• 자원환경지질
• /
• 제32권6호
• /
• pp.611-631
• /
• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 한국전기전자재료학회:학술대회논문집
• /
• 한국전기전자재료학회 2005년도 하계학술대회 논문집 Vol.6
• /
• pp.330-331
• /
• 2005

본 논문에서는 카메라폰용 광학중(Optical zooming) 과 자동초점조절장치 (Auto Focusing, AF)에 쓰일 초음파모터를 제작하였다. 초음파모터의제작 및 시뮬레이션은 유한요소해석 프로그램인 ATILA 5.2.1 (Magsoft co.)를 사용하여 디자인설계에 따른 구동특성을 고찰하였고 제작된 초음파모터는 한쪽 면이 없는 사작형의 탄성체를 제작하였으며 탄성체의 양쪽 다리에 각각 압전체를 부착하였다. 또한 압전세라믹의 조성은 $0.9Pb(Zr_{0.51}Ti_{0.49})O_3-0.1Pb(Mn_{1/3}Nb_{1/3}Sb_{1/3})O_3$의 조성으로 설계하였고 시편의 제조는 7-layer로 적층하였다. 제작된 압전세라믹의 치수는 6*2*0.35$mm^3$(길이*폭*두께)로 제작하였다 또한 탄성체의 외형치수는 10*10*2$mm^3$로 제작하였으며 두께를 각각 0.3[mm], 0.5[mm], 0.8[mm]으로 변화시키며 제작하였다. 두께가 0.8[mm]인경우 공진주파수는 60.5[kHz]를 나타내었으며 초음파모터의 압전세라믹에 인가전압이 증가함에 따라 회전속도와 모터에 흐르는 전류는 증가하였다. 인가전압이 40[Vpp] 일 때 회전속도는 206[rpm] 이며 소비전력은 0.3[W]로 제작된 시편은 카메라폰용 광학중 및 자동초점조절장치시스템 분야에 응용이 가능하다.

• Transactions on Electrical and Electronic Materials
• /
• 제18권4호
• /
• pp.181-184
• /
• 2017

Multilayer ceramics in which piezoelectric layers of $0.90Pb(Zr_{0.48}Ti_{0.52})O_3-0.05Pb(Mn_{1/3}Sb_{2/3})O_3-0.05Pb(Zn_{1/3}Nb_{2/3})O_3$ (0.90PZT-0.05PMS-0.05PZN) stack alternately with silver electrode layers were prepared by an advanced low-temperature co-fired ceramic (LTCC) method. The electrical properties and bonding strength of the multilayers were associated with the interface morphologies between the piezoelectric and silver-electrode layers. Usually, the inner silver electrodes are fabricated by sintering silver paste in multi-layer stacks. To improve the interface bonding strength, piezoelectric powders of 0.90PZT-0.05PMS-0.05PZN with an average particle size of $23{\mu}m$ were added to silver paste to form a gradient interface. SEM observation indicated clear interfaces in multilayer ceramics without powder addition. With the increase of piezoelectric powder addition in the silver paste, gradient interfaces were successfully obtained. The multilayer ceramics with gradient interfaces present greater bonding strength as well as excellent piezoelectric properties for 30~40 wt% of added powder. On the other hand, over addition greatly increased the resistance of the inner silver electrodes, leading to a piezoelectric behavior like that of bulk ceramics in multilayers.

