• 자원환경지질
• /
• 제25권3호
• /
• pp.317-336
• /
• 1992

The garden soils, main road dusts, residential road dusts, and playground soils/dusts of Seoul, Geumsan, Onsan, and Taebaek areas were analyzed in order to investigate the level of heavy metal pollution by urbanization and industrialization. The soil pH is in the range of 5.48~8.40 and was generally neutral. The color of soils and dusts is mainly Raw Umber to dark greyish Raw Umber. Some samples from Taebaek city, a coal mining area, showed a deep black color due to contamination by coal dusts. Major minerals of the dusts and soils are quartz, feldspars, and micas, reflecting the composition of the parent rocks. However, pyrite was found as a major mineral in the samples of industrial road dusts of Onsan, a smelting area, and resicential road dusts of Taebaek. Thus, the high level of heavy metals in mining and smelting areas can be explained with the sulfide minerals. The mode of occurences of heavy metals in Seoul, a comprehensive urbanized area, were related to the metallic pollutants and organic materials through observation by scanning eletron microscopy. In main road and residential road dusts of Onsan area, Cd, Zn, and Cu were extremely high. Some industrial road and residential road dusts of Seoul area showed high Cu, Zn, and Pb contents, wereas some garden soils and residential road dusts of Taebaek area were high in As content. In general, the heavy metal contents in dust samples were two to three times higher than those in soil samples. Main road dust samples were the most reflective from the discriminant analysis of multi-element data. Cadmium, Sb, and Se in Onsan area, As in Taebaek area, Pb and Te in Seoul area were most characteristic in discriminating the studied areas. Therefore, Cd in smelting areas, As in coal mining areas, and Pb in metropolitan areas can be suggested as the characteristic elements of each pollution pattern. The dispersion of heavy metal elements in urban areas tends to orignate in main roads and deposit in garden soils through the atmosphere and residential roads. The heavy metal contamination in Seoul is characteristic in areas with high population, factory, road, and traffic decsities. Heavy metal contents are high in the vicinity of smelters in Onsan area and are decayed to background levels from one kilometer away from the smelters.

• Environmental Engineering Research
• /
• 제22권1호
• /
• pp.31-39
• /
• 2017

The primary purpose of this research is to understand those elements that define heavy metals contamination and to propose a novel assessment method based on principal component analysis (PCA) in the Yangping River region of Lingbao City, China. This paper makes detailed calculations regarding such factors the single-factor assessment ($P_i$) and Nemerow's multi-factor index ($P_N$) of heavy metals found in the surface water of the Yangping River. The maximum values of $P_i$ (Cd) and $P_i$ (Pb) were determined to be 892.000 and 113.800 respectively. The maximum value of $P_N$ was calculated to be 639.836. The results of Pearson's correlation analysis, hierarchical cluster analysis, and PCA indicated heavy metal groupings as follows: Cu, Pb, Zn and As, Hg, Cd. The PCA-based pollution index ($P_{an}$) of samplings was subsequently calculated. The relative coefficient square was valued at 0.996 between $P_{an}$ and $P_N$, which indicated that $P_{an}$ is able to serve as a new heavy metal pollution index; not only this index able to eliminate the influence of the maximum value of $P_i$, but further, this index contains the principal component elements needed to evaluate heavy metal pollution levels.

• 자원환경지질
• /
• 제36권1호
• /
• pp.17-25
• /
• 2003

동명광산을 경유하는 수계의 pH는 5.9∼7.1의 변화를 보여 약산성 내지는 중성의 환경을 보인다. 하천수 중 중금속 원소함량의 분포는 자원소의 지구화학적 특성에 따라 다양한 분포 양상을 보이나 전반적으로 폐광산 주변에서 증가하는 경향을 보인다. 동명광산 지역의 광미, 폐석적치장토양, 농경지토양에 대한 성분분석 결과 농경지토양에는 중금속의 총 농토가 광미나 폐석적치장의 토양보다 훨씬 낮았을 뿐 아니라 총 중금속 농도 중 adsorbed, carbonate, reducible fraction들이 차지하는 비율이 낮아 이들이 농작물이나 주변 수계에 큰 영향을 미치지 못할 것으로 생각된다. 그러나 하천수중 중금속 원소함량 분포가 전반적으로 광산지역에서 증가하는 경향을 보이며, 광미나 폐석적치장 토양에서도 중금속의 총 농도가 매우 높았을 뿐 아니라 adsorbed, carbonate, reducible fractions들이 차지하는 비율이 농경지 보다 상대적으로 높았기 때문에 이들이 유실되거나 또는 산성우, 산성인 광산폐수의 유입 등으로 인해 화학적 환경변화가 발생할 경우 중금속 오염의 확산이 우려되므로 이에 대한 오염방지대책이 필요하다고 생각된다.

