• Title/Summary/Keyword: Naesung stream

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Weathering Characteristics of Granitic Grus in Naesung Stream Drainage, Yeongju-Bonghwa Basin, Korean Peninsula (내성천 유역분지인 영주-봉화 분지 화강암 구릉대의 풍화 특색)

  • Kim, Youngrae;Kee, Keundo
    • Journal of The Geomorphological Association of Korea
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    • v.21 no.4
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    • pp.97-108
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    • 2014
  • Naesung stream famous for 'sandy river', a tributary to the Nakdong River, flows through Yeongju-Bonghwa Basin, its drainage. If the dismantlement of granitic hills in basin is in final stage, weathering materials from hills into stream are finer materials like silty or sandy loam than coarse sand, because sand as weathering mantles is provided from granitic hills, in general. So the granitic hills in Yeongju-Bonghwa basin is dissecting present. As a results of the CIA analysis(A-CN-K and A-CNK-FM ternary diagram), chemical weathering of granitic grus in Yeongju-Bonghwa basin is too very weak for calcium and sodium to be dissolved and go as far as to be more weak than that of Jeongeup, Nonsan and Namwon, common granitic grus in Korean Peninsula. Therefore, the chemical characteristics of granitic hills in Yeongju-Bonghwa basin show that the alteration of weathering mantles just finished disintegration and is dissected at a standstill. Plenty of sands provided from granitic hills is filling the channel of Naesung stream.

Sediment discharge assessment and stable channel analysis using Model Tree of data mining for Naesung Stream (데이터 마이닝의 Model Tree를 활용한 내성천의 유사량 산정 및 안정하도 평가)

  • Jang, Eun-Kyung;Ji, Un;Ahn, Myeonghui
    • Journal of Korea Water Resources Association
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    • v.51 no.11
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    • pp.999-1009
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    • 2018
  • A Model Tree technique of data mining was applied to derive optimal equations for sediment discharge assessment based on the measured sediment data and then to evaluate stable channel design for Naesung Stream. The sediment discharge formula as a function of channel width, velocity, depth, slope and median grain diameter which was developed by a Model Tree technique with sediment discharge data measured in Korean River had a high goodness-of-fit between measured and calculated results. In case of the sediment discharge formula as a function of channel width, velocity, depth and median grain diameter which was developed by a Model Tree technique with sediment discharge data only measured in Naesung Stream represented the highest goodness-of-fit. Two types of sediment discharge formulas were applied to evaluate stable channel analysis for Yonghyeol Station of Naesung Stream. As a result, bed erosion was expected in the study section compared to the current section. It was also presented that the be slope might be changed to be a milder slope than the current slope to reach equilibrium condition in the long term.

Analysis of Correlation on Physical Characteristics and Bed Materials in Natural Rivers (자연하천에서 하도의 물리적 특성과 하상재료의 상관관계분석)

  • Kim, Ki-Heung
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.13 no.2
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    • pp.95-104
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    • 2010
  • The purpose of this study is to analyze the correlation between physical stream characteristics and bed materials in natural rivers. Accordingly, four natural rivers were selected reference streams, they were Nam river, Sumjin River, Naesung River and Han River. Grain size distributions of bed materials were gravels, cobbles and boulders in Han river and Nam river, were sand, gravels, cobbles and boulders in Sumjin river and were sand in Naesung river. Four reference streams were divided into each two reference reaches (straight and bend) by plan and profile characteristics of naturally meandering stream. Therefore various reference reaches were chosen in the aspect of physical stream characteristics and grain size distributions. The results investigated and analyzed are as follows. The streams that grain sizes distributions of river bed materials were coarse were stable because they had variety of bed slope without sediment deposition, and then the riffles frequency and the physical characteristics were various. Also, velocitydepth regime were various in four kinds, and the response parts for water level change were small, so that channel flow status were stable and excellent condition. On the other hand, sand river that grain sizes distributions of river bed materials were fine had not the variety of parameters as velocity-depth regimes, sediment deposition, channel flow status and riffles frequency, so that the physical stream characteristics were not various.

