• 제목/요약/키워드: Atmospheric deposition

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우리나라 도시지역의 $SO_2$건성침적 플럭스 산출 (Estimations of the $SO_2$Dry Deposition Flux at Urban Areas in Korea)

  • 이종범;김용국;박일환
    • 한국환경과학회지
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    • 제10권1호
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    • pp.1-8
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    • 2001
  • This study was carried out estimating the dry deposition flux of $SO_2$at eight urban areas in Korea during one year of 1996. To calculate the deposition flux, deposition velocities were calculated by turbulence parameters estimated from routine meteorological data. Also, hourly averaged $SO_2$concentrations which calculated from air pollution monitoring data of each city were used. The dry deposition velocities were mostly higher in the coastal areas than the other areas, which would be caused by relatively strong wind. And, they were high in the daytime because of turbulence activities. The deposition flux of $SO_2$is mainly related to the atmospheric concentration. The annual average $SO_2$concentration and the deposition flux were 22.62ppb and 1510.52g/$\textrm{km}^2$/hr at Pusan respectively. Also, the flux was higher in winter than other season, which was a significant contribution of exhausted fuel for heating. While the deposition velocity was high to 0.688cm/sec at Yosu in case of strong wind and small cloud cover, the deposition flux was high to 1597.4g/$\textrm{km}^2$/hr at Pusan in case of weak wind and small cloud cover.

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MONNTORING AIR QUALITY AND ACIDDEPOSITION IN SOUTHERN U.S.

  • Allen, Eric R.
    • 한국환경과학회:학술대회논문집
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    • 한국환경과학회 1997년도 가을 학술발표회 프로그램
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    • pp.1.1-32
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    • 1997
  • Atmospheric monitoring capabilities were established in 1988 by the University of Florida at Duke forest, near Durham. NC: Cary forest, near Gainesville, FL: and Austin forest, near Nacogdoches, TX. Continuous (hourly averaged) measurements of air quality (ozone, nitrogen oxides and sulfur dioxide) and meteorological variables were made at these three low elevation (< 200 meters), rural locations in the southeastern U.S. for more than three years. During the same period at these sites wet and dry acid deposition samples were collected and analyzed on an event and weekly basis, respectively The monitoring locations were selected to determine actual atmospheric exposure indices for southern pine species in support of on-site surrogate exposure chamber studies conducted by Southern Commercial Forest Research Cooperative (SCFRC) investigators. Daily and quarterly averaged ozone maxima were higher (55 ppb) at the northernmost site in the network (Duke forest) in the second and third quarters (spring and summer seasons) and lower (35 ppb) in the first and fourth quarters (winter and fall seasons), when compared to ozone levels at the two southernmost sites (Cary and Austin forests). Seasonal ozone levels at the latter two sites were similar Nitrogen oxieds and sulfur dioxide levels were insignificant (< 5 ppb) most of the time at all sites, although soil emissions of NO at two sites were found to influence nighttime ozone concentrations. Typical maximum quarterly and annual aggregate ozone exposure indices were significantly higher at Duke forest (92.5/259 ppm-hr) than those values observed at the two southern sites (65.6/210 ppm-hr). Acid deposition (wet and dry) components concentrations and deposition fluxes observed at the Duke forest, NC piedmont site, were generally greater, dependent on site and season, than corresponding variables measured at either of the two southern coastal plain sites (Cary and Austin forests). Acid deposition variables observed at the latter two sites were remarkably similar, both qualitatively and quantitatively, although the sites were located 1300 km apart. A comparison of deposition fluxes of elemental nitrogen (NO3, NH4') and sulfur (5042-, SO3) components in wet and dry forms indicated that wet deposition accounts for approximately 70% of the total nitrogen and 73% of the total sulfur input on an annual equivalent basis at all sites.