• International Journal of Oral Biology
• /
• 제49권1호
• /
• pp.1-9
• /
• 2024

Oral bacterial infections substantially affect the development of various periodontal diseases and oral cancers. However, the molecular mechanisms underlying the association between Fusobacterium nucleatum (F. nucleatum ), a major periodontitis (PT)-associated pathogen, and these diseases require extensive research. Previously, our RNA-sequencing analysis identified a few hundred differentially expressed genes in patients with PT and peri-implantitis (PI) than in healthy controls. Thus, in the present study using oral squamous cell carcinoma (OSCC) cells, we aimed to evaluate the effect of F. nucleatum infection on genes that are differentially regulated in patients with PT and PI. Human oral squamous cell carcinoma cell lines OSC-2O, HSC-4, and HN22 were used. These cells were infected with F. nucleatum at a multiplicity of infection of 100 for 3 hours at 37℃ in 5% CO₂. Gene expression was then measured using reverse-transcription polymerase chain reaction. Among 18 genes tested, the expression of CSF3, an inflammation-related cytokine, was increased by F. nucleatum infection. Additionally, F. nucleatum infection increased the phosphorylation of AKT, p38 MAPK, and JNK in OSC-20 cells. Treatment with p38 MAPK (SB202190) and JNK (SP600125) inhibitors reduced the enhanced CSF3 expression induced by F. nucleatum infection. Overall, this study demonstrated that F. nucleatum promotes CSF3 expression in OSCC cells through p38 MAPK and JNK signaling pathways, suggesting that p38 MAPK and JNK inhibitors may help treat F. nucleatum-related periodontal diseases by suppressing CSF3 expression.

• 대한전자공학회논문지SD
• /
• 제44권8호
• /
• pp.38-44
• /
• 2007

본 논문에서는 무선통신용 송신기에 적용 가능한 12비트 80MHz 전류구동 방식의 D/A 변환기를 설계하였다. 제안된 회로는 3비트 온도계 디코더 회로 4개를 병렬 연결한 혼합형 구조를 채택하였다. 제안된 D/A 변환기는 0.35um CMOS n-well 디지털 표준 공정을 사용하여 구현하였으며, 측정된 INL/DNL은 ${\pm}1.36SB/{\pm}0.62LSB$ 이하이며, 글리치 에너지는 $46pV{\cdot}s$이다. 샘플링 주파수 80MHz, 입력 주파수 19MHz에서 SNR과 SFDR은 58.5dB, 64.97dB로 측정되었다. 전력소모는 99mW로 나타났다. 본 논문에서 구현한 12비트 80MHz 전류구동 혼합구조 D/A 변환기는 고속, 고해상도의 성능을 필요로 하는 다양한 회로에 응용과 적용이 가능하다.

• 자원환경지질
• /
• 제38권4호
• /
• pp.481-492
• /
• 2005

이 연구에서는 광주지역 하상퇴적물에 대한 지질집단별 지구화학적 특성에 대해 규명 하고자 한다. 이를 위해 물이 흐르고 있는 1차 수계를 대상으로 하상퇴적물시료 104개를 채취하였고, 실험실에서 자연건조 시켰다. 화학분석을 위한 시료는 알루미나 몰타르를 이용하여 200메쉬 이하로 분쇄하였고, XRF ICP-AES, NAA분석을 실시하였다. 연구지역 하상퇴적물에 대해, 지질집단별 지구화학적 특성 비교와 기존 암석에 대한 연구에서 얻어진 암석화학적인 특성과의 비교를 위해, 선캠브리아기 화강편마암 지역, 쥬라기 화강암 지역, 백악기 화순안산암 지역으로 분리하였다 광주지역 하상퇴적물의 주성분원소 함량은 $SiO_2\;51.89\~70.63\;wt.\%,\;Al_2O-3\;12.91\~21.95\;wt.\%,\;Fe_2O_3\;3.22\~9.89\;wt.\%,\;K_2O\;1.85\~4.49\;wt.\%,\;MgO\;0.68\~2.90\;wt.\%,\;Na_2O\;0.48\~2.34\;wt.\%,\;CaO\;0.42\~6.72\;wt.\%,\;TiO_2\;0.53\~l.32\;wt.\%,\;P_2O_5\;0.06~0.51\;wt.\%\;and\;MnO\;0.05\~0.69\;wt.\%.$이다. 하상퇴적물과 암석에 대한 AMF 삼각도에서, 암석은 칼크-알칼리계열에 도시되는데 비하여, 하상퇴적물은 솔레아이트 계열과 칼크-알칼리계열의 경계부위에 도시된다. 이는 $Fe_2O_3$ 함량이 암석에서보다 하상퇴적물에 더 많이 함유되어 있는 것과 관련이 있는 것으로 보인다. $SiO_2$에 대한 $K_2O+Na_2O$의 비교그림에서, 하상퇴적물은 암석에서와 같이 subalkaline 계열에 점시된다. 하상퇴적물의 미량성분원소 및 희토류 원소 함량은 $Ba 590\~2170ppm$, Be$1\~2.4$ppm, Cu $13\~179ppm$, Nb $20\~34ppm$, Ni$10\~50ppm$, Pb $17\~30$ppm, Sr $70\~1025$ ppm, V$42\~135$ ppm, Zr$45\~171$ ppm, Li$19\~77$ppm, Co$4.3\~19.3$ppm, Cr$28\~131$ppm, Cs$3.1\~17.6$ ppm, Hf $5\~27.6$ ppm, Rb $388\~202$ ppm, Sb$0.2\~l.2$ ppm, Sc$6.4\~17$ ppm, Zn $47\~389$ ppm, Pa $8.8\~68.8$ ppm, Ce$62\~272$ppm, Eu$1\~2.7$ppm and Yb$0.9\~6$ppm의 범위를 보인다.

