• 한국대기환경학회지
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• 제29권5호
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• pp.642-655
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• 2013

In this study, semi-continuous measurements of $PM_{2.5}$ mass, organic and elemental carbon (OC and EC), black carbon (BC), and ionic species concentrations were made for the period of April 03~13, 2012, at a South Area Supersite at Gwangju. Possible sources causing the high concentrations of major chemical species in $PM_{2.5}$ observed during a haze episode were investigated. The measurement results, along with meteorological parameters, gaseous pollutants data, air mass back trajectory analyses and PSCF (potential source contribution function) results, were used to study the haze episode. Substantial enhancements of OC, EC, BC, $K^+$, $SO{_4}^{2-}$, $NO{_3}{^-}$, $NH{_4}{^+}$, and CO concentrations were closely associated with air masses coming from regions of forest fires in southeastern China, suggesting likely an impact of the forest fires. Also the PSCF maps for EC, OC, $SO{_4}^{2-}$, and $K^+$ demonstrate further that the long-range transport of smoke plumes of forest fires detected over the southeastern China could be a possible source of haze phenomena observed at the site. Another possible source leading to haze formation was likely from photochemistry of precursor gases such as volatile organic compounds, $SO_2$, and $NO_2$, resulting in accumulation of secondary organic aerosol, $SO{_4}^{2-}$ and $NO{_3}{^-}$. Throughout the episode, local wind directions were between 200 and $230^{\circ}C$, where two industrial areas are situated, with moderate wind speeds of 3~5 m/s, resulting in highly elevated concentration of $SO_2$ with a maximum of 15 ppb. The $SO{_4}^{2-}$ peak occurring in the afternoon hours coincided with maximum ambient temperature ($24^{\circ}C$) and ozone concentration (~100 ppb), and were driven by photochemistry of $SO_2$. As a result, the pattern of $SO{_4}^{2-}$ variations in relation to wind direction, $SO_2$ and $O_3$ concentrations, and the strong correlation between $SO_2$ and $SO{_4}^{2-}$ ($R^2=0.76$) suggests that in addition to the impact of smoke plumes from forest fires in the southeastern China, local $SO_2$ emissions were likely an important source of $SO{_4}^{2-}$ leading to haze formation at the site.

• KSBB Journal
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• 제10권1호
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• pp.63-70
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• 1995

실험실에서 자체 제작한 자유유통 전기이동 장치 에서 등전집속법을 이용한 대두 단백질의 분리를 통 해 운전 조건들이 분리에 미치는 영향을 조사하였 다. 매 실험마다 pH, 전기전도도, uv 흉광도 (280nm) 등을 측정하였고 시료의 순도는 SDS­P PAGE 분석을 통해 점검하였다. Tris와 boric acid로 처리한 대두단백질 추출액에 g glutamic acid, histidine, argmme, glycine 등 아 미노산 각 ImM과 dipeptide로 glycyl-glycine 2mM, 배경 전해액으로서 KCI ImM로 구성된 시료 의 완충액을 혼합하여 시료로 사용하였다. 분리막을 셀룰로오스 아세테이트를 사용할 경우 pH는 양극쪽에서 3, 음극쪽에서 8 정도의 값을 보였으며 2개의 변곡점을 나타내었다. 가해준 전압은 3 300V에서 lOOOV의 범위였으며 전압이 높을수록 더 나은 분리도를 얻었으나 전압을 더 높일 경우 과도한 Joule열의 발생으로 인해 한계가 있었다. 시간이 지남에 따라 단백질들은 분리조 중앙 부근에서 집속이 일어났으며 pH와 전기전도도의 변화로부터 분리 조내의 이온들이 막을 통해 전극쪽으로 이통해 가고 있음을 알 수 있었다. 완충용액의 농도를 5배로 증 가시킬 경우 300V에서 좋은 집속을 얻었으냐 10배 이상으로 농도를 높일 경우에는 분리조 입구와 출구 의 유체 온도차가 $25^{\circ}C$ 이상이 되어 단백질의 변성 이 일어날 수 있어 더 높일 수 없었다. 이온교환막을 사용할 경우 이온의 분극화현상을 일으켜 U자 형태 의 전기전도도 분포를 나타내었다. 아미노산 혼합물 대신 상용의 ampholyte를 사용하더라도 분리도에 있어 큰 차이가 없었다.