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중국의 서부 대개발에 따른 중국의 아황산가스 배출량과 주 배출 지역의 변화가 동아시아 황 침적량에 미치는 영향: RAINS-Asia 모델을 통한 분석 (Effects of Regional SO2 Emission Change due to the Western Development in China on the Deposition of sulfur in East Asia: Analysis Using the RAINS-Asia Model)

  • 여민주;김용표
    • 한국대기환경학회지
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    • 제21권1호
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    • pp.73-81
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    • 2005
  • It is widely accepted that, at present, the SO$_2$ emissions in China are not increasing thanks to the rigorous Chinese government policies. However, with the development of western China, it is possible that the SO$_2$ emission amounts might increase in regional scale. In this study, changes of sulfur deposition pattern and unprotected ecosystem in east Asia due to the sulfur emission pattern changes in China are studied by using the RAINS-Asia model. Five scenarios have been postulated to understand the effects on east Asia, especially, on Korea and Japan. It is found that the increase of SO$_2$ emission in western China might increase the total emission in whole China. And the amount of sulfur deposition from western China on east Asia would be higher than those from eastern China. The deposition amount of sulfur species on Asia is 3.2 Mt when SO$_2$ are emitted from western China only while 2.6 Mt from eastern China only. Generally, Korea and Japan are influenced more by emissions from eastern China than western China. However, if the SO$_2$ emissions from western China increase by 100% while those decrease by 10% in eastern China compared to the base case, the deposition amount of sulfur species on Korea and Japan would be higher than the base case. The fraction of unprotected ecosystem in Korea and Japan for the base case are 50 and 5%. However, if the emissions from western China increase by 100% while those decrease by 10% in eastern China, the fraction of unprotected ecosystem in Korea and Japan would be 52 and 6%.

대기 산성 강하물 : 삼림의 질소 포화 (Atmospheric Acid Deposition : Nitrogen Saturation of Forests)

  • 김준호
    • Journal of Ecology and Environment
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    • 제29권3호
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    • pp.305-321
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    • 2006
  • 대기 산성 강하물 : 삼림의 질소 포화 한국의 연평균 습성 질소 강하량은 12.78(범위: $7.28{\sim}21.05)\;kgN{\cdot}ha^{-1}{\cdot}yr^{-1}$이고, 이것에 건성 질소 강하량(43%)을 합하여 추정한 총질소 강하량은 18.26(10.41-30.10) $kgN{\cdot}ha^{-1}{\cdot}yr^{-1}$이 된다. 이 질소 강하량은 유럽과 북미 북동부의 질소 강하량과 비슷한 수준이다. 대기 질소 강하량이 많은 온대 삼림은 질소로 포화된다. 질소로 포화된 삼림은 계류수와 토양에 질산이온 ($NO_3^-$)과 질산태질소/암모늄태질소이($NO_{3}^{-}-N/NH_{4}^{+}-N$)의 비가 높아지고, 잎의 질소 농도가 높아지므로 N/P비, N/K비 및 N/Mg 비가 높아지는 것으로 보아 무기 영양소 교란이 일어나며, 상해와 병해에 걸리기 쉬워지고 세근과 근균의 활성이 낮아짐으로써 생산성이 낮아진다. 그러고 혐질소성 종이 호질소성 종에 의하여 대치된다. 질소로 포화된 토양에서는 온실가스인 메탄($CH_4$)의 흡수가 감소되고 일산화질소 (NO)와 아산화질소 ($N_{2}O$)의 배출이 증가되어 지구온난화를 촉진할 수 있다. 이 종설은 한국의 33장소에서 6년 동안 ($1999{\sim}2004$) 측정한 부피가중 연평균 습성 질소 강하량이 삼림의 질소 포화 수준에 달하고, 광릉시험림분수계와 그 밖의 삼림 계류수의 $NO_3$ 유출량으로 미루어 보아 한국의 삼림에 질소 포화의 징후가 나타났음을 제시하며, 문헌 자료를 통해서 외국의 삼림에서 일어나는 질소 포화의 징후를 체계적으로 논하는 데 목적이 있다.