• 자원환경지질
• /
• 제39권6호
• /
• pp.675-687
• /
• 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.

• 광물과 암석
• /
• 제35권2호
• /
• pp.125-140
• /
• 2022

Xiquegou 연-아연 광상은 중국 동북지역에선 가장 규모가 큰 연-아연 광화대 중의 하나인 Qingchengzi orefield에 위치한다. 이 광상의 주변지질은 시생대의 그래뉼라이트(granulite)와 이를 관입한 고원생대의 미그마타이트질 화강암과 고-중원생대의 소딕(sodic) 화강암을 부정합으로 피복한 고원생대의 Liaohe 층군 및 이들을 관입한 중생대의 섬록암과 몬조나이틱 화강암으로 구성된다. 이 광상은 고원생대의 Liaohe 층군내 Dashiqiao 층의 unit 3(돌로마이트질 대리암과 편암)내에 발달된 단층대를 따라 산출되는 맥상 광체로 트라이아스기의 마그마-열수형 광상에 해당된다. Xiquegou 연-아연 광상에서 석영, 인회석, 방해석, 황철석, 유비철석, 자류철석, 백철석, 섬아연석, 황동석, 황석석, 방연석, 사면동석, 에렉트럼, 휘은석, 자연은 및 농홍은석 등이 산출되며 모암변질로는 규화작용, 황철석화작용, 돌로마이트화작용, 녹니석화작용 및 견운모화작용 등이 관찰된다. 이 광상의 산출 광물조합 및 정출순서를 기초로, 돌로마이트는 1)모암인 돌로마이트(D₀) 및 2)연-아연 광화작용에 따른 모암변질 산물인 돌로마이트(D₁)로 두 유형이 확인된다. 이들 돌로마이트의 화학조성은 각각 Ca_1.03-1.01Mg_0.95-0.83 Fe_0.12-0.02Mn_0.02-0.00(CO₃)₂(D₀) 및 Ca_1.16-1.00Mg_0.79-0.44Fe_0.53-0.13Mn_0.03-0.00As_0.01-0.00(CO₃)₂(D₁)로써 이론적인 돌로마이트의 화학조성보다 미량원소들의 함량이 높다. 특히, FeO, PbO, Sb₂O₅ 및 As₂O₅ 원소들은 모암변질 산물인 돌로마이트(D₁)에서 높은 함량을 갖는다. 또한 이 광상의 모암에서 산출되는 돌로마이트(D₀)는 Ferroan 돌로마이트에 해당되며 모암변질 산물인 돌로마이트(D₁)는 철백운석 및 Ferroan 돌로마이트에 해당된다. 모암변질 산물인 녹니석의 화학조성은 (Mg_1.65-1.08Fe_2.94-2.50Mn_0.01-0.00Zn_0.01-0.00Ni_0.01-0.00Cr_0.02-0.00V_0.01-0.00Hf_0.01-0.00Pb_0.01-0.00Cu_0.01-0.00As_0.03-0.00Ca_0.02-0.01Al_1.68-1.61)_5.77-5.73(Si_2.84-2.76Al_1.24-1.16)_4.00O₁₀(OH)₈로써 이론적인 녹니석과 유사하며 Fe-rich 녹니석에 해당된다. 또한 이 녹니석의 화학조성 변화는 주로 팔면체적 Fe²⁺ <-> Mg²⁺ (Mn²⁺) 치환과 일부 팬자이틱 또는 Tschermark 치환(Al^3+,VI+Al^3+,IV <-> (Fe²⁺ 또는 Mg²⁺)^VI+(Si⁴⁺)^IV)메카니즘에 의해 일어났음을 알 수 있다.

