• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• 2011.05a
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• pp.425-428
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• 2011

인터넷 인프라와 기술의 발달로 세계가 인터넷으로 연결되면서, 전쟁과 테러공격의 한 방법으로 사이버테러가 발생하고 있다. 2009년 7월 7일 한국의 주요 홈페이지를 공격한 DDoS공격으로 인하여 사이버테러대응활동의 중요성이 더해졌다. 본 논문에서는 사이버테러대응활동에 대한 근거법률과 대응기관에 관한 연구이다. 상위법인 국가보안법과 법률 제8874호 국가안전보장회의법 등을 연구한다. 또한 사이버테러대응활동의 중요기관인 국가정보원법과, 대통령령훈령 제47호의 국가대테러활동지침, 대통령훈령 제267호인 국가사이버안전관리규정을 연구한다. 본 논문의 연구를 통하여 최근의 급격히 증가하는 사이버테러로부터 국가를 안전하게 지키고, 국민의 평안한 생활을 보장하는 기초 연구 자료로 활용될 것이다.

• The Science & Technology
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• s.509
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• pp.50-53
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• 2011

닭과 함께 한 80년 세월, 지난 1957년에 미국 미네소타대학에서 석사학위를 한 후, 귀국 길에 모교에서 개량 보존하고 있던 미국산 종계와 종란을 국내에 도입, 6.25 전쟁으로 황폐화한 우리나라 닭의 육종을 개량, 증식함으로써 국민 먹거리와 농가 소득 증대에 기여하였고, 1997년 멸종 위기에 놓여있던 '우리 재래닭' 4종류를 탄생시켜낸 오당(梧堂) 오봉국(嗚鳳國) 박사(86)를 서울 서초구에 있는 대한민국학술원에서 만났다. 오봉국 박사는 서울대학교 농대 교수로 40년간 재직하면서 150여 편의 연구논문을 발표하고 후학들을 이끌어 왔으며, '한국가금발달사'를 저술하여 우리나라의 가금학을 집대성했고, 서울대 농대 학장, 한국가금협회장 등을 역임했다. 평안남도 진남포 출생이며, 국민훈장 모란장을 수훈했다.

• Journal of the korean veterinary medical association
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• v.8 no.5
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• pp.64-65
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• 1964

우리는 헐벗은 나라에서 절대부족한 수입으로 먹고 배우며 살고 있다. 천연자원은 없고 기간산업은 발전되어 있지 않을 뿐더러 인구는 많아서 우리의 힘만으로는 좀처럼 잘사기 힘든 것이 오늘날 우리가 보고 듣고 있는 한국이다. 국가와 민족의 삶이 그럴진대 학문의 전당인들 평안할 리 없고 하물며 학문중의 한 분과인 수의학이 그 교육이나 실무면에서 만족스럽다고 할 정도로 이끌어져 나간다고는 기대하기 어려운 것이다. 그러나 교육은 인간이 영위하는 삶의 가치와 이들이 소유하는 학문의 발전을 기약해주는 커다란 지표요 나아가서는 남만치 잘 살수 있게 하는 하나의 국민에의 투자인 것이다. 이 사실들은 수의학에도 통용되어서 수의학을 보잘것 없다고 그릇 알고 있는 사람들에게는 수의학이 지니는 본연의 의의에 관한 $\ulcorner$오리엔테이션$\lrcorner$이 필요한 것이고 이 학문을 배우려는 수의학도에게는 그들이 지녀야 할 목적의식을 불어 넣어 주어야 할 것이다. 이러한 의미에서 여기에 수의교육에 따르는 몇 몇 문제를 들어 비교 분석하고 제언하려고 한다.

• Journal of the Korean Society of Laryngology, Phoniatrics and Logopedics
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• v.28 no.2
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• pp.138-140
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• 2017

Pharyngeal and laryngeal foreign bodies are common problem at ENT clinic. Removal of a foreign body is mostly simple with the manipulation of endoscope and various instruments. Rarely, migration of swallowed sharp foreign body makes complication. We describe a 74-year-old patient diagnosed with foreign body in larynx involving thyroid. In this case, we present this disease and the treatment course which has been successfully treated by surgical removal and conservative treatment. Furthermore, we discuss its symptoms, physical examinations through literature review.

