• 한국산림과학회지
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• 제112권3호
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• pp.374-381
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• 2023

산지하천에서 발생하는 돌발홍수는 특정 지점의 점(Point) 유속보다는 전체 구간의 평균 유속에 따라 이동속도가 결정되며, 구간 평균유속은 하천경사, 하상재료, 수리적 거칠기에 많은 영향을 받는다. 이 연구에서는 하천경사 및 거칠기 높이를 이용하여 산지하천의 구간 평균유속 추정방법을 개발하였다. 염료추적자법(Dye Tracing)을 이용하여 특정 구간의 평균유속을 측정하고, LiDAR 영상으로부터 하천 지형 및 형상을 추출하였다. 거칠기 높이를 산정하기 위해 표면 거칠기 변수(R_a, R_max, R_z )와 하상재료의 크기(D₅₀, D₈₄)를 이용하였다. 현장 계측자료로부터 무차원 접근법을 이용하여 구간 평균유속과 유량과의 관계식 v = 0.5499Q^0.6165 을 도출하였으며, R² =0.77의 설명력을 나타냈다. 이 연구에 이용된 5개의 거칠기 높이 중 평균 거칠기 높이(R_a)의 RMSE가 0.45로서 다른 거칠기 높이의 범위(0.47-1.04)보다 낮게 나타나 평균 거칠기 높이(R_a)가 구간 평균유속 산정을 위한 거칠기 높이 인자로 가장 적합하다고 판단되었다.

• Animal Systematics, Evolution and Diversity
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• 제30권1호
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• pp.1-8
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• 2014

The Dryopidae (Coleoptera) is composed of approximately 300 species worldwide belonging to 33 genera; however, members of the family have not been recorded in Korea. We collected and recorded adult specimens of Elmomorphus brevicornis Sharp (=E. brevicornis brevicornis Sharp) on piles of submerged twigs and branches of a decayed tree (Prunus sp.) from a mountain stream in southwestern Korea with a comparison of the type specimens of E. brevicornis amamiensis Nomura from Japan. Both of the subspecies are raised to the species level herein. Redescription, photographs, line drawings of diagnostic characteristics, distribution map, habitat, and taxonomic notes for Elmomorphus brevicornis are provided.

• Animal Systematics, Evolution and Diversity
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• 제33권1호
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• pp.56-59
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• 2017

The external anatomy of the immature stages (last instar larva and pupa) of the crane fly, Tipula (Nippotipula) sinica Alexander, 1935 (Diptera: Tipulidae) is described and illustrated from specimens first collected in Korean peninsula (South Korea). Comments concerning natural history and microhabitats of larvae are provided. This is the first detailed description with illustrations for the last instar larva and pupa of Tipula (Nippotipula) sinica. Pupal characteristics resemble those of most species from advanced lineages within the subfamily Tipulinae. And, also it described with habitats and biological notes of Tipula (Nippotipula) sinica. Crane fly larvae, categorization as found in this survey indicate a taxonomic stream and are expected to help.

• 동굴
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• 제67호
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• pp.21-34
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• 2005

점말동굴은 대부분이 퇴적기원인 석회 암 동굴이다. 토양은 산악지 역, 구릉지, 산록지 등에 다양한 종류의 토양이 분포한다. 동굴의 기본 골격은 주변을 통과하는 단층곡의 일부에 형성되었다. 동굴내의 소규모 수로는 절리의 방향이나 규모에 의해 유도된다. 동굴의 형태와 미지형은 그 지역의 지질구조 및 지하수의 유동과 밀접한 관련이 있다. 동굴내의 점토는 지표로부터 유입되었을 가능성이 크다. 동굴의 성인은 구조적으로 접근하는 것이 필요하다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 봄 학술발표회 논문집
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• pp.181-188
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• 2002

Water flow rate into the tunnel usually determined by numerical analyses and mathematical formulas using water levels and permeability is obtained only a few limited districts of the whole tunneling site. However, underground is not a homogeneous but complicated mass. Therefore these methods can't reflect structural and geological aspects. In this study, assuming that the mountain stream in droughty season is to be the same as baseflow of its basin, hydrological method is applied to predict the constant water flow rate into the tunnel on construction field. Prediction of constant water inflow rate is performed on each section of tunnel construction field divided into 20 sections.

• 한국디지털건축인테리어학회논문집
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• 제3권2호
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• pp.8-13
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• 2003

The purpose of this study was to analyze the Site layout of Buddhist Architicture by water space of landscape architecture. As a result, the following fact is identified; We knew that land scape of Buddhist Architecture is intentional device. Example from the Tong-do Temple, it leads cleary the intention of water-space. The case of Tong-do Temple, water space is divided into Yeon-ji(lotus pond) and the Yeong-gi(shadow pond) and Gye-ryu(mountain stream). The viewing intention of Gu-Ryong-ji where Yong-ji the construction intention characteristic is positive it was intended there is a possibility of knowing. From the research which it sees it is limited in case of the Tong-do Temple tries to search a concrete instance. but on this outside many multiple architectural space uses water space and It creates the space where it leads the harmony of architecture and intention it was plentifully included.