• 대한의생명과학회지
• /
• 제13권4호
• /
• pp.279-285
• /
• 2007

Although retinoic acid has been known as either anti-inflammatory or pro-inflammatory molecule, depending on the cell type, its exact role in mature human neutrophils has not been fully explored. In this study, we investigate the effects of retinoic acid on neutrophil apoptosis and the associated mechanism and found that 9-cis retinoic acid (9CRA) significantly inhibits the spontaneous apoptosis of neutrophils. Its effect is increased by co-treatment with $TNF-\alpha$ (P<0.05). The 9CRA-induced inhibition is blocked by the following enzyme inhibitors: Ly 294002, phosphoinoside (PI)-3 kinase inhibitor, U73122, a phospholipase C (PLC) inhibitor, PP2, Src family protein inhibitor, SB202190, p38 MAPK inhibitor, and BAY-11-7085, NF-kB inhibitor. This study also demonstrates that all-trans retinoic acid suppresses spontaneous apoptosis, similar to the mechanism of inhibition exhibited by 9CRA. Phosphorylation of p38 MAPK decreases by 9CRA treatment. $Ik-B{\alpha}$ is degraded until 30 minutes after a time-dependent 9CRA treatment, but degradation can be inhibited by Ly 294002. These results indicate that 9CRA decreases p38 MAPK activation, induces NF-kB activation via PI-3 kinase, and also blocks cleavage of caspase 3. As these findings suggest, 9CRA has a molecular mechanism which may help pro-inflammatory response by blocking neutrophil apoptosis.

• 자원환경지질
• /
• 제30권6호
• /
• pp.553-566
• /
• 1997

Origin, behavior and enrichment of environmental toxic elements from the Deokpyeong area were investigated on the basis of major, trace and rare earth element geochemistry. Coaly metapelites of the Deokpyeong area are subdivided into grey phyllite, dark grey phyllite, coaly slate and black slate, which are interbedded along the Ogcheon Supergroup. The coaly slate had been mined for coal, but mining is closed. The coaly and black slates are lower contents of $SiO_2$ and $Al_2O_3$, and higher contents of LOI, CaO, $Na_2O$ and BaO as compared with the phyllitic rocks. Rare earth elements are highly enriched in the coaly and black slate. Average compositions (ppm) of minor and/or environmental toxic elements in the coaly and black slate are revealed as As=127, Ba=30,163, Cd=18, Cr=740, Cu=84, Mo=378, Pb=43, Sb=12, Se=44, U=144, V=8,147 and Zn=292, which are extremely high concentrations than those in the NASC compositions. Major elements (average enrichment index; 5.34) in the coaly metapelites are mostly depleted, excepting $P_2O_5$ and BaO, normalized by NASC. Rare earth elements (average enrichment index; 1.48) are enriched in the coaly slate. On the basis of NASC, minor and/or environmental toxic elements in the coaly metapelites were strongly enriched of all the elements with the exception of Co, Cs, Ni and Sr. Average enrichment index of trace elements in coaly metapelite is 31.51 (coaly slate; 51.94 and black slate; 15.46). Especially, enrichment index of potentially toxic elements (As, Ba, Cr, Cu, Mo, Ni, Sb, Se, U, V and Zn) of the rock is 46.10 (grey phyllite; 7.15, dark grey phyllite; 4.77, coaly slate; 88.96 and black slate; 22.11). These coal formations were deposited in basin of boundary between terrestrial and marine environments deduced to carbon, sulfur (C/S=2.2 to 275.7), trace and rare earth elements characteristics. Irregular behavior and dispersion between major, minor and rare earth elements of those metapelites indicates a variable source materials, incomplete mixing of differential source and/or reequilibrium of diagenesis and metamorphism.