• 암석학회지
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• 제14권1호
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• pp.24-37
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• 2005

본 연구에서는 익산의 미륵산 일대의 화강암 지형경관에 대한 지형학적 및 지질학적 특성을 파악하고, 더불어 미륵사지 서탑에 사용된 석재의 공급지를 추정하였다. 절리는 익산 지역에서 가장 뚜렷한 지형학적 및 지질학적 구조이며, J1 절리의 방향은 N71°E∼EW이고 J2 절리의 방향은 N20°W∼N20°E의 범위를 나타낸다. 절리의 형태를 세분할 때 연구지역에서는 cross형의 절리가 우세하며 또한 linear형의 수직절리도 관찰된다. 지형적 특징으로 토어와 핵석도 관찰되는데, 토어를 이루는 핵석들은 2∼3m의 길이에 2∼3m 또는 5m 이상의 높이를 가진다. 그들의 경도는 주로 hammer bounce에 속한다. 미륵산 화강암에서 나타나는 토어는 tower형과 castle형이 우세하다. 한편 타포니와 나마 등과 같은 지형적 특징도 나타난다. 미륵사지 서탑의 석재와 인근 미륵산 화강암의 암석기재적 및 지구화학적 특징들을 비교할 때, 이 두 암석들은 매우 유사함이 지적되어 미륵산이 석재의 공급지일 가능성이 제기된다. 미륵산에서는 과거 채석의 흔적이 다수 발견되기도 한다.

• 천문학회보
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• 제36권1호
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• pp.27.1-27.1
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• 2011

We obtained the spectra of 93 Planet host stars and 73 normal field stars in F, G, K type using BOES at BOAO. We measured the equivalent width of Fe and 25 elements lines using the automatic EW measurement program, TAME(Tools for Automatic Measurement of Equivalent-widths) and estimated the elemental abundances by synth and abfind driver of MOOG code. Since the absence of planets in the normal field stars cannot be "completely" proved, this work focused on the chemical abundances and planet properties of planet host stars, which have the massive planets close to the parent star relatively. We carried out an investigation for the difference of abundances between stars with "Hot Jupiter" and normal field stars with no known planets. We examined the chemical composition of 25 elements, such as C, N, O, S, Na, Mg, Al, Si, K, Ca, Sc, Ti, V, Cr, Mn, Co, Ni, Cu, Zn, Sr, Y, Zr, Ba, Ce, Nd, and Eu by EW measurements, and the S abundances were estimated using synthetic spectrum. We have found that [Mg/Fe] and [Al/Fe] for planet host stars have lower limit comparing with those of comparison stars, and [Ca/Fe] of host star with Neptunian planets is relatively lower than the other host stars with massive planets. We have performed the Kolmogorov-Smirnov test, and examined the ratio of planet host stars to all stars for each bin of [X/H]. As a result, we noted that the O, Si, and Ca abfor undances are strongly related with the presence of planets.

• 암석학회지
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• 제17권2호
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• pp.83-94
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• 2008

