• 대한환경공학회지
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• 제30권2호
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• pp.225-233
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• 2008

지구 온난화에 대한 기여도가 50% 이상인 CO$_2$를 제어하려는 국제적 관심에 따라 CO$_2$ 제어에 대한 새로운 기술개발이 진행되고 있다. 따라서 본 연구에서는 PVA함량 및 소성온도에 따라 흡수제를 제조하여 고정층에서 CO$_2$ 흡수/재생 연속 실험 및 SO$_2$ 농도에 관한 실험을 수행하였다. 연구 결과, 비표면적은 832.79 m$^2$/g로 나타났고, SEM 측정결과 미세기공이 발달하여 건식흡수제로서의 가능성을 보였으며, CO$_2$ 흡수/재생 연속 실험에서는 SO$_2$ gas가 존재할 경우 부반응물질인 $Na_2SO_3$와 $Na_2SO_4$생성으로 CO$_2$ 흡수능 저하를 보였다.

• 대한화학회지
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• 제31권4호
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• pp.359-363
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• 1987

초음파(50KHz)가 상온 상압하에서 $BaMnO_4$ 및 $KMnO_4-CuSO_4{\cdot}5H_2O$를 이용한 1차, 벤질, 2차 알코올의 알데히드 및 케톤 생성반응을 가속 완결시켰으며 고속교반이나 가열 환류반응보다 높은 산화율을 주었다.

• 한국환경과학회지
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• 제9권2호
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• pp.145-149
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• 2000

The purpose of this study was to determine whether Vermi Cast could be used effectively to remove $SO_2$ from flue gas, and then to investigate optimum adsorption conditions. The Vermi Cast used as adsorbent was mechanically screened with 8~20 mesh sieve. The adsorption data for $SO_2$ were regressed using the Freundlich isotherm. The fit was generally satisfactory ($R^2$=0.945~0.982). With the temperature changes from 2$0^{\circ}C$ to 4$0^{\circ}C$, the constant k in Freundlich isotherm qe= $kCe^{1/n}$, decreased from 1.409 at 2$0^{\circ}C$to 0.297 at 4$0^{\circ}C$, and the exponent 1/n were decreased from 0.343 to 0.134. With the bed depth changes from 10cm to 30cm, the adsorption capacity expressed as mmol of $SO_2$ adsorbed per g of Vermi Cast increased from 0.247 to 0.381. Moisture content is an important parameter in the $SO_2$ adsorbed were observed over 0.3mmol $SO_2$ /g Vermi Cast. The best adsorption capacity was 0.487mmol $SO_2$ /g Vermi Cast, and it was obtained with moisture content 37%, temperature 2$0^{\circ}C$. From the above results, ti might be concluded that Vermi Cast is effectively as a good adsorbent to remove $SO_2$ from flue gas.

• Bulletin of the Korean Chemical Society
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• 제31권4호
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• pp.1077-1080
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• 2010

• 대한수학회논문집
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• 제11권4호
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• pp.1055-1059
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• 1996

We characterize the left invariant Riemannian metrics on SO(1,2) which give rise to 3- or 4-dimensional isometry groups.

• Journal of Life Science
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• 제12권2호
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• pp.47-52
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• 2002

Saccharomyces cerevisiae KNU5377 (KNU5377) and S. cerevisiae ATCC24858 (ATCC24858) were exposed to $H_2SO_4$ as a stress, which was added at various concentrations to a YPD media. The growth of KNU5377 was reduced to approximately 60% in the YPD media containing 40 nm sulfuric acid when compared to the non-stressed condition. When their growth was monitored during an overnight culture, two strains, KNU5377 and ATCC24858, could not grow when exposed to over 50 mM of sulfuric acid. After a short exposure to this acid for 1 h, KNU5377 exhibited stronger resistance against $H_2SO_4$ than ATCC24858. The neutral trehalase activity of KNU5377 unchanged despite under various concentrations of $H_2SO_4$. In contrast, It at of ATCC24858 was much low at higher $H_2SO_4$concentrations. Trehalose, a non-reducing disaccharide, was maximally accumulated after a short exposure to 60 nm $H_2SO_4$ for KNU5377, but it was reduced under more severe stressful conditions. These results suggest that KNU5377 should modulate the trehalose concentrations under the severe stress condition of high sulfuric acid concentrations. The most highly induced protein in the KNU5377 exposed to sulfuric acid was found to be an approximately 23 kDa protein, which was revealed to be the 605 large subunit ribosomal protein, Ll3 by FASTA search results.

• 한국대기환경학회지
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• 제9권2호
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• pp.147-153
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• 1993

From March 1990 to August 1991, every each 5mm bulk precipitation samples were collected at one residental area in Taejon City to investigate chemical characteristics of acid rain. Major ion concentrations of rain samples $(pH, SO_4^{2-}, NO_3^-, CL^-, NH_4^+, Na^+, K^+, Ca^{2+}, Mg^{2+})$ were analysed and compared with the concentration of air pollutants (T. S. P, $SO_2, NO_x$) that were measured by Ministry of Environment. The results of statistical analysis are as followings. Rain pH was relatively high on October and January and relatively low on August, November and February. Major anion is sulfate, and it's concentration is 2.36 times higher than nitrate's, and major cations are ammonium, sodium and calcium ion. Monthly variation of sulfate and calcium concentrations are higher than the others. Ion concentration and rain pH were correlated negatively with rainfall amount. Major ions in rain samples were $SO_4^{2-}, NO_3^-, NH_4^+, Ca^{2+}$ and regression equations are proposed by multiple regression of measured data. Also, regression equation between air pollutants(T. S. P, $SO_2$) and $SO_4^{2-}, Na^+, K^+, Ca^{2+}, Mg^{2+} ions in rain samples were made. From this wer can predict rain pH.

