• 한국세라믹학회지
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• 제30권1호
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• pp.7-16
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• 1993

Effect of sulfate on the reactionof C3S formation in presence of clinker melt and its appearance in clinker were investigated, using (NH4)2SO4 and CaSO4 as sulfate sources. When (NH4)2SO4 and CaSO4 were added, both showed the similar results, 1.0wt% of sulfate could promoted the reaction of C3S formation, however for its content of more than 2.0wt%, the formation of C3S was prevented. Residual limit of sulfate to C3S formation is about 1.4wt%. Appearances of sulfate were C4A3l and CaSO4 in interstitial phase. For the addition of (NH4)2SO4 or CaSO4 of 20wt%~4.0wt%, C3S grains showed the hypertrophic growth. We might consider that, because sulfate reduced the surface tension and viscosity of the clinker melt, C3S crystals were precipitated below 140$0^{\circ}C$, and the crystlas of C3S were coalesced and linked in the same crystallographical direction with increasing temperature becuase of their rapid growth rate.

• Asian Journal of Atmospheric Environment
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• 제6권1호
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• pp.41-52
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• 2012

Particulate sulfate in $PM_{2.5}$, sulfur dioxide ($SO_2$) and size-segregated aerosol particle number concentrations were measured at a site ($32^{\circ}19'N$, $129^{\circ}59'E$) on the southwestern Japan coast from 5 March to 10 April, 2010. Results show frequent episodic increases of sulfate and $SO_2$. Compared to the average concentration of sulfate $4.4{\pm}2.7\;{\mu}g\;m^{-3}$ in the whole observation period, episodic sulfate reached $10.5-20.1\;{\mu}g\;m^{-3}$. The variation of sulfate always synchronized with aerosol particles in the size range of $0.1-0.5 {\mu}m$, indicating the episodic sulfate was a consequence of the increase of the sub-micron particles. $SO_2$ did not have remarkable increase in any episodes of sulfate increase. During the passage of low pressure systems which loaded Asian dust in postfrontal air, concentrated sulfate appeared right behind the front but before dust arrival, suggesting the dominance of dust-free particulate sulfate. Weather and backward trajectory analyses revealed that air parcels with high sulfate passed eastern and northeastern China or Korean peninsula before arriving at the site. In contrast, those with high $SO_2$ passed an active volcano, Mt. Sakurajima, about 100 km in the south, suggesting the $SO_2$ was more likely from the volcanic emission. The ratio of sulfate to total sulfur compounds $({SO_4}^{2-})/({SO_4}^{2-}+SO_2)$ was 0.31-0.89 in continentally originated air while was 0.25-0.43 in the air having passed the volcano, showing more efficient conversions of $SO_2$ to sulfate in the air from the continent. The close dependence of the conversion on humidity in the continentally originated air was confirmed.

• Bulletin of the Korean Chemical Society
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• 제22권12호
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• pp.1309-1315
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• 2001

Zirconium sulfate supported on zirconia catalysts were prepared by impregnation of powdered $Zr(OH)_4$ with zirconium sulfate aqueous solution followed by calcining in air at high temperature. The characterization of prepared catalysts was performed using Fourier transform infrared (FTIR), X-ray diffraction (XRD), differential scanning calorimetry (DSC), and by the measurement of surface area. The addition of zirconium sulfate to zirconia increased the phase transition temperature of $ZrO_2$ from amorphous to tetragonal due to the interaction between zirconium sulfate and zirconia, and the specific surface area and acidity of catalysts increased in proportion to the zirconium sulfate content up to 10 wt% of $Zr(SO_4)_2$. Infrared spectra of ammonia adsorbed on $Zr(SO_4)2}ZrO_2$ showed the presence of Bronsted and Lewis acid sites on the surface. $10-Zr(SO_4)_2}ZrO_2$ calcined at $600^{\circ}C$ exhibited maximum catalytic activities for 2-propanol dehydration and cumene dealkylation. The catalytic activities for both reactions were correlated with the acidity of catalysts measured by ammonia chemisorption method.

• Bulletin of the Korean Chemical Society
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• 제25권5호
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• pp.657-664
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• 2004

Titanium sulfate supported on $TiO_2$was prepared by impregnation of powdered $TiO_2$with an aqueous solution of titanium sulfate followed by calcining in air at high temperature. For Ti$(SO_4)_2/TiO_2$ samples calcined at 300 $^{\circ}C$, no diffraction lines of titanium sulfate are observed at $Ti(SO_4)_2$loading up to 30 wt%, indicating good dispersion of $Ti(SO_4)_2$ on the surface of $TiO_2$. The acidity of the catalysts increased in proportion to the titanium sulfate content up to 20 wt% of $Ti(SO_4)_2$. 20 wt% $Ti(SO_4)_2/TiO_2$ calcined at 300 $^{\circ}C$ exhibited maximum catalytic activities for 2-propanol dehydration and cumene dealkylation. The catalytic activities for these reactions, were correlated with the acidity of catalysts measured by ammonia chemisorption method.