• 자원환경지질
• /
• 제37권1호
• /
• pp.21-33
• /
• 2004

이 연구의 목적은 국내의 휴폐광 금속광산의 중금속 오염을 종합적으로 평가하는 것이다. 그 동안 정부와 지방자치단체 및 개별 연구자에 의해 이루어진 휴폐광 금속광산의 중금속 오염도를 종합적으로 조사한 결과, 주요 오염물질은 광미를 포함한 광산폐기물이었다. 이들로부터 다양한 유독성 물질, 특히 As, Cd, Cu, Pb 및 Zn 등이 바람과 물에 의해 하부 수계로 이동되어 환경문제를 일으키고 있다. 그 결과 많은 광산들 주변에서 다량의 As 및 중금속이 검출되었으며, 일부는 토양환경보전법의 우려기준 및 대책기준을 초과하고 있다. 초과 항목 중에서는 비소의 초과 빈도가 가장 높았으며 그 다음으로 Cd, Cu, Pb, Zn 등의 오염 빈도도 높은 편이었다. 국가에서 지속적인 광해방지사업을 시행함에도 불구하고 아직도 많은 광산에서 오염물질이 배출되고 있는 실정이다. 특히, 다양한 추출법을 적용하여 오염물질의 추출량을 조사한 결과, 광미 및 토양은 지구화학적 특성을 잘 반영하고 있다. 종합적으로 볼 때, 정부주도로 휴폐광산의 관리를 위한 전담기구의 설치가 필요하다.

• 분석과학
• /
• 제13권1호
• /
• pp.96-100
• /
• 2000

제올라이트를 사용하여 폐수로부터 중금속 원소들을 제거하기 위하여 조건을 변화시키며 흡착 특성을 조사하였다. 시험한 원소는 독성이 강하여 중금속 오염과 관련이 많은 Cd, Cr, Cu, Pb의 네 가지 중금속 원소들을 선택하였다. 흡착에 영향을 주는 요소로서 제올라이트의 양, 흡착 시간 그리고 pH를 변화시키며 흡착에 의한 제거 효율을 측정하였다. 중금속 용액 50 mL에 대하여 투입된 제올라이트는 2 g 정도가 경제적인 분량이며, 흡착 시간은 30분 정도 반응시키면 최대 흡착을 얻을 수 있었다. Cr과 Cu는 전반적으로 높은 흡착율을 나타내며 낮은 pH 영역에서는 흡착효율이 보다 증가하였다. Cd와 Pb는 95% 내외의 약간 낮은 흡착율을 보이며, Cd는 pH가 낮으면 흡착율이 감소하는 특이한 경향을 보였다.

• Nuclear Engineering and Technology
• /
• 제50권1호
• /
• pp.80-87
• /
• 2018

Consideration is given to the possibility to use changes in buoyancy as a negative reactivity feedback mechanism during temperature transients in heavy liquid metal fast reactors. It is shown that by the proper use of heavy pellets in the fuel elements, fuel rods could be endowed with a passive self-ejection mechanism and then with a negative feedback. A first estimate of the feasibility of the mechanism is calculated by using a simplified geometry and model. If in addition, a neutron poison pellet is introduced at the bottom of the fuel, then when the fuel element is displaced upward by buoyancy force, the reactivity will be reduced not only by disassembly of the core but also by introducing the neutron poison from the bottom. The use of induced buoyancy opens up the possibility of introducing greater amounts of actinides into the core, as well as providing a palliative solution to the problem of positive coolant temperature reactivity coefficients that could be featured by the heavy liquid metal fast reactors.

• 한국해양학회지
• /
• 제18권1호
• /
• pp.29-42
• /
• 1983

濟州道周圍 大陸棚地域과 韓半島 南海沿岸에서 總 39個의 海底堆積物中의 重金屬含量이 測定되었다. 濟州道周圍의 平均含量은 Zn 59.1ppm, Mn 362.6ppm, Cr 63.8ppmiouPb 15-7ppm, Co 10.0ppm, Ni 28.9ppm, Cu 10.5ppm, Fe 2.7%로 나타났다. 南海沿岸에서는 Zn 79.5ppm, Mn 384ppm, Pb 8.6ppm, Ni 17.8ppm, Cu 23.2ppm, Fe 1.59%로 나타났다. 濟州道周圍에서는 細粒質堆積物이 分布하는 北西部가 기타 地域에 比해 높다. 反面 南海沿岸에서는 地域的 傾向成이 나타나지 않지만 馬山灣과 鎭海灣은 周圍隣近陸上의 産業活動에 의한 影響으로 他地域에 比해 높게 나타난다. 그러나 馬山灣과 鎭海內灣에서 Zn과 cu의 高含量을 除外 하고는 全體的으로 世界沿岸堆積物의 平均치에 미치지 못하는 낮은 含量이다. 각 表示成分間의 相關性은 濟州道周圍에서 Zn-Cu, Ni-Cu, Fe-cu, Cr-Cu, Co-Zn, Ni-Zn, Cr-Zn, Ni-Co, Fe-Co, Cr-Co, Fe-Ni, Cr-Ni, Cr-Fe간에 密集한 正의 相關性이 나타나며, Pb, Mn을 除外한 全元元素成分이 粒度와 良好한 正의 相關性을 나타내 粒子가 細立일수록 元素의 吸着率이 크다. 南海沿岸에서는 Cu-Zn, Cu-ni 및 Ni-Mn를 除外하고는 相關關係가 不良하다. 이는 堆積環境이 地域別로 다르고 또한 陸上의 人爲的 活動에 따른 流入含量의 差異에서 온 것으로 생각된다.

