• 제목/요약/키워드: particulate organic carbon

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팔당호 난분해성 유기물에 대한 조류기원 유기물의 기여 (Algal Contribution to the Occurrence of Refractory Organic Matter in Lake Paldang, South Korea: Inferred from Dual Stable Isotope (13C and 15N) Tracer Experiment)

  • 이연정;하선용;허진;신경훈
    • 생태와환경
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    • 제52권3호
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    • pp.192-201
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    • 2019
  • 효과적인 물환경관리계획을 수립하기 위해서는 다양한 기원의 유기물이 난분해성 유기물 농도 증가에 영향을 줄 수 있는지 여부를 파악하는 것이 중요하다. 특히 상당량의 광합성 산물은 식물플랑크톤에 의해 매일 생성되고 있지만, 이들이 수계 내 난분해성 유기물에 기여하는지에 대한 정보는 부족하다. 본 연구에서는 $^{13}C$$^{15}N$ 추적자 첨가실험을 통해 조류기원 유기물이 생분해(60일, 암배양) 및 산화제(과망간산칼륨) 처리 후 분해되지 않고 잔존하는지 여부를 확인하였다. 생분해 실험 결과 광합성을 통해 생성된 총 유기탄소($TO^{13}C$), 입자성 유기탄소($PO^{13}C$), 입자성 질소($P^{15}N$)는 각각 26%, 20%, 17%가 비 생분해성 유기물로 잔존하였다. 또한 상당량의 $PO^{13}C$가 과망간산칼륨에 의해 산화되지 않고 잔존하였다(초기: 12%, 60일 암배양 후: 38%). 이는 미생물에 의해 사용된 후 남아있는 조류기원 유기물이 난분해성 유기물에 기여할 수 있음을 의미한다. 또한 미생물에 의해 변형된 조류기원 유기물의 양은 COD 산화율 및 유기물 지표 간 격차에 영향을 줄 것으로 사료된다.

흡착제 세공 특성이 담배연기성분 제거에 미치는 영향 (Effect of Adsorbent Pore Characteristics on the Removal Efficiency of Smoke Components.)

  • 이영택;김영호;신창호;임광수
    • 한국연초학회지
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    • 제14권1호
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    • pp.87-93
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    • 1992
  • The adsorption efficiency of some adsorbents for the organic solvents and gas phase of smoke was investigated. 1. Specific surface area of activated carbon increased to 1900 mfg with increased activation time. 2. Adsorption efficiency of benzene and acetone increased with increasing total surface area. Adsorption capacity for gas phase such as hydrogen cyanide, aldehyde was proportional to the micro pore surface area under 20A. 3. The removal efficiency of particulate matter of smoke was higher with the adsorbents of relatively higher pore size compared to that of micro pore.

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도시환경의 총부유먼지 중 미지성분의 분포 특성에 대한 연구 (A study of distribution characteristics of unidentified particulate components in an urban area)

  • 김용현;김기현;박찬구;손장호;송상근
    • 분석과학
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    • 제25권2호
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    • pp.133-145
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    • 2012
  • 대기 중의 총부유먼지(total suspended particulate, TSP)를 구성하는 성분들 중 organic carbon (OC), element carbon (EC), 금속성분은 양적으로 중요한 구성인자에 해당한다. 이들을 제외한 나머지 부분은 아직까지 정성 및 정량분석이 취약한 미지 물질(${\Sigma}X$)에 해당한다. 본 연구에서는 서울시 강서 지역에서 2009년 2-12월 기간동안 관측한 자료를 이용하여, TSP의 주요 성분들 간의 관계에 대한 분석을 시도하였다. 이를 통해, TSP의 거동을 다양한 각도에서 해석하기 위한 기초 자료로 활용하고자 하였다. 전체 연구기간 동안, TSP를 이루는 주요인자로서 미지의 영역이 평균적으로 48.6%를 차지할 정도로 더 지배적이란 것을 확인하였다. 그리고 TSP에 대한 그 구성 성분들간의 관계를 검토하였을 때, 미지 물질들은 이온성분들과 밀접한 연관성을 보일뿐 아니라 TSP의 함량과 정비례 관계임을 확인하였다. 반면, 양자를 TSP의 농도로 표준화(normalization)를 하였을 경우, 뚜렷한 반비례 관계에(강한 역상관성)이 두드러지게 나타났다. 이러한 현상은 ${\Sigma}X$가 이온성분과는 달리 수용성이 떨어지는 특성을 지닌 것을 반영한 것으로 사료된다. TSP의 거동을 보다 체계적으로 이해하고 이를 도시 대기질 관리에 적용하기 위해서는, ${\Sigma}X$의 조성이나 거동을 명확하게 규정하기 위한 여러 가지 연구가 필요하다.