• Journal of Korean Society for Atmospheric Environment
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• 제22권E2호
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• pp.69-77
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• 2006

Combined gas and aerosol measurements at a downwind area of the volcanic plume would be essential for helping to access the impact of the volcanic eruption on the local ecosystem and residents. An intensive and the fine time resolution measurement of $SO_2$, sulfate and PM2.5 was made to estimate their distribution in the Kanto area of Japan during the Miyakejima volcanic eruption period. In Tokyo, the 1 hr average $SO_2$ concentration observed before the eruption was 23.9 ppbv, while that of after eruption was 140.4 ppbv. In the Saitama Prefecture, the average concentration of $SO_2$ marked in the present study was two times higher than the average before the volcanic eruption. The PM2.5 mass concentrations in Sitama ranged from 3.8 to $136{\mu}g\;m^{-3}$. Sulfate accounts for $4.4{\sim}39.6%$ of PM2.5 in Sitama. The good correlationship between the concentrations of $SO_2$ and sulfate was obtained. The results of the VAFTAD and HYSPLIT models indicate that $SO_2$, sulfate, and PM2.5 measured in the present study would be expected to be significantly affected by the Miyakejima volcanic plume.

• 콘크리트학회논문집
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• 제29권4호
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• pp.415-424
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• 2017

본 연구의 목적은 플라이애시 및 고로슬래그 미분말로 제조한 알칼리 활성화 결합재 모르타르의 황산염 저항성에 미치는 마그네슘(Magnesium, $Mg^{2+}$) 및 황산(Sulfate, ${SO_4}^{2-}$) 이온의 영향을 확인하는 것이다. 이를 위하여 고로슬래그 미분말 치환율을 30%, 50% 및 100%, $SiO_2$와 $Na_2O$의 몰 비($SiO_2/Na_2O$ molar ratio, Ms)를 1.0, 1.5 및 2.0으로 조정한 시험체를 제작하였다. 그리고 $Mg^{2+}$ 및 ${SO_4}^{2-}$의 영향을 확인하기 위하여 $Mg^{2+}$ 단독(10% $Mg(NO_3)_2$), ${SO_4}^{2-}$ 단독(10% $Na_2SO_4$), $Mg^{2+}$ 및 ${SO_4}^{2-}$ 복합(10% [$MgCl_2+Na_2SO_4$], 10% [$Mg(NO_3)_2+Na_2SO_4$]) 및 $MgSO_4$ 수용액(10%, 5% 및 2.5% $MgSO_4$)의 조건에서 압축강도, 길이변화, 질량변화 및 X선 회절 분석을 실시하였다. 그 결과, $Mg^{2+}$ 및 ${SO_4}^{2-}$가 공존하는 경우에만 황산염 침식에 의한 강도저하 및 팽창 등이 발생하는 것을 확인하였다. 이러한 현상은 $Mg^{2+}$이 규산칼슘 수화물(Calcium Silicate Hydrate, C-S-H)을 분해하여 $Ca^{2+}$이 용출되고, 용출된 $Ca^{2+}$과 ${SO_4}^{2-}$가 결합하여 석고($CaSO_4{\cdot}2H_2O$, Gypsum)를 생성하고, $Mg^{2+}$과 OH가 결합하여 수산화마그네슘(Magnesium hydroxide, $Mg(OH)_2$, Brucite)을 생성하는 것에 기인하는 것을 확인하였다.

• 대한토목학회논문집
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• 제28권5A호
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• pp.757-764
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• 2008

본 연구는 농도조건을 달리한 시험용액에 침지한 모르타르의 내구성을 평가하기 위하여 수행되었다. 3종류 시멘트 모르타르를 제조한 후, ${SO_4}^{2-}$ 이온의 농도가 4225, 8450, 16900 및 33800 ppm인 4종류 황산나트륨 용액에 540일간 침지하였으며, 침지재령별 압축강도 및 선형팽창을 측정하므로써 모르타르의 황산염침식 저항성을 실험적으로 평가하였다. 실험결과에 의하면, 고농도 황산나트륨 용액에 침지한 모르타르 공시체가 가장 심한 성능저하 현상을 나타내었다. 특히, 고농도 환경에서 모르타르의 팽창 특성은 사용된 시멘트의 $C_3A$량과 직접적인 관련이 있었으며, GGBS를 대체한 SGC 모르타르는 조직구조의 투수성이 상대적으로 낮은 탓으로 인하여 시험용액의 농도조건에 관계없이 우수한 황산염침식 저항성을 나타내었다.