• 한국조경학회지
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• 제23권2호
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• pp.44-62
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• 1995

This study investigated the landscape space of Chosun Dynasty pavilions in the Sang-ju Region. Five renowned pavilions were selected for study by Phenomenological and IDRISI (4.1) S/W. The results were as follows ; Pavilions were erected for studying cultivating moral sense admiring the view relieving illness and commemorat memoring people. A total of 248 pavilions were erected in the Sang-ju Region between 1392 and 1895 AD, most of them duing he golden age from 15001670 AD. Pavilions and open space were composed in harmony with nature borrowing natural landscape features. Landscape characteristics were analysised with IDRISI(4.1) S/W; pavilions were ma711y located at the bottom of a mountain with stream The Inner garden was formed by a fence and Lagerstroemia indica or a few trees. The Outer garden was formed by mixed stands of Pinus dentsiflora, Zelkowa serreta, Acer formosum and well conserved natural vegetation.

• 한국환경생태학회지
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• 제34권6호
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• pp.530-542
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• 2020

중부산악 DMZ 민통선이북지역의 담수어류 출현양상을 밝히기 위해 2018년 5월부터 10월까지 조사를 실시하였다. 조사기간동안 24개 지점에서 족대와 투망으로 12과 43종 7,744개체를 채집하였고, 우점종은 참갈겨니(30.3%), 아우점종은 피라미(18.5%)였으며, 그 다음으로 버들치(10.0%), 버들개(6.7%), 돌마자(5.9%), 묵납자루(4.5%), 돌고기(4.2%), 대륙종개(2.6%), 등의 순으로 우세하게 출현하였다. 출현종 중 법정보호종은 천연기념물 어름치 1종, 환경부지정 멸종위기야생생물 II급의 다묵장어, 묵납자루, 가는돌고기 3종 등 모두 4종이, 한국고유종은 20종(46.5%)이 채집되었다. 또한 기후변화민감종(냉수성어류)은 금강모치와 새미, 둑중개 3종이, 육봉형 어류는 다묵장어와 둑중개와 밀어 3종이, 외래종은 배스 1종이 출현하였다. 지점별 우점종은 참갈겨니(15개 지점), 피라미와 버들치(4개), 둑중개(1개)였으며, 우점도는 상류부에서 하류부(김화남 대천 본류)로 갈수록 낮아지고, 반대로 다양도와 종풍부도는 상류부에서 하류부로 갈수록 높아졌다. 군집구조는 크게 최상류, 상류, 한강, 임진강으로 구분되었다. 선행조사와 비교한 결과, 본 조사에서 가장 많은 종(43종)이 채집되었고, 새로 채집된 어류는 2종(참중고기, 배스), 채집되지 않은 종은 6종(쏘가리, 대농갱이, 열목어, 흰줄납줄개, 왜매치, 왜몰개)이었다. 김화남대천은 법정보호종(4종)을 비롯한 많은 종이 서식하고 다양도와 풍부도지수가 높아 생물학적 가치가 높았고, 끝으로 이 지역의 보전방안에 대해 논의하였다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2011년도 학술발표회
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• pp.46-46
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• 2011

