• 자원환경지질
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• 제3권1호
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• pp.17-24
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• 1970

The purpose of this report is to prepare a data for the economic evaluation on the Goobong Limestone Mine which is located at the south-eastern corner of the Yongchun Quadrangle scaled in 1:50,000. The accessibility from the mine to railroad was considered in two ways. One is to Dodam Station on Central Railway Line and the other is to reach Songjung-ni village which is near Sangyong Station on Hamback Railway Line. The distance of the former way is 26.7km and the later is 24.2km. Geologically the mine is situated near the base of the Greast Limestone Series which strikes generally $N25^{\circ}{\sim}30^{\circ}E$. The series comprises six different formations from older to younger; Pungchon Limestone Formation and Whajol Formation of Cambrian age, and Dongjum Quartzite Formation, Dumudong Formation, Maggol Limestone Formation and Goseong Formation of lower to middle Ordovician age. 82 samples; 48 from Pungchon Limestone Formation, 11 from Dumudong Formation, 15 from Maggol Limestone Formation and 8 from Goseong Formation, were taken from the series in the crossed direction to the general trend of the series as shown in geological map. They were chemically analyzed on the components of CaO, MgO, $SiO_2$, $R_2O_3(Al_2O_3+Fe_2O_3)$ and ignition loss as shown in table 2, table 3, table 4, and table 5. As seen from the tables, among the formations of the series, middle to upper parts of the Pungchon Limestone Formation and middle and upper parts of the Dumudong Formation have chemical composition as available source for the raw material of cement industry, not only that but also the part of the Pungchon Formation was highly evaluated as source for the flux of iron smelting and the raw material of carbide manufacturing because of its high purity of calcium carbonate.

• 한국약용작물학회지
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• 제6권1호
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• pp.51-56
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• 1998

본 연구는 1995년부터 1997년까지 경기도와 강원도 5개군 7개소를 중심으로 자생하는 삼지구엽초의 환경특성을 구명하여 삼지구엽초 작물화재 배연구의 기초자료로 제공하고자 수행하였던 바 그 결과를 요약하면 다음과 같다. 1. 조사된 자생지는 대체로 북서 사면에 표고 $60{\sim}400m$, 경사도 $2{\sim}20%$인 곳의 냇가에서 $5{\sim}80m$ 주위로 물줄기를 따라 장타원으로 위치하고 있었다. 2. 자생지 토양은 잔자갈이 있는 양토 또는 사양토로서 가비중이 $0.74{\sim}1.26g/cm^3$, 공극율 $52.5{\sim}72.1%$로 나타났다. 3. 토양화학성은 pH $4.1{\sim}5.8$, 유기물함량 $4.9{\sim}6.6%$, 유효인산 $21{\sim}125\;ppm$, 치환성양이온 (me/100g)은 $K^+\;0.35{\sim}1.09,\;Ca^{++}5.42{\sim}18.73,\;Mg^{++}\;0.99{\sim}1.53$, CEC는 $14.8{\sim}34.3me/100g$이었다. 4. 자생지는 주로 개암나무, 떡갈나무, 참나무 등 낙엽광엽활엽수에 의하여 차광되어 취, 둥굴레, 삽주, 뱀딸기, 제비꽃 등 반음지식물과 함께 자생하고 있었다. 5. 삼지구엽초 군락에 도달하는 광투과 정도는 노지 대비 relative photon flux density $3.5{\sim}13.1%$ 상대조도는 $3.3{\sim}11.9%$ 였으며 기온은 $4.3{\sim}6.5^{\circ}C$낮았다. 또한 지온은 5월에서 8월까지 $17.5{\sim}20.1^{\circ}C$로 경과되어 외기기온의 $25.1{\sim}30.8^{\circ}C$에 비하여 낮았으나 변화폭이 작았다.