• 한국환경과학회지
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• 제2권1호
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• pp.43-49
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• 1993

두개의 서로 다른 해양환경에서 수거된 토적물의 공극수로부터 황산염 농도와 황산염의 황 안정 동위원고값$({\delta}^{34}SO_4_){pw}$이 측정되었다. 한지역은 북동태평양 심해(ST-1)이었고, 다른 한 지역은 황해 경기만의 연안역(ST-2)이었다. 두 개의 시추 코아 공히 공극수 황산염의 농도가 김이세 따라 감소하는 것을 보였는데, 이것은 황산염 환원작용이 두 지역 퇴적환경에서 모두 일어나고 있음을 시사한다. 정점 ST-2에서 공극수 황산염의 감소가 더욱 현저한 것은 이곳에서 환산염 환원이 더욱 빠르게 일어나고 있음을 나타내는 것이며, 이것은 심해환경에 비해 연안환경에서 퇴적속도가 훨씬 빠르다는 사실을 고려할 때 예측된 결과이다. 공극수 황산염의 황 안정동위원소 측정값 $({\delta}^{34}SO_4_){pw}$ 들은 Rayleigh 동위원소 분화방정식이 예측한 값들과 매울 잘 일치하고 있다. 측정갑들은 정점 ST-2에서 26.7%~61.3%의 범위를 보이는데 이것은32.4%~97.8%의 분포를 보인 정점 ST-1에 비하면 적은 값들이다. 정점 ST-2에서 공극수 황산염의 농도변화가 훨씬 더 컷음에도 불구하고 동위원소값들은 적은 규모로 증가하였다. 황산염 농도변화와 동위원소값의 변화 사잉에 이와같은 역비례 관계는 다음과 같은 두가지 연속적인 요일들에 의해 설명될 수 있다. 황산염 환원이 진행됨에 따라 공극수에 남아있는 황산염내 황에는 무거운 $^{34}S$가 점차 농축되는 반응효과가 첫째 요인이며, 이러한 반응효과가 커지면 커질수록 최종값인 $({\delta}^{34}SO_4_){pw}$ 는 오히려 줄어들게 하는 Rayleigh 방정식 자체의 구조효과가 둘째 요인이다.

• 산업기술연구
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• 제30권A호
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• pp.127-132
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• 2010

We analyzed the effects of several process variables on the $SO_2$ removal and particle growth by the dielectric barrier discharge - photocatalysts hybrid process. In this process, $SO_2$ was converted into the ammonium sulfate ($(NH_4)_2SO_4$) particles. The size and crystallinity of ammonium sulfate particles were examined by using TEM and XRD analysis. The dielectric barrier discharge reactor consisted of two zones: the first is for plasma generation and the second is for ammonium sulfate particles formation and growth. The first zone of reactor was filled with glass beads as a dielectric material. To enhance $SO_2$ removal process, the $TiO_2$ photocatalysts were coated on glass beads by dip-coating method. As the voltage applied to the plasma reactor or the pulse frequency of applied voltage increases, the $SO_2$ removal efficiency increases. Also as the initial concentration of $SO_2$ decreases or as the residence time increases, the $SO_2$ removal efficiency increases. $(NH_4)_2SO_4$ particles continue to grow by particle coagulation and surface reaction, moving inside the reactor. Larger particles in site are produced according to the increase of residence time or $SO_2$ concentrations.

• 한국세라믹학회지
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• 제44권9호
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• pp.471-476
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• 2007

The hydration mechanism of the $3CaO{\cdot}Al_2O_3-CaSO_4{\cdot}2H_2O$ system in the presence of alkali sulfates has been investigated. The early hydration rate of $3CaO{\cdot}Al_2O_3$ was accelerated by the addition of $Na_2SO_4$ and $K_2SO_4$. This is closely related to the formation of syngenite $(CaSO_4{\cdot}K_2SO_4{\cdot}H_2O)$, and the U-phase added $K_2SO_4$ and $Na_SO_4$ in the $3CaO{\cdot}Al_2O_3-CaSO_4{\cdot}2H_2O$ system, respectively. The formation of the rigid syngenite and U-phase structure led to rapid setting and decreases the sulfate content in the liquid phase of the hydrating cement to the extent that it cannot adequately retard the hydration of $3CaO{\cdot}Al_2O_3$. In case of the alkali sulfate not added to the $3CaO{\cdot}Al_2O_3-CaSO_4{\cdot}2H_2O$ system, the ettringite was transformed to monosulfoaluminate immediately after the consumption of gypsum. However, when the alkali sulfates were added to this system, the ettringite did not transform to monosulfoaluminate immediately even though the gypsum was completely consumed. There was a stagnation period to transform to the monosufoaluminate after the consumption of gypsum because the syngenite and U-phase remained as the sulfate source.