안동시 풍천면 지역은 선캠브리아기 변성암류, 쥬라기 화성암류, 백악기 퇴적암류 (하산동층, 진주층, 일직층), 그리고 백악기 화성암류 (반려암체, 암맥류) 등으로 구성되어 있으며, 몇몇 주요 단층들이 발달한다. 이들은 백악기 경상분지와 선캠브리아기-쥬라기 기반암류(영남육괴)의 경계단층에 해당하는 동북동 방향의 안동단층, 이에 평행한 남후단층, 북북서 방향의 매봉단층, 남남동 방향으로 볼록한 활형의 광덕단층, 북북동 방향의 하회단층 등이다. 이 논문에서는 층리, 절리, 단층, 끌림 습곡에 대한 상세한 기하적인 분석을 통하여 이들 주요 단층 주변지역의 지질구조를 연구하였다. 그 결과, 활형의 광덕단층과 그의 동부 연장선상에 발달하는 하회단층 주변에서 측정된 층리의 극점 배열로부터 상부가 남남동 방향으로 충상하는 단층운동에 수반된 광역적인 끌림습곡작용이 인지되며, 광덕단층의 서부와 하회단층에서는 비교적 폭이 좁고 광덕단층의 중부와 동부에서는 비교적 폭이 넓은 약 150 m-300 m 폭의 광덕 끌림습곡대가 설정된다. 이는 이전 연구결과와 달리 하회단층과 광덕단층은 하나의 단층으로써 그 운동성과 운동시기가 광덕단층과 동일함을 의미한다. 연구지역에는 두 종류의 방향 단층[(동)북동${\sim}$동서 방향(단충 I), 서북서${\sim}$북북서 방향(단층 II)과 네 종류의 방향절리 [동서(I), (북)북서 (II),북북동 (III), 북동 (IV) 방향 절리]가 인지되며, 이들은 적어도 다음과 같은 네 번의 변형단계를 걸쳐 형성되었다 (1) Dn 단계; 동서 방향의 압축 응력에 의한 절리 (I) (광덕절리)의 형성과 동서 방향의 산성질 암맥의 관입작용, (2) Dn+1 단계, (북)북서 방향의 압축 응력에 의한 절리 (II) (매봉절리) 형성, 산성질 암맥의 렌즈상 부딘작용, 광덕절리의 사교이동성 역단층운동 (단층 I-광덕단층 형성)과 이에 수반된 광역적인 광덕 끌림습곡대 형성, (3) Dn+2 단계; 북북동 방향의 압축 응력에 의한 절리 (III) 형성, 매봉절리의 우수 주향이동 단층운동 (단층 II-매봉단층 형성)과 이에 수반된 Dn+1 구조물의 연장성 단절작용, (4) Dn+3 단계; 북동 방향의 압축 응력에 의한 절리 (IV) 형성과 단층 II의 우수향 성분이 우세한 사교이동성 단층으로의 재활동 등이다. 이러한 연구결과는 매봉단층은 안동단층과 광덕단층의 충상 지구조운동과 관련된 인열단층이라기 보다는 이들 단층보다 후기에 생성되었음을 지시한다.

• 자원환경지질
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• 제32권1호
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• pp.19-31
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• 1999

In this study, we have estimated lineaments in the Euiseong area, Kyungbuk Province, from Landsat TM by applying the algorithm developed by Kim and Won et al. which can effectively reduce the look direction bias associated with the Sun's azimuth angle. Fratures over the study area were also mapped in the field at 57 selected sites to compare them with the results from the satellite image. The trends of lineaments estimated from the Landsat TM images are characterized as $N50^{\circ}$~70W, NS~$N10^{\circ}$W, and $N10^{\circ}$~$60^{\circ}$E trends. The spatial distribution of lineaments is also studied using a circular grid, and the results show that the area can be divided into two domains : domain A in which NS~$N20^{\circ}$E direction is dominant, and domain B in which west-north-west direction is prominent. The trends of lineaments can also be classified into seven groups. Among them, only C, D and G trends are found to be dominant based upon Donnelly's nearest neighbor analysis and correlations of lineament desities. In the color composite image produced by overlaying the lineament density map of these C-, D-, and G-trends, G-trend is shown to be developed in the whole study area while the eastern part of the area is dominated by D-trend. C-trend develops extensively over the whole are except the southeastern part. The orientation of fractures measured at 35 points in the field shows major trends of NS~$N30^{\circ}$E, $N50^{\circ}$~$80^{\circ}$W, and N80$^{\circ}$E~EW, which agree relatively well with the lineaments estimated form the satellite image. The rose diagram analysis fo field data shows that WNW-ESE trending discontinuities are developed in the whole area while discontinuities of NS~$N20^{\circ}$E are develped only in the estern part, which also coincide with the result from the satellite image. The combined results of lineaments from the satellite image and fracture orientation of field data at 22 points including 18 minor faults in Sindong Group imply that the WNW-ESE trend is so prominent that Gumchun and Gaum faults are possibly extended up to the lower Sindong Group in the study area.

