• Journal of Microbiology and Biotechnology
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• 제10권1호
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• pp.69-74
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• 2000

The medium for erythritol production by Torula sp. in a 500-ml baffled flask was optimized to be 300 g/I sucrose, 10 g/I yeast extract, 3 g/I $KH_2PO_4$, and 10 mg/I $CuSO_4{\cdot}5H_2O{\;}at{\;}34^{\circ}C$ with initial pH of 5.5. Using this optimal medium, erythritol of 166 g/I was obtained after 140 h of cultivation, corresponding to 55.3% of the erythritol yield from sucrose with a productivity of 1.11 g/I/h. Optimal concentrations of carbbon and nitrogen sources in a fermentor were higher than that in a flask due to the higher oxygen supply of the fermentor. Employing the medium containing 300 g/I or 400 g/I sucrose for the determination of optimal C/N ratio, the C/N ratio was found to be more important than the nitrogen concentration for effective erythritol production, The optimal ratio of yeast extract to sucrose (g/g) was 20. The yield and productivity of erythritol were maximal in the medium containing 400 g/I sucrose and 20 g/I yeast extract. when dissolved oxygen in the culture was increased, the cell mass increased but the erythritol production was manimal in the range of 5 to 10% of dissolved oxygen. Under the optimal the rane of 5 to 10% of dissolved oxygen. Under the optimal culture condition of the fermentor, a final erythritol concentration of 200 gI was obtained after 120 h with a yield of 50% and the productivity was 1.67 g/I/h. The yield was the highest among erythritol-producting microorganisms

• 한국재료학회지
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• 제19권7호
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• pp.349-355
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• 2009

Metal thin film patterns on a LTCC substrate, which was connected through inner via and metal paste for electrical signals, were formed by a screen printing process that used electric paste, such as silver and copper, in a conventional method. This method brought about many problems, such as non uniform thickness in printing, large line spaces, and non-clearance. As a result of these problems, it was very difficult to perform fine and high resolution for high frequency signals. In this study, the electric signal patterns were formed with the sputtered metal thin films (Ti, Cu) on an LTCC substrate that was coated with protective oxide layers, such as $TiO_2$ and $SiO_2$. These electric signal patterns' morphology, surface bonding strength, and effect on electro plating were also investigated. After putting a sold ball on the sputtered metal thin films, their adhesion strength on the LTCC substrate was also evaluated. The protective oxide layers were found to play important roles in creating a strong design for electric components and integrating circuit modules in high frequency ranges.

• Journal of Nutrition and Health
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• 제40권2호
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• pp.111-117
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• 2007

시판 목초액 A (원액 35%)을 사용하여 음용수에 0%, 1.0%, 25.0%, 50.0%, 75.0%가 되도록 조제한 다음, CD계 수컷 흰쥐 (150 ${\pm}$ 10 g)에 2개월 동안 조제사료와 함께 자유 음용케 하여 간조직 중의 활성산소로서 수퍼옥시드 라디칼(O$_{2}\;^-$), 히디록시 라디칼, 과산화수소 및 제거효소로서 수퍼옥시드 디스무타아제 (SOD), 글루타치온 퍼옥시다아제 (GPx) 및 카탈라아제 (CAT)에 미치는 영향을 평가하였다. 목초액 PL-25 및 PL-50 투여군의 간조직의 미토콘드리아 획분에서는 O$_{2}\;^-$의 생성량은 대조군 대비 12${\sim}$14%의 O$_{2}\;^-$의 생성량 억제효과가 나타났고, 간조직의 마이크로솜획분에서는 대조군 대비 각각 11.0${\sim}$15.0의 O$_{2}\;^-$의 생성량 억제효과가 나타났다. 간조직 미토콘드리아획분에서 ${\cdot}$OH 생성량이 목초액 PL-25 및 PL-50 투여군에서 대조군 대비 12${\sim}$20%의 ${\cdot}$OH 생성 억제효과가 나타났고, 간조직의 마이크로솜획분에서는 대조군 대비 17${\sim}$20%의 ${\cdot}$OH 생성 억제효과가 나타났다. 목초액 PL-25 및 PL-50 투여군의 간조직의 미토콘드리아획분에서는 대조군 대비 12${\sim}$15%의 유의적인 H$_{2}$O$_{2}$의 생성 억제효과가 나타났고, 간조직의 마이크로솜획분에서는 대조군 대비 20${\sim}$22%의 상당히 유의적인 H$_{2}$O$_{2}$의 생성 억제효과가 나타났다. 목초액 PL-25 및 PL-50 투여군의 간조직의 Mn-SOD 활성은 대조군 대비 15${\sim}$25%나 유의적인 활성 증가효과가 인정되었고, 간조직의 Cu/Zn-SOD 활성은 대조군 대비 11${\sim}$16%의 유의적인 SOD활성 증가효과가 인정되었다. 목초액 PL-25 및 PL-50 투여군의 간조직의 미토콘드리아획분의 GPx 활성은 대조군 대비 10${\sim}$17%의 GPx 활성 증가효과가 인정되었고, 간조직의 마이크로솜획분의 GPx 활성 증가효과가 인정되었다. 목초액 PL-25 및 PL-50 투여군의 간조직의 미트콘드리아획분의 CAT 활성은 대조군 대비 12${\sim}$14%의 유의적인 CAT 활성 증가효과가 나타났고, 간조직의 시토졸 1획분에서는 대조군 대비 15${\sim}$27%의 CAT 활성 증가효과가 인정되었다. 이상의 결과에서 목초액의 장기간 투여는 간조직 중의 활성산소의 억제효과뿐만 아니라 방어시스템으로서 활성산소 제거효소의 역할도 충실히 수행하여 노화를 효과적으로 예방하고 억제할 수 있을 것으로 기대된다.

