• 한국환경과학회지
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• 제13권8호
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• pp.721-731
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• 2004

The dispersion of suspended particulates in the coastal complex terrain of mountain-inland basin (city)-sea, considering their recycling was investigated using three-dimensional non-hydrostatic numerical model and lagrangian particle model (or random walk model). Convective boundary layer under synoptic scale westerly wind is developed with a thickness of about I km over the ground in the west of the mountain, while a thickness of thermal internal boundary layer (TIBL) is only confined to less than 200m along the eastern slope of the mountain, below an easterly sea breeze circulation. At the mid of the eastern slop of the mountain, westerly wind confronts easterly sea breeze, which goes to the height of 1700 m above sea level and is finally eastward return flow toward the sea. At this time, particulates floated from the ground surface of the city to the top of TIBL go along the eastern slope of the mountain in the passage of sea breeze, being away the TIBL and reach near the top of the mountain. Then those particulates disperse eastward below the height of sea-breeze circulation and widely spread out over the coastal sea. Total suspended particulate concentration near the ground surface of the city is very low. On the other hand, nighttime radiative cooling produces a shallow nocturnal surface inversion layer (NSIL) of 200 m thickness over the inland surface, but relatively thin thickness less than 100m is found near the mountain surface. As synoptic scale westerly wind should be intensified under the association of mountain wind along the eastern slope of mountain to inland plain and further combine with land-breeze from inland plain toward sea, resulting in strong wind as internal gravity waves with a hydraulic jump motion bounding up to about 1km upper level in the atmosphere in the west of the city and becoming a eastward return flow. Simultaneously, wind near the eastern coastal side of the city was moderate. Since the downward strong wind penetrated into the city, the particulate matters floated near the top of the mountain in the day also moved down along the eastern slope of the mountain, reaching the. downtown and merging in the ground surface inside the NSIL with a maximum ground level concentration of total suspended particulates (TSP) at 0300 LST. Some of them were bounded up from the ground surface to the 1km upper level and the others were forward to the coastal sea surface, showing their dispersions from the coastal NSIL toward the propagation area of internal gravity waves. On the next day at 0600 LST and 0900 LST, the dispersed particulates into the coastal sea could return to the coastal inland area under the influence of sea breeze and the recycled particulates combine with emitted ones from the ground surface, resulting in relatively high TSP concentration. Later, they float again up to the thermal internal boundary layer, following sea breeze circulation.

• Structural Engineering and Mechanics
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• 제76권2호
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• pp.207-222
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• 2020

Due to the rugged terrain, metro lines in mountain city across numerous wide rivers and deep valleys, resulting in instability of high-pier bridge and insecurity of metro train subjected to fluctuating crosswind. To ensure the safe operation in metro lines in mountain cities, running safety of the metro train over the high-pier bridge under crosswind is analyzed in this paper. Firstly, the dynamic model of the wind-train-bridge (WTB) system is built, in which the speed-up effect of crosswind is fully considered. On the basis of time domain analysis, the basic characteristics of the WTB system with high-pier are analyzed. Afterwards, the dynamic responses varies with train speed and wind speed are calculated, and the safety zone of metro train over a high-pier bridge subjected to fluctuating crosswind in mountain city is determined. The results indicate that, fluctuating crosswind triggers drastic vibration to the metro train and high-pier bridges, which in turn causes running instability of the train. For this reason, the corresponding safety zone for metro train running on the high-pier is proposed, and the metro traffic on the high-pier bridge should be closed as the mean wind speed of standard height reaches 9 m/s (15.6 m/s for the train).

• 상하수도학회지
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• 제23권5호
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• pp.631-636
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• 2009

This study has its intention to investigate the water quality of non-point source which is runoff from roads. We have classified and selected twelve sites as city road, industrial road, national road and mountain road by considering their traffic volume and surroundings. Water quality was analyzed based on BOD, COD, SS, T-N and T-P and the concentrations were measured by sampling after rainfall with the interval of 10 minutes, 20 minutes, and 30 minutes. BOD was the highest in city road with 57.6 mg/L and the lowest in mountain road with 45.0 mg/L. For COD, the highest concentration in industrial road was 146.5 mg/L and the lowest was in mountain road with 98.0 mg/L. The run off concentration of SS was up to maximum 630.0 mg/L (average 280.4 mg/L) which was remarkable compared to other types of road. It showed its lowest concentration in national road with 76.0 mg/L. T-N and T-P were the highest in industrial road and the lowest in mountain road. We found out that the runoff concentration was high with large amount of traffic volume and it seemed to be high in city road and industrial road where they were largely affected by their surroundings. Relatively, national road and mountain road seemed to show low concentration as they have less traffic volume and less affected by their surroundings.

