• Title/Summary/Keyword: 종단 및 횡단 폭

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Correlation Analysis of Rainfall Critical Duration and Time of Concentration by Road Surface Conditions and Rainfall Intensity (도로표면 조건과 강우강도 변화에 따른 임계지속기간과 도달시간의 상관관계 분석)

  • Lee, Sung Ho;Kim, Jung Soo;Lee, Jae Joon
    • Proceedings of the Korea Water Resources Association Conference
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    • 2019.05a
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    • pp.204-204
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    • 2019
  • 국지성 호우의 증가로 인해 도시 지역의 내수침수피해가 빈번하게 발생하고 있다. 특히 배수의 흐름이 집중되는 저지대 지역과 노후화된 하수관거가 설치된 지역에서 특히 피해가 집중되고 있으며, 이는 도로 측면에 설치된 빗물받이와 같은 하수시설에서 원활하게 배수가 되지 않기 때문에 강우 발생시 도로표면에 노면수가 정체되어 피해가 발생하고 있다. 과거 도로 노면의 형상과 강우의 임계 지속시간을 고려한 적정 우수 유출량 산정에 관한 연구가 진행된 바 있으나, 현재 발생하는 국지성 호우의 형태나 강우강도의 변화에 따른 유출량의 변화가 발생하였으며, 도달시간 산정식에 따른 매개변수의 차이와 새로운 도달시간 산정식의 개발로 도달시간의 결과가 크게 차이가 날 수 있다. 따라서 도로의 침수피해를 막고 교통 안정을 유지하기 위해서는 도로 조건을 고려한 도로 입구 및 하수관의 적절한 설계 등 다양한 연구가 주기적으로 이루어져야 한다. 본 연구에서는 강우 유출 모델인 SWMM 모형과 계산식을 이용하여 도로 표면의 폭과 길이, 도로 종횡단의 변화량, 재 산정한 강우강도에 따른 유출량을 계산하였다. 도로 표면의 폭과 길이, 경사를 다양하게 입력하였으며, 또한 각 Case에 따라 최대 유출량을 생성하는 임계지속기간을 결정하고 다양한 도달시간 산정식의 결과와 비교하여 상관관계를 분석하였다. 분석결과 도달시간은 산정식의 매개변수에 따라 차이가 발생하였으며, 도로표면의 길이와 횡단경사에 크게 영향을 받는 것으로 분석되었으며, 횡단경사보다 종단경사가 클 경우 도달시간이 길어져 유량의 집중을 막는 효과가 있는 것으로 나타났다.

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Study on Response of River Geomorphology due to Human-Induced Disturbance (인위적 교란에 의한 하도지형의 응답에 관한 연구)

  • Kim, Ki-Heung;Jung, Hea-Reyn
    • Proceedings of the Korea Water Resources Association Conference
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    • 2010.05a
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    • pp.1011-1015
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    • 2010
  • 하천의 이용과 관리적 측면에서 가장 빈번하게 발생하는 하도의 직선화, 홍수량의 변화, 하상굴착, 하폭의 확대 축소 및 횡단구조물 등은 중규모 스케일의 하천지형을 인위적으로 교란시키는 대표적인 사례이다. 따라서, 이러한 인위적 교란은 하천생태계의 기반인 하천의 물리적 구조를 크게 변화시키므로 하도지형의 응답방향을 규명할 필요가 있다. 하천 유역의 지형은 여러 가지 스케일의 지형단위가 조직화되어 있는 것이므로 대(大) 중(中) 소(小)의 3가지 스케일 지형단위로서 계(系, system)를 계층화하고, 작은 계층의 계(系)에서는 큰 계층의 계(系)를 고정적인 경계조건으로 하여, 그 내부의 여러 가지 특징이나 변화를 규정하는 주요 인자를 이용하여 분석해야 한다. 또한 대(大) 스케일은 유역스케일의 지형스케일이며, 하도의 수계망이나 하도종단형 형상 등이다. 중(中) 스케일은 segment에서 reach 스케일의 지형이며 사행형상, 하천 폭 등이다. 소(小)스케일은 수심의 10배 정도이하의 지형스케일이며, 소규모 하상파 등의 미지형(微地形)이다. 따라서, 본 연구에서는 남강과 황강을 대상하천으로 유량 조절과 유사공급이 차단되는 댐하류 및 골재채취와 같은 인위적 교란요인에 의한 중규모(segment scale) 하도지형의 변화와 응답방향을 조사, 분석하였다. 연구결과 유량 및 유사공급량의 변동의 크기에 따라 전체적인 하상저하와 더불어 사주와 소가 소멸되면서 여울과 소가 사라지는 현상이 동조하는 것으로 분석되었으며, 하상의 평탄화에 의하여 저수로의 폭이 넓어져 복열사주가 발달하면서 수심 및 유속의 다양성이 감소되는 것으로 분석되었다.