Channel change of the Naesung Stream during 2012~201 (2012~2016년 기간 내성천의 하도 변화)

  • Lee, Chanjoo;Kim, Donggu;Kim, Ji-Sung
    • Proceedings of the Korea Water Resources Association Conference
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    • 2017.05a
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    • pp.333-333
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    • 2017
  • Recently, long-lasting landscape of the Naesung Stream has been changed due to encroachment of vegetation. To analyze patterns and causes of these changes, Korea Institute of Civil Engineering and Building Technology (KICT) has been carried out long-term monitoring research for the 56.8 km long study reach of the Naeseong Stream. Using the consecutive airborne LiDAR survey data obtained from 2012~2016, changes of channel bed forms such as bars could be detected. For the last four years of monitoring, mid-channel bars has been formed along the straight reaches and the existing bars showed vertical accretion caused by deposition on the vegetated surfaces.

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Development of the Estimation Model on Daily Pollutant Loads for the Nakdong River Basin II. Application of the Model (낙동강 유역에 대한 일별 유달부하량 산정모델개발 II. 모델식의 활용)

  • Yoon, Young-Sam;Yu, Jae-Jeong;Kim, Moon-Soo;Lee, Hae-Jin;Lee, Jun-Bae;Yang, Sang-Yong
    • Journal of Environmental Science International
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    • v.16 no.3
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    • pp.333-345
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    • 2007
  • As analyzed the estimated values of the daily delivery loads from thirteen major side streams such as Naesung-river, Keumho-river, Hwang-river, Nam-river during five years (from 1999 to 2003), the daily BOD inflow into the main stream of Nakdong river in 2003 shows the highest quantity as 31.1 ton and the daily BOD inflows in 1999, 2000, 2001, and 2002 are 26.7 ton, 22.5 ton, 21.0 ton, 25.8 ton, respectively. The daily TN in-flow into the main stream of Nakdong river in 2003 shows also the highest quantity as 64.9 ton and the daily TN inflows in 1999, 2000, 2001, and 2002 are 55.19 ton, 46.27 ton, 39.5 ton, 53.38 ton, respectively. The daily TP inflow into the main stream of Nakdong river in 2003 shows the highest quantity as 2.70 ton likewise and the daily TP inflows in 1999, 2000, 2001, and 2002 are 2.17 ton, 1.87 ton, 1.60 ton, 2.10 ton, respectively The rate of BOD loads from each side main stream into the main stream of Nakdong river shows that the BOD loads of Keumho-river are the highest as the values range from 32.8 % (2002) ${\sim}$ 35.1 % (2003) and the BOD loads of Nam-river, Naesung-river, Hwang-river are high in the order named. The rate of TN loads to the main stream is also similar to the trend of BOD loads. The contribution of the TN loads of Geumho-river to the contamination of the main stream is also the highest having a range from 27.0 % (2002) to 28.8 % (1999) among the main side streams and the TN loads of Naesung-river, Nam-river, and Heachun-river are high in the order named. The rate of TP loads is quite different from the trend of BOD and TN loads. The TP rate of Keumho-river, however, is still the highest as ranging 58.6 % (2002) to 61.7 % (2003) and the river has the biggest portion (over 50%) of the entire pollution to the main stream of Nakdong river.

Flow Resistance Analysis for Lower Naesung Stream Considering Grain and Bedform Roughness (사립조도와 하상형상조도를 고려한 내성천 하류의 흐름저항 분석)

  • Ji, Un;Kim, Ji-Sung;Lee, Chan Joo
    • Journal of Korea Water Resources Association
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    • v.46 no.12
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    • pp.1209-1220
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    • 2013
  • Roughness coefficients calibrated by flow modeling using the 1-dimensional numerical model were analyzed for the downstream section of Naesung Stream in this study. Also, the bedform configuration at the Hyangseok Station was predicted for measured and simulated hydraulic conditions of flows and total flow roughness was estimated with the coefficient of grain roughness. The Manning's n coefficients calibrated by numerical modeling and estimated by considering of grain and bedform roughness were compared and examined. As a result, the Manning's n by numerical modeling was greater than the coefficient range estimated by grain and bedform roughness at the low flow regime due to the other factors such as vegetation, sinuosity, and sand bar. However, the Manning's n by numerical modeling was included in the coefficient range by grain and bedform roughness at the transition and high flow regime over $500m^3/s$ of flow discharge.