• 자원환경지질
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• 제3권4호
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• pp.199-222
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• 1970

One of the biggest sulfide metallic (Cu, Pb, Zn) ore deposits of South Korea is located in the area of Seo-myeon, Shiheung-gun, Gyeonggi-do. Geology of the region is mostly composed of metasediments of biotite schist, graphite schist, injection gneiss, sericite schist, limesilicate and quartzite from bottom, those are applicable to so-called Yeoncheon System of Pre-Cambrian, and granodiorite, quartz porphyry, basic dykes are outcroped in a small scope as intrusives. The origin of the ore deposit is pyrometasomatic contact deposits due to hydrothermal replacement and the ore bodies are imbedded in lower bed of limesilicate formation as impregnation and ore minerals are galena, sphalerite, marmatite, chalcopyrite, bornite, chalcocite, covellite, and the later two minerals are both hypogene and supergene. Gangue minerals are mostly skarn minerals those hornblende, diopside, epidote, hedenbergite, chlorite, garnet and quartz except primary calcite and quartz. Boundary plane (NS strike) between schists and limesilicate seemed to be primary opening of ore solution and fractures bearing $N50^{\circ}{\sim}80^{\circ}W$ are secondary structural control for localization of ore minerals and the third structural controls are both irregular gashes and schistosity in small scale. Photogeological study was carried with vertical aerial photo scaled 1: 38,000 and enlarged 1 : 10,000 under stereoscope. The study on the area convinced the fact that the geologic boundaries between rocks, limesilicates and quartzites, are traced easily by their typical topographic feature and drainage, and the main fracture patterns which derived from the result of fracture traces, that photogeologic lineament observed under stereoscope, are those bearing (1) $N20^{\circ}W$, (2) $N58^{\circ}W$, (3) $N76^{\circ}W$, (4) EW, (5) $N20^{\circ}W$, (6) $N62^{\circ}W$, (7) $N77^{\circ}W$. Among the written fractures, (5) (not schistosity, in case of fault) (6) (7) are post-mineral faults and others are pre-mineral faults and others are pre-mineral structures, and (2) (3) (6) (7) are coincided with statistical figure of 208 fractures surveyed in underground. By the result of the study, mineralized zone, are presumed to extend north and southward, total length about 4km.

• 천문학회지
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• 제36권2호
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• pp.55-60
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• 2003

In Lee, Kang & Byun (2001) the discovery of Raman scattered 6545 A feature was reported in symbiotic stars and the planetary nebula M2-9. The broad emission feature around 6545 A is formed as a result of Raman scattering of He II n = 6 $\to$ n = 2 photons by atomic hydrogen. In this paper, we introduce a method to compute the equivalent width of He II $\lambda$ 1025 line and present an optical spectrum of the symbiotic star RR Telescopii as an example for a detailed illustration. In this spectrum, we pay attention to the broad H$\alpha$ wings and the Raman scattered He II 6545 feature. The broad Ha wings are also proposed to be formed through Raman scattering of continuum around Ly$\beta$ by Lee (2000), and therefore we propose that the equivalent width of the He II $\lambda$ 1025 emission line is obtained by a simple comparison of the strengths of the 6545 feature and the broad H$\alpha$ wings. We prepare a template H$\alpha$ wing profile from continuum radiation around Ly$\beta$ with the neutral scattering region that is supposed to be responsible for the formation of Raman scattered He II 6545 feature. Isolation of the 6545 feature that is blended with [N II] $\lambda$ 6548 is made by using the fact that [N II] $\lambda$ 6584 is always 3 times stronger than [N II] $\lambda$ 6548. We also fit the 6545 feature by a Gaussian which has a width 6.4 times that of the He II $\lambda$ 6527 line. A direct comparison of these two features for RR Tel yields the equivalent width $EW_{Hel025} = 2.3{\AA}$ of He II $\lambda$ 1025 line. Even though this far UV emission line is not directly observable due to heavy interstellar extinction, nearby He II lines such as He II $\lambda$ 1085 line may be observed using far UV space instruments, which will verify this calculation and hence the origins of various features occurring in spectra around H$\alpha$.