• 한국해양학회지:바다
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• 제24권4호
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• pp.519-534
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• 2019

여름철 인공호수(간월호, 부남호)로 부터의 담수방류시 천수만 수질(영양염, 유기물, 미량금속)에 미치는 영향을 평가하기 위해 2011년 6, 7, 8, 10월에 평상시와 담수방류 시기 각 2회씩의 해수를 채취하였다. 담수가 방류되면 용존 무기 질소(DIN)의 농도가 만내의 모든 수층에서 약 3-4배 증가하였고, 평상시 암모니아성 질소(NH₄⁺-N)가 우세하다가 담수방류시 질산성 질소(NO₃^--N)가 우세하였다. 용존 무기인(DIP)의 경우 내만 표층에서 절반으로 감소하였고 저층에서는 1.5배 증가하였으며 규산염(Si(OH)₄)은 내만 저층에서 2배 증가하는 모습을 보였다. Redfield ratio는 담수 방류시 인 제한 환경으로 바뀌었다. 용존 유기 탄소(DOC) 및 질소(DON)는 약 2배 증가하였고, 입자상 유기 탄소(POC), 질소(PON), 인(POP) 및 생물기원 규소(Bio-SiO₂)는 내만 표층에서 약 2배 이상 증가했다. 용존 금속(Fe, Co, Ni, Cu)은 내만의 표층에서 증가하였으나, 용존 Cd의 경우 만의 표층에서 절반으로 감소하였다. 이와 같은 결과로 미루어 볼 때 영양염, 유기물 및 금속 농도가 높은 인공호수의 물이 만으로 유입되면, 천수만 내의 영양염 및 용존 유기물, 금속농도가 증가하고, 식물플랑크톤 대증식이 발생하여 표층에서 산소 과포화, 저층에서 빈산소를 발생시킨다. 빈산소와 함께 내만의 저층에서는 매우 높은 농도의 영양염(DIN, DIP, Si(OH)₄) 농도가 존재하였다. 수질 평가 지수값을 통해 천수만의 부영양화 정도를 평가한 결과, 평상시에는 3등급 이하로 나타나다가 방류시 5등급으로 바뀌게 됨을 알 수 있었다.

• Bulletin of the Korean Chemical Society
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• 제32권9호
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• pp.3223-3228
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• 2011

To quantify the presence of mercuric ions in aqueous solution, double-stranded DNA (dsDNA) of poly(dT) was employed using a light switch compound, $Ru(phen)_2(dppz)^{2+}$ (1) which is reported to intercalate into dsDNA of a right-handed B-form. Addition of mercuric ions induced the dehybridization of poly(dT)${\cdot}$poly(dA) duplexes to form a hairpin structure of poly(dT) at room temperature and the metal-to-ligand charge transfer emission derived from the intercalation of 1 was reduced due to the dehybridization of dsDNA. As the concentration of $Hg^{2+}$ was increased, the emission of 1 progressively decreased. This label-free emission method had a detection limit of 0.2 nM. Other metal ions, such as $K^+$, $Ag^+$, $Ca^{2+}$, $Mg^{2+}$, $Zn^{2+}$, $Mn^{2+}$, $Co^{2+}$, $Ni^{2+}$, $Cu^{2+}$, $Cd^{2+}$, $Cr^{3+}$, $Fe^{3+}$, had no significant effect on reducing emission. This emission method can differentiate matched and mismatched poly(dT) sequences based on the emission intensity of dsDNA.

