• 동아시아식생활학회지
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• 제10권6호
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• pp.507-513
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• 2000

This study was conducted to investigate the shelf life of beef stored in antimicrobial pottery during 12days storage at 4'C and Five kinds of antimicrobial potteries were prepared with antimicrobial materials such as TiO$_2$, Ag (NO$_3$)$_2$, Cu(NO$_3$)$_2$ and Zn(NO$_3$)$_2$. In changes of color during storage, Hunter's L- and b-value of beef were not changed, but Hunter's a-value was low significantly. The pH of beef meats were low at 6 days, but were added from 6 days. TBA value of beef in "A" pottery containing TiO$_2$ 1% and "C" Pottery containing TiO$_2$ 0.5%, Cu(NO$_3$)$_2$ were lower than "B", "D" and "I" pottery. VBN contents of beef in "A", "B", "C", "D" and "I" Pottery stored during 12 days were 9.8, 12.5, 9.3, 11.9 and 13.7mg%, respectively. In changes of total plate count of beef during storage at 4$^{\circ}C$, the antimicrobial activity of "A" and "C" pottery were superior.g storage at 4$^{\circ}C$, the antimicrobial activity of "A" and "C" pottery were superior.ttery were superior.

• 자원환경지질
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• 제39권6호
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• pp.675-687
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• 2006

이 연구에서는 청풍지역 하상퇴적물에 대한 지구화학적 특성 규명을 통해, 주성분원소 및 미량원소에 대한 청풍지역의 자연배경치를 제시하고, 지구화학적 재해에 대해 예견하고자 한다. 이를 위해 물이 흐르고 있는 1차 수계를 대상으로 하상퇴적물시료를 채취하였고, 실험실에서 자연건조 시켰으며, 화학적 분석을 위해 알루미나 몰타르를 이용하여 200메쉬 이하로 분쇄하였다. 주성분원소 및 미량성분원소는 XRD, XRF, ICP-AES, NAA를 이용하여 분석하였다. 청풍지역 하상퇴적물의 기반암에 따른 지질집단별 지구화학적 특성 비교를 위해, 화강암질편마암지역, 메타텍틱편마암지역, 다도응회암지역, 유치역암 지역, 능주용암지역으로 분류하였다. 청풍지역 하상퇴적물 전체에 대한 주성분원소 함량은 $SiO_2\;47.31{\sim}72.81\;wt.%,\;Al_2O_3 \;11.26{\sim}21.88\;wt.%,\;Fe_2O_3\;2.83{\sim}8.39\;wt.%,\;CaO\;0.34{\sim}7.54\;wt.%,\;MgO\; 0.55{\sim}3.59\;wt.%,\;K_2O\;1.71{\sim}4.31\;wt.%,\;Na_2O\;0.56{\sim}2.28\;wt.%,\;TiO_2\;0.46{\sim}1.24\;wt.%,\;MnO\;0.04{\sim}0.27\;wt.%,\;P_2O_5\;0.02{\sim}0.45\;wt.%$이다. 청풍지역 하상퇴적물 전체에 대한 미량성분원소 및 희토류원소 함량은 $Ba\;700ppm{\sim}8990ppm,\;Be\;1.0{\sim}3.50ppm,\;Cu\;6.20{\sim}60ppm,\;Nb\;12{\sim}28ppm,\;Ni\;4.4{\sim}61ppm,\;Pb\;13{\sim}34ppm,\;Sr\;65{\sim}787ppm,\;V\;4{\sim}98ppm,\;Zr\;32{\sim}164ppm,\;Li\;21{\sim}827ppm,\;Co\;3.68{\sim}65ppm,\;Cr\;16.7{\sim}409ppm,\;Cs\;72{\sim}37.1ppm,\;Hf\;4.99{\sim}49.2ppm,\;Rb\;71.9{\sim}649ppm,\;Sb\;0.16{\sim}5.03ppm,\;Sc\;4.97{\sim}5ppm,\;Zn\;26.3{\sim}375ppm,\;Ce\;60.6{\sim}373ppm,\;Eu\;0.82{\sim}6ppm,\;Yb\;0.71{\sim}10ppm$의 범위를 보였다.

