황해와 북동중국해에는 중국의 황하와 양쯔강 그리고 한국의 강들로부터 많은 양의 부유물질이 공급되어 대륙붕 해역에 여러 개의 니질 퇴적체가 발달하고 있으나, 이들 퇴적체에서 두 기원을 설명할 수 있는 퇴적-지화학적 요인은 아직까지 명확하게 제시되고 있지 않다. 본 논문에서는 한국과 중국 기원 강 퇴적물의 주성분 원소의 함량 특성을 비교 연구하고, 그 결과를 토대로 황해와 북동중국해 퇴적물에 적용 가능한 기원지 추적자를 제시하였다. 본 연구를 위해 총 102개의 강과 연안 퇴적물에 대한 주성분 원소(Al, Fe, Mg, K, Ca, Na, Ti)들의 함량을 유도결합플라즈마 분석기를 이용하여 분석하였으며, 이와 함께 입도효과를 최소화하기위해 원시료를 실트(60∼20μm)와 점토 구간(<20μm)으로 분리하여 주성분 원소 함량과 스트론튬 동위원소 비(87Sr/86Sr)를 분석하였다. 연구결과, 새로운 방법의 입도보정을 통한 Fe/Al과 Mg/Al 함량 비는 매우 유용한 잠재적 추적자로 제시되며, 이러한 결과는 입자 분리된 실트와 점토 퇴적물에서 더욱 뚜렷하다. 또한 실트 구간의 퇴적물에서 한국 기원의 87Sr/86Sr 비는 0.7229∼0.7253(평균 0.7243) 범위로 중국 기원 퇴적물(0.7169∼0.7189, 평균 0.7179)과 뚜렷한 차이를 보여, 황해와 북동중국해에서 한국과 중국 기원의 퇴적물을 구분할 수 있는 중요한 지화학적 성분으로 평가된다. 이러한 잠재적 추적자들에 근거할 때, 한국 서남해에 발달하고 있는 니질 퇴적대의 전퇴적물은 한국과 중국의 혼합 기원으로 해석되나, 실트와 점토 구간의 퇴적물로 나누어 볼 때 그기원이 각각 다르게 나타났다. 즉, 점토 퇴적물은 한국과 중국의 혼합 기원으로, 실트 퇴적물은 한국 기원이 우세한 것으로 해석된다.

This study aimed to determine the elemental compositions of selected edible wild plant species, Hemerocallis fulva, Allium victorialis, Syneilesis palmata and Ligularia fischeri. The samples were dried, crushed, and subjected to microwave-assisted digestion. The macro and micro elements were analyzed by inductively coupled plasma-optical emission spectrometery (ICP-OES), and ICP-mass spectrometry (ICP-MS), respectively. The macro elements in the analyzed species decreased in the order K Ca P Mg S Fe Zn Na, and the micro elements ˃ ˃ ˃ ˃ ˃ ˃ ˃ followed the order Mn˃Ba˃Rb˃Cu˃Ni˃Ga˃Li˃Cr˃V˃Co˃Be˃Se. The percentage ratio of calcium content for potassium in the samples was 42.9% (A. victorialis) > 42.4% (S. palmata) > 33.8% (L. fischeri) > 25.3% (H. fulva). The calcium content was 13.7, 10.9, 6.4, and 2.9 times higher than the phosphorus content in S. palmata, L. fischeri, A. victorialis, and H. fulva, respectively (p<0.05). Manganese was the most predominant among the trace minerals, and it followed the order of A. victorialis > H. fulva > L. fischeri > S. palmata. In general, these wild plants are richer in calcium as compared to other common vegetables, and hence can be considered a good source for calcium that is lacking in Korean food products.

In this study, mass concentrations and chemical compositions of PM2.5, including water-soluble ions and elements were determined at the 1,100 m-highland of Mt. Hallasan in Jeju Island across four seasons from August 2013 to August 2014. The average mass concentration of PM2.5 was 12.5±8.41 /m3 with 45.8% of the contribution from eight water-soluble ionic species. Three ionic species (SO4 2-, NH4 +, and NO3 -) comprised 96.2% of the total concentration of ions contained in PM2.5 and were the dominant ions, accounting for 43.5% of the PM2.5 mass at Mt. Hallasan. On the basis of the mass concentration level, seasonal variation, enrichment factor, and relationship among elements, we can presume that Mg, K, Ca, Mn, Fe, Co, Sr, Ba, Nd, and Dy originated mainly from crust or soil and that V, Cr, Ni, Cu, Zn, As, Cd, and Pb were significantly enriched in PM2.5 owing to the effects of the anthropogenic emissions. These results and the local distribution of emission sources and topographic characteristics near this sampling site suggest that the compositions of PM2.5 collected at the 1100 m-highland of Mt. Hallasan were largely influenced by inflow from outside of Jeju Island.

The number concentrations, the mass concentrations and the elemental concentrations of PM10 have measured at Gosan site in Jeju, Korea, from March 2010 to December 2010. And the correlation and the factor analysis for the number, the mass and the elemental concentrations of PM10 are performed to identify their relationships and sources. The average PM10 number concentration is observed 246 particles/㎝3(35.7∼1,017 particles/㎝3) and the average PM10 mass concentration is shown 50.1 ㎍/㎥(16.7∼441.4 ㎍/㎥) during this experimental period. The number concentrations are significantly decreased with increasing particle size, hence the concentrations for the smaller particles less than 2.5 ㎛(PM2.5) are contributed 99.6% to the total PM10 number concentrations. The highest concentration of the 20 elements in PM10 determined in this study is shown by S with a mean value of 1,497 ng/㎥ and the lowest concentration of them is found by Cd with a mean value of 0.57 ng/㎥. The elements in PM10 are evidently classified into two group based on their concentrations: In group 1, including S>Na> Al>Fe>Ca>Mg>K, the elemental mean concentrations are higher than several hundred ng/㎥, on the other hand, the concentrations are lower than several ten ng/㎥ in group 2, including Zn>Mn>Ni>Ti>Cr>Co>Cu>Mo>Sr>Ba>V >Cd. The size-separated number concentrations are shown positively correlated with the mass concentrations in overall size ranges, although their correlation coefficients, which are monotonously increased or decreased with size range, are not high. The concentrations of the elements in group 1 are shown highly correlated with the mass concentrations, but the concentrations in group 2 are shown hardly correlated with the mass concentrations. The elements originated from natural sources have been predominantly related to the mass concentrations while the elements from anthropogenic sources have mainly affected on the number concentrations of PM10.

Characteristics and variations of chemical compositions in Co-rich crusts occurred in the EEZ of the Republic of Marshall Islands were reviewed. Correlation coefficient analysis, hierarchical cluster analysis, and Q-mode factor analysis for 62 samples were done in this study. All data were selected and gathered from the open file report of the cooperative cruise done by United States Geological Survey with Scripps Institute of Oceanography, University of Hawaii or Korea Ocean Research Development Institute. The average of crust thickness. Co content, and Ni content of 62 samples from the 21 seamounts were 30mm, 0.58 wt% and 0.40%, respectively. The mineral phases and associated elements assigned by correlation coefficients, cluster analysis and Q-mode factor analysis are following four. 1) CFA: P, Ca, CO2, Y, Sr: 2) Mn-oxide mineral: As, Mn, Co, Na: 3) Al-silicate mineral: Pd,Si, Al, Cu, Fe: 4) PGE-bearing mineral: Rh, Pt, Ir.