• 암석학회지
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• 제11권1호
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• pp.1-16
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• 2002

1/5만 포천-기산리도폭에 넓게 분포하는 쥬라기의 대보화강암류는 선캠브리아기의 편마암 복합체를 관입한다. 이들은 모우드 분석결과 거의가 몬조화강암에 해당하며, 구성광물특성상 흑운모화강암(Gb), 석류석흑운모화강암(Ggb) 그리고 복운모화강암(Gtm)으로 구분된다. 주변지역의 야외조사와 K-Ar 운모류 연령해석에 의하면 Ggb가 Gb를 관입하였으며 Gtm은 가장 후기로 해석된다. 연구대상인 Gb와 Ggb는 서브알카린과 캘크알칼린 계열의 산성암류이다. $SiO_2$ 증가에 따라 주 원소의 대부분이 완만한 부의 경향을 뚜렷히 가지나, $TiO_2$, MgO 및 CaO등은 두 개의 다소 다른 선상분포를 이룬다. 이와 더불어 선상의 분포경향을 이룬 AMF, Sr대 Ba 그리고 Rb-Ba-Sr 관계 등으로 미루어, 이들은 동일마그마에서 기원되었으며 Ggb가 Gb보다 분화후기의 산물로 해석된다. Sr 대 CaO와 Sr 대 $K_2O$는 모두 정의 관계를 이루나, Sr이 알칼리장석보다 사장석의 분별결정작용에 보다 더 관여한 경향을 이룬다. 콘드라이트 값으로 표준화한 변화도에서 이들은 LREE에서 HREE로 갈수록 점진적으로 뚜렷이 결핍된다. 그러나 Ggb의 한 개 시료는 HREE가 점이적 증가경향을 이루며, 이는 석류석의 수반에 의한 것으로 해석된다. Eu 부의 이상으로 미루어 Gb에 비해 Ggb에서 사장석의 분별결정작용이 매우 강하게 일어난 것으로 보인다. (Qz+Af) 대 Op의 모우드 상관도에서 Gb는 거의가 자철석 계열에, Ggb는 모두 티탄철석 계열에 속한다. 모우드 분석과 대자율 역산에서 Gb와 Ggb의 대자율은 각각 339.3 ${\mu}SI$와 2.3 ${\mu}SI$로써 뚜렷이 구분되며, 이는 각각 자철석과 흑운모가 주도하는 것으로 분석된다 Gb와 Ggb의 $SiO_2$는 각각 높은 함량과 좁은 범위값을, $K_2O/Na_2O$는 각각 1.29와 1.27을, 그리고 A/CNK 몰비는 거의가 1.05 이상의 값을 가진다. 그 밖에 ACF도와 대자율값에서도 모두 S-형에 속하는 암석성인적 특성을 보인다.

• 상하수도학회지
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• 제28권2호
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• pp.181-193
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• 2014

Various treatment system for residuals have applied to save water resources, but most of them were not be satisfied with legal standard consistently. In this study, submerged membrane treatment system was operated to treat water treatment plant residuals and operation parameters was evaluated. Result of this experiment, high concentration organic matters contributed to high increase Transmembrane pressure(TMP) of membrane system(from 0.05 bar to 0.35 bar). And backwash process was effective to stabilize membrane system operation. After Cleaning-In-Place(CIP), permeability was recovered about 100 % from first operation condition. Inorganic matters (Fe, Mn, Al, Ca, Mg) were not effective membrane filtration performance. The quality of residual treatment was satisfied with drinking water quality standard and a treated water from that system was suitable for water reuse.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2001년도 총회 및 춘계학술발표회
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• pp.182-186
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• 2001

An acid forest surface soil as a land farming medium was treated with a water plant alum sludge at 0 to 18%. Indian mustard was grown in the treated soil in a greenhouse for 5 weeks and watered with pH 4 tap water adjusted with a mixed acid (1HNO$_3$: 2H$_2$SO$_4$) during plant growth. Changes in soil property, leachate chemistry, plant growth, and plant uptake of elements by the sludge treatment were determined. The alum sludge treatment increased buffer capacity to acidity, hydraulic conductivity, water holding capacity, and phosphate adsorption of the soil and decreased bulk density and mobility of small particles. The sludge treatment reduced leaching of Al, Mg, K, Na, and root elongation. Plant did uptake less amount of the cations and P but more Ca with the sludge treatment.