• 분석과학
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• 제13권6호
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• pp.766-774
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• 2000

유도결합 플라스마 원자방출분광법(ICP-AES)을 이용하여 몽골산 크롬철광의 성분을 분석하였다. 크롬철광을 용해시키기 위하여 과염소산-인산의 흔합산과 융제로서 $Na_2O_2$의 적용성을 검토한 결과 최적의 용해방법은 용융법이었다. 크롬광의 주성분과 미량성분을 ICP-AES로 정량할 때 과량의 Na가 측정파장에 미치는 영향을 조사하였다. Al, Cr, Fe 및 Mg과 같은 주성분원소의 경우 Na가 250 mg/L까지 영향을 받지 않았으나, Co, Ni, Ti, V 및 Zn과 같은 미량성분들은 Na가 1,250 mg/L인 경우 측정원소와 파장에 따라 방출선의 세기는 1-5% 정도 감소하였다. 본 방법의 정확도를 확인하기 위하여 중성자방사화분석으로 얻은 결과와 상대편차를 비교하였다. $Al_2O_3$, $Cr_2O_3$, FeO 및 MgO의 경우에는 FeO를 제외하고 상대편차가 5% 이내이며, Co, Mn, V 및 Zn의 경우에는 ~20-8% 범위였다.

• 자원환경지질
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• 제34권1호
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• pp.55-70
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• 2001

영광-김제 지역에는 두 가지 형의 화강암류가 분포한다. 하나는 NE-SW방향의 광주단층계에 연하여 발달된 정읍, 고창엽리상화강암이고, 다른 하나는 광주단층계의 서편으로 발달괸 변형 되지 않은 김제화강암과 영광화강암이다. $SiO_2$의 함량은 영광화강암은 62.8~74.0% 고창엽리상화강암은 64.5~74.4%, 정읍엽리상화강암은 64.5~70.2% 김제화강암은 63.4~72.0% 으로, 이들 화강암류는 중성암과 산성암 영역에 포함된다. 하커의 변화도에서 $SiO_2$의 증가에 따라 $Al_2O_3$, $Fe_2O_3$, MgO, CaO, $TiO_2$, $P_2O_{5}$, MnO는 감소하는 경향을 보이고 $K_2$O는 증가하는 경향을 보이는데, 이와 같은 결과는 화강암류에서 보이는 정상적인 분화경향을 나타낸다. AFM 삼각도에서 보면 각 화강암류는 칼크 -알칼린계열에 속함을 알 수 있다. 화강암류들을 norm값으로 구분한 Qz-Or-Pl 삼각도와 An-Ab-Or삼각도에 도시해보면, 각각에서 화강섬록암과 화강암의 영역에 도시됨을 알 수 있다. 미량성분은 $SiO_2$의 증가에 따라 Ba, Co, Li, Nb, Zn, Rb는 증가하는 경향을 보여주고, ACF diagram 과 $Na_2O$ vs $K_2O$ 변화도에서 연구지역의 화강암류는 I-type에 속함을 알 수 있다.

• 한국지구과학회지
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• 제22권3호
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• pp.208-222
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• 2001

