ml, which was 5.4 times higher than that before optimization. In this study, rice bran and ammonium chloride were developed as carbon and nitrogen sources for the production of cellobiase by C. lytica LBH-14. The time for the production of cellobiase by the marine bacterium with submerged fermentations was reduced from 7 to 3 days, which resulted in enhanced productivity of cellobiase and a decrease in its production cost. This study found that the optimal conditions for the production of cellobiase were different from those of CMCase by C. lytica LBH-14.

La pensée sérieuse sur la mort et le sens métaphysique sur la mort chez Kierkegaard (키르케고르: 죽음에 관한 진지한 사유와 죽음의 형이상학적 의미)

  • Lee, Myung-gon
    • Journal of Korean Philosophical Society
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    • v.131
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    • pp.303-330
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    • 2014
  • Les avis des philosophes sur la mort sont $diff{\acute{e}}rentes$ selon leurs visions du monde. Certains essaient de surmonter la peur sur la mort, en $n{\acute{e}}gligeant$ la mort, et certains essaient de vivre le vraie vie par la $m{\acute{e}}ditation$ de la mort. Chez Kierkegaard la notion de la mort se $pr{\acute{e}}sente$ comme key-world $tr{\grave{e}}s$ important, et cela signifie qu'il parle par la mort une vie $s{\acute{e}}rieuse$ et vraie. Pour Kierkegaard la mort signifie d'abord la mort de la vie mondaine ou la $n{\acute{e}}gation$ de soi, cela est en faveur de sa conception de la nature humaine $o{\grave{u}}$ l'homme est fondamentalement un ${\hat{e}}tre$ $probl{\grave{e}}matique$ et ${\grave{a}}$ la fois ceuli qui a un rapport avec $l^{\prime}{\acute{e}}ternel$. Le $d{\acute{e}}sespoir$ de l'homme sur la vie $pr{\acute{e}}sente$ peut devenir 'la maladie qui entraîne la mort' c'est-${\grave{a}}$-dire la mort spirituelle, mais il peut donner aussi une chemin par laquelle l'homme se dirige en tant qu'individu vers l'Absolu. Chez lui ${\hat{e}}tre$ $s{\acute{e}}rieux$ signifie devenir existentiellement par la $n{\acute{e}}gation$ de soi. Et l'absence de la $sinc{\acute{e}}rit{\acute{e}}$ signifie l'absence de soi en tnat $qu^{\prime}{\hat{e}}tre$ spirituel. Ainsi la $pens{\acute{e}}e$ $s{\acute{e}}rieuse$ sur la mort $n^{\prime}{\acute{e}}tant$ autre chose que de penser la mort comme la partie de $l^{\prime}{\hat{e}}tre$ $pr{\acute{e}}sent$, elle devient la source ${\acute{e}}nergique$ qui permet de vivre pleinement le $pr{\acute{e}}sent$ comme $r{\acute{e}}alit{\acute{e}}$ $li{\acute{e}}$ ${\acute{a}}$ $l^{\prime}{\acute{e}}ternit{\acute{e}}$. Sa $pens{\acute{e}}e$ $s{\acute{e}}rieuse$ sur la mort permet d'avoir une conviction religieuse par laquelle l'homme peut penser la mort corporelle comme aventure $li{\acute{e}}e$ ${\grave{a}}$ $l^{\prime}{\acute{e}}ternit{\acute{e}}$ et par laquelle l'homme peut penser aussi la vie $apr{\grave{e}}s$ la mort comme vraie vie que les justes avaient $d{\acute{e}}sir{\acute{e}}s$. Cette $pens{\acute{e}}e$ de Kierkegaard sur la mort signifie le sens $m{\acute{e}}taphysique$ sur la mort au sens $o{\grave{u}}$ elle est une $r{\acute{e}}alit{\acute{e}}$ $v{\acute{e}}cue$, et aussi la $pens{\acute{e}}e$ qui ${\acute{e}}claircit$ la sagesse des philosophes antiques ${\grave{a}}$ la perspective $chr{\acute{e}}tienne$ qui dit philosopher, c'est apprendre ${\grave{a}}$ mourir.