• 환경영향평가
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• 제23권3호
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• pp.208-219
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• 2014

This work aims to establish the landscape ecological countermeasures to improve the sustainability of urban mountain forest and to enrich the biodiversity in twenty mountains of the Seoul Metropolitan City. Landscape ecological analysis was conducted based upon various criteria, such as area and elevation of mountains, flora, naturalized plants, vegetation, forest types, mountain trails, and public facilities. Various measures were suggested for the better maintenances of floristic diversity, introduced plants, vegetation and forest types of urban mountain forests. Sustainable recommendations for land use adminstration were developed for the preparations of a climate change-adapted urban mountain forests, as well as rational managements of ecosystem, walking trails, and public facilities within mountain forest. Rich and diverse natural vegetation as well as high floristic diversity were reported at mountains with higher elevations, larger area size, and rich landscape diversity. Mountains with low elevation, small size with easy public access, however, might require an urgent action to decrease the burdens by anthropogenic disturbances and urban development.

• 건축역사연구
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• 제24권3호
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• pp.31-41
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• 2015

This study aims to draw out planning principles and structure of Iksan imperial capital city in late Baekje, especially in view of the relationship among imperial capital city planning area, skeletal axis and the location of royal castle. With site survey and analysis of historical records, old maps, topographical maps, archeological excavation data, land registration map of 1915, some significant inferences were drawn out. Firstly from the point of topological conditions, the contiguous line of a stratum from Mireuk mountain(彌勒山) to Wangkung-ri castle(王宮里遺蹟) and two waterways made a topological axis of Iksan Imperial capital city. Secondly district of Iksan imperial capital city can be deduced to the inner area north to Kummado soil wall(金馬都土城), south to the confluence of Iksan river(益山川) and Busang river(扶桑川), west to Okum mountain fortress(五金山城) and Galjeon river(葛田川), east to line near to eastern wall of Jesuksa temple(帝釋寺). Iksan ssang-reung(益山雙陵) was located outside western boundary line of capital city. Thirdly axis from Wangkung-ri castle to northern Kummado soil wall made a skeletal axis of city structure. It got through northern lowland along Buk river(北川) between Yonghwa(龍華山) and Mireuk mountain. Fourthly the location of royal palace can be deduced to the north part of the city around Kumma town area along the planning principle of northern royal palace.

• 한국산림과학회지
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• 제104권3호
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• pp.466-475
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• 2015

본 연구는 귀산촌 교육프로그램을 기획하고 실행하는데 기초자료를 제공하기 위해 산촌으로 이주를 희망하는 도시민들을 대상으로 귀산촌 교육 요구도를 조사 분석 하였다. 2014년 산촌미리살아보기캠프에 참여한 80명의 교육생을 대상으로 설문조사를 실시하여 분석한 결과, 중규모(20-40명)의 인원을 대상으로 한 합숙 및 현장 체험형 교육에 대한 요구도가 높은 것으로 나타났다. 그리고 실제 산촌의 특성을 잘 알고, 이주 경험이 있는 교육 강사에 대한 요구도가 높게 나타났다. Borich 요구도 공식과 IPA 분석법을 활용하여 교육 내용에 대해 분석한 결과, 임야 토지확보, 임산물 재배관리, 성공사례방문실습, 산촌관광 등 이주 후 삶을 지속하기 위해 주거지를 확보하고 경제 활동에 실질적으로 활용될 수 있는 교육에 대한 요구도가 높은 것으로 확인되었다. 하지만 보다 효율적인 귀산촌 교육을 위해서는 실제 지역에서 적응하고 있는 귀산촌인들을 대상으로 추가 조사를 진행하여 지역 정착에 필요한 다각적인 교육내용과 지원방식에 대한 논의가 필요할 것으로 보인다.