• 대한용접접합학회:학술대회논문집
• /
• 대한용접접합학회 2000년도 특별강연 및 춘계학술발표대회 개요집
• /
• pp.292-294
• /
• 2000

• 자원환경지질
• /
• 제33권2호
• /
• pp.91-100
• /
• 2000

It has been more than ten years since Dukun mine was abandoned. Tailings of waste deposits and slime dumps in the abandoned Dukum mine have been left to be deserted for fifty years. The results of fifty years of neglecting are nothing short of major environmental problems. Slime dumps have been exposed to air and water in the mine over ten years and then soil profile has been formed well. Soil in the upper layer (A horizon) is the light gray color due to the leaching of cations. Soil in the lower layer (A2 horizon, 0.2∼0.3m)is tinted with reddish brown and yellowish brown color due to the development of iron oxides and iron hydroxides. Soil in the lower part of B horizon of (1.0∼3.0m) with the growth of copper and zinc oxides exposes to the bluish green, light blue, and dark gray. Ranging from 3m to 8m in depth, 85 samples were taken from 22 sampling sites with 50m intervals located on the slime dump area with hand auger and trench (open cut). As tailings was distributed, heavy metal elements extracted by the process of surface water and ground water move and disperse in to the hydrosphere. Waste dumps were distributed in and around the mine and water draining from those dumps be a potential source of contamination. Soils, thus, can be dispersed into downslope and downstream through wind and water by clastic movement. These materials may be deposited in another horizon if the water is withdrawn, or if the materials are precipitated as a result of differences in pH, or other conditions in deeper horizons. These were primarily associated with acid mine drainage. The characteristics and rate of release of acid mine drainage are influenced by various chemical and biological reactions at the source of acid generations. Prolonged extration of heavy metal elements has a detrimental effect on the agricultural land and residental area. Twenty soil samples were collected from the agricultural land in the area (0∼30 cm). Seventeen samples were also taken from the sediment in the stream running alongside the dumps. The dispersion patterns of heavy metal elements are as follows: The content of As ranged 2∼6 ppm in a horizon, 20∼125 ppm in B horizon with large amount of clay mineral is concentrated and the content of Cd ranged 1∼2 ppm in A horizon, 4∼22 ppm in B horizon. Like Cd, the content of As, Cu, Zn, Pb in B horizon is higher than that in A horizon (approximately 5∼100 times). When soil formation proceeds in stages, it is necessary to investicate the B horizon with the concentration of heavy metal and preventive measures will have to established.

• 한국수산과학회지
• /
• 제44권6호
• /
• pp.772-784
• /
• 2011

We measured grain size, organic matter, and metallic elements (Fe, Cu, Pb, Zn, Cd, Cr, Mn, Hg, and As) in intertidal sediments collected from six islands in the western part of Jellanam Province in order to evaluate heavy metal contamination in the tidal flat sediments of coastal islands. The evaluation of metal contamination was carried out using geochemical assessment techniques such as sediment quality guidelines (SQGs), enrichment factor (EF), and geoaccumulation index ($I_{geo}$). Surface sediments were classified into four sedimentary facies: sand, gravelly muddy sand, slightly gravelly mud, and silt. The concentrations of heavy metals in intertidal sediments from Jaeun, Amtae, Biguem, and Docho islands showed good positive correlations with mean grain size and ignition loss, indicating that the concentrations of metallic elements in these sediments were dependent on grain size and the organic matter content. The concentrations of heavy metals in sediments from almost all of the stations were lower than two criterion values proposed by the National Oceanic and Atmospheric Administration (NOAA) in the United States. Based on the EF and $I_{geo}$ results, surface sediments were a little polluted for Cr and were moderately polluted for As. Our results suggest that more intensive studies are necessary in the future in order to determine the major source of As in intertidal sediment and to evaluate the As pollution level in macrobenthos.