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Investigation Study on Underground Cavity Scale Estimation Based on GPR Exploration (지하공동 규모 평가를 위한 GPR 탐사 기반의 조사 연구)

  • Byoung-Jo Yoon;Han-Joo Lim;Yeon-Gyu Kim
    • Journal of the Society of Disaster Information
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    • v.19 no.3
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    • pp.737-746
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    • 2023
  • Purpose: Ground subsidence due to cavity can bring about various problems, such as casualties, decrease of the safety of the structures, and indirect social costs. Therefore, ground subsidence should be prevented through the exploration and recovery of the cavity under the pavements. Method: In this study, GPR exploration method was carried out on both actual roadway and mock-up site to compensate for the problems caused by excavation and restoration process. Result: This study compared the cavity scales obtained from GPR exploration results and the direct excavation of the identified cavity. It was confirmed that the predicted soil depth by GPR exploration was similar to the identified soil depth, but the predicted cavity scale by GPR exploration overestimated the longitudinal and cross-sectional widths compared to the identified cavity scale. Conclusion: Based on the correlation between the predicted cavity scales by GPR exploration, it is possible to qualitatively estimate the cavity scales using the empirical formula proposed in this study.

Analysis of Landslides Characteristics in Korean National Parks (우리나라 국립공원지역의 산사태 발생특성 분석)

  • Ma, Ho-Seop;Jeong, Won-Ok
    • Journal of Korean Society of Forest Science
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    • v.96 no.6
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    • pp.611-619
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    • 2007
  • This study was carried out to analyze the landslide characteristics and forest environment factors on the landslide area of 7 national parks in korea. The results obtained from this study were summarized as follows; The total number of landslide occurrence was 44 areas. The average length of the landslides scar was 152 m, average width was 17 m. And the average area was $2,818m^2$. The factors influencing landslides were highly occurred in Metamorphic rock, mixed forest type. And also, $30{\sim}35^{\circ}$ in slope gradient, NE in slope aspect, slope higher than 1,000 m, concave (凹) type in vertical and cross slope, 0 ordered stream. The main factors affecting landslide area in stepwise regression analysis were sheet type in landslided shape, NE in slope aspect, 2 ordered stream, SE in slope aspect, slope gradient and complex slope in cross slope type in order of regression coefficient.

Development of an Automatic Transverse and Longitudinal Road Profile Measurement System (노면 종.횡단 요철 자동 측정 시스템 개발)

  • Eom, Jung-Hyun;Seo, Dong-Sun;Huh, Woong;Roo, Myong-Chan;Kim, Joon-Bum
    • Journal of IKEEE
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    • v.5 no.1 s.8
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    • pp.75-84
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    • 2001
  • The reliable data relating to the condition of road surface is of increasing importance to deliver the road condition to driver and road management authority. This paper describes the development of a new high-speed. automatic, road data collection system, which collects the longitudinal road data with ${\sim}30cm$ interval covering full width of the road at 100km/h speed. The system calculates the international roughness index (IRI) from the collected data and displays the IRI and road profile data on the screen. To develope the system, we implement an optical range finder, advanced distance and motion detectors, and signal processing and display modules. The measurement accuracy of the system at 70km/h operation speed shows ${\pm}0.1m/km$ in the IRI for the standard road. To confirm the performance of the developed system, we also measure the IRI of a deployed highway road and compare the results with a conventional system and human eye measurement results.