• Ecology and Resilient Infrastructure
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• 제4권4호
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• pp.193-199
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• 2017

본 연구에서는 강산 및 강염기 유출사고가 발생하였을 때 육상생물의 생육에 영향을 미칠 수 있는 토양특성의 변화를 살펴보았다. 강산과 강염기 화학물질로 HCl과 NaOH을 선정하였으며 이들 물질을 토양과 반응시킨 후 토양의 토성, 비표면적, 유기물함량, pH, 양이온교환능력 및 치환성양이온 함량 변화를 측정하였다. 토양과 반응한 HCl 및 NaOH 농도가 각각 10 M과 1 M인 경우 (즉, 토양 1 g 당 50 mmol의 HCl이나 5 mmol의 NaOH가 유입된 경우) 유의한 수준의 토양 특성 변화가 관찰되었다. 10 M HCl 및 1 M NaOH 용액과 반응한 토양의 토성은 sandy loam에서 loamy sand로 변하였으며, 비표면적은 $5.84m^2/g$에서 각각 4.85 및 $1.92m^2/g$으로 감소하였다. 토양 유기물 함량은 3.23%에서 0.96 및 0.44%로 크게 감소하였으며, 반응 전 pH 5.05로 약산성인 토양의 pH는 각각 2.35 및 10.65로 변하였다. 토양 내 양이온교환능력은 10.27 cmol/kg에서 4.52 및 5.60 cmol/kg으로 크게 감소하였으며 $Na^+$을 제외한 알칼리성 양이온 ($K^+$, $Mg^{2+}$, $Ca^{2+}$)의 함량이 감소하였다. HCl과 반응한 경우 $Na^+$ 함량은 감소, $Al^{3+}$ 함량은 증가하였으나 반대로 NaOH와 반응한 경우 $Na^+$ 함량은 증가, $Al^{3+}$ 함량은 감소하였다. 높은 농도의 $Al^{3+}$과 $Na^+$은 각각 토양생물에게 직접적인 독성을 발현하거나 토양의 투수성을 감소시키고 중탄산염의 농도를 증가시켜 독성을 발현할 수 있다. 본 연구는 강산 및 강염기유출사고로 인하여 변화한 토양특성이 토양의 생태기능에 영향을 줄 수 있음을 보여준다.

• Geosciences Journal
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• 제22권6호
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• pp.989-1000
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• 2018

The provenance of the Central Yellow Sea Mud (CYSM) in the Yellow Sea has been attracted a great deal of attention over the last three decades, but a consensus is not yet reached. In this study, 101 surface sediment samples collected from the CYSM were investigated to determine provenance and transport mechanisms in the area using the clay minerals and major element components. The Huanghe sediments are characterized by higher smectite, but the Changjiang sediments are more abundant illite contents. Western Korean rivers contain more kaolinite and chlorite than do Chinese rivers. The Chinese rivers have higher $Fe_2O_3$, MgO, and CaO than the Korean rivers at the same $Al_2O_3$ concentration. Therefore, the clay minerals and major element concentrations can be useful indicator for the source. Based on our results, we suggest that the surface sediments in CYSM were composed mainly of Changjiang sediments, mixed a partly with sediments from the Huanghe and the western Korean rivers. Although the northwestern part of CYSM is proximate to the Huanghe, the contents of smectite and CaO were extremely low. It could be evidence that the Huanghe materials do not enter directly into the CYSM due to the Shandong Peninsula Front. Considering the oceanic circulation in the Yellow Sea, the Changjiang sediments could be transported eastward with the Changjiang Diluted Water and then mixed in CYSM via the Yellow Sea Warm Current (YSWC). Huanghe sediments could be provided by coastal currents (Shandong Coastal Current and Yellow Sea Coastal Current) and the YSWC. In addition, sediments from western Korean rivers might be supplied into the CYSM deposit via the Korean Coastal Current, Transversal Current, and YSWC.

