• 한국제4기학회지
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• 제11권1호
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• pp.57-68
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• 1997

Climatic change of the late-Quaternary period has been record-ed in the loess deposits of the central Great plains and the record of such change is extractable using a number of approaches and parameters. The stratigraphy of loess deposits which have been investigated on Fort Riley exhibits the same sequence of loess units and intercalated buried soils as is found elsewhere in the re-gion but adds detail unique to the reservation Upland late-Qua-ternary composite stratigraphy preserved on the reservation con-sists of the basal Sangamon soil of the Last interglacial(c. 120-110ka), Gilman Canyon Formation(c. >40 -20ka), Peoria loess(c. 20 -10ka) Brady soil(c. 11 -10ka) Bignell loess(c. 9-\ulcornerka). and mod-ern surface soil. Application of magnetic analyses has provided proxy data sets that represent a time series of climatically regulated pedogenesis/weathering and botanical composition. magetic data have yielded an impression of the variation in climate from Sangamon time to the late Holocene through a reconstruction of the history of pedogenesis/weathering. Sangamon soil formation dominated the reservation durin the Last interglacial as indicated by magnetic parameters. During Gil-man Canyon time loess influx was usually sufficiently slow as to permit pedogenesis which appears to have been at a maximum twice during that time. Warm season grasses were important dur-ing soil formation but diminished in importance during the peri-ods of more rapid loess fall which were cooler and perhaps wet-ter. Peoria loess fall a function of the deterioration of climate during the last Glacial Maximum thinly blanketed the reservation with thickest accumulations occurring to the north-west(Bala Cemetery site)proximal to the source region. Long-term surface stability did not apparently occur within Peoria time but short-term stability may be indicaed by the presence of thin weathering zones(incipient soils) in the Peoria loess. Re-gional landscape stability prevailed during the environmental shift at the Pleistocene/Holocene transition resulting in forma-tion of the well expressed Brady soil. One or more weak soils developed in the Bignell loess as it ac-cumulated. A notable feature of the Bignell loess is the appear-ance of the Altithermal dry period: the loess experienced little weathering and was dominated by warm season grasses until the latter of the Holocene.

• 한국해양환경ㆍ에너지학회지
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• 제2권2호
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• pp.20-30
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• 1999

영국의 북서 Fylde 연안역에서, 수영객들을 위한 수질을 개선하기 위해, 방류구에서 흘러나온 오수를 수치모의실험을 통하여 연구하였다. 수질모델의이류확산방정식에서 확산항과 이류항은 양해법 이차정밀도의 중앙차분법과 삼차정밀도의 QUICKEST 법을 사용하여 표현하였다. 수리역학모델은 광역과 세부역으로 나누어지며, 이때 격자는 각기 1km와 200m를 사용하였고, 모의실험의 (유속과조위)결과는 관측값과 잘 일치하였다. 그 다음 단계로서 수질모델을 사용하여 faecal coliform 의 농도분포를 예측하였다. 이 때 4가지의 시나리오가 사용되었다:-(i) Fleetwood outfall,(ii) River Ribble for summer condition,(iii)River Ribble for winter condition 그리고 (iv) Combined Sewer Overflows. 모의 실험의 주요 결과는 다음과 같다:- (i) Fleetwood 방류구에서 방류된 coliform은 Fylde 연안에 거의 미치지 않는다:(ii)여름과 겨울, Ribble에서 유입된 coliform은 Lytham St.Annes에서 10-500(counts/100ml)농도분포를 보였다;(iii)CSO에서 방류된 오수는 해안에서 벗어나 offshore로 이동되지 못하는 것으로 예측되었다.

