항공기 부품국산화 진흥방안 - 항공기 엔진 국산화 방안

이대성,Lee, Dae-Seong 한국항공우주산업진흥협회 1995 航空宇宙 Vol.29 No.-

IGCP, Circum-Pacific Plutonism Project 제(第) 7차회의(次會議)(일본측(日本側)) 참석보고(參席報告)

이대성,Lee, Dae-Seong 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.3

강원도 영월군 남면 광천리 석회석 광산 조사

이대성,Lee, Dai Sung 대한자원환경지질학회 1974 자원환경지질 Vol.7 No.4

This report deals with the stratigraphy and chemical composition of calcareous sedimentary rocks of upper Choseon System, Cambro-Ordovician, in the titled area, for the evaluation of limestone resources of cement manufacture.

옥천대(沃川帶) 우라늄광층(鑛層)의 구조규제(構造規制) 및 지구화학적(地球化學的) 특성연구(特性硏究)

이대성,윤석규,이종혁,김정택,Lee, Dai Sung,Yun, Suckew,Lee, Jong Hyeog,Kim, Jeong Taeg 대한자원환경지질학회 1986 자원환경지질 Vol.19 No.no.spc

Structural, radioactive, petrological, petrochemical, mineralogical and stable isotopic study as well as the review of previous studies of the uranium-bearing slates in the Ogcheon sequence were carried out to examine the lithological and structural controls, and geochemical environment in the uranium deposition in the sequence. And the study was extended to the coal-bearing formation (Jangseong Series-Permian) to compare the geochemical and sedimentologic aspects of uranium chemistry between Ogcheon and Hambaegsan areas. The results obtained are as follows: 1. The uranium mineralization occurs in the carbonaceous black slates of the middle to lower Guryongsan formation and its equivalents in the Ogcheon sequence. In general, two or three uranium-bearing carbonaceous beds are found with about 1 to 1.5km stratigraphic interval and they extend from Chungju to Jinsan for 90km in distance, with intermittent igneous intrusions and structural Jisturbances. Average thickness of the beds ranges from 20 to 1,500m. 2. These carbonaceous slate beds were folded by a strong $F_1$-fold and were refolded by subsequent $F_1$-fold, nearly co-axial with the $F_1$, resulting in a repeated occurrence of similar slate. The carbonaceous beds were swelled in hing zones and were shrinked or thined out in limb by the these foldings. Minor faulting and brecciation of the carbonaceous beds were followed causing metamorphism of these beds and secondary migration and alteration of uranium minerals and their close associations. 3. Uranium-rich zones with high radioactive anomalies are found in Chungju, Deogpyong-Yongyuri, MiwonBoun, Daejeon-Geumsan areas in the range of 500~3,700 cps (corresponds to 0.017~0.087%U). These zones continue along strike of the beds for several tens to a few hundred meters but also discontinue with swelling and pinches at places that should be analogously developed toward underground in their vertical extentions. The drilling surveyings in those area, more than 120 holes, indicate that the depth-frequency to uranium rich bed ranging 40~160 meter is greater. 4. The features that higher radioactive anomalies occur particularly from the carbonaceous beds among the argillaceous lithologic units, are well demonstrated on the cross sections of the lithology and radioactive values of the major uranium deposits in the Ogcheon zone. However, one anomalous radioactive zone is found in a l:ornfels bed in Samgoe, near Daejeon city. This is interpreted as a thermal metamorphic effect by which original uranium contents in the underlying black slate were migrated into the hornfels bed. 5. Principal minerals of the uranium-bearing black slates are quartz, sericite, biotite and chlorite, and as to chemical composition of the black slates, $Al_2O_3$ contents appear to be much lower than the average values by its clarke suggesting that the Changri basin has rather proximal to its source area. 6. The uranium-bearing carbonaceous beds contain minor amounts of phosphorite minerals, pyrite, pyrrhotite and other sulfides but not contain iron oxides. Vanadium. Molybdenum, Barium, Nickel, Zirconium, Lead, Cromium and fixed Carbon, and some other heavy metals appear to be positive by correlative with uranium in their concentrations, suggesting a possibility of their genetic relationships. The estimated pH and Eh of the slate suggests an euxenic marine to organic-rich saline water environment during uranium was deposited in the middle part of Ogcheon zone. 7. The Carboniferous shale of Jangseong Series(Sadong Series) of Permian in Hambaegsan area having low radioactivity and in fluvial to beach deposits is entirely different in geochemical property and depositional environment from the middle part of Ogcheon zone, so-called "Pibanryong-Type Ogcheon Zone". 8. Synthesizing various data obtained by several aspects of research on uranium mineralization in the studied sequence, it is concluded that the processes of ur