• Asian-Australasian Journal of Animal Sciences
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• 제18권12호
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• pp.1752-1760
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• 2005

In this experiment, the effects of cage density (CD) and probiotic supplementation (PS) on laying performance, metabolic profile, and egg quality in peak-producing hens were evaluated. After blocking according to the cage location, Lohman layers (n = 180, 46 wks of age) were allocated randomly to two levels of CD (540 vs. 360 $cm^2$/hen) and three levels of PS (0, 0.15, and 0.30%). Probiotic contained Enterococcus faecium culture (10${\times}$10$^9$ cfu/g). Egg production (EP) and feed consumption (FC) were measured daily; egg weight (EW) was measured bi-weekly; BW was measured before and after the experiment; and blood samples were obtained at the end of the experiment. The data were analyzed using two-way ANOVA. Increasing CD decreased FC (125.0 vs. 120.8 g/d, p<0.0001) and FCR (1.93 vs. 1.87, p<0.0001) and did not alter EP, EW, and BW. Increasing level of PS linearly decreased FC (p<0.02) and FCR (p<0.006). Averages were 123.9, 123.2, and 121.6 g/d for FC and 1.91, 1.92, and 1.86 for FCR in hens supplemented with 0, 0.15, and 0.30% probiotic, respectively. Hens placed in high-density cages had greater serum corticosterone concentration than hens placed in normal-density cages (12.8 vs. 11.3 $\mu$g/dL, p<0.04); CD did not affect concentrations of other metabolites. Increasing level of PS linearly increased serum glucose, albumin, and creatine concentrations and quadratically increased total protein, globulin, Ca, and P concentrations. Average concentrations (mg/dL) were 260, 297, and 305 for glucose; 6.28, 8.09, and 7.58 for total protein; 1.98, 2.48, and 2.38 for albumin; 4.30, 5.62, and 5.19 for globulin; 0.40, 0.52, and 0.54 for creatine; 16.0, 16.5, and 16.3 for Ca; and 6.27, 8.14, and 7.17 for P in hens supplemented with 0, 0.15, and 0.30% probiotic, respectively. There was no effect of CD on egg quality. Increasing level of PS linearly improved yolk color (YC) and quadratically increased albumen index (AI) and Haugh unit (HU). The mean values were 9.67, 9.75, and 10.58 for YC; 8.94, 6.93, and 8.72% for AI; and 85.6, 74.9, and 82.9 for HU for hens supplemented with 0, 0.15, and 0.30% probiotic, respectively. There was also CD by PS effect on FC, EP, and serum glucose, total protein, albumin, globulin, creatine, Ca and P concentrations. In conclusion, increased CD partially depressed laying performance and caused stress. Probiotic supplementation improved laying performance and metabolic profile. It also partially alleviated the adverse effects of stress resulting from increased caging density.

• 한국작물학회:학술대회논문집
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• 한국작물학회 2017년도 9th Asian Crop Science Association conference
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• pp.150-150
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• 2017

Plants suffer from various abiotic stresses among them; soil salinity is one of major adverse factor in declining agricultural productivity. So, development of salt stress tolerance crops have potential role to increase crop production. The RING finger proteins are known to play crucial roles in abiotic stress environment to plants. In this study, we identified one Salt-responsive Really${\underline{I}nteresting}$ ${\underline{n}ew}$ ${\underline{g}ene}$ (RING) E3 ubiquitin ligase gene OsSIRF1 from rice root tissues during salt stress and studied its molecular function. Expression of OsSIRF1 was induced under various abiotic stress conditions, including salt, heat, drought, and ABA. Result of an in vitro ubiquitination assay clearly showed that OsSIRF1 Possess an E3 ligase activity. Moreover, OsSIRF1 was found to be localized to the nucleus within the cell. Heterogeneous overexpression of OsSIRF1 in Arabidopsis improved seed germination and increased root length under salt and Manitol stress conditions. Taking together, these results suggested that OsSIRF1 may be associated with plant responses to abiotic stressors and positively regulates salt and osmotic stress environment.