• 대한지리학회지
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• 제51권2호
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• pp.235-253
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• 2016

중국은 2004년부터 자동차 공업 관련 신산업 정책을 추진하기 시작하였다. 이와 함께 기존의 맹목적인 외자유치에서 높은 기술수준을 지닌 외자기업을 유치하는 방향으로 선회하였다. 이러한 정책적 환경 변화는 수많은 다국적 기업들 및 협력기업들의 중국 진출을 본격화시켰으며, 한국의 완성차 및 부품기업 또한 진출이 이루어졌다. 외자기업의 착근과정에서 나타난 제도적 변화에 의한 혁신적인 기술 적용 필요성은 기업의 기술 혁신 필요성과 조응하였는데, 효율적 공간 전략이 요구되었다. 첫째, 제도적 변화에 따른 로컬 파트너십 활용과 부품기업 동반진출 전략, 둘째, 기술혁신을 통한 모듈화 및 공용 플랫폼 전략, 셋째, 지방정부 인센티브 정책 활용 전략이 그것이다. 특히 생산 네트워크 내 행위자들은 직서열 공급방식을 통한 부품 공급망을 따라 전후방 연계의 흐름이 나타났으며 관계성이 강화되었다. 따라서 부품기업들은 원활한 협력 체제를 위해 전방기업 및 모듈 단위 중심으로 집적하였다. 그 결과 북쪽의 베이징 현대를 중심으로 하는 북쪽 지역, 남쪽의 동풍열달기아를 중심으로 하는 남쪽 지역, 공용 부품을 공급하기 위한 칭다오를 중심으로 하는 중부 지역, 일반 공용 부품 및 원자재를 공급하는 상하이를 중심으로 하는 기타 지역으로 생산 공간의 분화가 나타났다.

• 한국의류학회지
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• 제32권6호
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• pp.902-910
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• 2008

Orientalism은 동양을 서양과는 다른 이질적 인 대상, 괴상하고 후진적이며 수동적 인 특성을 지닌 열등한 타자로 서양인의 무의식 속에 내면화되어 왔다. 아시아를 일정한 지배의 틀 속에 가두는 문화적 장치와 담론의 체계인 Orientalism은 원래 남유럽과 북아프리카를 포함한 서남아시아에 해당하는 서유럽 중심의 용어였으며, 비 서구사회는 서구문명을 수용함으로써만 발전할 수 있다는 논리의 사상이다. 따라서 이러한 용어의 무분별한 사용은 부적절하다. 또한 아시아의 이미지나 복식양식을 차용한 서구의 아시안 룩에 아시아 본래의 정신은 사라졌다고 하여도 아시아를 저급한 타자로 인식한 것에서 비롯된 것이 아니다. Asian Ethnic Look은 동양적 미학에 매료되어 동양의 이미지나 양식을 차용한 서양의 복식이므로 Orientalism의 속성과는 차이가 있다. 국내의 패션계에서는 이에 대한 분별없이 혼용하여 사용하고 있고, 특히 Orientalism Fashion 또는 Oriental Look이라고 자주 사용하고 있다. 아시아의 복식이나 이미지를 기괴하게 조작한 일부 특정한 복식만을 Orientalism Fashion 또는 Oriental Look이라 해야 하며, 이를 제외하고는 'Asian Look', 'Asian Fashion', 'Asian Ethnic Look' 등으로 바꾸어 쓰거나, 'Korean Look' 등의 개별 국가나 지역 명으로 바꾸어 쓰는 것을 분명히 해야 한다 한국을 비롯한 아시아는 서구 중심의 수동적 입장이 아니라, 세계 패션산업의 중심축 중 하나로써 세계 패션을 리드하고 있다. 이제는 우리 스스로가 서구중심의 이분법적 편견을 해체해 나가야 할 것이다.

• 한국전통조경학회지
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• 제36권4호
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• pp.18-27
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• 2018

본 연구는 황가원림이 중국 고전원림을 집대성한 산물임을 상정하고 황가원림에 연출된 경관 특성을 분석한 연구이다. 이화원에는 아름다운 경관을 감상하고자 한 황제의 욕망을 위해 다양한 경관연출기법이 적용되었는데 이에 따른 경관 특성은 다음과 같이 정리할 수 있다. 첫째, 이화원은 차경, 주경, 배경, 대경, 협경, 분경, 광경, 누경, 첨경 등 다양한 조망처리기법을 통해 다양한 원림경관을 형성하고 있다. 둘째, 남북의 중축선을 기준으로 한 건축물을 대칭구도 및 장랑구조, 시각생리를 고려한 경점의 배치를 통해 경관 감상에 집중할 수 있도록 하였다. 셋째, 중국 각지의 명승지 경관을 이화원의 고유한 지형적 특성에 맞게 도입하는 명경이식기법을 활용하였다. 이화원에는 항주와 기창원, 소주의 산당가의 경관이 재현 이식되어 공통적으로 강남지역의 경관이 이식되어 있음을 확인하였다. 이상의 3가지 기법들은 원림 내에 공간감을 살리고, 풍부한 경관을 연출할 뿐 아니라 유람객의 시선을 자연스럽게 유도하고 집중시키는 효과가 있음을 확인하였다.