• 한국토양비료학회지
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• 제36권4호
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• pp.210-217
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• 2003

산화물에 대한 카드뮴의 흡착특성을 모사하기 위하여 토양에 존재하는 대표적 산화광물인 침철광과 석영을 대상으로 회분형 카드뮴 흡착실험을 수행하였다. 토양 광물에 대한 카드뮴의 흡착을 예측하기 위해 기존의 경험적 흡착모델 대신 표면착물 모델을 적용하였다. 모델을 검증하기 위하여 카드뮴의 흡착에 영향을 미치는 pH, 중금속 농도, 산화물 농도 및 이온강도 등의 인자를 조절하며, 다양한 조건하에서 회분형 흡착실험을 수행하였다. 실험결과, 카드뮴의 농도가 증가함에 따라 pH에 따른 흡착 곡선은 알칼리 쪽으로 평행하게 이동하였다. 흡착 실험으로부터 계산한 50%의 카드뮴이 흡착되는 pH인 $pH_{50}$은 합성 침철광이 5.25로 석영의 7.83에 비해 매우 낮아 카드뮴에 대한 표면 결합력이 석영에 비해 합성 침철광이 우세함을 시사하였고 이는 모델의 모사 결과와도 잘 부합하였다. 또한 배경전해질로 사용한 $KNO_3$의 이온강도는 카드뮴의 흡착에 영향을 미치지 않았다. 따라서 카드뮴은 산화광물 표면에 내부이온흡착 메커니즘에 의하여 흡착되는 것으로 판단할 수 있었다.

• 에너지공학
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• 제19권2호
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• pp.116-120
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• 2010

국내 집단에너지 사업의 대표적인 지역난방시스템은 전체 배관망이 약 3,000 km에 이르고 있다. 이러한 장거리 배관망을 통한 열수송에서는 마찰 저항으로 인해 많은 펌프동력이 필요하게 된다. 효율적인 장거리 열수송을 위한 연구로서 대표적인 방법 중 하나가 마찰저감제를 투입하는 것이다. 이러한 마찰저감제는 파이프내 표면의 마찰저항을 감소시킴으로써 유체의 유동을 향상시키게 되는 것이다. 본 연구에서는 친환경 계면활성제인 Amine Oxide $C_{18}$을 이용하여 $80{\sim}110^{\circ}C$의 온도범위에서 단기간 동안에 마찰저감 특성을 비교하고, 장기간 동안 퇴화현상을 비교 평가함으로써 향후 지역난방 시스템에서 적용 가능성을 평가하기 위하여 지역 난방시스템을 축소하여 실험장치를 제작하였다. 마찰저감제를 첨가하지 않은 파이프내의 차압과 마찰저감제를 첨가하였을때의 차압을 비교하여 마찰저감율을 측정하였다. 단기성능 실험결과 마찰저감제는 온도의 영향을 받아 유체의 온도가 높아질수록 마찰저감율이 낮게 나타났다. $80^{\circ}C$의 실험에서 최대 30%의 마찰저감율이 나타났으며, $100^{\circ}C$ 이상에서는 마찰저감율이 감소하여 약 15%의 마찰저감율을 보였다. 장기성능 실험결과 $80^{\circ}C$의 실험에서는 1000 ppm 0.8 m/s의 유속에서 마찰저감율의 지속시간이 155시간동안 유지되었으며 온도가 높아질수록 지속시간이 감소하였다.