잣나무 인공림의 1차 및 2차 간벌에 따른 입목생장 특성 분석

이대성,정성훈,최정기,Lee, Daesung,Jung, Sunghoon,Choi, Jungkee 한국산림과학회 2022 한국산림과학회지 Vol.111 No.1

본 연구는 잣나무(Pinus koraiensis Siebold & Zucc.) 인공림을 대상으로 1차 및 2차 간벌에 따른 입목의 생장특성을 규명하여 산림시업지침 및 매뉴얼 개발을 위한 기초자료를 제공하고자 수행되었다. 사용된 연구자료는 간벌강도에 따라 설치된 잣나무 인공림 영구고정표준지로부터 수집되었으며, 각 간벌시험림별 4~5회 반복조사된 자료를 토대로 임령 19~43년생 시기의 흉고직경, 재적, 고사목 등 주요 입목 및 임분 현황을 분석하였다. 간벌강도에 따른 일원분산분석에서 개체목의 흉고직경 및 재적 변화는 유의적인 차이를 보였으며(p<0.05), 특히 간벌강도가 클수록 시간이 경과함에 따라 경급분포는 더 오른쪽에 위치하여 입목의 경급이 더 큰 것으로 관측되었다. 흉고직경 정기평균생장량의 경우, 간벌강도가 강하고 간벌 후 경과기간이 짧을수록 생장량이 높았는데, 구체적으로 임령 19~24년생 때 간벌강도별 생장량 범위는 0.48~0.95 cm/year이었다. 이후 2차 간벌에 따른 정기평균생장량도 강도간벌구에서 더 큰 것으로 분석되었으며, 임령 37~42년생 때 간벌강도별 생장량 범위는 0.29~0.67 cm/year이었다. 개체목 재적의 정기평균생장량은 간벌강도에 따라 차이가 있었으며, 흉고직경과 달리 시간이 지나도 크게 줄어들지 않는 경향이 나타났다. 임분 재적은 전반적으로 임분밀도가 밀한 표준지에서 높은 경향이었으나, 임분재적 정기평균생장량은 시기에 따라 무간벌뿐만 아니라 약도간벌이 이루어진 임분에서 더 높은 것으로도 분석되었다. 고사목은 무간벌구에서 가장 많이 발생하였으며, 반복조사가 진행될수록 임분밀도에 따른 고사목 본수 차이는 더욱 증가하였다. 종합적으로 임분밀도가 밀할수록 개체목의 흉고직경과 재적 생장량은 낮아지는 경향이었으나, 적절한 1차 및 2차 간벌이 시행되면 생장량은 다시 촉진되었다. This study was conducted to provide basic information for the development of silvicultural guidelines and manuals. This was achieved through analysis of tree and stand characteristics according to the first and second thinning in Korean white pine plantations. Data were collected from permanent plots installed at Korean white pine plantations according to thinning intensity, and residual tree and stand variables, including diameter at breast height (DBH), volume, and mortality at age 19-43, were analyzed using data repeatedly collected in 4-5 measurements by experiments. According to one-way variance of analysis, tree DBH and volume were significantly different according to thinning intensity (p<0.05). DBH distribution was skewed to the left side over time as thinning intensity was heavier. Thus, tree DBH values were larger in heavy thinning plots with increased age. The periodic annual increment (PAI) of DBH was higher with heavier thinning intensity and fewer years after thinning. The PAI range by thinning intensity was 0.48-0.95 cm/year at age 19-24. In addition, the PAI increased in heavy thinning plots after the second thinning; The PAI range by thinning intensity was 0.29-0.67 cm/year after the second thinning at age 37-42. The PAI of tree volume differed according to thinning intensity, and the PAI value did not decrease obviously, in contrast to the pattern of the DBH PAI. Stand volume was generally higher in high-density stands, and the PAI of stand volume was high in unthinned and light thinning plots. Mortality was highest in unthinned plots, and the differences in mortality according to thinning intensity increased over time. Consequently, the growth of DBH and tree volume was lower as stand density increased, but this growth was facilitated with appropriate first and second thinning operations.

