• 환경영향평가
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• 제9권3호
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• pp.239-248
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• 2000

The aggravating water quality from the expansion of industrialization along with increasing population lead to develop more intensive physical measures to secure better drinking water quality. This study was mainly initiated to establish a water-pollutant buffering zone for the upper stream basin of Paldang--the major source area of drinking water for the metropolitan Seoul and suburban areas with a population more than 13 million. Two different criteria were considered in determining the buffering distance from the edge of the streamflow : 1km-width buffer zone for the special protection area which has been strictly controlled by the conventional laws for the protection of drinking water supply, and 500m-width buffer zone for the rest of the area. To delineate the exact boundaries of the water-pollutant buffering zone, GIS database was created integrating topography, hydrography, cadastral, and other related layers. The newly designated water-pollutant buffering zone would contribute to improve the water quality in a long term along with the conservation of the wet land. More study, however, should be made within the water-pollutant buffering zone such as the detailed survey of the pollutants, vegetation, and ecosystem for more effective management of the buffering zone.

• 복식
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• 제34권
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• pp.169-182
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• 1997

Focusing on khotan located in the southern Silk Route which was one of the most important kingdoms in the Tarim Basin this study attempts to examine the changes of costume in Khotan by compar-ing the costumes in the painted panel showing the story of silk princess with the excavated costumes from ancient tombs. Furthermore this study attempts to inves-tigate the impacts of cultural exchange be-tween China and its western neighboring country Eastern and Western Turkestan on costume. Excavated costumes from the Shanpula ancient tomb in the region of Khotan and from ancient Niya in the esat-ern border of Khotan and discoveries from Rawak and Dandan-oilik near by Yotkan the ancient capital of Khotan are exam-ined. Basic Khotan's costume was the two piece style of tops and trousers. Over the basic costume wearing a top wear with half sleeves was popular. Skirt was worn by women. Even though there were many kinds tops were classified into the two types kaftan and tunic. Thouth Khotan maintained a association with China for a long time the style of Khotan costume had imbued to China. Top wear with half sleeves was worn frequently in Khotan. Also in China top wear with half sleeves was worn as over-wear which was called ban-xiu ban-bi bei-zi Costume style of China is covering the body profoundly and wrapping front edge toward the right. The types of chi-nese top wear with half sleeves for exam-ple round-neck·confronting front edge crossing-neck·confronting front edge tu-nic type discord with the traditional chi-nese costume style There were many cas-es that half sleeved top wear was worn as over wear in T'ang dynasty. The phenom-enon was due to the prevalence of 'ho' (foreign) and half sleeved top wear was introduced by the countries to the west of China Khotan. A round neck garment was a general type for the men of cuntries to the westof China. Also Chinese wore round neck garment since South and North Dynasty The type of Chinese round neck garment was not tunic but kaftan. From costume relics and ancient paintings the type of Khotan's round neck garment was tunic which was recorded on the Chinese histori-cal documents as " guan-tou-shan" that is tunic the type of persian costume, Even thgough the painted panel showing the sto-ry of silk princess was made in the it me when Turks was a dominion on Central Asia Khotan's costume style was not changed toward Turk's costume style and remained tunic style.

• 한국조경학회지
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• 제37권1호
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• pp.50-64
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• 2009

도시 근교에 입지한 담수호소는 다양한 생물이 서식하는 생물다양성의 보고이나, 무계획적인 이용의 증가로 수질오염과 식생훼손의 위험에 직면해 있다. 이에 본 연구는 사천시 두량저수지를 대상으로 담수호소의 생물다양성 유지와 이용의 조화를 추구하기 위한 관리방안을 제안하고자 동 식물 생태계의 정밀한 조사 분석 자료에 근거한 관리지역 설정 과정을 거쳐 생물다양성 증진을 위한 생태적인 관리방안을 제안하였다. 생태계 조사 분석 자료를 바탕으로 비오톱 유형 평가, 야생동물 서식처 평가, 보호종 출현 유무를 종합한 결과, 생태계 보전지역으로 설정된 지역은 층위 구조가 형성된 자연림과 생물서식의 기반을 제공하는 수면 및 습지, 서식처 다양성이 높은 주연부 지역이 보전가치가 있었다. 관리지역은 식생이 교란된 지역, 오염강도가 높은 상업지, 공업지 등과 낚시로 인해 훼손된 수변지역으로, 식생천이 유도, 관목식재 등의 식생관리와 오염물질관리 체계 구축을 통한 적극적인 관리가 시도되어야 할 것이다. 담수호소에 있어 수변식생과 산림식생 훼손은 생물다양성 및 수질에 직접적인 영향을 미치므로 보존지역과 이용지역을 명확하게 구분하고 이용지역 이외에는 엄정하게 복원 관리하여야 할 것이다.