• 한국전기전자재료학회논문지
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• 제26권8호
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• pp.597-601
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• 2013

The accelerated thermal aging of a CSPE were carried out for 0, 80.82, 161.63 days at $100^{\circ}C$, which are equal to 0, 40 and 80 years of aging at $50^{\circ}C$, respectively. The volume electrical resistivities of the seawater and freshwater flooding were measured through 3-terminal circuit diagram. The volume electrical resistivities of the 0y, 40y and 80y were $2.454{\times}10^{13}{\sim}1.377{\times}10^{14}{\Omega}{\cdot}cm$, $1.121{\times}10^{13}{\sim}7.529{\times}10^{13}{\Omega}{\cdot}cm$ and $1.284{\times}10^{13}{\sim}8.974{\times}10^{13}{\Omega}{\cdot}cm$ at room temperature, respectively. The dielectric constant of the 0y, 40y and 80y were 2.922~3.431, 2.613~3.285 and 2.921~3.332 at room temperature, respectively. It is certain that the ionic ($Na^+$, $Cl^-$, $Mg^{2+}$, ${SO_4}^{2-}$, $Ca^{2+}$, $K^+$) conduction current was formed by the salinity of the seawater. The volume electrical resistivity of the cleaned CSPE via freshwater trends slightly upward with the number of dried days at room temperature. As a result, the $CH_2$ component of thermally accelerated aged CSPE decreased after seawater and freshwater flooding for 5 days respectively, whereas the atoms such as Cl, O, Pb, Al, Si, Sb, S related with the conducting ion ($Na^+$, $Cl^-$, $Mg^{2+}$, ${SO_4}^{2-}$, $Ca^{2+}$, $K^+$) component increased relatively.

• Journal of Chest Surgery
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• 제29권12호
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• pp.1299-1305
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• 1996

고칼륨과 저온이 혈관내피세포의 acetylcholine(Ach)에 의한 혈관이완에 미치는 영향을 알아보기 위하여 흰쥐의 흉부 대동맥을 이용하여 Ach과 sodium nitroprusside(SNP)에 대한 이완 반응을 측정하였다. 실험은 다섯 군으로 나누어서 실시하였으며 각 군을 10례로 하였다. 1군은 대조군으로 어떤 조작도 가하지 않고 organ bath에서 등랑성 긴장도를 측정하였고, 2군(내피세포 제거군)은 내피세포를 물리적으로 제거후 1군과 같은 방법으로 긴장도를 측정하였고, 37$^{\circ}C$ 57에 45분간 처리후 혈관의 등장성 긴장도를 측정하였다. 대조군, 457,4mST및 3757군에서의 Ach에 대한 혈관의 이완은 유의한 차이가 없었으며,내피세포 제거군에서는 Ach에 대한 혈관의 이완이 대조군에 비해 현저하게 감소되었으며, SUP에 대한 혈관의 이완은 모든 군에서 유의한 차이가 없었다. 이에 저자들은 다음과 같은 결론을 내릴 수 있었다. 고농도의 칼륨과 저온자체는 흰쥐의 흉부대동맥 내피세포의 Ach에 대한 이완능을 저해하지 않는다.

• 자원환경지질
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• 제23권1호
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• pp.35-57
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• 1990

This study has been carried out on the Pegmatites, Naedeogri Granites, Nonggeori Granites and Metasedimentary rocks in the middle area of Taebaeksan region to investigate the geochemical properties and possibility of productivity. Pegmatites are characterized by metamorphosed anatectic pegmatite and differentiated magmatic pegmatite, and are mixed type of rare-element pegmatite and mica-bearing pegmatite by the classification of Ginsburg(1979). The petrological type of the igneous rocks is thought to be calcalkali, subalkaline and peralumious. According to chemical variations against D. I., differentiation trends from Naedeogri and Nonggeori Granites through non-mineralized pegmatites to mineralized pegmatites are supposed. From the relationship between oxided and $SiO_2$, pegmatites and Nonggeori Granite have shown similar tendencies and bulk composition of pegmatites and similar to metasedimentary rocks near the intrusives. By judging the correlations of trace elements, it is elucidated that pegmatites adjacent to Naedeogri and Nonggeori Granites have been originated in magma differentiation from these granites and the others have been differentiated by remelting or partial melting from metasedimentary rocks. $Sp_5$, $Sp_8$, and $Sp_9$ pegmatites are considered as productive rocks, and $Sp_4$, $Sp_6$, $Sp_7$, $Sp_{10}$, $Sp_{11}$, and $Sp_{12}$ pegmatites and granites are supposed to have a weak productivity, in terms of element ratios related with Sn mineralizations. Tourmalines in productive pegmatites are formed under the circumstance of Li-poor granitoids and associated with pegmatites, and the others are seemed to be originated in metapelites and metapsammites which are not coexisting with an Al-saturating phase. Three types of chemical zoning are noticed in tourmalines: (1) apparently homogeneous compositional patterns, (2) a continuous core-to-rim zoning and, (3) a discontinuous core-to-rim zoning. From results of EPMA of tourmalines, Al, Mg and Ca increase closer to rim, while Fe decreases.