• 한국환경농학회지
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• 제30권2호
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• pp.153-159
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• 2011

태안지역 영농기 빗물의 중금속 농도 및 부화특성을 구명하기 위하여 2002년과 2003년 4~10월 사이에 빗물을 채수하여 중금속 분포와 가중평균 변화, 화학성분과의 관계 및 부화정도를 비교 검토하였다. 빗물 중 화학성분 함량은 조사 시기에 따라 함량변이가 심하였고, 강우량 대비 pH의 가중평균 값은 5.0~5.1 수준이었다. 빗물의 중금속 가중평균은 Pb > Zn > Cu > Ni > As > Cr > Cd 순이었고, 2002년과 비교하여 2003년에 Cu, Pb, 및 Zn 성분이 상대적으로 높게 나타났다. 강우중의 주 이온성분(${NH_4}^+$, $Ca^{2+}$, $Mg^{2+}$, $K^+$, $Na^+$, ${SO_4}^{2-}$ 및 ${NO_3}^-$)은 중금속 중 As, Cd, Zn, Cr 및 Ni 성분함량과 고도의 정의 상관을 보였다. 빗물의 중금속 농도분포를 이해하기 위하여 부화계수(Enrichment factor)를 조사한 결과, 부화계수 평균치가 대체로 Cd > Pb > AS > Cu > Zn > Ni > Cr 순이었고, 주로 자연적 발생 유래원소로 알려진 Fe, Mg 및 Ca 등보다 상대적으로 높은 경향을 보였다. 월별 빗물의 중금속부하계수는 8~9월이 상대적으로 높았고, 중금속의 습식침적은 대체로 강우량의 영향을 받아 강우기인 7~8월에 높은 경향을 보였다.

• 천문학회보
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• 제38권2호
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• pp.87.2-87.2
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• 2013

We studied a fine-scale half ring-like structure around a pore seen from the high spectral and the high spatial resolution data. Our observations were carried out using the Fast Imaging Solar Spectrograph (FISS) and the InfraRed Imaging Magnetograph (IRIM) installed at the 1.6 meter New Solar Telescope of Big Bear Solar Observatory (BBSO) on 2012 July 19. During the observations, we found a fine-scale half ring-like structure located very close to a pore (~0.4 arcsec apart from the pore). It was seen in the far wing images of the $H{\alpha}$ and Ca II $8542{\AA}$ lines, but it was not seen in the line center images of two lines. The length of the structure is about 4200 km and the width is about 350 km. We determined its line-of-sight velocity using the Doppler shift of the centroid of the Ti II line ($6559.6{\AA}$, close to the $H{\alpha}$ line) and determined horizontal velocity using the NAVE method. we also investigated the magnetic configurations using the Stokes I, Q, U, and V maps of the IRIM. As a results, we found that it has a high blue-shift velocity (~2km) faster than the photospheric features and has a strong horizontal component of the magnetic field. Based on our findings, we suggest that it is associated with small flux emergence, which occurs very close to the pore. Even though it is very small structure, this kind of magnetic configuration can be in chare of the upper chromosphere heating, especially above the pore.

• 분석과학
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• 제26권3호
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• pp.211-221
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• 2013

본 연구는 원주 법천사지에서 출토된 분청사기의 화학조성과 미세조직, 결정상을 X-선형광분석기와 주사전자현미경-에너지분산형엑스선분석기, X-선회절분석기를 이용하여 알아보았다. 태토의 화학성분 분석 결과, 낮은 실리카($RO_2$) 함량과 높은 융제(RO+$R_2O$) 함량임을 알 수 있다. 유약의 경우 융제 성분 중 CaO 함량이 높은 전형적인 석회계열(lime type)과 석회-알칼리 계열(lime-alkali type) 유약을 사용하였으며 태토의 결정상으로는 quarts, mullite, microcline, albite가 확인되었다. 특히 원주 법천사지에서 출토된 분청사기 태토의 화학적 조성은 제겔식을 이용하여 이미 연구된 다른 유적에서 출토된 분청사기와 비교하였으며 화학조성은 서로 상이한 결과를 보였다.