• 대기
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• 제27권3호
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• pp.277-290
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• 2017

Characteristics of precipitation in South Korea during the 2016 Changma period (6/18~7/30) are analyzed in great details. El $Ni{\tilde{n}}o$-induced tropical Indian Ocean (IO) basin-wide warming lasts from spring to early summer and induces the western North Pacific subtropical high (WNPSH) circulation anomaly through an equatorial Kelvin wave during the 2016 Changma period. Along the northern edge of the WNPSH, strong precipitation occurred, in particular, over eastern China and southern Japan. During the Changma period, South Korea had the near-normal mean precipitation amount (~332 mm). However, about 226 mm of rain fell in South Korea during 1 July to 6 July, which amounts to 67% of total Changma precipitation in that year. Upper-level synoptic migratory lows and low-level moisture transport played an essential role, especially from 1 July to 3 July, in triggering an abrupt development of fronts over the Korean Peninsula and the eastern continent China. The front over the eastern China migrates progressively eastward, which results in heavy rainfall over the Korean peninsula from 1 to 3 July. In contrast, from 4 to 6 July, the typhoon (NEPARTAK) affected an abrupt northward advance of the North Pacific subtropical high (NPSH). The northward extension of the NPSH strengthens the Changma front and induces the southerly flows toward the Korean peninsula, giving rise to an increase in heavy rainfall. The NEPARTAK is generated due to interaction of the Madden-Julian Oscillation (MJO), equatorial Rossby wave and Kelvin waves.

• 전자공학회논문지
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• 제51권2호
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• pp.182-189
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• 2014

본 논문은 탁도의 영향으로 사용이 제한적인 수중 광학 카메라의 대안으로 수중 영상 소나(imaging sonar)를 사용하여 수중 물체를 인식하여 추종하는 구조를 제안한다. Part 1에서, 영상 소나의 현실적인 성능을 고려한 2차원 인공 표식의 설계 방법과 인식 방법을 제안한다. 특히 영상 소나와 초음파의 특성을 분석하여 피인식성을 극대화 할 수 있는 재료를 선택하였으며, 물체의 모델링이 쉬운 무지향성이며 단순한 외형을 채택하고, 표식으로 사용이 가능한 영역 기반 특징 요소를 포함한 내부 형태를 제안하였다. 또한 제안한 인공 표식을 실시간으로 인식할 수 있는 방법을 제안하였다. 이 방법은 외곽선 추출, 허프-원-검출기에 의한 유사도 및 위치 추정, 형상 행렬의 비교에 의한 표식의 분류하는 알고리즘을 포함하고 있다. 제안한 인공 표식과 인식 알고리즘의 유용함을 DIDSON (영상 소나)를 사용한 수조 실험으로 검증하였다.

• 암석학회지
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• 제2권2호
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• pp.104-121
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• 1993

Fission track (FT) thermochronological analyses on Mesozoic granites provide new information about cooling and uplift histories in Southeast Korea. Twenty-nine new FT sphene, zircon and apatite ages and seven track length measurements are presented for eleven granite samples. Measured mineral ages against assumed closure temperatures yield cooling rates for each sample. Relatively rapid (7-$15^{\circ}C$/Ma) and simple cooling patterns from the middle Cretaceouss (ca. 90-100 Ma) granites are caused mainly by a high thermal contrast between the intruding magma and country rocks at shallow crustal levels (ca. 1-2.5 km-depths). On the contrary, a slow overall cooling (1-$4^{\circ}C$/Ma) of the Triassic to Jurassic granites (ca. 250-200 Ma), emplaced at deep depths (>>9 km), may mainly depend upon very slow denudation of the overlying crust. The uplift history of the Triassic Yeongdeog Pluton in the Yeongyang Subbasin, west of the Yangsan Fault, is characterized by a relatively rapid uplift (~0.4 mm/a) before the total unroofing of the pluton in the earliest Cretaceous (~140 Ma) followed by a subsidence (~0.2mm/a) during the Hayang Group sedimentation. Stability of original FT zircon ages (156 Ma) and complete erasure of apatite ages suggest a range of 3 to 5.5 km for the basin subsidence. Since 120 Ma up to present, the Yeongyang Subbasin has been slowly uplifted (~0.04 mm/a). The FT age patterns of Jurassic granites both from the northeastern wing of the Ryeongnam Massif and from the northern edge of the Pohang-Kampo Block indicate that the two geologic units have been slowly uplifted with a same mean rate (~0.04 mm/a) since early Cretaceous. Estimates of Cenozoic total uplifts since 100 Ma are different: Ryeongnam Massif (~6 km)=Pohang-Kampo Block (~6 km)>Yeongyang Subbasin(~4 km).