$\textrm{O}_3$/TEOS를 이용한 후막 $\textrm{SiO}_2$의 성장특성 연구 (Growth Characteristics of Thick $\textrm{SiO}_2$ Using $\textrm{O}_3$/TEOS APCVD)

  • 이우형;최진경;김현수;유지범
    • 한국재료학회지
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    • 제9권2호
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    • pp.144-148
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    • 1999
  • We have studied the deposition characteristics of thick silicon dioxide film on Si substrate by $O_3$/TEOS APCVD(Atmospheric Pressure Chemical Vapor Deposition). The effect of deposition parameters such as the distance between showerhead and substrate, deposition temperature, TEOS flow rate and $O_3$/TEOS ratio on deposition rate, surface morphology, and properties of films as investigated. As deposition temperature increased, deposition rate decreased but the surface morphology and adhesion of film to substrate improved. As the distance between showerhead and substrate decreased, the deposition rate increased. Etching rate using the BOE increased as TEOS flow rate increased, but was independent of$ O_3$/TEOS ratio. Deposition rate of $5\mu\textrm{m}$/hour was obtained under the condition that the distance between showerhead and substrate was 5mm and the deposition temperature was $370^{\circ}C$.

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수질에 대한 대기건식침적의 영향 - 건식침적량 추정 방법론의 비교를 중심으로 (Effect of Dry Deposition on Water Quality -The comparison of several methodologies for estimating dry deposition flux)

  • 정장표
    • 상하수도학회지
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    • 제22권1호
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    • pp.159-168
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    • 2008
  • A special field experiment has been carried out from March 2001 to June 2001 at the Changhowon in Kyunggi to investigate a better methodology for the estimation of dry deposition of pollutions applicable in Korea. In this study, dry deposition plate was used to measure of total and water soluble acidic mass fluxes, and CPRI(Coarse Particle Rotary Impactor), CI(Cascade Impactor) were also used to measure ambient concentrations in various particle size ranges. Sehmel-Hodgson model was used to estimate dry depostion velocity and Weibull probability distribution function was applied to get generalized particle size distribution for the size fractioned concentration data sampled by CPRI and CI. Atmospheric dry deposition fluxes of mass and ionic matters estimated by the various techniques(one-step, multi-step, equi-concentration, subdivision for only the coarse particle range, applying Weibull distribution function, etc.) were compared to flux data sampled by DDP. It was found out that the deposition fluxes estimation methodology calculated by the each particle size range devided by particle size distribution characteristics and the rapidly changed points of deposition velocity using Weibull probability distribution function was the most applicable.

IDENTIFICATION OF POSSIBLE MERCURY SOURCES AND ESTIMATION OF MERCURY WET DEPOSITION FLUX IN LAKE ONTARIO FROM LAKE ONTARIO ATMOSPHERIC DEPOSITION STUDY (LOADS)

  • Han, Young-Ji
    • Environmental Engineering Research
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    • 제10권6호
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    • pp.306-315
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    • 2005
  • Total gas phase mercury (TGM) concentrations and event wet-only precipitation for Hg were collected for nine months (from April, 2002 to Dec., 2002) at Sterling, NY on the shoreline of Lake Ontario. TGM concentrations measured in this study ($3.02{\pm}2.14\;ng/m^3$) were in somewhat high range compared to other background sites. Using simplified quantitative transport bias analysis (SQTBA) possible sources affecting high Hg concentration in Sterling was identified, and they are coal-fired power plants located in southern NY and Pennsylvania. Wet deposition measured at Mercury Deposition Network (MDN) sites including Pt. Petre and Egbert, ON were compared with data obtained at the Sterling to estimate the total mercury wet deposition flux to Lake Ontario. The wet deposition flux was calculated to be the highest at the Sterling site ($7.94\;{\mu}g/m^2$ from April, 2002 to Dec. 2002) and the lowest at the Egbert ($3.92\;{\mu}g/m^2$), due to the both the difference in precipitation depth and Hg concentration in the precipitation. The deposition measured at the Sterling site is similar to Lake Michigan deposition of $6-14\;{\mu}g/m^2$ (converted for ninth months) measured for Lake Michigan Mass Balance Study (LMMBS).