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Analysis of Landslide Characteristics in Jeonlabuk-do, Korea (전라북도 지역의 산사태발생 특성분석)

  • Park, Chong-Min;Ma, Ho-Seop;Kang, Won-Seok;Oh, Kyeong-Won;Park, Seong-Hak;Lee, Sung-Jae
    • Journal of agriculture & life science
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    • v.44 no.4
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    • pp.9-20
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    • 2010
  • This study was carried out to analyze the landslide characteristics and forest environment factors on the landslide area of Jeonlabuk-do province in korea. The results obtained from this study were summarized as follows; The total number of landslide occurrence was 182 areas. The average area of landslide scar was $1,859m^2$, average length of the landslides was 139m, average width was 13m. The landslides were highly occurred in igneous rock and coniferous. And also, slope gradient was $21{\sim}30^{\circ}$, aspect was NE, altitude was 401~500m, vertical and cross slope was concave (凹),stream order was 1 order, soil depth was 15m below, landslide type was linear, forest type was artificial. The relationship between landslide area and environmental factors was a positive correlation with cross slope (convex), position (upper), altitude (501m), forest type (coniferous), parent rock (sedimentary rock), D.B.H. (over 17cm), but was negative correlation with slope gradient ($31{\sim}40^{\circ}$), parent rock (igneous rock), D.B.H. (6~16cm).

Improvement of Small Wetland and Stream in Cultivated Area in point of Landscape Ecology (경작지 내 소규모 습지 및 소하천의 경관생태적 개선방안)

  • Cho, Hyun-Ju;Ra, Jung-Hwa;Kim, Jin-Hyo
    • Current Research on Agriculture and Life Sciences
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    • v.29
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    • pp.11-19
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    • 2011
  • This research gives weight to establish practical improvement based on analysis of the landscape ecological character and value to realize the importance of small wetland and stream in cultivated areas functioning as a residual landscape element in rural landscape and to deal with ecological depression effectively. The results of summary are as follows. 1) The results of landscape ecological character analysis of wetlands biotop in total of 7 sites, for example, size of surface in site 5 was widely formed about $10,600m^2$, which was assessed satisfactory in terms of slope of waterfront, width of hedgerow, vegetation condition of composition and so on. Also, The number of flexibility showed 2 in site 8-1, the highest, and morphological diversity showed 1.47, the highest. 2) The results of problem analysis of wetland biotop, most of wetlands are analyzed that the width of hedgerow was below 1m. Also, the 4 wetlands in site 8 are appeared that hard to live slope vegetation in there because of slope of waterfronts are above $45^{\circ}$. 3) The results of landscape ecological character analysis of stream in total of 6 sites, for example, width of waterfront in site 4 showed 55m, the widest, and investigated consist of natural ingredients such as soil, rock, gravel. However, width of waterfront in site 2-2 showed 4m, the narrowest, and inclined angle of slope was formed a right angle. 4) The results of problem analysis of stream, width of waterfront hedgerow in site 2-1 showed about 5m, which was very narrower than width of waterfront, and toxic chemicals discharged from near cultivated area without any filtering. Also, all areas of site 2-2 was formed concrete, and was assessed dissatisfactory in terms of capacity of nature purification, flood control, habitat living space because of straight stream. 5) Based on the result above landscape ecological character and problem analysis, main improvement guidelines are set in terms of shape, vegetation, topography in case of wetlands, and which are set in terms of vertical, horizontal structure in case of stream.

