• 분석과학
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• 제21권4호
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• pp.304-315
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• 2008

한라산 1100 고지에서 채취한 대기 부유분진의 조성은 인위적 기원의 성분들이 가장 높고, 다음으로 해양 기원 성분과 토양 기원 성분들이 높은 함량을 나타내었다. 계절별로는 봄철에 토양 성분인 nss-$Ca^{2+}$, Al, Fe, Ca 성분의 농도가 크게 증가하였고, 인위적 기원의 $NH{_4}^+$, $K^+$, nss-$SO{_4}^{2-}$은 6월에 가장 높은 농도를 보였다. 반면에 $NO{_3}^-$은 봄철에 nss-$Ca^{2+}$과 함께 농도가 상승하였고, 이는 중국으로부터 장거리 이동에 의한 영향으로 추정된다. 황사와 비황사 때의 농도를 비교해 본 결과, 황사 때에 nss-$Ca^{2+}$, Al, Ca, Fe 농도가 7.2~9.5배 증가하였고, nss-$SO{_4}^{2-}$과 $NO{_3}^-$은 각각 1.3, 3.8배 정도 더 증가한 것으로 확인되었다. 요인분석법으로 분진성분의 발생기원을 조사해 본 결과, 한라산 1100 고지 부유분진은 토양의 영향을 가장 많이 받고, 다음으로 인위적 영향과 해염 영향을 많이 받고 있는 것으로 추정된다. 역궤적분석에 의해 분진 성분의 유입경로를 조사한 결과, 공기덩어리가 중국대륙을 거쳐 제주지역으로 이동한 북서풍 계열의 풍향일 때 주요 인위적 기원의 성분과 토양 성분의 농도가 상승하고, 공기가 북태평양을 거쳐 제주지역으로 유입되었을 때 이들 성분들의 농도가 상대적으로 감소하는 경향을 보였다.

• 한국해양학회지:바다
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• 제28권4호
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• pp.143-157
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• 2023

본 연구는 바지락과 쏙의 서식 구역이 대비되는 보령 주교 갯벌의 인위적인 환경 영향에 의한 저서동물 군집 특성을 확인하였다. 조사 기간 내 대형저서동물은 총 55종이 출현하였으며, 평균 서식밀도는 338 ind./m², 생체량은 212.2 gWWt/m²이었다. 출현 종수는 상부(27종)에서 하부(37종)로 갈수록 증가하였고, 우점종은(상부: 둥근가시사자머리참갯지렁이, 중부: 고리버들갯지렁이, 하부: 바지락) 조위별로 다르게 나타났다. 집괴분석과 다차원척도법을 이용한 상위 10종의 저서동물 군집구조는 하부의 바지락 어장과 쏙 서식공 밀도가 높은 중부 정점 중심의 두 그룹으로 나뉘며, 특정 생물 종의 영향을 반영하였다. 쏙 서식 공간의 퇴적물 입도 조성은 변동 폭이 컸으나 연간 유지되었으며, 분급은 2.1 𝜑로 낮아져 같은 입자로 구성된 비율이 증가하였다. 특히, 중부는 인위적인 영향이 높음에도 고리버들갯지렁이가 우점하고, 쏙 서식공 밀도와의 연관성을 보여 이는 종간 상호작용에 기인하는 것으로 판단된다.

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2008년도 춘계학술대회 논문집
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• pp.289-294
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• 2008

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2005년도 학술발표회(2)
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• pp.1008-1009
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• 2005

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2002년도 춘계 공동학술발표회
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• pp.59-61
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• 2002

• 한국환경보건학회지
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• 제24권3호
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• pp.114-123
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• 1998

Particulate matters(less than 10 $\mu$m, PM10) at Kanghwa and Yangyang, which are located in the western and the eastern coastal regions in Korea, were measured in using low volume air sampler from December 1995 to November 1996, and their characteristics were investigated from the view point of background level.(and in order to characterize the particulate matters.) The particulate matters were analyzed for major water soluble ionic components(SO$_{4}^{2-}$, NO$_{3}^{-}$, Cl$^{-}$, Na$^{+}$, NH$_{4}^{+}$, K$^{+}$, Mg$^{2+}$ and Ca$^{2+}$) by ion chromatography. Mass concentrations of particulate matters were $48.77 \pm 22.45 \mug/m^{3}$ at Kanghwa and $54.04 \pm 32.98 \mug/m^{3}$ at Yangyang and SO$_{4}^{2-}$, NO$_{3}^{-}$ and NH$_{4}^{+}$ contributed largely to water soluble ionic components. nss(non sea salt)-SO$_{4}^{2-}$, contributed more than 95 percentage to SO$_{4}^{2-}$ and nss-K$^{+}$ and nss-Ca$^{2+}$ also contributed high percentages to K$^{+}$ and Ca$^{2+}$. It was supposed that most SO$_{4}^{2-}$, was originated from anthropogenic sources, and K$^{+}$ and Ca$^{+}$ were mainty originated from soil. The results of factor analysis suggested possibility of interpreting the correlation between air pollutants and regional characteristics.

