항공기 부품국산화 진흥방안 - 항공기 엔진 국산화 방안

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

석질문화재에 미치는 자연환경 조사

이대성,Lee, Dae-Seong 국립문화재연구소 1980 保存科學硏究 Vol.1 No.-

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.

중국의 반(反)테러리즘법 제정을 위한 검토: 미국.영국.독일과 비교하여

이대성,안영규,Lee, Dae Sung,Ahn, Young Kyu 한국융합보안학회 2014 융합보안 논문지 Vol.14 No.6

중국은 광대한 영토와 다양한 민족, 종교, 그리고 문화 등이 공존하고 있다. 이러한 중국은 민족, 종교, 자원 등의 갈등으로 인하여 테러리즘 위협에 직면해 있다. 중국은 2011년 10월 29일 제11대 전국인민대표대회 상무위원회에서 반(反)테러리즘 업무강화와 관련한 결정(決定)을 하였다. 이 연구는 중국의 반(反)테러리즘 관련 결정과 미국, 영국, 독일의 대(對)테러리즘 관련법을 분석 및 평가하였다. 미국, 영국, 독일의 대(對)테러리즘 관련법은 크게 사전예방(事前豫防)과 사후진압(事後鎭壓) 측면, 대인적(對人的)과 대물적(對物的) 측면으로 구분하여 제정하였고, 대(對)테러리즘 관련 국가기관의 권한(權限)과 역할(役割)도 재조정(再調整)하였으며, 대(對)테러리즘 관련법 내용도 명시적이고 구체적이며 체계적이라고 할 수 있다. 그러나 중국의 반(反)테러리즘 관련 결정은 사전예방(事前豫防) 진압(鎭壓), 대인(對人) 대물적(對物的), 국가기관(國家機關)의 권한과 역할 등에 대한 한계가 있다. 이 연구에서는 중국이 향후에 반(反)테러리즘 관련법을 제정함에 있어, 외국의 대(對)테러리즘 관련법에 대한 시사점을 검토하였고, 개정된 중국 형법의 테러리즘 관련 범죄에 관한 규정을 반(反)테러리즘 관련 결정과 어떻게 접목할 것인가를 논의하였다. China has vast land, variety of people, religions and cultures. China has faced terrorism threat from the struggles of people, religions and resources. The 11thStanding Committee of the National People's Congress of China decided to strengthen the anti-terrorism action on October 29, 2011. This study compared, analyzed and estimated the counter-terrorism laws of the USA, Britain and Germany thinking about the China's anti-terrorism decision. The counter-terrorism laws of the USA, Britain and Germany are largely composed of previous prevention of terror and oppression of it later. They enacted the laws both for people and property. They also rearranged the power and role of governmental institutes on counter-terrorism. The contents of the counter-terrorism laws are specific, detailed and systematic. But the anti-terrorism law of China has restriction on the power and roles for previous prevention and oppression of terrorism, handling of people and property. This study reviewed the foreign countries' counter-terrorism laws and the way to connect the regulations on terrorism crimes of the revised Chinese criminal law and the anti-terrorism decision, when they enact the anti-terrorism laws in China in the future.

양평화성(楊平火成) 복합체(複合體)에 대(對)한 암석학적(岩石學的) 연구(硏究)

이대성,김용준,Lee, Dai Sung,Kim, Yong Jun 대한자원환경지질학회 1974 자원환경지질 Vol.7 No.3

The study focused to the so called "Yangpyeong Igneous Complex" which intruded into the Gyeong Gi gneiss complex of Pre-cambrian basement of Yangpyeong area. The geologic sequence of the mapped area was shown in table 1. In laboratory work, 31 modal analyses and 7 chemical analyses on the rock samples taken from the igneous complex have been made to discuss the nomenclature of the rocks and the petrological relationship between rock types. The petrographical and petrochemical features based on the analyses are as follow; 1) The classification of this rocks based on the systematics of igneous rocks of IUGS showed that Yangpyeong Igneous complex consist of hornblende gabbro, diorite and porphyritic monzonite. The major rock forming minerals in hornblende gabbro are hornblende and plagiodase ($An_{46{\sim}55}$), in diorite, hornblende, biotite and plagioclase ($An_{23{\sim}33}$) and in porphyritic monzonite, K-feldspar, plagioclase ($An_{21{\sim}35}$), hornblende and biotite. Hornblende gabbro and diorite show coarse to medium grained hypidiomorphic granular texture and porphyritic monzonite was named by the characteristically porphyritic texture of K-feldspar phenocrysts. 2) Silica-oxides variation diagram (Fig.4) illustrate that the igneous complex is similar ttl that of Daly's average basalt-andesite-dacite-rhyolite and equivalent to the calc-alkalic rock series of Peacock's rock series. In AMF diagram (Fig. 5), the trend of the igneous complex is nearly pararell to that of the Skaergaard intrusion which shows the trend of the fractional crystalization of magma. 3) In normative Or-Ab-An diagram (Fig. 6) the general trend of the data points from gabbro to porphyritic monzonite of the igneous complex directs to a point of Or/Ab=1:1 on the side of Or-Ab. The field and laboratory evidences suggested that the Yangpyeong igneous complex was thought to be a series of comagmatic differential products.

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.