Severe sediment erosion during floods occur disaster and economic losses, but general sediment erosion is basic mechanism to move sediment from upstream to downstream river. In addition, it is important process to change river form. Check dam, which is constructed in mountain stream, play a vital role such as control of sudden debris flow, but it has negative aspects to river ecosystem. Now a day, check dam of open type is an alternative plan to recover river biological diversity and ecosystem through sediment transport while maintaining the function of disaster control. The purpose of this paper is to verify sediment erosion progress of river bottom and bank as first step for river restoration after dam slit by cross-sectional shear stress and critical shear stress. Study area is upstream reach of slit check dam in mountain stream, named Wasada, in Japan. The check dam was slit with two passages in August, 2010. The transects were surveyed for four upstream cross-sections, 7.4 m, 34 m, 86 m, and 150 m distance from dam in October 2010. Sediment size was surveyed at river bottom and bank. Sediment of cobble size was found at the wetted bottom, and small size particles of sand to medium gravel composed river bank. Discharge was $2.5\;m^3/s$ and bottom slope was 0.027 m/m. Excess shear stress (${\tau}_{ex}$) was calculated for hydraulic erosion by subtracting the values of critical shear stress (${\tau}_{c}$) from the value of shear stress (${\tau}$) at river bottom and bank (${\tau}_{ex}=\tau-{\tau}_c$). Shear stress of river bottom (${\tau}_{bottom}$) was calculated using the cross-sectional shear stress, and bank shear stress (${\tau}_{bank}$) was calculated from the method of Flintham and Carling (1988). $${\tau}_{bank}={\tau}^*SF_{bank}((B+P_{bed})/(2^*P_{bank}))$$ where $SF_{bank}=1.77(P_{bed}/p_{bank}+1.5)^{-1.4}$, B is the water surface width, $P_{bed}$ and $P_{bank}$ are wetted parameter of the bed and bank. Estimated values for ${\tau}_{bottom}$ for a flow of $2.5\;m^3/s$ were lower as 25.0 (7.5 m cross-section), 25.7 (34 m), 21.3 (86 m) and 19.8 (150 m), in N/$m^2$, than critical shear stress (${\tau}_c=62.1\;N/m^2$) with cobble of 64 mm. The values were insufficient to erode cobble sediment. In contrast, even if the values of ${\tau}_{bank}$ were lower than the values for ${\tau}_{bottom}$ as 18.7 (7.5 m), 19.3 (34 m), 16.1 (86 m) and 14.7 (150 m), in N/$m^2$, excess shear stresses were calculated at the three cross-sections of 7.5 m, 34 m, and 86 m distances compare with ${\tau}_c$ is 15.5 N/$m^2$ of 16mm gravel. Bank shear stresses were sufficient for erosion of the medium gravel to sand. Therefore there is potential to erode lateral bank than downward erosion in a flow of $2.5\;m^3/s$. Undercutting of the wetted bank can causes bank scour or collapse, therefore this channel has potential to become wider at the same time. This research is about a potential of sediment erosion, and the result could not verify with real data. Therefore it need next step for verification. In addition an erosion mechanism for river restoration is not simple because discharge distribution is variable by snow-melting or rainy season, and a function for disaster control will recover by big precipitation event. Therefore it needs to consider the relationship between continuous discharge change and sediment erosion.

• 건축역사연구
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• 제1권1호
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• pp.68-87
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• 1992

This study is the conditions of location according to formed the times in the clan village. The results of this study are as follows ; 1. in the 15th century, the characterestics of the village established residencial place where mountain stream flowed surrounded by the mountain and deep in the mountains with superior quality land. That's because Sa-dae-bu put equal importance on beautiful scenery and practical benefit for living. Stream House provided economical foundation for Sa-dae-bu to be able to keep confucial manners by putting limit their economic status to small medium sized land owner. Topographical condition such as valley or hollow separated from the exterior maintained unification of consanguineous village in self sufficient farming society and held on to independent territory against external to be able to stay away from turbulent days so that they formed residential area of Sa-dae-bu clan. And the valley where flowed clean water was considered as the connection of continuous place where distinctiveness of form in each curve and and factor of calm and dynamic scenery of the clean stream. Scholars in the middle of Chosun Dynasty located in the utopia as place for confucious retirement to study, a place for refinement by combination with the nature or as a way of spacial practice based on Confucious view of nature. 2. in the 16th-l7th century, Most of existing consanguineous villages adopt deep in the mountains for refuge. at that place, upward rank was established by settlement of the ancestor who entered in the village first, the principal was placed in the center of the village and since descendants became numerous, it was serialized as the space of descendants. So, it was arranged in the order of social rank. Most of the villages showed development step by step started from precaution by apperance of the mountain to the lower part. It's because the topography of valley around the village worked as the natural hedge against external force and genealogy of the clan, regularity of social status, order of entrance into the village were reflected into residencial destribution. Also, order of the rank coincided with the one of aspects on geomancy. Genealogical rank within the village represented spacial rank. Houses of descendants and branch families were placed lower than the principal which showed worship to the principal. 3. In 18th century after, as the village was settled nearby cultivated land considering economical loss caused by long distance between residencial area and cultivated land, direction of sect followed by development of village expanded from the front part of the village to the rear part. The principal that was poped out to the front presented frontage over exterior. Therefore, residencial area of branch families expanded to the rear starting from the principal. This represented a slice of social structure at that time. after 18th century, spirit was percieved superior over material, After then, development of cultivation and expantion of land created difference of economic strength within one village. In order to maintain and show off the status of Yang-ban, economic power of indigenous land owner became fundamental, so, sense to worship and to keep the principal became weak eventually. Taking advantage of that situation, residencial area of branch family expanded to the rear part of the principal which showed dual disposition conflicted with each other. However, these clan rules were destroyed and new rules were created after 18th century because of the situation and consciousness at that time.