• 자원환경지질
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• 제33권3호
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• pp.181-193
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• 2000

This study was undertaken to evaluate the drinking water quality based on physicochemical properties and chemical compositions of the supply water in the Daedeok Campus, and to verify the analytical reliabilities of ICP-MS and IC equipped in the Central Research Facilities at Chungnam National University , Korea. The supply water belongs to $Ca^{2+}-({HCO_3}^-+{SO_4}^{2-})$type, whereas the original water from the Daecheong lake belongs to $(Ca^{2+}-(Mg^{2+})-{HCO_3}^-$ type. Generally, temperature (14.1$^{\circ}C$), pH (6.95), Eh (0 mV), electrical conductivity (117${\mu}$S/cm) and TDS (86.975mg/l) of supply water were higher than those of original lake water . Results using WATEQ4F revealed that potentially toxic ions of the supply water might exist mainly as free metals ($M^{2+}$) and a small amount as ${CO_3}^{2-}$ and $OH^-$ complexes. Also, the water composition belongs to the kaolinite field. Calculated average enrichment indies of the supply water normalized to lake water for anions, mamor cations, toxic cations and total ions are 1.05 , 1.56, 13.05 and 1.17 , respectively. Those values of the ground water in the Daedeok Campus showed 1.71, 4.78, 5.71 and 2.49 , respectively. However , contents of all constituents of these water are within the drinking water standard. All samples were filtered before the chemical analysis. Pale yellow or yellowish brown colored materials of colloidal particles coated the filter paper to thickness of 0.02 to 0.2mm. these are mainly Fe-Cy-Zn compounds with traces of Ni and Pb, the net weights of which compounds range from 0.01to 3.20mg/l. Most elements did not show any conceivable filtering effect of Cu, Fe and Zn. Especially, mean concentration of total Fe decreased considerably from 168.52${\mu}g$/lto 42.58${\mu}g$/l by filtering .

• 자원환경지질
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• 제32권6호
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• pp.611-631
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• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 광물과 암석
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• 제35권2호
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• pp.125-140
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• 2022

Xiquegou 연-아연 광상은 중국 동북지역에선 가장 규모가 큰 연-아연 광화대 중의 하나인 Qingchengzi orefield에 위치한다. 이 광상의 주변지질은 시생대의 그래뉼라이트(granulite)와 이를 관입한 고원생대의 미그마타이트질 화강암과 고-중원생대의 소딕(sodic) 화강암을 부정합으로 피복한 고원생대의 Liaohe 층군 및 이들을 관입한 중생대의 섬록암과 몬조나이틱 화강암으로 구성된다. 이 광상은 고원생대의 Liaohe 층군내 Dashiqiao 층의 unit 3(돌로마이트질 대리암과 편암)내에 발달된 단층대를 따라 산출되는 맥상 광체로 트라이아스기의 마그마-열수형 광상에 해당된다. Xiquegou 연-아연 광상에서 석영, 인회석, 방해석, 황철석, 유비철석, 자류철석, 백철석, 섬아연석, 황동석, 황석석, 방연석, 사면동석, 에렉트럼, 휘은석, 자연은 및 농홍은석 등이 산출되며 모암변질로는 규화작용, 황철석화작용, 돌로마이트화작용, 녹니석화작용 및 견운모화작용 등이 관찰된다. 이 광상의 산출 광물조합 및 정출순서를 기초로, 돌로마이트는 1)모암인 돌로마이트(D₀) 및 2)연-아연 광화작용에 따른 모암변질 산물인 돌로마이트(D₁)로 두 유형이 확인된다. 이들 돌로마이트의 화학조성은 각각 Ca_1.03-1.01Mg_0.95-0.83 Fe_0.12-0.02Mn_0.02-0.00(CO₃)₂(D₀) 및 Ca_1.16-1.00Mg_0.79-0.44Fe_0.53-0.13Mn_0.03-0.00As_0.01-0.00(CO₃)₂(D₁)로써 이론적인 돌로마이트의 화학조성보다 미량원소들의 함량이 높다. 특히, FeO, PbO, Sb₂O₅ 및 As₂O₅ 원소들은 모암변질 산물인 돌로마이트(D₁)에서 높은 함량을 갖는다. 또한 이 광상의 모암에서 산출되는 돌로마이트(D₀)는 Ferroan 돌로마이트에 해당되며 모암변질 산물인 돌로마이트(D₁)는 철백운석 및 Ferroan 돌로마이트에 해당된다. 모암변질 산물인 녹니석의 화학조성은 (Mg_1.65-1.08Fe_2.94-2.50Mn_0.01-0.00Zn_0.01-0.00Ni_0.01-0.00Cr_0.02-0.00V_0.01-0.00Hf_0.01-0.00Pb_0.01-0.00Cu_0.01-0.00As_0.03-0.00Ca_0.02-0.01Al_1.68-1.61)_5.77-5.73(Si_2.84-2.76Al_1.24-1.16)_4.00O₁₀(OH)₈로써 이론적인 녹니석과 유사하며 Fe-rich 녹니석에 해당된다. 또한 이 녹니석의 화학조성 변화는 주로 팔면체적 Fe²⁺ <-> Mg²⁺ (Mn²⁺) 치환과 일부 팬자이틱 또는 Tschermark 치환(Al^3+,VI+Al^3+,IV <-> (Fe²⁺ 또는 Mg²⁺)^VI+(Si⁴⁺)^IV)메카니즘에 의해 일어났음을 알 수 있다.