• 환경생물
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• 제40권4호
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• pp.567-578
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• 2022

본 연구는 국내 주요 용재수종인 잣나무와 삼나무, 편백에 대한 종 분포 예측 모델의 결과를 앙상블하여 기후 시나리오에 따라 현재, 근미래, 먼미래의 서식 적합지를 예측하였고 잣나무와 삼나무, 편백의 기후변화 시나리오별 분포 적합지를 분석하였다. 특히, 잣나무를 삼나무와 편백이 대체할 수 있는지 평가하였다. 기준연도(현재) 잣나무의 매우 적합한 서식지는 전국의 약 13.87%를 차지하지만 SSP5-8.5 하의 먼미래에서는 약 0.11%까지 낮아진다. 삼나무의 경우 기준연도의 서식 적합지는 약 7.08%이며 SSP5-8.5하의 먼미래에서는 약 18.21%까지 증가한다. 편백의 경우 기준연도의 서식 적합지는 약 19.32%이며 SSP5-8.5 하의 먼미래에서는 약 90.93%까지 차지하는 것으로 예측되었다. 전국적으로 조림하던 잣나무는 기후변화의 영향으로 서식처가 점차 북상하여 우리나라에서 적합한 서식처가 크게 감소하였으므로 21세기 중반 이후에는 국내에서 용재수종으로 조림하기에는 부적합하며 높은 수준의 서식 적합도를 갖는 편백이나 삼나무로 대체될 필요가 있다고 전망된다. 특히, 편백은 대부분의 영역에서 잣나무를 대체 가능하며, 삼나무의 경우 남해안과 중부지방 일부분을 대체할 수 있다고 평가되었다. 결론적으로 미래에는 조림하는 용재수종의 변화가 생길 것이며 다양한 수종을 대상으로 한 연구를 통해 기후변화에 대응하는 방안이 마련되기를 기대한다.

• 한국산림과학회지
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• 제110권3호
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• pp.322-340
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• 2021

최근 급격한 봄철 기온 상승과 기후변화의 영향으로 한반도에 분포하고 있는 아까시나무의 개화 시기가 변화하면서 지역간에 동시 개화 현상(simultaneous blooming)이 관측되고 있다. 이러한 변화는 국내 양봉 산업에 큰 변화를 초래하였고, 이로 인해 정확도 높은 아까시나무 개화시기 정보에 대한 수요가 증가하고 있다. 따라서, 본 연구를 통해 아까시나무의 지역별 개화 시기 변화를 잘 설명할 수 있는 신뢰도 높은 개화 시기 예측 모형을 개발하고자 하였다. 이를 위해 지난 12년(2006~2017년)간 전국 26개 지점에서 관측된 아까시나무 만개일 자료와 과거 일기온 복원 자료를 활용하여 봄철 기온 및 아까시나무 만개일 변화의 경향성을 권역별로 파악하고, 과정기반모형을 활용하여 지역 통합 모형(SM)과 함께 지역적 특성을 반영하는 세 모형-SM에 지점별 보정계수를 도입한 수정 통합 모형(MSM), 권역별로 모수를 추정하는 권역별 통합 모형(GM), 관측 지점별로 모수를 추정하는 지역 모형(LM)-을 도출, 성능을 비교하였다. 기온 및 만개일의 경향 분석 결과, 남부 지역에 비해 봄철 기온 상승률이 2배 이상 높았던 중북부 내륙 지역의 경우 만개일이 빠른 속도로 앞당겨져, 결과적으로 남서부 해안 지역과의 만개일 차이는 1년에 0.7098일씩 감소하였다(p-value=0.0417). 전체 지역에 대한 모형의 성능 비교 결과, 지역 특이성이 반영되지 않은 SM에 비해서 MSM은 24% 이상, LM은 15% 이상 감소한 RMSE 값을 나타냈다. 또한 LM과 MSM의 예측 알고리즘을 전국 범위로 확대하여 4년 간(2014~2017년) 16개의 추가 관측 지점을 대상으로 검증한 결과, LM에 코크리깅(Co-kriging)기법을 적용한 방법이 보정계수 전국 분포도를 추정하여 SM을 보정하는 방법보다 예측력이 더 뛰어났으며, 오차의 분포는 두 모형 간에 통계적으로 유의한 차이를 보였다(RMSE: p-value=0.0118, Bias: p-value=0.0471). 본 연구는 아까시나무의 개화 시기 예측에 있어 지역 단위 예측의 신뢰도를 향상시키고 모형을 넓은 지역 범위로 확대, 적용하기 위한 방안을 제시하였다.