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A Review of Current Status and Placeness on the Yusang-Goksu Ruins in Hwanggak-dong, Geumma, Iksan (익산 금마 황각동 유상곡수 유적 일대의 현황과 장소성에 대한 일고찰)

  • Rho, Jae-Hyun;Han, Min-Soon;Seo, Youn-Mi;Park, Yool-Jin
    • Journal of the Korean Institute of Traditional Landscape Architecture
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    • v.40 no.3
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    • pp.20-35
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    • 2022
  • This study was conducted on the locational results of the 'Yusanggoksu(流觴曲水)' petroglyphs located in Hwanggak-dong(黃閣洞), Shinsong-ri, Geumma-myeon, Iksan-si through literature study, analysis of old maps and aerial photos, field observations, drone photography, elevation surveys, and interviews with residents. It was attempted for the purpose of illuminating and preserving the relics of the domestic Yusanggoksu garden by clarifying the spatiality of this place by tracing the spatiality and examining the possibility of enjoying the Yusanggoksu water system in this place. The conclusion of this study is as follows. The area around Hwanggak-dong, where the Yusanggoksu remains, has been selected as the most beautiful scenic spot in Iksan in various documents. The origin of 'Hwanggak' is considered to be closely related to the nickname of Uijeongbu(議政府). In other words, he paid attention to the relationship with Yanggok, So Se-yang(蘇世讓), who served as Chan-seong Jwa(左贊成). In particular, he paid attention to the relationship with his birthplace, Taeheojeong, a separate book, and Toehyudang, a retreat hall), tombs, and posthumous Confucian academies were distributed in the vicinity. Haseo-dae(荷鋤臺), a wide rock on which a hoe is hung on a rock after field work, seems to express a leisurely rural life and a simple and hermit life, based on the examples of Chinese and Korean poetry. The dark blood on the upper part of the Seobwi Rock with the inscription 'Yusanggoksu', which is the core of this site, is identified as a chailgong(遮日孔) to support the water system, and Ilgan-pavilion and Mojeong(茅亭) nearby are to support the yusanggoksu. It seems to have performed a spatial function for The inscription 'Hwanggak-dong' engraved on the front of Deungzanbawi is the gateway to Hwanggakdongcheon(黃閣洞天) and identified the idealized world existing in the village. Judging from the documentary records of the Iksan-gun 『Chongswaelog(叢瑣錄)』, the rock letters 'Hwanggak-dong' and 'Haseodae' were engraved on March 29, 1901, the 5th year of Gwangmu, the 5th year of the Korean Empire, by Iksan-gun Governor Oh Haeng-mook(吳宖默) and his acquaintance Seokseong Kim In-gil(金寅吉) Confirmed. Also, considering the tense of Lee Bong-gu's 「Hwanggakdongun(黃閣洞韻)」 and So Jin-deok, a descendant of Yanggok, 「Hwanggakdongsihoe(黃閣洞詩會)」, it is presumed that it was related to Goksuyeon(曲水宴) in Hwanggak-dong. It can be inferred that the current affairs meetings were held at least until the early days of Japanese colonial rule. Meanwhile, the maximum width of the current curved waterway was calculated as 11.3m and the transverse slope was 15.0%. If so, it is estimated that the width and extension distance of the curved waterway would have been much longer. Judging from the use of mochun(暮春), drinking and poetry, the tense 'Hwanggakdongsihoe' related to the Yusanggoksu relics in Hwanggak-dong, and the existence of a pavilion presumed to be Yusangjeong(流觴亭) called Ilgan-pavilion in the nearby Yusanggoksu site It is confirmed that it was a space where Yusanggoksuyeon(流觴曲水宴) spread at least until the end of the Joseon Dynasty. Unfortunately, it remains a limitation of the study that it cannot be confirmed due to lack of data on the rock characters of 'Yusanggoksu' and those who enjoyed it before the end of the Joseon Dynasty. This is an area that needs to be elucidated through continuous efforts to find data on this issue in the future.