• 동아시아식생활학회지
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• 제22권3호
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• pp.365-370
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• 2012

Proximate composition, reducing sugar, and mineral content of several cultivars of Rehmannia glutinosa were analyzed. the moisture and soluble solid content of fresh Rehmannia glutinosa ('Korea', 'Kokang', 'Sewon 10', 'Sewon 11' and 'Jihwang 1') were 74.6~78.4% and $19.6{\sim}22.4^{\circ}Brix$, respectively. Proximate composition of dried Rehmannia glutinosa ranged from 82.91~86.94% carbohydrate, 3.38~5.70% crude protein, 2.5~3.0% crude ash and 3.47~3.80% fiber. Sugar composition by HPLC/ELSD showed that sucrose (4.49~7.75 g/100 g), raffinose (2.96~4.78 g/100 g) and stachyose (42.36~45.87 g/100 g) were present, whereas monosaccharides were not detected in 5 cultivars of dried Rehmannia glutinosa. Mineral compositions of dried Rehmannia glutinosa by ICP-AES were Ca (639.9~782.0 ppm), Fe (128.5~634.9 ppm), Na (119~150 ppm), K (6,639.1~10,448.0 ppm), Mg (372.2~981.8 ppm) and Zn (8.8~474.2 ppm). However, Co and Mo were not detected. Among 5 cultivars of Rehmannia glutinosa, 'Kokang' and 'Sewon 10' contain higher amounts of Fe, Ca, K, Mg, Cu and Zn than the other cultivars.

• 대한화학회지
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• 제59권3호
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• pp.215-224
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• 2015

Unsymmetrical tetradentate Schiff base N-(2-hydroxy-5-methylacetophenone)-N'-(2-hydroxy acetophenone) ethylene diamine (H₂L) and its complexes with Cr(III), Mn(II), Fe(III), Co(II), Ni(II) and Cu(II) have been synthesized and characterized by elemental analyses, magnetic susceptibility measurements, IR, electronic spectra and thermogravimetric analyses. ¹H, ¹³C-NMR and FAB Mass spectra of ligand clearly indicate the presence of OH and azomethine groups. Elemental analyses of the complexes indicate that the metal to ligand ratio is 1:1 in all complexes. Infrared spectra of complexes indicate a dibasic quadridentate nature of the ligand and its coordination to metal ions through phenolic oxygen and azomethine nitrogen atoms. The thermal behavior of these complexes showed the loss of lattice water in the first step followed by decomposition of the ligand in subsequent steps. The thermal data have also been analyzed for the kinetic parameters by using Horowitz-Metzger method. The dependence of the electrical conductivity on the temperature has been studied over the temperature range 313-403 K and the complexes are found to show semiconducting behavior. XRD and SEM images of some representative complexes have been recorded. The antimicrobial activity of the ligand and its complexes has been screened against various microorganisms and all of them were found to be active against the test organisms. The Fe(III) and Ni(II) complex have been tested for the catalytic oxidation of styrene.