• 자원환경지질
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• 제2권4호
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• pp.73-90
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• 1969

The area studied is a southwestern part of Okcheon geosynclinal zone which streches diagonally across the Korean peninsula in the mid-central parts of South Korea, and is bounded by Charyeong mountain chains in the north and by Sobaek mountain chains in the south. The general trend of the zone is of NE-SW direction known as Sinian direction. Okcheon system of pre-Cambrian age occupies southwestern portion of Okcheon geosynclinal zone, and Choseon and Pyeongan systems of Cambrian to Triassic age in northeastern portion of the zone. It was defined by the writer that the former was called "Okcheon Paleogeosynclinal zone" and the latter "Okcheon Neogeosynclinal zone," although T. Kobayashi named them "Metamorphosed Okcheon zone" and "Non-metamorphosed Okcheon zone" respectively and thought that sedimentary formations in both zones were same in origin and of Paleozonic age, and C.M. Son also described that Okchon system was of post-Choseon (Ordovician) and pre-Kyeongsang (Cretaceous) in age. According to the present study two zones are separated by great fault so that the geology in both zones is not only entirely different in origin and age, but also their geolosical structures are discontinuous. Stratigraphy and structure of Okcheon system are clearly established and defined by the writer and its age is definitely pre-Cambrian. It is clarified by present study that the meta-sediments in and at vicinity of Charyeong mountain chains are correlated to Weonnam series of pre-Cambrian age which occupies and continues from northeast to southwest in and at south of Sobaek mountain chains, and both metasediments constitute basement of Okcheon system. Pyeongan, Daedong and Kyeongsang systems were deposited in few narrow intermontain basins in Okcheon paleogeosynclinal zone after it was emerged at the end of Carboniferous period. Granites of Jurassic and Cretaceous ages and volcanics of Cretaceous age are cropped out in the zone. Jurassic granite is aligned generally with the trend of Okcheon geosynclinal zone, whereas Cretaceous granite lacks of trend in distribution. Many isoclinal folds and thrust faults caused by Taebo orogeny at the end of Jurassic period are also parallel with Sinian directieon and dip steeply to northwest. Charyeong, Noryeong, Sobaek, and Deogyu mountain chains are located in areas of anticlinorium, and Kyongsang system in narrow synclinal zones. Folds in Okcheon neogeosynclinal zone are generally of N 70-80W direction but deviate to Sinian direction at the western parts of the zone. This phenomena is interpreted by the fact that the folds were originated by Songrim disturbance at the end of Triassic period and later partly modified by Taebo orogeny. Thrust faults of Taebo orogeny coentinue from Okcheon paleogeosynclinal zone into neogeosynclinal zone, forming imbricated structure as previously described. Strike-slip faults perpendicular to Sinian direction and shear faults diagonally across it by 55 degrees also prevail in neogeosynclinal zone. It is concluded from viewpoints on geology and geological structure that l)Okchon geosyncline had changed its location and affected by numerous disturbances through geologic time, and 2)mountain chains in the area such as Charyeong, Noryeong, Sobaek, and Deogyu were originated as folded mountains. Differing from others, however, Sobaek range was probably formed at the time of Songrim disturbance and modified later by Taebo orogeny. It is cut by Danyang-Jeomchon fault at the vicinity of Joryeong near Munkyeong village and does not continue to southwest beyond the fault, whereas southwestern portion of erstwhile Sobaek range continues to Taebaek rangd northeastward from Deogyusan passing through Sangju, Yecheon, and Andong. From these evidences, the writer has newly defined the erstwhile Sobaek range in such a way that Sobaek range is restricted only to northeastern portion and Deogyu range is named for the southwestern portion of previous Bobaek range.