Channel-forming discharge calculation and stable channel section evaluation for downstream reach of Yeongju dam in Naesung stream (내성천의 영주댐 하류 구간의 하도형성유량 산정 및 안정하도 단면 평가)

  • Jang, Eun-Kyung;Ahn, Myeonghui;Ji, Un
    • Journal of Korea Water Resources Association
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    • v.51 no.3
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    • pp.183-193
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    • 2018
  • Channel-forming discharge for downstream section of Yeongju dam in Naesung stream was calculated to analyze stable channel geometry. Determined channel-forming discharge was applied to design stable channel slope, depth, and base width at Yonghyeol station. Used data for channel-forming discharge and stable channel analysis were collected in downstream section of Yeongju dam in Naesung stream before the dam construction. Specified recurrence interval discharge, effective discharge, and bankfull discharge were analyzed and compared to decide final channel-forming discharge which was $260m^3/s$ of bankfull discharge. Stable channel analysis and design program was applied to predict stable channel section of width, depth, and slope with various sediment transport equations of Ackers and White, Brownlie, Engelund and Hansen, and Yang's equations. As a result, all equations of sediment transport produced milder slopes compared to current bed slope of 0.00177 and Ackers and White equation presented the most similar flow depth of current section with the design constraint of current channel width.

Determination of Prior Areas for Livestock Excreta Pollution Survey (가축분뇨실태조사를 위한 우선 조사 대상지역 선정 방안 도출)

  • Ryu, Hong-Duck;Park, Bae Kyung;Chung, Eu Gene;Ahn, Ki Hong;Choi, Won-Sik;Kim, Yongseok;Rhew, Doughee
    • Journal of Environmental Science International
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    • v.24 no.8
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    • pp.1085-1099
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    • 2015
  • The purposes of this study were to suggest the methodology to select prior areas in the environmental pollution survey for livestock excreta (EPSLE) as well as to elucidate the validity of the methodology. In this study, the prior areas in the EPSLE were determined by examining the number of compost facilities categorized according to the three levels of size including the basin, the sub-basin and the watershed, respectively, based on the data from "Annual Nation-wide Pollution Sources Survey (2012)". The results suggested that the list of prior basins were Nakdong, Geum, Youngsan and Han river basins in order. Also, it was examined that the prior sub-basins in the four river basins including Nakdong, Geum, Youngsan and Han rivers were Naesung Stream, Geumgang Gongju, Juam Dam and Namhan Downstream, respectively. The prior watersheds in the sub-basins of Naesung stream, Geumgang Gongju, Juam Dam and Namhan Downstream were Seocheon Downstream, Geum Stream, Gyeombaek Suwipyo and Yanghwa Stream, respectively. The validity of the methodology used in this study was elucidated by analyzing the correlation of the number of compost facilities with the concentrations of T-N and T-P observed in the end-points of sub-basins. The results of correlation analysis showed that the concentrations of T-N and T-P increased with the number of compost facilities. Specifically, there was the stronger correlation between the number of compost facilities and the concentrations of T-N than that for T-P. Consequently, it was proved that the methodology used in this work was valid and rational for the selection of prior areas in environmental pollution survey for EPSLE.

Numerical Analysis for Bed Changes at the Meandering Stream due to a Short Term Flood Event (단기 홍수사상으로 인한 사행하천의 하상변동 수치모의 분석)

  • Ji, Un;Jang, Eun Kyung;Lee, Chan Joo
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.35 no.6
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    • pp.1229-1236
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    • 2015
  • In this study, flow characteristics and bed changes during a short term flood event were analyzed using the two-dimensional CCHE2D model for a meandering sand-bed river, the Naesung Stream. Flow and bed change simulation was carried along the three sub-reaches with sinuosity of 1.2, 1.6 and 2.2 for the 6-day flood event occurring in June 2011. The simulation results indicated that velocity variation due to flow concentration was larger along the sub-reach with the sinuosity less than 1.5 and bed erosion at the outside of the bend was increased by time. In the sub-reach with the sinuosity less than 1.5, the maximum flood discharge produced the maximum flow velocity over 1.6 m/s to 2 m/s locally.