• Journal of the Mineralogical Society of Korea
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• v.7 no.2
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• pp.128-137
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• 1994

예산-공주-청양 지역에는 여러 큰 규모의 활석 광상이 분포한다. 이 지역에서 산출되는 활석 광석은 초염기성암 기원의 사문암이 열수변질작용을 받아서 주로 생성된 것으로알려져 있으며 녹니석, 운모, 각섬석 등의 규산염 광물들은 불순물로 다량 함유하고 있다. 활성 광석에 포함되어 있는 이들 함철규산염 광물들을 분리해 내고 활석 광석의 품질을 향상시키기 위하여 고구려배자력분리방법을 실험적으로 적용함으로써 활석 광석의 정제법을 강구하고자 하였다. 활석광석을 구성하고 있는 광물들의 자기적, 광물학적 특성을 토대로 하여 인공 혼합 표준 시료와 활석 광석 시료를 준비하고 이들을 대상으로 각각 실험하였다. 정제 실험 결과 고구배자력분리기를 통과한 정광의 경우 활석의 양이 증가하였고 다른 불순광물들의 양은 현저히 감소하였으며 활석 광석의 백색도에 있어서는 대흥광산의 원광석의 경우 60.6에서 65.5로, 평안광산의 경우 61.6에서 65.0으로, 신양광산의 경우 71.2에서 74.5로 향상되었다.

• Journal of The Korean Society of Grassland and Forage Science
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• v.33 no.2
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• pp.123-130
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• 2013

This study was conducted to investigate the effects of climate change on the growth characteristics and dry matter yields of silage corn hybrids in fields of forage crops of Hanwoo Experiment Station, National Institute of Animal Science, RDA, from Apr. 2009 to Sep. 2011. Corn hybrids were cultivated in Daegwallyeong of Gangwon Province, at an altitude of 760 m. Corn varieties used in this study consisted of 5 domestic varieties and 5 foreign varieties. Differences of silk days according to years occurred at an average of 5.5 days. The silk periods of domestic varieties occurred from Aug. 8 to 12, while that of overseas varieties was from Aug. 5 to 11. Silk days of domestic varieties occurred approximately 3 to 4 days earlier than those of oversea varieties. Silk days of Kwangpyeongok and P3156 belonging to the early varieties were Aug. 8 and 5, respectively. Kwangpyeongok and P3156 were Aug. 8 and 5, respectively. Pyeonganok and DK729 belonged to late varieties. The mean plant height of corn was approximately 231 cm, while those of Kwangpyeongok and Pyeonganok were 236 cm and 237 cm, respectively. The mean stem diameter and ear height of corn were approximately 23.2 mm and 94 cm, respectively. In the case of stem diameters, those of Cheonganok and 33J56 were 86 cm and 80 cm, respectively, while Gangdaok grew to a greater height (enter height) than other varieties. Dry matter yields of Kwangpyeongok and Pyeonganok were higher than those of other varieties. The mean leaf ratio of corn was 39.3%, while that of domestic varieties increased as compared to foreign varieties. The average DM yield of corn was 16,653 kg/ha, while those of 32P75, P3156, Pyeonganok, P3394 and Kwangpyeongok were 18,901, 17,997, 17,675, 17,194, 17,188 kg/ha, respectively. Total digestible nutrient (TDN) yields of 32P75, P3156, P3394, Pyeonganok and Kwangpyeongok were 13,381, 12,590, 12,532, 12,140 and 12,036 kg/ha, respectively. Corn crude protein (CP), in vitro dry matter digestibility (IVDMD), neutral detergent fiber (NDF), acid detergent fiber (ADF) and TDN were 7.8%, 74.2%, 42.4%, 23.5% and 70.3%, respectively. In the case of nutritive values of corn, there was no significant difference between of corn varieties of domestic and foreign origin.