• 한국환경과학회지
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• 제5권4호
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• pp.429-440
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• 1996

A global carbon cycle model (GCCM), that incorporates interaction among the terrestrial biosphere, ocean, and atmosphere, was developed to study the carbon cycling aid global carbon budget, especially due to anthropogenic $CO_2$ emission. The model that is based on C, 13C and 14C mass balance, was calibrated with the observed $CO_2$ concentration, $\delta$13C and $\Delta$14C in the atmosphere, Δ14C in the soil, and $\Delta$14C in the ocean. Also, GCCM was constrained by the literature values of oceanic carbon uptake and CO, emissions from deforestation. Inputs (forcing functions in the model) were the C, 13C and 14C as $CO_2$ emissions from fossil fuel use, and 14C injection into the stratosphere by bomb-tests. The simulated annual carbon budget of 1980s due to anthropoRenic $CO_2$ shows that the global sources were 5.43 Gt-C/yr from fossil fuel use and 0.91 Gt-C/yr from deforestation, and the sinks were 3.29 Gt-C/yr in the atmosphere, 0.90 Gt-C/yr in the terrestrial biosphere and 2.15 Gt-C/yr in the ocean. The terrestrial biosphere is currently at zero net exchange with the atmosphere, but carbon is lost cia organic carbon runoff to the ocean. The model could be utilized for a variety of studies in $CO_2$ policy and management, climate modeling, $CO_2$ impacts, and crop models.

• 한국대기환경학회지
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• 제19권2호
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• pp.179-189
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• 2003

The concentration of gaseous elemental mercury (Hg) was measured concurrently with relevant environmental parameters from Yang-Jae monitoring station in Seoul during Sept. 1997 to June 2002. Although data collection was disrupted for certain periods, the grand mean concentration of Hg for this five year period was found at 5.32 $\pm$ 3.53 ng m$^{-3}$ (N = 27,170). Because of short resolution of data acquisition, we were able to examine the temporal variability of Hg at varying time scale. The diurnal variability of Hg, when investigated for each of those five years, indicated consistently the dominance of nighttime over daytime. If examined at seasonal scale, Hg level was systematically higher during winter/spring than summer/fall period. The results of this short-term variability were best explained by the combined effects of such factors as meteorological conditions (formation of inversion layer and seasonal changes) and anthropogenic source processes. However, examination of long-term variation Pattern was much more complicated to explain. Thus, extension of our study is needed to diagnose the future direction in long-term trend of Hg behavior.

• 한국대기환경학회지
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• 제1권1호
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• pp.71-82
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• 1985

The effect on the particulate matters in the atmosphere was investigated in Seoul area from March, 1984 to Aprill, 1985. Aerosols were collected by filters on nine stages Andrsen Air Sampler, and size distribution and total concentration of the aerosols, Fe and Pb were measured. In spring with Yellow Sand the concentration of particles in aerosols was 185.55$\mug/m^3$ and CP/TA was 65.9%. But in spring without Yellow Sand those of particles was 135.45$\mug/m^3$ and CP/TA was 58.6%. Accordingly the concentration of coarse particles with Yellow Sand was higher than without them in Spring. Above results indicate that in Seoul Area the main source of air pollution originated from natural burdens, especially from soil. The concentration of Pb was similarly valued through both seasons in Seoul area but fine particles valued above coarse particles. On the other hand, in urban area, the natural and anthropogenic sources have influenced on the concentration of Pb. With referred to particle size distribution for Fe, the concentration of coarse particles was 0.168$\etag/m^3$ (CP/TA: 74.3%) in Spring with Yellow Sand, 0.096$\mug/m^3$ (CP/TA: 71.6%) without Yellow Sand and 0.083$\mug/m^3$ (CP/TA: 67.4%) in winter, respectively. Compared with fine particles, all of them were higher. It indicated that the origin of coarse particles in urban air was not related to anthropogenic source. The concentration of Fe was influenced by Yellow Sand and contributed to air pollution.

• 한국대기환경학회지
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• 제16권4호
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• pp.415-420
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• 2000

The daily mean concentrations of PM2.5 mass ionic species carbonaceous species and HNO3, HCl, and NH3 were analyzed at three background sites in Korea : Kangwha, Kosan, and Dongbaik during two intensive field studies between December 1996 and January 1997, Four-day backward trajectory analysis was also carried out. The mean concentrations of anthropogenic species were higher at Kangwha and Dongbaik than Kosan. At these two sites themean concentrations of nitrate and ammonium/ammonia were higher than those of Kosan. It was suggested that these two sites be considered as the background sites of the Seoul Metropolitan Area and Pusan respectively. Major chemical components in fine particles were sulfate organic carbon nitrate and ammonium for all the sites. More than 90% of sulfate were non-sea-salt(nss) sulfates and most of the nss sulfate in PM2.5 might be present as ammonium sulfates at all sites. Most of air parcels arriving a Kangwha and Dongbaik were from the northern China. At Kosan during the measurement period half of air parcels were from the northern China and the other half from the southern China. At Kosan the concentrations of anthropogenic air pollutants originated from the southern China were higher than those typically observed from the northern China.