• 한국수소및신에너지학회논문집
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• 제27권1호
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• pp.13-21
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• 2016

The Sulfur-Iodine thermochemical hydrogen production process (SI process) consists of the Bunsen reaction section, the $H_2SO_4$ decomposition section, and the HI decomposition section. The $HI_x$ solution ($I_2-HI-H_2O$) could be recycled to Bunsen reaction section from the HI decomposition section in the operation of the integrated SI process. The phase separation characteristic of the Bunsen reaction using the $HI_x$ solution was similar to that of $I_2-H_2O-SO_2$ system. On the other hands, the amount of produced $H_2SO_4$ phase was small. To investigate the effects of $SO_2$ solubility on Bunsen reaction, the continuous Bunsen reaction was performed at variation of the amounts of $SO_2$ gas. Also, it was carried out to make sure of the effects of partial pressure of $SO_2$ in the condition of 3bar of $SO_2-O_2$ atmosphere. As the results, the characteristic of Bunsen reaction was improved with increasing the amounts and solubility of $SO_2$ gas. The concentration of Bunsen products was changed by reverse Bunsen reaction and evaporation of HI after 12 h.

• 한국환경복원기술학회지
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• 제9권4호
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• pp.52-59
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• 2006

This study was conducted to find end-members and tracers which are effective to be applied in the End Member Mixing Analysis (EMMA) model for runoff separation at the Gwangneung coniferous forest catchment (13.6ha), Gyeonggido, Korea. We monitored three successive rainfall events during two weeks from June 26, 2005 to July 10, 2005, and analysed chemical properties of rainfall, throughfall, stemflow, groundwater and soil water considered as main components of storm runoff. The followings are the results of analyses of each component and tracer. Groundwater, soil water and rainfall (or throughfall) were dominant runoff components. Rainfall and groundwater were selected as main components for the two components-one tracer mixing model, and groundwater, soilwater and throughfall were selected as main components for the three components-two tracers mixing model. Tracers were selected from anion ($Cl^-$ and ${SO_4}^{2-}$), cation ($Na^+$, $K^+$, $Mg^{2+}$, and $Ca^{2+}$) and Acid Neutralizing Capacity (ANC) in event 1, 2, and 3. $Na^+$, $Ca^{2+}$ and ANC were selected in the two components-one tracer mixing model and ${SO_4}^{2-}-K^+$, ${SO_4}^{2-}-Na^+$, ${SO_4}^{2-}-Ca^{2+}$, ${SO_4}^{2-}$-ANC, and $Ca^{2+}$-ANC were selected in the three components-two tracers mixing model. Selected main runoff components and tracers can provide basic information to determine the contribution rate of each runoff component and identify the runoff process in a forest watershed.

• 지질공학
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• 제19권2호
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• pp.235-250
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• 2009

경북 영천 북안면 일대 지하수의 수질화학적 특정과 붕소, 브롬, 스트론튬 성인에 대하여 연구하였다. pH는 7.37${\sim}$8.39 범위로서 중성 내지 약알칼리성이다. B는 0.41${\sim}$4.62mg/L범위로 평균 1.74mg/L 함유된다. Br은 0${\sim}$3.24mg/L 범위, 평균 2.22mg/L 함유되어 있다. Sr은 0.93${\sim}$8.64mg/L 범위, 평균 2.76mg/L 함유되어 있다. 지하수의 수질유형은 $Ca-HCO_3$가 가장 흔하다. EC에 가장 크게 기여하는 주요 성분들은 Na, $SO_4$, Cl 등인데, 이들의 결정계수는 각각 0.85, 0.70, 0.90이다. 염소이온에 대한 Na, K, $SO_4$는 결정계수가 각각 0.54, 0.68, 0.53으로서 서로 비례함을 나타낸다. 특히 B-Sr와 $Sr-SO_4$간의 결정계수는 각각 0.65, 0.64로 상관성이 높다. 지하수의 경우 Cl/Br 비는 5.21${\sim}$30.70 범위인데 이는 염소가 상당히 결핍되어 있음을 지시한다. $SO_4/Cl$의 비는 1.32${\sim}$27.24 평균 5.92범위인데, 이는 지하수에 다량의 $SO_4$ 이온이 유입되거나, 염소결핍 현상으로 해석된다. 화학종의 존재형태를 계산결과 B는 대부분 $H_3BO_3$형을 가지며, 일부는 $H_2BO_3$로서 존재한다. Br은 $Br^-$ 이온으로서만 존재한다. Sr은 대부분 $Sr^{2+}$로서 존재하며, 일부는 $SrSO_4$로 존재한다. 포화지수를 계산한 결과 중정석, 카올리나이트, 일라이트, K-운모, 스멕타이트와 같은 점토광물군은 과포화상태이며, 실리카 광물, 석고, 경석고, 활석, 녹니석, 크리소타일, 장석 등은 거의 포화상태에 근접한다. 셀레스타이트의 포화지수는 -2.23${\sim}$-0.13 범위로서 여전히 불포화상태이다. halite의 경우 상당한 불포화상태에 있다. B, Sr의 경우 본 역에 널리 분포하는 백악기말-신생대초의 유천층군 화산활동과 관련되었을 가능성이 가장 높다. 본 지역에서의 Br은 주로 지질과 관련되나 외부 오염물의 유입에 의한 특징도 있다고 볼 수 있다.