• 대한수의학회지
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• 제38권2호
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• pp.280-289
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• 1998

Voltage-sensitive ion channels contribute to establishment of the cell excitablity and the generation of the cellular function. At hamster oocytes in the primitive stage during developing process, an inward current elicited by voltage pulses was found to be carried mainly by $Ca^{2+}$. Even at present, $Ca^{2+}$ channels serve as the most probable route to pass this inward current but there is no evidence of the presence of this channels in eggs. To date, both the characteristic properties and the physiological role in the early stage of development remain unclear. Here we examined the characteristic properties of the inward current and changes in this currents at unfertilized oocytes, fertilized zygotes and two-cell embryos using whole-cell voltage clamp technique. The inward current carried reportedly by $Ca^{2+}$ was remained following removing external $Ca^{2+}$ but completely abolished by further replacement of impermeants such as tetramethylammonium ion ($TMA^+$) or $choline^+$ instead of $[Na^+]_0$. Tetrodotoxin did not affect on this inward current remained at $[Ca^{2+}]_0$-free condition. Removal of $Na^+$ ion out of the experimental solution clearly decreased the current. After adding 2mM $Ca^{2+}$ to the $Na^+$-free media, the inward current was restored. Interestingly, this current carried by either $Ca^{2+}$ or $Na^+$ was decreased by the reduction of intracellular $Cl^-$ concentration, or by $Cl^-$ channel blockers such as niflumic acid, DIDS and SITS. When $Cl^-$ concentration was lowered without changes in other ionic components, this inward current was reduced. At fertilized oocytes and two-cell embryos, the inward current carried by $Ca^{2+}$ and $Na^+$ was severely reduced. Also $Cl^-$ component could not be observed. From these results, the inward current is composed of $Ca^{2+}$, $Na^+$ and $Cl^-$ component, suggesting that the channel carrying this inward current is not selective specifically to $Ca^{2+}$. During early stage of development, the voltage-sensitive ion current seems not to contribute essentially to the cell cleavage and differentiation. The loss of $Cl^-$ component after fertilization suggests that $Cl^-$ may play a role in maintaining the viability of unfertilized ova.

• 대한수의학회지
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• 제43권1호
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• pp.31-39
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• 2003

We have investigated the effect of extracellular $Mg^{2+}$ ($[Mg^2+]_o$) on action potential duration (APD) in guinea pig papillary muscles by using microelectrodes. Increasing $[Mg^2+]_o$ resulted in progressive negative inotropic effect, progressive ascending depolarization of membrane potential, and increase in intracellular $Mg^{2+}$ concentration. In addition, increase in $[Mg^2+]_o$ from 1.1 to 3, 6, 10, and 20 mM produced a reversible dose-dependent shortening of both APD at 30% ($APD_{30}$) and 90% repolarization ($APD_{90}$), especially showing a tendency towards more remarkable prominent shortening in $APD_{30}$ than $APD_{90}$. Cooling from 37 to 33 and $27^{\circ}C$ diminished the $[Mg^2+]_o$-induced APD shortening. Increase in extracellular $Ca^{2+}$ concentration from 1.8 to 3.6 and 5.4 mM caused a significant depressed effect on the increasing $[Mg^2+]_o$-induced APD shortening. Furthermore, increase in $[Mg^2+]_o$ from 1.1 to 10 and 20 mM produced a significant depressed effect on the APD shortening induced by extracellular $Ca^{2+}$. Pretreatment of verapamil and imipramine significantly attenuated the increasing $[Mg^2+]_o$-induced APD shortening in both $APD_{30}$ and $APD_{90}$, whereas the $[Mg^2+]_o$-induced APD shortening was not affected by strophanthidin, glibenclamide and tetrabutylammonium. These findings suggest that the effects of $[Mg^2+]_o$ on APD are probably due to a decrease in ionic transport across plasma membrane. In conclusion, the present study indicates that $[Mg^2+]_o$ exerts antiarrhythmic activities by antagonistic actions on intracellular $Ca^{2+}$.