• 한국환경복원기술학회지
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• 제21권5호
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• pp.1-16
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• 2018

The purpose of this study is to identify the fragmented points of mountain ranges in Daegu metropolitan city using New Sangyeongpyo (Chart of Mountain Ranges), road system map and GIS spatial analysis, and to prioritize the identified fragmented points for restoration based on quantitative assessment. Moreover, this study proposes restoration plans reflecting the assessment results and characteristics of each fragmented point. The results of this study are summarized as follows: First of all, analysis of the distribution of mountain ranges in Daegu metropolitan city showed that jimaek and semaek in Daegu account for 2% of all mountain ranges in the country, implying that the mountain ranges of Daegu do not hold significant ranking on a national level. However, it was found that numerous fragmented points are appearing due to roads. According to the analysis, 35 fragmented points were identified, of which 15 were found to be restorable. In terms of restoration potential and involved risks, assessment results of the 15 fragmented points indicated that 6 points are at Grade I, 3 points are at Grade II and 6 points are at Grade III. Therefore, a methodology of restoring fragmented mountain ranges was proposed through three suggestions of restoration plans that consider the characteristics of each fragmented points. The results of this study are expected to be highly useful as basic data for effective restoration of mountain ranges in connection with mountain range restorations and relevant projects implemented on a national level in the future.

• 문화기술의 융합
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• 제9권4호
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• pp.121-125
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• 2023

겨울철에는 제주의 서귀포와 중문 등지는 제주시 지역에 비해 기온이 2~3℃가 따뜻하다. 이유는 한라산을 넘은 북풍이 한라산 백록담을 넘고 해발 1600m의 돈내코의 세로 300m 가로 260m 수직 암벽면을 지나면 차가운 공기가 따뜻한 공기로 변하는 단열압축으로 그 온기가 돈내코를 타서 서귀포와 중문으로 날아가기 때문이다. 반대로 여름철에 서귀포 바다를 오른 남풍은 한라산을 넘고 아흔(99)골을 지나면 후덥지근한 습도를 머금은 기온으로 변해 제주시는 무덥다. 즉, 제귀지풍과 귀제지풍 때문이다.

• 농촌계획
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• 제13권4호
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• pp.43-51
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• 2007

The propose of this paper is to study a theory on the research of mountain village region in korea of globalization age. The theory of this study is over-depopulation region study, endogenous regional development theory and resident organization, localities and new regional studies The case of over-depopulation region study, which population and land use of mountain village region due to urbanization and industrialization are changed by external factors. However, the case of some region is changed by internal factors of community residents. The endogenous regional development theory and have approached by investment policy of authorities of the mountain village region development and resident organization. The development of mountain village region have to described simultaneously both behavior strategy of community residents and investment policy of the authorities. According to localities and new regional studies, which agricultural products of mountain village region is extended to big-scale city by the progress transportation-communication and globalzation So, the research of mountain village region have to explained together intra with inter region. In the future, the research of mountain village region has to described all of case of over-depopulation region study, endogenous regional development theory, localities and new regional studies.

• 암석학회지
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• 제24권3호
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• pp.193-207
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• 2015

이 연구에서는 한양도성 석재공급지 추정을 위해 고문헌을 분석하고 산지탐색 지점에 대한 광역조사를 수행하여 암석학적 기초 데이터베이스를 구축하였다. 고문헌 분석 결과를 종합하면 성돌은 조선 초기에 주로 도성과 인접한 석산에서 조달된 반면 후기로 갈수록 도성 외부의 고정 채석장으로부터 공급되었다. 따라서 고문헌에 기록된 채석 산지를 중심으로 암석학적 조사를 수행한 결과, 산지탐색 전역에 걸쳐 담홍색화강암과 우백질화강암이 분포하였으며, 이들 화강암류는 광물조성 및 지구화학적 거동특성이 거의 유사하였다. 그러나 담홍색화강암은 남산 북사면에서 불암산의 북동방향으로 갈수록 대자율 값이 증가하는 자철석 계열을 보였으며, 우백질화강암은 용마산을 시작으로 남산과 인왕산 등의 편마암 경계부에 주로 나타나고 티탄철석계열의 낮은 대자율 특성을 가졌다. 이상의 내용을 종합할 때, 한양도성 석재공급지 추정을 위한 중요한 암석학적 지시자는 색상과 대자율로 판단된다. 이와 함께 채석장의 석재 양, 운반거리 및 기술력 등을 고려하여 원산지 해석의 신뢰도를 높일 필요가 있다.