이 연구는 전남 광양광산과 그 주변의 하천에 형성되어 있는 부유성 비정질 퇴적물의 지구화학적 특성을 밝히기 위해 수행되었다. 부유성 비정질 퇴적물의 주요성분은 Fe$_2$O$_3$이며, Fe$_2$O$_3$의 함량은 17.9${\cdot}$72.3wt.% 범위로 나타난다. Fe함량이 증가하면 Si, Al, Mg, Na, K, Mn 및 Ti 함량이 감소하며 Te, Au, Ga, Bi, Cd, Hg, Sb, 및 Se등의 함량은 증가한다. 하상 침전물인 비정질 퇴적물에는 As(최대 54.9ppm), Bi(최대 3.77ppm), Cd(최대 3.65ppm), Hg(최대64ppm), Sb(최대 10.1ppm), Cu (최대 37.1ppm), Mo(최대 8.86ppm), Pb(최대 9.45ppm) 및 Zn(최대 29.7ppm) 등의 중금속원소가 농집되어 있다. 황갈색 침전물에는 Au(최대 4.40ppm)와 Ag(최대 0.24ppm) 함량이 매우 높게 나타나며, Au함량은 하천의 상류지역에 높은 함량을 보이다가 하류지역으로 갈수록 그 함량이 감소한다. 반면에 Ag 함량은 상류지역의 하천에 낮은 함량을 보이다가 하류지역으로 갈수록 그 함량이 증가하여 나타난다. XRD분석에서 하상의 황갈색 침전물은 X-선회절선이 뚜렷하지 않은 비정질이거나 결정도가 미약한 철수산화물로 밝혀졌으며, 석영, 침철석, 고령토, 일라이트 등이 관찰된다. IR분석에서 비정질 하상 퇴적물은 OH기, H$_2$O, SO$_4$ 및 Fe-O 기에 의한 흡수밴드가 관찰된다.

• 자원환경지질
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• 제31권4호
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• pp.297-310
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• 1998

Geochemical characteristics of environmental toxic elements at the Narim mine area were investigated on the basis of major, minor, rare earth element geochemistry and mineralogy. Ratios of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in soils and sediments range from 11.57 to 22.21 and from 1.86 to 3.93, and are partly negative and positive correlation against $SiO_2/Al_2O_3$ (3.41 to 4.78), respectively. These suggested that sediment source of host granitic gneiss could be due to rocks of high grade metamorphism originated by sedimentary rocks. Characteristics of some trace and rare earth elements of V/Ni (0.33 to 1.95), Ni/Co (2.00 to 6.50), Zr/Hf (11.27 to 53.10), La/Ce (0.44 to 0.55), Th/Yb (4.07 to 7.14), La/Th (2.35 to 3.93), $La_N/Yb_N$ (6.58 to 13.67), Co/Th (0.63 to 2.68), La/Sc (3.29 to 5.94) and Sc/Th (0.49 to 1.00) are revealed a narrow range and homogeneous compositions may be explained by simple source lithology. Major elements in all samples are enriched $Al_2O_3$, MgO, $TiO_2$ and LOI, especially $Fe_2O_3$ (mean=7.36 wt.%) in sediments than the composition of host granitic gneiss. The average enrichment indices of major and rare earth elements from the mining drainage are 2.05 and 2.91 of the sediments and are 2.02 and 2.60 of the soils, normalizing by composition of host granitic gneiss, respectively. Average composition (ppm) of minor and/or environmental toxic elements in sediments and soils are Ag=14 and 1, As=199 and 14, Cd=22 and 1, Cu=215 and 42, Pb=1770 and 65, Sb=18 and 3, Zn=3333 and 170, respectively, and extremely high concentrations are found in the subsurface sediments near the ore dump. Environmental toxic elements were strongly enriched in all samples, especially As, Cd, Cu, Pb, Sb and Zn. The level of enrichment was very severe in mining drainage sediments, while it was not so great in the soils. Based on the EPA value, enrichment index of toxic elements is 8.63 of mining drainage sediments and 0.54 of soils on the mining drainage. Mineral composition of soils and sediments near the mining area were partly variable being composed of quartz, mica, feldspar, amphibole, chlorite and clay minerals. From the gravity separated mineralogy, soils and sediments are composed of some pyrite, arsenopyrite, chalcopyrite, sphalerite, galena, goethite and various hydroxide minerals.