• Journal of Korean Society for Atmospheric Environment
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• 제10권E호
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• pp.311-324
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• 1994

The quantitative knowledge of N $O_{\gamma}$ (＝N $O_{x}$ ＋HN $O_3$＋/PAN＋N $O_3$ ＋$N_2$ $O_{5}$ ＋HN $O_2$＋N $O_3$$^{-10}$ ＋organic nitrates＋......)distribution is essential in tropospheric chemistry, especially, especially that related to understanding the processes leading to ozone production. Ambient concentrations of NO, N $O_2$, HN $O_3$ and PAN as well as total N $O_{\gamma}$ were measured during June and early July 1992 at a rural site(Candor, NC), in the central Piedmont region of NC. The measurements of N $O_{\gamma}$ species were made in an effort to provide a comprehensive understanding of nitrogen chemistry and to investigate the total nitrogen budget at the site. N $O_{\gamma}$, N $O_2$, and NO showed diurnal variations with maxima in the morning. The maximum N $O_{\gamma}$ concentration reached was 14.5 ppbv, and the maximum concentrations of NO and N $O_2$ were 5.4 and 7.8 PPbv, respectively. The mean N $O_{\gamma}$ concentration as found to be 2.88$\pm$1.58 ppbv(n=743). The mean concentrations of NO and N $O_2$, were found to be 0.15 $\pm$ 0.29 ppbv(n＝785) and 1.31 $\pm$ 0.99 ppbv(n＝769). Products of photochemical oxidants, (N <$O_{\gamma}$-N $O_{x}$ ), such as HN $O_3$ and PAN, as well as ozone showed diurnal variation with maxima in the afternoon and minima at night The fractions of individual reactive nitrogen species to total N $O_{\gamma}$ were investigated and contrasted to the results from remote marine site and rural continental sites. N $O_{x}$ was the major species to total N $O_{\gamma}$(45%). NO concentrations appeared to be nearly constant whether the Prevailing winds were from continental areas or from oceanic areas. Linear regression of $O_3$ with (N $O_{\gamma}$- N $O_{x}$ )/N $O_{\gamma}$ (i.e. percent N $O_{x}$ converted to the photochemical products of N $O_{\gamma}$) yielded ( $O_3$) ＝25.8 〔 N $O_{\gamma}$-N $O_{x}$ 〕/(N $O_{\gamma}$) ＋27, ( $r^{2}$＝0.58). The regression intercept is interpreted as the ozone back ground (intercept=27ppbv) and the slope suggests that 8.6 molecules of ozone are formed per molecule of N $O_{x}$ oxidized products (when the average N $O_{\gamma}$ concentration, about 3 ppbv at the site, is used). The N $O_{x}$ N $O_{\gamma}$ ratio was used as an indicator of the chemical age of airmasses and the ratio showed strong positive correlations with HN $O_3$( $r^{2}$=0.58), PAN ( $r^{2}$=0.46) and $O_3$( $r^{2}$=0.62). Larger N $O_{\gamma}$ and N $O_{x}$ N $O_{\gamma}$ ratio were found when winds came from continental sides. It may suggest that synoptic meteorological conditions and transport of N $O_{x}$ are important in the distribution of N $O_{\gamma}$ and its relationship with photochemical oxidants at the site.