Monitoring of Atmospheric Corrosivity inside Steel Upper Box Girder in Yeongjong Grand Bridge

  • Li, SeonYeob
    • Corrosion Science and Technology
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    • 제10권3호
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    • pp.87-94
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    • 2011
  • The typical corrosion prevention method inside the steel upper box girder in a suspension bridge involves the use of paints. However, in an effort to reduce environmental impact and cost, the suspension portion of the Yeongjong Bridge, Korea utilizes dehumidification systems to control humidity and prevent corrosion inside its box girder. Maintaining a uniform humidity distribution at the proper level inside the box girder is critical to the successful corrosion control. In this study, the humidity and the resultant atmospheric corrosivity inside the box girder of the Yeongjong Bridge was monitored. The corrosion rate of the steel inside the box girder was obtained using thin-film electrical resistance (TFER) corrosion sensors. Time-of-wetness (TOW) measurements and the deposition rates of atmospheric pollutants such as $Cl^{-}$ and $SO_{x}$ were also obtained. Classification of the atmospheric corrosivity inside the box girder was evaluated according to ISO 9223. As a result, no corrosion was found in the upper box girder, indicating that the dehumidification system used in the Yeongjong Bridge is an effective corrosion control method.

황사현상시 대기에어로졸 중 무기물질의 동태 (Behaviors of Inorganic Components in Atmospheric Aerosols on the Yellow Sand Phenomena)

  • 이민희;한의정;신찬기;한진석;김상균
    • 한국대기환경학회지
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    • 제9권3호
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    • pp.230-235
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    • 1993
  • The atmospheric aerosol samples during the Yellow Sand Phenomena in April 1993 were analyzed, and they were compared with those during the normal time. The conclusions are as follows: 1) TSP concentrations in the case of Yellow Sand Phenomena appeared to be 2.2times higher than those of normal conditions. 2) The concentration of aerosols; Inorganic components of soil-originated elements (Ca, Fe, Mn, Mg, K) during the Yellow Sand Phenomena were measured to be 1.9-2.1times higher than those during normal time. 3) During the Yellow Sand Phenomena the EF values of soil-originated metal contents except for elements Cd, Ni, Pb, Zn in the atmospheric aerosol were close to unity. 4) The concentrations of $Ca^{2+}, SO_4^{2-}, F^-$ in water soluble ionic components were higher than those during the normal time. 5) Washout factor by rain fall during the Yellow Sand Phenomena were estimated to 1268. 6) During the Yellow Sand Phenomina average deposition was 37.8ton/$km^2$.

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Experimental Studies on Wet Scavenging of Atmospheric Aerosols by Rain Drops

  • Park Jeong-Ho;Suh Jeong-Min;Choi Kum-Chan
    • Journal of Korean Society for Atmospheric Environment
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    • 제21권E3호
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    • pp.87-94
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    • 2005
  • Wet scavenging by rain drops is a most important removal process of air pollutants. In order to study the scavenging mechanisms of aerosol particles, the characteristics of chemical components in the rain water were examined as a function of the amount of rainfall. Rain water were collected continuously and separated into the soluble and insoluble components. The elemental concentrations in both components were determined by a PIXE analysis. The physical and chemical characteristics of atmospheric aerosols during the rainfall events were measured simultaneously. The elemental concentrations in rain water decreased substantially just after rain started and then gradually declined in subsequential rain fall exceeding 1.0 mm. The large particles were scavenged more easily than the fine particles. Fe, Ti and Si in rain water were in high insoluble state. Contrarily, almost whole of S was dissolved in rain water.