상동중석광상(上東重石鑛床)의 현미경적(顯微鏡的) 연구(硏究)

이대성,김서운,Lee, Dai Sung,Kim, Suh-Woon 대한자원환경지질학회 1969 자원환경지질 Vol.2 No.1

In the Sangdong Mine area, Taebaegsan series (Pre-Cambrian) and Chosun System (Cambro-ordovician) are widely distributed. The Chosun System consists of Yangdug Series (Jangsan Quartzite and Myobong Slate) and The Great Limestone Series (Pungchon Limestone, Shesong Shale, Hwajeol Formation and Dongjeom Quartzite). The mineralized zone containing the main ore body of the Sangdong Mine was developed in the Myobong Slate formation. The result of the field and microscopic study on the mineral paragenesis and it's wall rock alteration in the tungsten ore deposit shows the following features. The orogenic movements of the Post-Chosun System in the Hambaeg Geosyncline are closely related to the tungsten ore deposition in the area, the ore minerals are composed mainly of scheelite, powelite molybdenite and sulfide minerals, and gangue minerals are hornblende, diopside, garnet, quartz, phlogopite, tremolite, biotite, muscovite, fluorite, etc., main ore body was enriched by scheelite bearing quartz vein filling into interstices of formerly mineralized zones, and the minor faults, faults of N $60^{\circ}-70^{\circ}W$, $45^{\circ}-60^{\circ}NE$ and joints, which were formed at the end of the mineralization and the slate. Country rock of the ore body was altered into the following several zones from the outside to the inside; lowgrade recrystalline aureole, silicified sericite zone, and diopside-hornblende zone. Under the microscopic observation of 195 samples taken from throughout ore body can be classified into 10 different groups by their mineral paragenesis as shown in table 2. The garnet-diopside group is primary skarn and it shows gradational change to the groups of later stage by the successive processes of metasomatism. From the stage of quartz-bearing group, the dissemination of scheelite is seen. The crystallization of scheelite in the bed started with the quartz deposition and continued to the last stage when quartz vein intruded into the main ore body. In the field and the under ground investigation a durable limestone bed in thickeness about 20 meters and their remnants in ore body are observed and under microscope calcite remnants are recognized. Hence it is posturated that the ore material moved up through the faults, shear zones or feather cracks and was assimilated with the interbeded limestone, after that the body was affected by the successive differentiated ore solution by gradational increasing in $SiO_2$, $K_2O$ and $H_2O$. Evidently this ore deposit shows the features resulted from pyrometasomatic processes.

구봉석회석광산의 지질조사보고(地質調査報告)

이대성,Lee, Dai Sung 대한자원환경지질학회 1970 자원환경지질 Vol.3 No.1

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.

옥천대(沃川帶)에서의 화성활동(火成活動) -특(特)히 옥천대동북부(沃川帶東北部)에서의 화성활동(火成活動)-

이대성,김용준,Lee, Dai Sung,Kim, Yong Jun 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.1

The northeastern part of Ogcheon zone which consisted mainly of Cambro-Ordovician arenaceous, argillaceous and calcareous formations and Carboni-Triassic arenaceous and argillaceous formations is delineated as the eastern mass of a thrust fault along Choongju-Moongyong-Cheongsan in the middle of the zone. The present study proposes a geotectonic line, Imgye-Samchog fault(see, figure 1) which divides the northeastern part into two blocks, Hambacksan block in the west and East coast block in the east. The igneous rocks in the Hambacksan block ranging from granite to gabbro are distributed in a symmetrical zones parallel to general direction of Ogcheon zone as follows (Fig. 2 and Table 2). Southeast igneous rock zone: it aligns Jurassic granites in its south and Precambrian leucocratic granites in its north. Central igneous rock zone: it aligns Cretaceous granites in its south and Jurassic granites, and some of diorite and gabbro in its north. Northwest igneous rock zone: aligns Jurassic granites in its south and huge batholithic granodiorite in its north. The distribution of the igneous rocks in the East coast block shows an entirely different features from those of Hanbacksan block. In the southern part of the block they assemble in a narrow area ranging in age from Early Proterozoic, through Middle to Late Proterozoic, Devonian, Jurassic, Cretaceous to Tertiary, whereas, the igneous rocks in the northern part of the block gathered to a restricted area, in ages of Middle Proterozoic and Cretaceous. The assemblage of the igneous rocks in the studied area shows a compositionally restricted, mixed S-type and I-type granites, $^{87}Sr/^{86}Sr$ > 0.706, rare volcanics and shortening with upright folding. These lithologic and structural features suggest that the igneous activity in this part related intimately to Hercynotype Orogeny of Pitcher(1979). Chronological episodes of igneous activity from Early Proterozoic to Early Tertiary in the northeastern part are figured.