• 멤브레인
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• 제18권4호
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• pp.261-267
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• 2008

Poly(vinyl chloride) (PVC) 주사슬과 poly(hydroxyethyl acrylate) (PHEA) 곁사슬로 구성된 가지형 공중합체를 원자전달라디칼 중합을 통해 합성하였다. PVC의 2차 염소원자의 직접적인 개시반응에 의해 친수성인 PHEA 단량체를 그래프팅시켰다. 이렇게 합성된 PVC-g-PHEA을 술포석시닉산(SA)를 사용하여 가교시켰으며, 이는 가지형 공중합체의 -OH 그룹과 SA의 -COOH와의 에스테르 반응임을 FT-IR 분광법을 이용하여 분석하였다. 이온교환능(IEC)은 SA 함량이 증가함에 따라 계속하여 증가하여 0.87 meq/g까지 도달하였고, 이는 전해질막에 이온 그룹수가 증가하기 때문이다. 하지만, 함수 율은 SA 함량이 20 wt%까지는 증가하다 그 이상에서는 감소하였다. 또한 수소 이온 전도도도 SA 함량에 따라 증가하여 20 wt% SA 농도에서 0.025 S/cm의 최대값을 나타내었고, 이는 SA 함량이 증가함에 따라 이온 그룹의 수가 증가하는 효과와 가교가 증가하는 효과가 서로 경쟁적으로 일어나기 때문으로 사료된다.

• 대기
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• 제27권1호
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• pp.29-40
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• 2017

The $PM_{10}$ and $PM_{2.5}$ particles over the Yellow Sea of Korea were collected by ship-borne observation during two cruises in spring, 2015. Their water-soluble ionic components such as $NH_4^+$, $Na^+$, $K^+$, $Mg^{2+}$, $Ca^{2+}$, $SO_4^{2-}$, $NO_3^-$, $Cl^-$, $F^-$, $CH_3COO^-$, $HCOO^-$, and $CH_3SO_3^-$ were analyzed, in order to examine the pollution characteristics of the secondary aerosol components. The comparative study of particle size distribution has resulted that $NH_4^+$, $nss-SO_4^{2-}$, $nss-Mg2+$, $nss-K^+$, $HCOO^-$, and $CH_3SO_3^-$ species mostly existed in fine particle mode. Meanwhile, nss-F-and sea-salt species were distributed in both fine and coarse particle mode, $NO_3^-$, $nss-Ca^{2+}$, $CH_3COO^-$ species were rich in coarse particle mode. The concentrations of secondary pollutants($nss-SO_4^{2-}$, $NO_3^-$, $NH_4^+$) increased in fine particles, and those of natural components ($nss-Ca^{2+}$, Sea-salt) increased in coarse particles. $NH_4^+$ exists as the form of $(NH_4)_2SO_4$ and $NH_4NO_3$, and mostly as $(NH_4)_2SO_4$ in fine particles. $NH_4NO_3$ has lower content compared to $(NH_4)_2SO_4$, and it mostly existed in fine particles at Yellow Sea I and in coarse particles at Yellow Sea II. The concentration ratios of $NO_3^-/nss-SO_4^{2-}$ for Yellow Sea I and Yellow Sea II were 0.52 and 0.16 in coarse particles, and they were 0.64 and 0.38 in fine particles, respectively, showing that the stationary source emissions were more important than mobile source emissions in Yellow Sea II (except Passage II-4).