해남지역(海南地域)에 분포(分布)된 우항리층내(牛項里層內) 흑색(黑色)셰일의 유기지화학적(有機地化學的) 연구(硏究)

이대성,윤현수,Lee, Dai Sung,Yun, Hyun Soo 대한자원환경지질학회 1979 자원환경지질 Vol.12 No.4

The studied area occupies the southern part of Haenam peninsula located in the southwestern corner of Korea. The stratigraphic sequences of the area are grouped into following three units in ascending order. (1) Late Cretaceous sedimentary rocks of Uhangri Formation which consist of the alternative beds of black shales and tuffaceous sediments, Hwangsan acidic fine grained tuffs and Jindo rhyolite flows. (2) Late Cretaceous biotite granite and acidic porphyries which intruded the Late Cretaceous sedimentary rocks. (3) Tertiary(?) pitchstone. The study purposes to delineate any of geochemical aspects on the deposition of the sequences, the average amounts of organic materials and the effect to the maturation of hydrocarbonization which has been occured by the intrusives. Sixty nine black shale samples were collected from Uhangri Formation in the northern and southern coasts of the peninsula. Organic carbons, total extracted organic matters and hydrocarbons were mainly determined by the Soxhlet extraction method, together with C-H-N elemental analyses. Based on the field and laboratory studies, the following interpretations have been obtained. (1) The paleohydrostatic condition of the sedimentation which took place was relatively calm and stable to delineate a lacustrine environment. (2) The amounts of organic material were more or less constant throughout the period of the deposition of the sediments. (3) The degree of hydrocarbonization of the Uhangri Formation in the northern coast was taken place higher than that in the southern coast due to the differences of thermal effect by the biotite granite which is assumed to be as a heat source in the area. Among the northern coast, some black shales in Uhangri and Mogsam areas which had been under the most moderate temperature environment snow symptomatic oily material, whereas, those in Sinseongri area do not, which were presumably to be intensive thermal alteration by the later acidic porphyries.

괴산부근(槐山附近)에 분포(分布)하는 옥천층군(沃川層群)의 지질구조(地質構造)에 관(關)하여

이대성,김용준,채인철,Lee, Dai Sung,Kim, Yong Jun,Chai, In Chul 대한자원환경지질학회 1977 자원환경지질 Vol.10 No.4

This study is focused on the geological structure of Igog-Jangam folded zone in the vicinity of Goesan town where Ogcheon group distributes. The geology is composed of Gyemyungsan formation, Daehyangsan quartzite, Munjuri formation and Hwanggangri formation of Ogcheon group unknown age in descending order, and porphyritic biotite granite and dyke rocks that intruded into the Ogcheon group. The study revealed that Igog-Jangam folded zone is a plunged synclinal fold based on the following evidences; 1) Some pebbles in Hwanggangri formation at Minaemi-gol (a name of village) consists of phyllite of Munjuri formation. 2) The pebble bearing phyllitic bed in this area, Hwanggangri formation was recognized as the uppermost member in Ogcheon group instead of the basal one of the group. 3) A crest of anticlinal fold has been appeared near the Goegang bridge as a structural counter-part of that of the present area. 4) The study of lineation of minor fold in Munjuri formation also suggests that Igog-Jangam folded zone manifests to be a synclinal structure.

옥천지향사대(沃川地向斜帶)의 화성활동(火成活動)에 의한 광화작용(鑛化作用)의 유형(類型)에 관(關)한 연구(硏究)

이대성,지정만,이대운,Lee, Dai Sung,Chi, Jeong Mann,Lee, Dai Woon 대한자원환경지질학회 1980 자원환경지질 Vol.13 No.3

The granitic plutons associated with Ogcheon geosynclinal zone can be grouped into three different subzones; SE-Subzone for the migmatitic and schistose granites of the southeast margin, 101-181m.y. old; NW-Subzone for those of the northwest margin, 112-163m. y. old; and C-Subzone for those of central part of the zone, 63-183m.y. old. The intrusives in C-Subzone are further subdivided into the older, adamellite to granodiorite (148-183m.y. old) and the younger, perthitic granites (63-106m,y. old). The metallogenic distribution of South Korea suggests that, in the Ogcheon Zone, it is possible to delineate an elongated polymetallogenic province in the general orientation of the zone intimately related with the migmatite and plutonic zones mentioned. Moreover, the mineralization in the province was basically controlled by the patterns of local geology involving country rocks and related igneous bodies, that permit subdivision of the province into the following three parts: Northeast (NE) Province consists dominantly of thick Paleozoic calcareous sediments; Middle (M) Province is characterized by predominant argillaceous and partly calcareous sediments of Precambrian to Late Paleozoic age; and Southwest (SW) Province consisting mainly of volcanic and arenaceous sediments of Mesozoic age. The three different plutonic zones with three different country rock provinces above mentioned make a combination which consists of nine classes. Each class can be assumed to be characterized by specific mineralization type. In order to classify the mineralization types, the present study sampled twenty six ore deposits and mineralized areas in Ogcheon zone as shown figure 2; eight ore deposits from plutonic SE-Subzone, ten from the plutonic NE-Subzone and eight from the plutonic C-Subzone. The characteristics of the classes are as follows: NE-SE is predominant in Au-Ag vein and Sn-migmatite of katazonal occurrence; NE-C is most productive in Pb-Zn and remarkable in Fe contact deposit in mesozone and partly Pb-Zn-Cu skarn in limestone and subordinate in mesozone and partly Pb-Zn pipes; M-SE is considerable in Au-Ag vein and rare elements (Nb, Ta, etc.) of pegmatite; M-C is predominant in F-veins in epizone and Mo-W, Fe, Cu veins occur in replacement type; M-NW is productive in Fe metamorphic and skarn types, partly remarkable in Cu, Pb-Zn contact; SW-SE is barren in mineralization related to Jurassic igneous rocks; SW-C is predominant in alunite and pyrophyllite in tuffs; and SW-NW is scarece in Pb-Zn, Cu, As and Au-Ag veins.

가스터빈 엔진의 연소기 성능 시험

이대성,Lee, Dae-Seong 재료연구소 1995 機械와 材料 Vol.7 No.3