기체 유량 측정에서 몬테 카를로 모사를 이용한 측정불확도 평가

이대성,양인영,김춘택,양수석,Lee, Dae-Sung,Yang, In-Young,Kim, Chun-Taek,Yang, Soo-Seok 대한기계학회 2003 大韓機械學會論文集B Vol.27 No.12

Monte Carlo simulation(MC) method was used as an uncertainty assessment tool for gas flow measurement in this paper. Uncertainty sources for gas flow measurement were analyzed, and probability distribution characteristics of each source were discussed. Detailed MC methodology was described including the effect of the number of simulation. The uncertainty result was compared with that of the conventional sensitivity coefficient method, and it was revealed that the results were different from each other for this particular gas flow measurement case of which the modelling equation was nonlinear. The MC was comparatively simple, convenient and accurate as an uncertainty assessment method, especially in cases of complex, nonlinear measurement modelling equations. It was noted that the uncertainty assessment method should be selected carefully according to the mathematical characteristics of the measurement.

대(對)테러리즘 분야 연구경향분석:치안본부 대테러연구를 중심으로

이대성,류상일,Lee, Dae sung,Ryu, Sang Il 한국융합보안학회 2014 융합보안 논문지 Vol.14 No.3

국제사회는 서독 뮌헨올림픽에서 팔레스타인 테러조직 검은 9월단(Black September)이 이스라엘 선수단을 대상으로 자행한 인질 납치 살해 테러리즘에 큰 충격을 받았다. 한국도 1986년 아시안게임과 1988년 서울 올림픽 개최를 앞두고, 북한의 국가지원 테러리즘, 무력도발, 국지전 등의 위협에 직 간접적으로 노출되어 있었다. 이에 한국 정부는 1982년 1월 대통령훈령 제47호 '국가대테러활동지침'을 제정하여 국가 대(對)테러리즘 업무수행을 위한 필요 사항을 규정하였고, 국가안전기획부와 치안본부가 주무부서의 역할을 수행하게 되었다. 이 연구에서는 치안본부 시절 경찰의 대테러관련 역할을 고찰하고, 1983년부터 1990년까지 동 기관에서 발간한 '대테러연구'의 학문적 연구경향을 분석하였는데, 이를 살펴보면 첫째, 공통적으로 빈도가 높은 주제어는 "테러", "인질", "대책", "국제" 등이다. 둘째, 88년 올림픽 전후로 "올림픽" 주제어가 빈번하게 언급되었다. 셋째, 연도별로 차이점을 살펴보면, 83-84년에는 "관방정책" 주제어가 언급되었고, 85년에는 "대남테러", "민간항공기" 등의 주제어가 언급되었으며, 86년에는 "기업체"가 언급되었다. 87년에는 "테러경향"이라는 주제어가 언급되었고, 90년에는 "국제테러리즘", "분리주의"등의 주제어가 사용되었다. International society got a severe shock from terrorism of hostage, abduction and murder that was committed on a target of Israel athlete delegation in Munich Olympics, West Germany by Black September, a Palestine terrorism organization. Korea with 1986 Asian Games and 1988 Olympics ahead was directly and indirectly exposed to threats of North Korea's nation-support terrorism, a military provocation and a local war limited warfare. This study explores the roles of the police at the time of the National Police Headquarters with regard to counter-terrorism, and analyzed academic research trends of Studies of Counter-terrorism published by the same office between 1983 and 1990. Looking into them shows a fact firstly, that the most frequently appearing key words in common were "terrorism," "hostages," "measures," and "international," etc. Secondly, before and after 1988 Olympics, the key word "Olympics" was frequently addressed. Thirdly, looking at the difference by the year, the key word, "policies of defense and borderlands" was frequently addressed between 1983 and 1984, "terrorism against South Korea," and "civil aircraft" frequently addressed in 1985, and "corporate" in 1986. In 1987, the key word "terrorism trends" was addressed, and in 1990, "international terrorism," and "separatism" were used.