• 보존과학회지
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• 제16권
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• pp.89-103
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• 2004

우리나라 구석기 및 신석기 유적에서 출토된 흑요석 그리고 백두산과 일본 Kyushu지방에서 입수된 흑요석 원석 등 총 64점에 대하여 주요성분, 미량성분 및 자기적 특성을 이용하여 산지별로 분류하였다. 주요성분 중 $Al_2O_3,\;CaO,\;Na_2O+K_2O$의 농도값을 사용하여 흑요석을 분류한 결과 대부분의 흑요석이 Subalkaline 계열이었다. 또한 흑요석을 주요성분 및 미량성분 함량을 사용한 통계적 분류 결과 세 개의 그룹을 형성하였다. 이러한 결과는 각 그룹간의 상관관계가 없으며 산지가 다름을 의미한다. 자기적 특성을 이용한 산지분류에서는 각 지역별로 정확하게 그룹을 이루지 않았으나, 대자율과 포화등온잔류자화의 이 변량분석에서는 주요성분 및 미량성분을 이용한 산지분류와 유사한 결과를 얻었다.

• 한국환경보건학회지
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• 제27권4호
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• pp.63-71
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• 2001

PM 2.5/ samples were measured at two sites, Hadan(suburban site) and Anrak (roadside site) in Busan area. PM 2.5/ sampling was performed for 24-hour intervals by the FH9.5 particulate sampler. Aerosol samples were collected on PTFE filter. A total of 60 particulate samples were collected, dad samples were measured for Particulate mass concentration, metallic elements (Cr, Mn, Ni. Cu. Se, Fe, Pb, and Zn) and waer-soluble elements (C $l^{[-10]}$ , N $O_{3}$$^{[-10]}$ ,S $O_{4}$$^{2-}$, N $H_{4}$$^{+}$, $Ca_{2}$$^{+}$, $Mg_{2}$$^{+}$ and $^{+}$.Mass concentration in Hadan ranged 24.23~57.12 $\mu\textrm{g}$/㎥ and 60.22~72.12 $\mu\textrm{g}$/㎥m Yellow Sand Events. Major cations in Hadan and Anrak site is N $H_{4}$$^{+}$and N $a^{+}$ respectively. SO42$^{[-10]}$ was the abundant specie in the PM 2.5 fraction for Hadan site an dAnrak site. Hadan site showed igher concentration in S $O_{4}$$^{2.1}$ and N $H_{4}$ $^{+}$ In Anrak site the concentration of S $O_{4}$/sip 2-/and N $a^{+}$ was higher than other ions Prominent metallic elements were Fe and Pb in two sites. Principal component analysis showed that main source of PM 2.5 aerosol particles was non-metal related source which was resulted in relating elements as Cr, Ni, and Pb at Hadan site, Anrak site also has resulted PM2.5 aerosol paricles source, which was related its element like Zn, and Ni,. The SAS package analysis also showed that long-range transport effect at Hadan area due to Yellow Sand Event by the prevailing weaterlies.ling weaterlies.

• 보존과학연구
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• 통권10호
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• pp.1-40
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• 1989