• Nuclear Engineering and Technology
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• 제53권1호
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• pp.282-293
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• 2021

This paper examines gamma-ray shielding properties of SBC-Bx glass system with the chemical composition of 40SiO₂-10B₂O₃-xBaO-(45-x)CaO- yZnO- zMgO (where x = 0, 10, 20, 30, and 35 mol% and y = z = 6 mol%). Mass attenuation coefficient (µ/ρ) which is an essential parameter to study gamma-ray shielding properties was obtained in the photon energy range of 0.015-15 MeV using PHITS Monte Carlo code for the proposed glasses. The obtained results were compared with those calculated by WinXCOM program. Both the values of PHITS code and WinXCOM program were observed in very good agreement. The (µ/ρ values were then used to derive mean free path (MFP), electron density (N_eff), effective atomic number (Z_eff), and half value layer (HVL) for all the glasses involved. Additionally, G-P method was employed to estimate exposure buildup factor (EBF) for each glass in the energy range of 0.015-15 MeV up to penetration depths of 40 mfp. The results reveal that gamma-ray shielding effectiveness of the SBC-Bx glasses evolves with increasing BaO content in the glass sample. Such that SBC-B35 glass has superior shielding capacity against gamma-rays among the studied glasses. Gamma-ray shielding properties of SBC-B35 glass were compared with different conventional shielding materials, commercial glasses, and newly developed HMO glasse. Therefore, the investigated glasses have potential uses in gamma shielding applications.

• 자원환경지질
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• 제56권6호
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• pp.745-764
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• 2023

In the Republic of Congo, Banded iron formations (BIFs) occur in two areas: the Chaillu Massif and the Ivindo Basement Complex, which are segments of the Archean Congo craton outcropping in the northwestern and southwestern parts of the country. They show interesting potential with significant mineral resources reaching 2 Bt and grades up to 60% Fe. BIFs consist mostly of oxide-rich facies (hematite/magnetite), but carbonate-rich facies are also highlighted. They are found across the country within the similar geological sequences composed of amphibolites, gneisses and greenschists. The Post-Archean Australian Shale (PAAS)-normalized patterns of BIFs show enrichment in elements such as SiO₂, Fe₂O₃, CaO, P₂O₅, Cr, Cu, Zn, Nb, Hf, U and depletion in TiO₂, Al₂O₃, MgO, Na₂O, K₂O, Sc, Th, Ba, Zr, Rb, Ni, V. REE diagrams show slight light REEs (rare earth elements; LREEs) compared to heavy REEs (HREEs), and positive La and Eu anomalies. The lithological associations, as well as the very high (Eu/Eu^*)_SN ratios> 1.8 shown by the BIFs, suggest that they are related to Algoma-type BIFs. The positive correlations between Zr and TiO₂, Al₂O₃, Hf suggest that the contamination comes mainly from felsic rocks, while the absence of correlations between MgO and Cr, Ni argues for negligeable contributions from mafic sources. Pr/Pr^* vs. Ce/Ce^* diagram indicates that the Congolese BIFs were formed in basins with redox heterogeneity, which varies from suboxic to anoxic and from oxic to anoxic conditions. They were formed through hydrothermal vents in the seawater, with relatively low proportions of detrital inputs derived from igneous sources through continental weathering. Some Congolese BIFs show high contents in Cr, Ni and Cu, which suggest that iron (Fe) and silicon (Si) have been leached through hydrothermal processes associated with submarine volcanism. We discussed their tectonic setting and depositional environment and proposed that they were deposited in extensional back-arc basins, which also recorded hydrothermal vent fluids.