• Journal of the korean society of oceanography
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• 제35권2호
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• pp.98-108
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• 2000

A geochemical study on a hemipelagic core sediment taken from the northwest Pacific Ocean (eastern edge of the Shikoku Basin) was conducted to use of excess barium (Ba(ex)) for evaluate the paleoceano-graphic changes. Also, the excursion of sedimentary Ba(ex) was compared with those of biogenic opal, carbonate and organic carbon content in the sediment during the last glacial and interglacial periods. The calculated Ba(ex) derived from the major and minor element shows a distinctive glacial-interglacial variations, and the mass accumulation rate (MAR) of Ba(ex) shows coincident variations with the MARs of biogenic fractions. Especially, strong positive correlation (r$^2$=0.85) between the MAR of Ba(ex) and the MAR of biogenic carbonate is recognized. Based on the strong positive correlation(r$^2$=0.85) between the MAR of Ba(ex) and the MAR of carbonate content, we estimated the degree of carbonate dissolution rate during the glacial and interglacial periods. Assuming the proportional variation and the refractory nature of barium exist between two factors, the variation of index Ca/Ba ratio in sediment indicates the degree of carbonate dissolution. Sedimentary Ca/Ba ratios index clearly show a striking fluctuation between the glacial and interglacial periods with higher positive correlation during glacial and lower correlation during interglacial. This fact indicates enhanced carbonate dissolution during interglacial period. Thus, the sedimentary Ca/Ba ratio in sedimentary records can be used as one of the useful tools for estimation of the relative degree of carbonate dissolution. The excursion of Ba(ex) and the sedimentary Ca/Ba ratio follows the typical pacific carbonate dissolution type(enhanced dissolution during interglacial and reduced dissolution during glacial time) as suggested by previous work (e.g., Wu et al., 1990). Variation in sedimentary Ca/Ba ratio thus strongly supports that glacial-interglacial fluctuation in carbonate dissolution has been prevailed in the northwest Pacific Ocean.

• 한국습지학회지
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• 제22권2호
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• pp.121-129
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• 2020

본 논문은 자유수면을 가지는 와류유동 내 저낙차에서 마이크로 소수력에 관한 실험 연구이다. 내부 곡선 모서리가 있는 직선, 곡선, 비틀린 블레이드의 와류 높이, 터빈 회전 및 토크를 개수로 유입구의 유량 0.0069 ㎥/s 조건에서 측정하였다. 실험결과로서 최적의 와류 강도는 와류 발생부의 외부직경과 유출구 직경 비율 0.17~18.5 범위에서 발생했다. 직선 블레이드 출력과 효율은 다른 블레이드와 비교하여 높게 나타났다. 가장 높게 생성된 에너지는 12.33 W이고, 토크는 0.91 N·m이다. 유효낙차를 고려한 경우 가장 높은 효율은 29.5 %인 반면 와류 높이를 고려한 가장 높은 효율은 회전수 132 rpm에서 80.5 %이다. 직선 블레이드의 와류 유속은 개수로 유입구의 평균 유속보다 약 2.8배 더 크게 나타난다.

• 한국환경생태학회지
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• 제22권2호
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• pp.128-137
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• 2008

본 연구는 북한산 국립공원을 대상으로 등산로가 산림경관의 파편화에 미치는 영향을 분석한 후, 이를 토대로 소유역별 경관생태학적 건전성을 평가하였다. 등산로 개설에 의한 영향 분석 결과에 따르면, 산림패치의 크기는 감소한 반면 패치 및 가장자리 밀도는 증가한 것으로 나타났다. 또한, 패치형태는 보다 복잡해지고, 핵심지역의 면적은 뚜렷하게 감소하였고, 패치간의 근접도는 증가하는 것으로 나타났다. 한편, 소유역별 경관생태학적 건전성 평가 결과, 종합적인 건전성은 북한산유역이 3.7점으로 가장 높게 나타났으며, 구기유역이 1.6점으로 가장 낮게 평가되었다. 이상의 결과를 종합해 볼 때, 산림의 경관생태학적 보전과 관리를 위해서는 불필요한 등산로의 개설을 금지하고, 훼손 및 교란 지역에 대한 자연적인 생태학적 복원이 이루어져야 할 것으로 판단된다.

• 한국농공학회논문집
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• 제53권1호
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• pp.37-45
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• 2011

Mandae watershed in Gangwon province has been known as one of soil erosion hot spot watersheds within Hanggang basin. Thus numerous efforts have been made to reduce soil erosion and pollutant loads into receiving watershed. However, proper best management practices have not been suggested because no monitoring flow and water quality data were available. Thus, modeling technique could not be utilized to evaluate water quality issue properly at Mandae watershed to develop and implement the best management practices. In this study, the SWAT model was applied to the Mandae watershed, Gangwon province to evaluate the SWAT prediction ability and water quality improvement with vegetated filter strip (VFS) in this study. The Nash-Sutcliffe model efficiency (NSE) and Coefficient of determination ($R^2$) values for flow simulation were 0.715 and 0.802, respectively, and the NSE and $R^2$ values were 0.903 and 0.920 for T-P simulation indicating the SWAT can be used to simulate flow and T-P with acceptable accuracies. The SWAT model, calibrated for flow and T-P, was used to evaluate water quality improvement with the VFS in agricultural fields. It was found that approximately 56.19 % of T-P could be reduced with vegetated filter strip of 5 m at the edge of agricultural fields within the watershed (34.86 % reduction with VFS of 1m, 48.29 % with VFS of 3 m). As shown in this study, the T-P, which plays key roles in eutrophication in the waterbodies, can be reduced with proper installation of the VFS.