Between 1976 and 1984 approximately 26.7 tons of Chinese coins were recovered from a shipwreck which was found at the seabed of the Shin an area in the south-western coast of the Korean peninsula. Elements, Cu, Pb, Sn, Fe, Sb, As, Zn, Ag, Ni, Co and Mn, of 54 pieces of the coins were determined by Inductively Coupled Plasma Atomic Emission Spectroscopy(ICP-AIS). The result shows that Ch, Pb, and Sn were found to be major elements roughly the coins with the ratio of 7 : 2 : 1, respectively. Trace elements were classified into 3 levels according to the avarage concentration : Fe,As and Sb(0.1-0.5%), Ag, Mi, Co and Zn(100-1000ppm) and Mn(10ppm). Some systematic tendencies are observed in the composition change with a function of their minting ages .The Wuzhu coins(오수전) from the Eastern Han dynasty(A.D.25-219 )are much more abundant in Cu than the coins of Tang dynasty(A.D.618-907) and later periods. Major element compositions of the Kai -tong Vuan-Bao(개통원보) coins from the Tang dynasty, were remarkably variable. In general, however, the Tang dynasty coins were much more abundant in Cu than the Song dynasty(A.S.S60-1279) coins. The amount of major elements Cu and Sn decreases while that of Pb in creasesby passage of age from the Bei Song dynasty(A.D.960-1127) to later Nam Song dynasty (A.D.1127-1279 ). It means that the quality of coins mere degraded. The amounts of trace elemends(Fe, As, Co, Hn) increases with the above age. High amounts of trace elements are supposed to be a reflection of immaturity of minting techniques or use of impurity-rich raw materials. The Jin dynasty(A.D.1125-1234) coins are found to be rich in Sn and thus contain Pb as the third component. It is quite different from the coins of the Song dynasty. The Zhi-dai Tong-Bao(지대통보) coins of the Yuan dynasty from A.0.1310 are much more abundant in Cu and Sn than those of the Nam Song dynasty .

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 추계학술발표회
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• pp.148-151
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• 2002

To clarify of chemical contents for the Keumsan ginseng, two attempts have been done for two year: 2 year and 4 year-ginsengs coilected from the phyllite(Ph0 and granite area(Gr), and 1 year, 2 year and 3 year-ginsengs collected from the phyllite(Ph), shale(Sh) and granite (Gr), In the first attempt, the soil contents of the Ph are high in most of elements. In the comparisons between ages of the ginseng, regardless the area, most of the elements are high in the 4 year and these trends are distinctive in the granite area. In the comparisons of the areas, 2 year-ginsengs of the Ph show high contents in the most of the elements. Comparisons between upper part(leaf and branch) and root part of the ginsengs show that in the 2 year-ginseng, the Gr is high in the root part and the Ph is high in the upper part, while in the 4 year-ginseng, most of the elements are high in the root part. Comparisons between contents of soil and ginsengs show similar in crease and decrese trends. However, the 2 year-ginsengs show clear differences between two areas while in the 4 year-ginseng, differences between the Gr and Ph is not clear. It suggest that the ginsengs absorb eligible element contents with ages, despite of clear content differences of the different soils. In the second attempt, the Gr shows high W, Pb, Th, U, Sn and B contents wlile Ph and Sh show high Ni, Cr, Co, Sc, V, As, Cu and Zn contents. In the comparisons between ages of the ginseng, regardless the area, most of the elements are high in the 2 year, especially in the Gr and Ph. In the comparisons of the areas, 2 year-ginsengs of the Gr show low contents in the most of the elements, and the S1 show higher Ni, V, Th and U contents than the Ph. 3 year-ginsengs of the Gr show low contents in the most of the elements, while the S1 show high contents in the most of elements. relative to the Ph. Comparisons between upper part and root part of the ginsengs show that in the ginseng, regardless the ages, the upper part is high. Comparisons between contents of soil and ginsengs show similar increase and decrese trends, and soil is low than the ginsengs in the most of the elements

• 한국수산과학회지
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• 제39권2호
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• pp.106-117
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• 2006