• 한국응용과학기술학회지
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• 제7권1호
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• pp.93-105
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• 1990

Semicarbazone formation of nine monosubstituted benzaldehydes was studied kinetically in 20% methanol buffer solution at 15, 25, 35, and $45^{circ}C$. The rate of p-nitrobenzaldehyde semicarbazone formation is 2.7 times as fast as that of benzaldehyde, while p-hvdroxybenzaldehyde is 3.6 times as slow as that of benzaldehyde. Activation energies for p-chlorobenzaldehyde, benzaldehyde, p-methylbenzaldehyde, p-methoxybenzaldshyde, p-hydroxybenzaldehyde, and p-dimethylaminobenzaldehyde semicarbazone formation are calculated as 5.80, 6.19, 6.57, 7.06, 8.03, and 6.46 kcal/mol respectively. It is concluded from the effect of ionic strength that the reaction is affected by not ions but neutral molecules involving hydrogen bonding between oxygen atom of carbonyl group and hydrogen atom of acid-catalyst, and concerted attack of the necleophilic reagent, free base on carbonyl compound. Also, the effect of solvent composition is small in 20% and 50% methanol (and ethanol) aqueous solutions. The ${\rho}-{\sigma}$ plots for the rates of semicarbazone formation at pH 7.1 show a linear ${\rho}-{\sigma}$ relationship (${\rho}=0.14l$, in contrast to that at pH 2.75 and pH 5.4 corresponding to ${\rho}-{\sigma}$ correlations reparted by Jencks. The rate of semicarbazone formation at pH 5.4 show a relationship which is convex upward, resulting in a break in the curve but at pH 2.75, slight difference from a linear relationship. As a result of studying citric acid catalysis, second-order rate constants increase linearly with citric acid concentration and show a 2 times increase as the catalyst concentration is varied from 0.025 to 0.1 mol/1 at pH 2,9, but slight increase at pH 5.3. The rate-determining step is addition below pH 5 but is dehydration between pH 5 and 7. Conclusively, the rate-determining step of the reaction changes from dehydration to addition in respect to hydrogen ion activity near pH 5. The ortho: para rate ratio of the hydroxybenzaldehydes for semicarbazone formation is about 17 at $15^{\circ}C$. It is concluded that the results constitute strong evidence in favor of greater stabilization of p- than o-hydroxybenzaldehyde by substituent which donate electrons by resonance and is due to hydrogen bonding between the carbon-bound hydrogen of the-CHO group and the oxygen atom of the substituent.

• 한국대기환경학회지
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• 제22권4호
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• pp.459-467
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• 2006

This study was carried out to characteristics and distributions of acid deposition in Korea. Precipitation was collected by acid deposition monitoring networks and analyzed for pH, conductivity, and following major ionic components $SO_4^{2-}$, $CI^-$, $NO_3^-$, $NH_4^+$, $Na^+$, $K^+$, $Ca^{2+}$, $Mg{2+}$. During the investigation period, Volume weighted annual mean pH of precipitation in Korea is 4.8, showing slightly acidic level. The amount of rainfall in the range of pH 5.1$\sim$5.5 charged approximately 28% of annual precipitation,23.4% in pH 4.6$\sim$5.0, and contributed 16.2% under pH 4.5. Among seasons, alkaline precipitation has occurred more often in spring, meanwhile acidic precipitation in which pH is under 4.5 has frequently occurred in autumn. Volume weighted annual mean concentrations of $SO_4^{2-}$, $NO_3^-$, $CI^-$ are 2.558 mg/L, 1.590 mg/L, 1.286 mg/L respectively, and provided that $SO_4^{2-}$, is the major contributor, followed by $NO_3^-$, $CI^-$. In case of cation, annual mean concentration for $NH_4^+$, $Na^+$, $K^+$, $Ca^{2+}$, $Mg{2+}$, $H^+$ are 0.693 mg/L, 0.528 mg/L, 0.439 mg/L, 0.455 mg/L, 0.089 mg/L,0.015 mg/L, and $NH_4$ were decided as the main contributor, followed by $Na^+$, $K^+$, $Ca^{2+}$, $Mg{2+}$, $H^+$. Annual wet deposition rate for sulfate, nitrate and ammonia are $3.316gm^{-2}yr^{-1}$, $2.057gm^{-2}yr{-1}$, $0.894gm^{-2}yr{-1}$, respectively, and it was founded that the deposition flux in summer contributes about 38.42% to 67.62% to total deposition.