Assessment of Organic Matter Sources in the Singil Stream Flowing into Lake Shihwa, South Korea

  • Kim, Dahae;Kim, Jung-Hyun;Kang, Sujin;Kim, Min-Seob;Shin, Kyung-Hoon
    • 생태와환경
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    • 제53권2호
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    • pp.138-147
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    • 2020
  • The Singil Stream, flowing into an artificial lake, Lake Shihwa (South Korea), experiences a strong anthropogenic pressure with continuous organic matter (OM) inputs from rural, urban, and industrial areas. In this study, we investigated suspended particulate matter (SPM) and streambed sediments collected along the Singil Stream in 2014 and 2016, by applying a dual element approach (δ13C and δ15N) to identify OM sources. The SPM and streambed sediment samples from the indusrial area showed higher organic carbon and nitrogen concentrations (or contents) than those from the other areas, with distinctively lower δ15N values. Accordingly, our dual element approach indicates that the industrial area was the predominant OM source influencing OM quality and thus water quality of the Singil Stream flowing into Lake Shihwa during the study periods. However, further studies are necessary to better constrain OM sources in the Singil Stream since OM sources from the industrial area appear to be complex.

황사시와 비황사시 대기 입자상 탄소성분의 농도 특성 (Concentration Characteristics of Elemental and Organic Carbons During Asian Dust Episode and Non-Episode)

  • 황경철;조기철;신은상
    • 환경위생공학
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    • 제24권4호
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    • pp.102-111
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    • 2009
  • In this study, Particulate carbon were determined from 1990 to 1995. The annual variation were investigated. The sampling was carried out using high volume air sampler. Average concentrations of EC and OC during the yellow sand event were $25.70{\mu}g/m^3$ and $13.91{\mu}g/m^3$, respectively, $22.10{\mu}g/m^3$ and $10.33{\mu}g/m^3$ during the non-yellow sand event. TC concentration of TSP were 10.7% during the yellow sand event and 20.6% during the non-yellow sand event. Average concentration rate of EC and OC of TC were 64.9% and 35.1%, respectively during the yellow sand event, 67.6% and 32.4% during the non-yellow sand event.

Comparison of a Microbiological Model Simulation with Microcosm Data

  • Lee, Jae-Young;Tett, Paul;Jones, Ken
    • Journal of the korean society of oceanography
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    • 제39권4호
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    • pp.222-233
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    • 2004
  • Using nitrogen as the limiting nutrient, the default version of a microplankton-detritus model linked chlorophyll concentration to the autotroph nitrogen. However, phosphorus dynamics were added to simulate the results of a microcosm experiment. Using standard parameter values with a single value of microheterotroph fraction in the microplankton taken from the observed range, the best simulation successfully captured the main features of the time-courses of chlorophyll and particulate organic carbon, nitrogen and phosphorus, with root-mean-square error equivalent to 29% of particulate concentration. A standard version of microbiological model assumes complete internal cycling of nutrient elements; adding a term for ammonium and phosphate excretion by microheterotrophs did not significantly improve predictions. Relaxing the requirement for constant microheterotroph fraction resulted in an autotroph-heterotroph model AH, with dynamics resembling those of a Lotka-Volterra predator-prey system. AH fitted the microcosm data worse than did MP, justifying the suppression of Lotka-Volterra dynamics in MP. The paper concludes with a discussion of possible reasons for the success of the simple bulk dynamics of MP in simulating microplankton behaviour.

강화도 지역에서 겨울철 $PM_{205}$의 화학적 성분 특성 (Characteristics of Chemical Species in $PM_{205}$ during the Winter in Kangwha)

  • 여현구
    • 한국대기환경학회지
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    • 제16권4호
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    • pp.309-316
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    • 2000
  • Chemical compositions of air pollutants with fine particles (<2.5 ${\mu}{\textrm}{m}$, PB2.5) were evaluated at background site. Kangwha. in Korea during the winter season. The data set was obtained for seventeed days with 24-hour sampling from December 11 to 16, 1996 and from January 9 to 1997. The chemical species have been measured {{{{ {SO }`_{4 } ^{2- } }}}}, {{{{ { NO}`_{3 } ^{- } }}}}, {{{{ { NH}`_{4 } ^{+ } }}}}. OC and EC in the particulate phase, NH3 HNO3, HCl and SO2 in the gas phase using the three stage filter pack method. Mean concentration ($\mu\textrm{g}$/m3) of this study were : 35.42 for PM2.5 8.78 for organic carbon (OC) 7.25 for nss {{{{ {SO }`_{4 } ^{2- } }}}}, 4.94 for {{{{ { NO}`_{3 } ^{- } }}}}, 3.58 for {{{{ { NH}`_{4 } ^{+ } }}}} and 1.48 for elemental carbon (EC) respectively. Contributive rates of major particulate components in PM2.5 were OC (25%) nss- {{{{ {SO }`_{4 } ^{2- } }}}}(20%) ,{{{{ { NO}`_{3 } ^{- } }}}}(14%) {{{{ { NH}`_{4 } ^{+ } }}}}(10%) and EC (4%) respectively and these components could be accounted for 73% of PM2.5 mass. Reactive forms of {{{{ { NH}`_{4 } ^{+ } }}}} were considered as NH4HO3 and NH4{{{{ {SO }`_{4 } ^{2- } }}}} during the sampling periods. {{{{ { NO}`_{3 } ^{- } }}}}/({{{{ { NO}`_{3 } ^{- } }}}} + HNO3) and {{{{ {SO }`_{4 } ^{2- } }}}}/({{{{ {SO }`_{4 } ^{2- } }}}} + SO2) were calculated 0.8 and 0.9 respectively. Most of these compounds might be formed in partiiculate phase in the air. Correlation coefficient between OC and EC was 0.866 which might have the same sources during the sampling periods,.