• Molecules and Cells
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• 제44권7호
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• pp.458-467
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• 2021

GPR43 (also known as FFAR2 or FFA2) is a G-protein-coupled receptor primarily expressed in immune cells, enteroendocrine cells and adipocytes that recognizes short-chain fatty acids, such as acetate, propionate, and butyrate, likely to be implicated in innate immunity and host energy homeostasis. Activated GPR43 suppresses the cAMP level and induces Ca²⁺ flux via coupling to Gα_i and Gα_q families, respectively. Additionally, GPR43 is reported to facilitate phosphorylation of ERK through G-protein-dependent pathways and interacts with β-arrestin 2 to inhibit NF-κB signaling. However, other G-protein-dependent and independent signaling pathways involving GPR43 remain to be established. Here, we have demonstrated that GPR43 augments Rho GTPase signaling. Acetate and a synthetic agonist effectively activated RhoA and stabilized YAP/TAZ transcriptional coactivators through interactions of GPR43 with Gα_q/11 and Gα_12/13. Acetate-induced nuclear accumulation of YAP was blocked by a GPR43-specific inverse agonist. The target genes induced by YAP/TAZ were further regulated by GPR43. Moreover, in THP-1-derived M1-like macrophage cells, the Rho-YAP/TAZ pathway was activated by acetate and a synthetic agonist. Our collective findings suggest that GPR43 acts as a mediator of the Rho-YAP/TAZ pathway.

• 대한환경공학회지
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• 제22권1호
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• pp.33-42
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• 2000

중금속은 토양 내에서 비보존성 화학물질로 작용하므로 흡착에 의해 지연효과가 발생할 수 있고 흡착은 pH에 영향을 받는다고 보고된 바 있다. 그러므로 토양 및 지하수 오염을 예방하고 복구하기 위해서는 다양한 pH조건에서 중금속의 이동형태를 파악하는 것이 중요한 연구과제가 된다. 본 연구에서는 사질토양에서 pH에 따른 중금속의 이동특성을 연구하기 위하여 배치실험과 주상실험올 수행하였다. 배치실험의 경우 초기농도별로 11가지의 $ZnCl_2$ 40 mL 용액과 사질토양 10g을 교반기에서 72시간 반응시켜 평형상태에 도달하게 한 후 용액을 채취하여 Zn, Ca, Mg의 세 가지 양이온을 ICP-AES로 분석하였다. 주상실험은 3가지 pH조건 (7.7, 5.8, 4.1)에서 10 g/L의 KCl과 $ZnCl_2$를 추적자로 사용하여 순간주입 (pulse injection) 형태로 토양시료 상부에 투입한 후 Time Domain Reflectometry (TDR)를 사용하여 10 cm 깊이에서 잔존수농도를, EC-meter와 ICP분석을 통하여 20 cm 깊이의 하부 경계면에서 침출수농도를 분석하였다. 배치실험 결과, Zn은 Ca, Mg와 이온교환의 형태로 흡착이 발생하였고 등온 흡착방정식의 각 모델 (Linear, Freundlich, Langmuir)별로 최저 1.2에서 최고 614.1의 지연계수를 나타냈다. 주상실험에서도 모든 pH조건에서 Zn이온이 이온교환을 하여 흡착이 발생하였으나, 잔존수와 침출수 형태의 파과곡선 모두에서 Zn이용의 첨두농도 도달시간이 K이온과 일치하여 지연효과는 발생하지 않은 것으로 나타났다. 이는 정상류 상태로 부과한 낮은 배경농도의 용탈수내에 Zn보다 강한 이온교환능을 가지는 원소가 존재하지 않아 Zn의 탈착이 발생하지 않았기 때문이다. pH가 낮을수록 Zn는 용액내 수소이온 ($H^+$)의 증가로 치환능이 감소하여 첨두농도가 높게 나타났고, 상대적으로 치환되는 Ca, Mg의 양은 줄어들었다. 따라서 본 연구에 적용된 배치실험과 주상실험의 조건하에서는 Zn이온이 이온교환반응에 의한 흡착이 발생하였으나 지연효과는 발생하지 않았고 가장 낮은 pH에서 첨두농도가 최고 12.7배까지 증가하였다.