We measured the concentrations of organic matter and metallic elements (Al, Fe, Cr, Mn, Ni, Cu, Zn, As, Cd, Pb and Hg) in the surface sediments of Masan Harbor (in the southern sea, Korea) to evaluate the geochemical characters of sediment and the pollutions by organic matter and metallic elements. The mean grain size of the surface sediments in the study area ranged from $5.6{\phi}$ to $7.8{\phi}$, indicating silt sediment. The water content of the surface sediments exceeded 60% except at some stations. The contents of ignition loss (IL), total organic carbon (TOC) and total nitrogen (TN) ranged from 7.2-14.3%, 1.2-3.2%, and 0.10-0.28%, respectively. Based on the C/N ratios, the organic matter in the surface sediments of Masan Harbor may originate from terrigenous sources including fluvial inputs (mainly sewage in urban areas). The chemical oxygen demand (COD) and acid volatile sulfide (AVS) ranged from $11.3-29.9\;mgO_2/g\;dry$ and 0.20-4.47 mgS/g dry, respectively, and low concentrations were observed near a shipping route. In addition, the concentrations of metallic elements showed large spatial variations in Masan Harbor and the distributions of metallic elements were also comparable to those of organic matter. This implies that the distributions of organic matter and metallic elements in the surface sediments of Masan Harbor are mainly controlled by biogenic matter and artificial action (mainly dredging). In addition, we calculated the enrichment facto. (EF) and geoaccumulation index (Igeo) in order to evaluate pollution by metallic elements. The enrichment of metallic elements relative to Al was three to eighteen times higher at the study sites, compared to levels in the Earth's crust except for Fe, Ni and Mn. In addition, the Igeo class indicated that the surface sediments in the study area were moderately to strongly polluted in terms of metallic elements.

• 자원환경지질
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• 제45권3호
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• pp.217-235
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• 2012

본 연구에서는 2007년도 봄철 대전 지역에서 발생한 황사(황사 기간) 및 대기부유물(비황사 기간)의 미량원소의 지구화학적 특성과 정량적 오염정도를 평가하였다. 황사 내 미량원소의 함량은 황사발원지 토양의 평균 함량에 비하여 수십에서 수백 배 높은 함량을 보여주고 있으며, 비황사 시기의 대기부유물에서도 유사한 특성을 보이고 있어, 황사 시기뿐만 아니라 비황사 시기에도 중국으로부터 이동되는 오염물질의 영향을 받고 있음을 지시하고 있다. 입도별 미량원소의 함량은 $PM_{2.5}$에서 Cr, Cu, Pb, Zn, V, S, As, Cd, Co, Ni, Mo, Sb, Cs, Rb, Th, Sc, Y 등이, 그리고 TSP에서는 Zr, Sr, Ba, Li, Th, U 등의 함량이 가장 높은 것으로 나타났다. 황사의 S, Cd, Mo, Zn, Pb, Sb, Cu 및 Zr 함량은대기부유물과 큰 차이를 보이지 않으나, 대기오염으로 부화가 발생하지 않는 Li, Cs, Co, U, Cr, Ni, Rb, V, Th, Y, Sr, Sc 등은 황사에서 2-4.2배 높아졌다. 그러므로 이들 원소들을 황사발생의 지시원소로 사용할 수 있으며, 특히 Sr, V, Cr 및 Li 등은 황사 발생을 판단하기 위한 지시원소로 사용하기에 적합한 것으로 보인다. 한편 황사의 이동경로에 따른 미량원소의 함량을 살펴본 결과, 중국의 대도시 및 산업단지를 경유하여 국내 유입된 황사가, 북한을 경유하여 국내에 도달한 황사에 비해서, S, Cd, Zn, Pb, Cu, Mo 및 As 함량이 높게 나타나, 황사의 이동경로가 이들 미량원소 오염 여부 및 오염도를 결정하는데 중요한 역할을 하는 것으로 판단된다. 황사 및 대기부유물 내 미량원소의 부화지수(Enrichment factor)을 기준으로 오염정도를 분류한 결과, 환경재해 측면에서 가장 문제가 되는 미량원소는 S, Zn, Cu, Pb, As, Mo, Cd이며, 이들은 인간의 건강 뿐만 아니라, 오랜 기간 토양과 수계환경에 퇴적될 경우 환경오염으로 인한 주변 생태계에 해로운 영향을 미치게 될 것으로 판단된다.