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Preparation of Rubber Particulates for Micro Dust Study using Cryogenic Crushing

  • Chae, Eunji;Son, Chae Eun;Choi, Sung-Seen
    • Elastomers and Composites
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    • 제54권4호
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    • pp.330-334
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    • 2019
  • Cryogenic crushing techniques have been employed for recycling waste rubber articles and for extracting residual organic additives present in rubber samples. Rubber particulate derived from tire tread abrasion is one of the key components of road dust. Therefore, in this work, we prepared rubber particulates using a cryogenic crusher and characterized their shapes as well as size distributions according to the type of rubber. The rubber particulates exhibited uneven surfaces with the presence of some small pieces. The order of the particle size distribution was observed to be: NR > BR > SBR. Subsequently, carbon black was added; this led to a decrease in the particle size and the shape becoming rougher. The crushed particulates of the carbon black-filled samples comprised agglomerated shapes of small pieces, which were similar in shape to that of wear debris in tire tread. It was discovered that crosslink density was one of the principal factors that led to the formation of small crushed particulates. The small particulates obtained by cryogenic crushing can be utilized as model rubber particulates for researching micro dust.

Carbon Stable Isotope Ratios of Phytoplankton and Benthic Diatoms in Lake Katanuma with Reference to Those of Other Lakes

  • Kikuchi, Eisuke;Takagi, Shigeto;Shikano, Shuichi;Hideyuki, Doi
    • 생태와환경
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    • 제38권spc호
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    • pp.8-11
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    • 2005
  • Carbon stable isotope ratios of producers varied in lake ecosystems. In tile present study, we tried to estimate the seasonal variations of carbon isotope ratios of phytoplankton and benthic diatoms in a strongly acidic lake ecosystem. Lake Katanuma is a volcanic, strongly acidic lake (average pH of 2.2), located in Miyagi, Japan. Only two algal species dominate in Lake Katanuma; Pinnularia acidojaponica as a benthic diatom, and Chlamydomonas acidophila as a green alga. Carbon isotope values of P. acidojaponica varied seasonally, while those of particulate organic matter, which were mainly composed of C. acidophila remained fairly stable. The differences suggested that $CO_2$ gas was more frequently limited for P. acidojaponica than C. acidophila, since high density patches of benthic diatoms were sometimes observed on the lake sediment. Generally, carbon concentration mechanisms (CCMs)of microalgae can fix bicarbonate in lakes, and affect the carbon isotope values of microalgae. While, in Lake Katanuma, CCMs of the microalgae may scarcely function because of high $CO_2$ gas concentration and low pH. This is the reason for low seasonal amplitude of carbon isotope values of phytoplankton relative to those in other lakes.

하천·호소의 유기물 지표 평가 (Index of Organic Matter in Stream and Lake)

  • 유순주;황종연;윤영삼;천세억;한의정
    • 환경영향평가
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    • 제8권1호
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    • pp.81-92
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    • 1999
  • This study discussed the appropriateness of organic matter indexes such as biochemical oxygen demand(BOD) and chemical oxygen demand with potassium permanganate($COD_{Mn}$) in water quality environmental standard of streams and lakes and the applicability of the items to water quality environmental standard to add or substitute COD with potassium dichromate ($COD_{Cr}$) and total organic carbon(TOC) being used as index of organic matter. And indexes of organic matter content and organic carbon concentration were distinguished between dissolved and particulate component in water sample to estimate their effect on pollutants loading in lake and stream. The ratio of $COD_{Cr}$/BOD was 5.1 under BOD concentration 3mg/L in river water quality environmental standard II, and 2.67 above it. This ratio was diminished to 2.04 when BOD concentration was more than 8mg/L, in river quality environmental standard IV. Also the ratio of $COD_{Mn}$/BOD showed 2.16 under 3mg/L(BOD), and 1.1 above it. This ratio is also diminished to 0.84 over 8mg/L(BOD). Accordingly, we should apply this ratio depending on the concentration level to add and change organic matter index of water quality environmental standard newly. The ratio $COD_{Cr}/COD_{Mn}$ both in lake and stream shows 2.37(r=0.986, p<0.001). But the ratios showed range of 2.34~2.50, which is no much difference of this ratio according to $COD_{Mn}$ concentration.

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