• The Journal of the Petrological Society of Korea
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• v.21 no.2
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• pp.151-171
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• 2012

The Permo-Triassic Songrim orogeny in the Korean peninsula was a major tectonic event involving complicated continental collisions at the eastern margin of Eurasia. Based on the previous studies on the metamorphic and deformations features of the Songrim orogeny, this paper presents metamorphic and structural characteristics and timing of the Songrim orogeny in the Taebaeksan basin, and discuss about correlation of the tectono-metamorphic evolution of the Taebaeksan basin with the Okcheon basin and the Imjingang belt with a combined analysis of bulk crustal shortening direction, metamorphic P-T and T-t (time) paths. The metapelites in the Pyeongan Supergroup in the northeastern margin of the Taebaeksan basin have experienced lower-temperature/medium-pressure (LT/MP) regional metamorphism followed by high-temperature contact metamorphism due to the Jurassic granite intrusion. The earlier LT/MP regional metamorphism produced two loops of clockwise P-T-d (deformation) paths combined with four deformation events ($D_1-D_4$). The first loop concomitant with $D_1$ and $D_2$ occurred at $400-500^{\circ}C$, 1.5-3.0 kbar, and related with growth of syn-$D_1$ chloritoid and andalusite, post-$D_1$ margarite, Ca-rich syn-$D_2$ or post-$D_2$ plagioclase. The second loop accompanying $D_3$ and $D_4$ occurred at $520-580^{\circ}C$, 2.0-6.0 kbar, and associated with the growth of syn-$D_3$ garnet and staurolite, and syn-$D_4$ and/or post-$D_4$ andalusite porphyroblasts. Furthermore the syn-$D_1$ chloritoid and andalusite porphyroblasts grew during E-W bulk crustal shortening, whereas the syn-$D_3$ garnet and staurolite, and the syn-$D_4$ and/or post-$D_4$ andalusite porphyroblasts have grown under N-S bulk crustal shortening. The similarity in the characteristics and timing of the metamorphism and bulk crustal shortening directions between the Okcheon and Imjingang belts suggest that the peak metamorphic conditions tend to increase toward the western part (Imjingang belt and southwestern part of the Gyeonggi Massif) from the eastern part (Taebaeksan basin). The E-W bulk crustal shortening influenced the eastern part of the Okcheon belt, whereas the N-S bulk crustal shortening resulted in strong deformation in the Imjingang and Okcheon belts. Consequently, the Permo-Triassic Songrim orogeny in the Korean peninsula is probably not only related to collision of the North and South China blocks, but also to the amalgamation of terrane fragments at the eastern Eurasia margin (e.g., collision of the Sino-Korean continent and the Hida-Oki terrane).

• Economic and Environmental Geology
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• v.53 no.4
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• pp.383-395
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• 2020

The stratigraphical position of the Haengmae Formation can provide clues towards solving the hot issue on the Silurian formation, also known as Hoedongri Formation. Since the 2010s, there have been several reports denying the Haengmae Formation as a lithostratigraphic unit. This study aimed to clarify the lithostratigraphic and chronostratigraphic significance of the Haengmae Formation. The distribution and structural geometry of the Haengmae Formation were studied through geologic mapping, and the correlation of relative geologic age and the absolute age was performed through conodont biostratigraphy and zircon U-Pb dating respectively. The representative rock of the Haengmae Formation is massive and yellow-yellowish brown pebble-bearing carbonate rocks with a granular texture similar to sandstone. Its surface is rough with a considerable amount of pores. By studying the mineral composition, contents, and microstructure of the rocks, they have been classified as pebble-bearing clastic rocks composed of dolomite pebbles and matrix. They chiefly comprise of euhedral or subhedral dolomite, and rounded, well-sorted fine-grained quartz, which are continuously distributed in the study area from Biryong-dong to Pyeongan-ri. Bedding attitude and the thickness of the Haengmae Formation are similar to that of the Hoedongri Formation in the north-eastern area (Biryong-dong to Haengmae-dong). The dip-direction attitudes were maintained 340°/15° from Biryong-dong to Haengmae-dong with a thickness of ca. 200 m. However, around the southwest of the studied area, the attitude is suddenly changed and the stratigraphic sequence is in disorder because of fold and thrust. Consequently, the formation is exposed to a wide low-relief area of 1.5 km × 2.5 km. Zircon U-Pb age dating results ranged from 470 to 449 Ma, which indicates that the Haengmae Formation formed during the Upper Ordovician or later. The pebble-bearing carbonate rock consisted of clastic sediments, suggesting that the Middle Ordovician conodonts from the Haengmae Formation must be reworked. Therefore, the above-stated evidence supports that the geologic age of the Haengmae Formation should be Upper Ordovician or later. This study revealed that the Haengmae Formation is neither shear zone, nor an upper part of the Jeongseon Limestone, and is also not the same age as the Jeongseon Limestone. Furthermore, it was confirmed that the Haengmae Formation should be considered a unit of lithostratigraphy in accordance with the stratigraphic guide of the International Commission on Stratigraphy (ICS).