• Journal of Microbiology
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• 제42권1호
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• pp.56-59
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• 2004

Together with the previous reports, my computer survey revealed that several bacteria contain six copies of the type group II intron IntA. The sequence analysis of IntAs showed the high level of homology in the nucleotide sequence (91.9-99.8%). The consensus sequence, 2,270 base pair long, was derived from the nucleotide sequences of all IntA members. The size of the open reading frame intA was 502 amino acids long, that is homologous to reverse transcriptase-like proteins encoded within the group II introns. It was reported that EPEC.IntA and Sf.IntA were inserted into IS911 and IS629, respectively. The sequence of the flanking region IntA was analyzed here. The data show the insertion of EC.IntA into IS629, the insertion of EHEC.IntA into IS3, the insertion of Yp.IntA into IS904-like sequence, and the insertion of EK12.IntA into IS911. Interestingly, these IS elements nested by IntAs were the members of IS3 family elements. The sequences of the IS3 members correspond to the OrfB with the DDE motif conserved in retroviral integrases. Alignment of the flanking sequences of IntAs revealed that the flanking regions -25 to + 10 of insertion sites, that are generally believed to be required for the retrohoming, were not strongly conserved. The data presented here suggests that the retrohoming pathway of IntA seems to differ from those of other group II introns.

• 한국대기환경학회지
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• 제20권2호
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• pp.143-151
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• 2004

The chemical composition of PM$_{2.5}$ was measured at Gosan, Jeju for two weeks each in November 2001 and spring 2002. In the latter part of the measurement period of November 2001, designated as the polluted period in this work, secondarily formed ion components as well as primarily emitted elemental carbon were high. PM$_{2.5}$ mass concentration was also high in this polluted period compared with the yellow sand period, in which daily average of PM $_{10}$ peaked up to 520 $\mu\textrm{g}$/㎥. Increase of major components of anthropogenic origin in the polluted period was not correlated with the variation in sea salt components while increase of crustal components in the yellow sand period was highly correlated with the variation in sea salt components. Trace elements were generally higher in the yellow sand period; however, toxic heavy metals such as zinc, cadmium and lead were the highest in the polluted period.d.d.d.

• 한국환경과학회지
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• 제11권9호
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• pp.881-895
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• 2002

Sediments and river waters form the channel of Hwasun-cheon were studied in sedimentological size and geochemical analyses of metallic elements for the purposes of identification of depositional environments and geochemical characteristics. The sizes of sediments are assigned to pebble to coarse sand in mean size and polymodal in distribution. And the sediments are poorly to very poorly sorted and positively skewed. According to the grain size distributions of the sediments, the Hwasun-cheon belongs to gravel-bed river on the basis of the grain size distribution of the sediments. The behaviors of metallic elements in the sediments mainly depend on not grain size distribution but the geology connected with geomorphological reliefs near the stream. Contamination indices(CI) of Zn, Cu and Pb are 2.83 to 6.96 with average 4.31 in the sediments. Hwasun-cheon is assigned to general stream type in accordance with water quality of physical factors and chemical characteristics by Piper's diagram. Though meaningful values of BOD, T-N, T-P were locally depicted near Masan-ri, Hwasun-eup and Jiseok-cheon areas, artificial metal concentration do not represent in the most area of the stream. Sediments and river water are considered that the relatively more or less high metallic contents in the stream are originated from coal mine and urban area.

• 한국결정성장학회지
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• 제13권6호
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• pp.315-319
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• 2003

양식된 해수진주와 담수진주의 품질, 수량, 색상 등과 특성을 알아보았다. XRF 측정에서는 Ca 화합물이 주성분이며 해수진주에서는 Sr이 담수진주는 Si, S, Ca, Mn, P 등의 원소가 더 많이 검출되었다. 이러한 차이는 해수와 담수에 녹아 있는 이온이 진주성분에 영향을 준 것으로 판단된다. FT-IR 측정에서 거의 동일한 구조적인 peak를 나타내지만 2344$\textrm {cm}^{-1}$에서 담수진주의 흡수대가 나타났다. 광원으로 He-Cd Laser 사용으로 455 nm에서 peak는 담수진주가 높았고, Ar Laser 사용으로 담수진주는 545 nm에서 해수진주는 570 nm에서의 peak가 높았다