• Ocean and Polar Research
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• 제36권4호
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• pp.407-421
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• 2014

The benthic environmental impact experiment addresses environmental impacts at a specific site related to deep-sea mineral resource development. We have acquired several tens of multi- or box core samples at 31 sites within the Benthic environmental Impact Site (BIS) since 2010, aiming to examine the basic properties of surficial deep-sea sediment as a potential source for deep-water plumes. In this study, we present the geochemical properties such as major elements, rare earth elements (REEs), and heavy metal contents at the BIS. Such proxies vary distinctly according to the Facies association. The lithology of all core sediments in the BIS corresponds to both Association Ib and Association IIIb. The vertical profiles of some major elements ($SiO_2$, $Fe_2O_3$, CaO, $P_2O_5$, MgO, MnO) show noticeable differences between Association Ib and IIIb, while others ($Al_2O_3$, $TiO_2$, $Na_2O$, and $K_2O$) do not vary between Association Ib and IIIb. REEs are also distinctly different for Associations Ib and IIIb; in Association Ib, REY and HREE/LREE are uniform through the sediment section, while they increase downward in Association IIIb like the major elements; below a depth of 8 cm, REY is over 500 ppm. The metal enrichment factor (EF) evaluates the anthropogenic influences of some metals (Cu, Ni, Pb, Zn, and Cd) in marine sediments. In both Associations, the EF for Cu is over 1.5, the EF for Ni and Pb ranges from 0.5 to 1.5, and the EF for Zn and Cd are less than 0.5, indicating Cu is enriched but Zn and Cd are relatively depleted in the BIS. The vertical variations of geochemical properties between Association Ib and IIIb are shown to be clearly different, which seems to be related to the global climate changes such as the shift of Intertropical convergence zone (ITCZ).

• 자원환경지질
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• 제23권2호
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• pp.245-259
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• 1990

Petrochemical analyses of granitic rocks including trace element, REE and oxygen isotope were carried out to understand petrogenesis of plutonic rocks from the Chungju, Wolaksan and Jecheon granite batholiths, which might be related with tungsten-base metal-fluorite mineralization in the Hwanggangri metallogenic province. Different geochemical characteristics such as major and trace elements were found between Jurassic Daebo granitic rocks (Chungju, Jecheon, Wonju, and Boeun granitic rocks) and Cretaceous Bulgugsa granitic rocks (Wolaksan, Muamsa and Sokrisan granitic rocks). Cretaceous granitoids are characterized by high $SiO_2$and $K_2O$ contents and low $TiO_2$, $Al_2O_3$, MgO and CaO contents. They also have relatively high contents of trace elements(Zn, V, Co, Cr, Sr, and Ba) in comparison with the Jurassic granitoids. (Eu)/($Eu^*$) and $(La/Lu)_{CN}$ ratios of Jurassic plutons vary from 0.78 to 1.13 and from 26.02 to 30.5, respectively, while the ratios of Cretaceous ones range from 0.22 to 0.28 and from 4.42 to 14.2, respectively. The REE patterns of the Cretaceous and Jurassic granitic rocks have quite different Eu anomalies: large negative Eu anomaly in the former, and mild or absent Eu anomaly in the latter. The large Eu negative of Cretaceous granitic rocks are interpreted as a differentiated product of fractional crystallization of granitic magma deduced by Rayleigh fractionation model(Tsusue et al., 1987). Oxygen isotopic compositions of quartz for Daebo and Bulgugsa granitic rocks range from 9.98 to 10.51‰ and from 8.26 to 9.56‰, respectively. The Daebo granitic rocks enriched in $^{18}0$ suggest that the magma be undergone different partial melting processes from the Bulgugsa ones. Of the Bulgugsa granitoids, Wolaksan and Sokrisan mass have different contents of trace elements and ${\delta}\;^{18}0$ values of the silicate minerals, which indicate that they are not from the identical source of magma. Many mineral deposits are distributed in and/or near the Wolaksan and Muamsa granitic rocks, but a few mineral deposits are found in and near the Chungju and Jecheon granite batholiths. It might be depend on geochemisty of the related igneous rocks which have low contents of Ba, Sr, Co, V, Cr, Ni, Zn and high contents of Nb and Y, and on lithology of country rocks such as cabonate and noncarbonate rocks.