• (The)Study of the Eastern Classic
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• no.72
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• pp.299-327
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• 2018

The objective of this study is to examine the regional distribution of Ssireum(Traditional Wrestling) of South and North Korea in the Japanese colonial era. The conclusions of this study are as follows. First, the "Joseon ui hyangto orak(Folk play in Joseon)" showed the record of performing 272 times of Ssireum in 226 regions of the whole nation. Second, the Ssireum of South Korea could be divided into five regions. Seoul/Gyeonggi-do performed Ssireum the most in Dano, Baekjung, and Chuseok while Chungcheong-do performed Ssireum in Baekjung and Chuseok. Jeolla-do and Gyeongsang-do performed Ssireum in Chuseok while Gangwon-do performed Ssireum in Dano and Chuseok. Third, the Ssireum of North Korea could be divided into three regions. All the Hwanghae-do, Pyeongan-do, and Hamgyeong-do performed Ssireum the most in Dano. Fourth, as the period when Ssireum was held the most in the whole nation, Dano, Baekjung, and Chuseok could be pointed out. Ssireum has the characteristics of large-scale play between village communities or regions, instead of individual game. Thus, the Ssireum that was played as a sport event under certain rules for a long time was settled down as a folk play of regional festivals such as Dano, Baekjung, and Chuseok. Fifth, as a folk play and a representative play of seasonal customs, Ssireum was distributed in the whole nation and handed down till today under the regional deviation of South and North Korea. Sixth, the unidentified regions of South Korea that did not perform Ssireum were six places including five dos such as Gapyeong Gyeonggi-do, Boseong Jeollanam-do, Jeju-do, Gunwi and Cheongsong Gyeongsanbuk-do, and Inje Gangwon-do. The regions of North Korea were six places including three dos such as Pyeongyang, Yangdeok, Gangdong, and Gaecheon of Pyeongannam-do, Bakcheon Pyeonganbuk-do, and Dancheon Hamgyeongnam-do. Total 12 places in eight regions were included. Seventh, the number of total items of play names presented in the "Joseon ui hyangto orak(Folk play in Joseon)" was about 6,400 types. Out of them, about 1,300 types were the items including how to play while about 5,100 types were the items presenting the play names only without explanations. Especially, in case of Ssireum, the periods of the lunar calendar were only specified in each region. Unfortunately, it was not possible to check the contents about the actual performance methods and types of Ssireum as they were omitted.

• The Journal of Engineering Geology
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• v.22 no.1
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• pp.59-65
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• 2012

The purpose of this study is to analyze the direction of slope sliding that occurred at the highland ${\bigcirc}{\bigcirc}$ district in the Samcheok coalfield, using geological and structural detail surveys. The study area is dominated by the Paleozoic Pyong-an Group, and sliding is concentrated in zones of alternating sandstone and shale beds in the Geumcheon and Jangsung Formations. Discontinuities in the area have a strike of NE-SW and dip at 30~$80^{\circ}$ to the NW and 40~$80^{\circ}$ to the SE. However, some have strikes of NW-SE. In slide area group 1 (P1 to P4), en echelon tension gashes were caused by shearing. The surface in the areas of group 2 (P5 to P7) and group 3 (P8 and P9) is marked by step-type tension cracks that formed due to extension. This phenomenon caused anticlockwise rotation of the sliding slope. Otherwise, the cutting of the road side through the eastern slope of the mountain contributed to surface sliding due to geographical equilibrium loss.