• Asian-Australasian Journal of Animal Sciences
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• 제19권4호
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• pp.573-581
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• 2006

This experiment was conducted to determine the effects of supplemental methionine, lysine, choline, and sulfur on laying performance, metabolic parameters, and egg quality of hens fed diets containing sorghum (Sorghum vulgare) during the peak laying period. Lohman layers (n = 144), 30-wk of age as 6 replicate cages of 4 hens, were allocated randomly to receive basal diets containing either 22% corn (B) or 22% sorghum (BS) and diets BS plus 0.57% methionine, 0.66% lysine, 0.47% choline, or 0.05% sulfur for 98 d. Feed intake (FI) and egg production (EP) were recorded daily, egg weight (EW) was measured bi-weekly, and body weight (BW) was measured monthly. A sample of 12 eggs from each experimental group was collected every month to evaluate egg quality. At the end of the experiment, blood samples were collected for metabolite concentrations. Data were analyzed using one-way ANOVA as repeated measures and significant differences between the experimental groups were assessed using Duncan's Multiple Range test. Partial replacement of corn with sorghum in the basal diet did not affect BW, EP, and FCR but increased FI by 5.7% and EW by 2.4%. The effects of additives on laying performance were variable. Except for serum total protein (STP) concentration, other metabolic parameters were not affected by partial replacement of corn with sorghum in the basal diet. Hens fed diet BS had lower SPT concentration than hens fed diet B. Except for methionine supplementation, other supplements ameliorated depression in STP concentration. The additives did not affect other metabolic parameters. Egg quality responses to the experimental diets were also variable. Partial replacement of corn with sorghum in the basal diet did not affect eggshell characteristics (both thickness and stiffness), whereas it had variable effects on inner egg quality parameters (increased yolk index, depressed yolk color, and unaltered albumen index and Haugh unit). In conclusion, laying hen diets could include low-tannin sorghum (0.26%) up to 22% without necessitating extra supplements to overcome compromised performance.

• 암석학회지
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• 제11권3_4호
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• pp.169-181
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• 2002

한반도 남동부의 울산단층 동편에는 염기성~중성 암맥군들이 우세하게 발달한다. 이 암맥들은 대부분 동해가 활발히 확장되었던 전기 마이오세(약 17 Ma 이전)의 지각 변형기 동안 동서방향의 지각 신장에 의해 만들어진 남북방향의 인장 균열을 통로로 관입하였다. 연일구조선을 경계로 서쪽지역과 인근지역 그리고 동쪽지역의 화강암체에서 관찰된 염기성 암맥의 평균 관입면 주향 방향은 동쪽으로 갈수록 시계방향으로 회전된다(N06$^{\circ}$E$\longrightarrow$N15$^{\circ}$E$\longrightarrow$N37$^{\circ}$E). 또한 연일구조선 동편의 염기성 암맥의 주향 방향은 동쪽 해안에 가까워질수록 시계방향으로 보다 많이 회전된 특징(구룡포반도에서 N75$^{\circ}$E)을 보여주었다 이는 이들 암맥들이 정치 이후 연일구조선 동쪽의 것들만 시계방향 수평 회전운동을 겪었으며, 이들 중 동쪽 해안에 가까운 것일수록 보다 많은 앙의 회전운동을 겪었음을 의미한다. 또한 동해의 확장으로 인해 대륙연변을 따라 발생한 북북서방향 우수향 전단력이 시간이 경과함에 따라 동에서 서로 전파되는 과정을 겪었으며, 연일구조선이 마이오세 분지 지역에서 흔히 관찰되는 지괴의 수평 회전운동을 규제한 주요 서쪽 한계선임을 지시하고 있다.