• ALGAE
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• 제21권3호
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• pp.311-316
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• 2006

The effects of light quality and irradiance on the growth of Cochlodinium polykrikoides were investigated in the laboratory. At 25°C and 30 psu the irradiance-growth curve was described as μ = 0.34 (I-9.76)/(I+12.5), (r=0.98). This suggests half-saturation photon flux density (PFD) (Ks) of 32.0 μmol photons m–2 s–1, and a compensation PFD (Ic) of 9.76 μmol photons m–2 s–1. Because the Ic equates to a depth of ca. 15.4 m, these responses suggest that irradiance at the depth around and below the thermocline in Yeosuhae Bay would provide favorable conditions for C. polykrikoides. Photoinhibition did not occur at 300 μmol photons m–2 s–1, which was the maximum irradiance used in this study. Blue (450 nm), yellow (590 nm) and red (650 nm) light had different effects on the growth of C. polykrikoides: it grew well under blue light, but not under yellow light. This implies that C. polykrikoides is more likely to cause an outbreak of red tide in the open sea where blue-green wavelengths predominate, rather than in enclosed water bodies where suspended particles absorb most of the blue wavelengths, and yellow-orange wavelengths predominate.

• 천문학회보
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• 제37권2호
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• pp.111.2-111.2
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• 2012

We observed an Ellerman bomb(EB) and its associated surge using the Fast Imaging Solar Spectrograph(FISS) and the broadband TiO filter of the 1.6 meter New Solar Telescope at Big Bear Solar Observatory. As is well-known, the EB appears as a feature that is very bright at the far wings of the H alpha line. The lambdameter method applied to these wings indicates that the EB is blue-shifted up to 6km/s in velocity. In the photospheric level below the EB, we see rapidly growing "granule-like" feature. The transverse velocity of the dark lane at the edge of the "granule" increased with time as reached a peak of 6km/s, at the time of the EB's occurrence. The surge was seen in absorption and varied rapidly both in the H alpha and the Ca II 8542 line. It originated from the Ellerman bomb, and was impulsively accelerated to 20km/s toward us(blueshift). Then the velocity of the surge gradually changed from blueshift of 20km/s to redshift of 40km/s. By adopting the cloud model, we estimated the temperature of the surge material at about 27000K and the non-thermal velocity at about 10km/s. Our results shed light on the conventional idea that an EB results from the magnetic reconnection of an emerging flux tube and pre-existing field line.

• Biomolecules & Therapeutics
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• 제30권1호
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• pp.48-54
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• 2022

GPR43 (also known as FFAR2), a metabolite-sensing G-protein-coupled receptor stimulated by short-chain fatty acid (SCFA) ligands is involved in innate immunity and metabolism. GPR43 couples with Gα_i/o and Gα_q/11 heterotrimeric proteins and is capable of decreasing cyclic AMP and inducing Ca²⁺ flux. The GPR43 receptor has additionally been shown to bind β-arrestin 2 and inhibit inflammatory pathways, such as NF-κB. However, GPR43 shares the same ligands as GPR41, including acetate, propionate, and butyrate, and determination of its precise functions in association with endogenous ligands, such as SCFAs alone, therefore remains a considerable challenge. In this study, we generated novel synthetic agonists that display allosteric modulatory effects on GPR43 and downregulate NF-κB activity. In particular, the potency of compound 187 was significantly superior to that of pre-existing compounds in vitro. However, in the colitis model in vivo, compound 110 induced more potent attenuation of inflammation. These novel allosteric agonists of GPR43 clearly display anti-inflammatory potential, supporting their clinical utility as therapeutic drugs.