• 한국환경보건학회지
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• 제10권2호
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• pp.9-40
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• 1984

This thesis purports to overview the diverse administrative and organizational factors and plannings developed by the government organizations, municipal or otherwise, to tackle the Han River water pollution issues in the past years. This thesis also looks into the ever-worsening Han River water pollution problems, in particular, in terms of the various government plans ostensibly designed to reduce the pollution level but with little success. Also dealt with are the efficiencies with which the laws and decrees on water pollution the administrative organizations put to use in the prosecution of the diverse antiwater pollution projects involving the Han River basin. From the early 1960's up to the 1970's the government had concentrated on the growth-oriented economic policy with the result that little attention had been paid to the water pollution and other environmental issues that are bound to arise from the massive economic growth. Belatedly, the five-year Hah River Development Project was initiated in 1982 with emphasis on reducing the water pollution level at Hah River to the minimum. The following are the gists of the thesis and recommendations for the future antiwater pollution plans by the administrative organizations: 1. Documents to date indicate that the irrigation projects along the Han River area had been the main focus of attention during the Yi Dynasty and under the Japanese rule of the country. 2. Despite that the water pollution issue became the subject of many debates among the academic and research institutions in the 1960's and in the 1970's, the administrative organizations in charge of the Han River water quality control failed to come up with a concrete plan for the river's water quality control. 3. Nevertheless, the water pollution of the Han River area in fact began in the 1950's, with the unprecedented concentration into Seoul of population and the industrial facilities on a larger scale, in particular, enforced by the government's strong growthoriented policy in its Economic Development plans in the 1960's. 4. Starting in the 1960's, the Han River water pollution level dramatically increased, but the government was reluctant to promulgate or put into effect strong measures to curb the many factors contributing to the river water pollution, thus worsening the environmental issues along the Han River basin. 5. The environmental protection law and other laws and decrees relating to the antiwater and air pollution issues that were subsequently put into effect underwent so many changes that efficient anti-water pollution policies could not be effected for the Han River basin. The frequent organizational reshuffle within the administrative units concerned with environmental problems has resulted in the undue waste in personnel management and finance. 6. The administration on the environmental protection could not be efficiently carried out due to the organizational overlapping. Under the existing law, frequent organizational frictions and inefficiency are bound to occur among the central government offices themselves, as well as between the central government and the Seoul city administration, and among the city's administrative offices over the conservation of the Han River basin and over the river's anti-water pollution issue. 7. In the planning and prosecution of the Han River project, political influences from the president down to the lower-level politicious appear to have been involved. These political influences in the past had certainly had negative influence on the project, nevertheless, it appears that in the recent years, these political influences are not all that negative in view of the fact that they serve as a positive contributing factor in developing a better water quality control project along the Han River basin. The following are a few recommendations based on the data from the thesis: First, officials in charge of the Han River water quality control should pay attention to a careful screening of the opinions and recommendations from the academic circles and from the public should be made so that the government could better grasp the core issues in the environmental problems that require preventive and other necessary measures. Second, vigorous redistribution policies of population and industrial facilities away from the Seoul area should be pursued. Third, the government should refrain from revising or revamping too frequently the laws and decrees on the anti-water pollution, which is feared to cause undue inconveniences in the environmental administration. Fourth, a large-scale streamlining should be made to the existing administrative organization in an effort to do away with the inter- and intra-organizational friction. It is recommended that a secretariat for the Hah River basis conservation be established. Fifth, High-level administrative officials, with a thorough knowledge and vision on the Han River water quality control, should be prepared to better deal with the budgeting and personnel management for the Han River water pollution control not only at the control government, but also at the Seoul city municipal government levels. Environmental issues should be kept distinct from political issues. Environmental issues should not serve as a window-dressing for sheer political purposes. Sixth, the Hah River proiect should also include, along with the main Han River basin, those areas covering North Han River, South Han River, and the tributaries to the main river basin. The 'Han River Basin Water Quality Control Board' should be established immediately as a means of strengthening the current Han River basin water quality control policy. Seventh, in drawing up the Han River proiect, the administrative officials should be aware that Han River basin is a life line for those people in the region, providing them with not only a sheer physical space, but with a psychological living space for their everyday life.