• Title/Summary/Keyword: Dong-Jin river

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Post LGM Fluvial Environment and Palynological Changes of South Korea

  • Kim, Ju-Yong;Yang, Dong-Yoon;Bong, Pil-Yoon;Nahm, Wook-Hyun;Lee, Heon-Jong;Lee, Yung-Jo;Hong, Sei-Sun;Lee, Jin-Young;Kim, Jin-Wkan;Oh, Keun-Chang
    • The Korean Journal of Quaternary Research
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    • v.17 no.2
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    • pp.17-23
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    • 2003
  • In Korea terrestrial fluvial sequences can be used as pedological and sedimentological markers indicating a millenium-scale environmental and climatic changes imprinted in fluvial sub-environments, which in turn are represented by the cyclicity of fluvial sands, backswamp organic muds, and flooding muds intercalations of frostcracked or dessicated brown paleosols. Post LGM and Holocene fluvial and alluvial sedimentary sequences of Korea are formed in such landscapes of coastal, floodplain, backswamp and hillslope areas. Among them, the most outstanding depositional sequences are fluvial gravels, sands and organic mud deposits in coastal, fluvial, or alluvial wetlands. The aim of this study is to explain the sedimentary sequences and palynofloral zones since the last 15,000years, on the basis of organic muds layers intercalated in fluvial sand deposits. Jangheung-ri site of Nam river, Soro-ri site of Miho river, Youngsan rivermouth site in Muan, Oksan-ri site of Hampyeong and Sanggap-ri site of Gochang are illustrated to interpret their sedimentary facies, radiocarbon datings, and palynofloral zonation. Up to the Middle to Late Last Glacial(up to 30-35Ka), old river-bed, flooding, and backswamp sequences contain such arboreal pollens as Pinus, Abies, and Picea, and rich in non-arboreal pollens like Cyperaceae, Gramineae, Ranunculaceae, and Compositae. During the LGM and post-LGM periods until Younger Dryas, vegetation has changes from the sub-alpine conifer forest(up to about 17-11Ka), through the conifer and broad-leaved deciduous forest, or mixed forest (formed during 16,680-13,010yrB.P), to the deciduous and broad-leaved forest (older than 9,500yrB.P). In the Earliest Holocene flooding deposits, fragments of plant roots are abundant and subjected to intensive pedogenic processes. During Holocene, three arboreal pollen zones are identified in the ascending order of strata; Pinus-Colyus zone(mixed conifer and deciduous broad-leaved forest, about up to 10Ka), Alnus-Quercus forest (the cool temperate deciduous broad-leaved forest, about 10Ka-2Ka), and Pinus forest (the conifer forest, about after 2Ka), as examplified in Soro-ri site of Cheonwon county. The palynological zonations of Soro-ri, Oksan-ri, Sanggap-ri, Youngsan estuary, and Gimhae fluvial plain have been recognized as a provisional correlation tool, and zonations based on fluvial backswamp and flooding deposits shows a similar result with those of previous researchers.

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Water Quality Modelling of Flood Control Dam by HSPF and EFDC (HSPF-EFDC 모델을 연계한 홍수조절댐 수질 변화 예측)

  • Lee, Young-Gi;Hwang, Sang-Chul;Hwang, Hyun-Dong;Na, Jin-Young;Yu, Na-Young;Lee, Han-Jin
    • Journal of Environmental Impact Assessment
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    • v.27 no.3
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    • pp.251-266
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    • 2018
  • This study predicted the effect of operation pattern of flood control dam on water quality. Flood control dam temporarily impound floodwaters and then release them under control to the river below the dam preventing the river ecosystem from the extreme flood. The Hydrological Simulation Program Fortran (HSPF) and the Environmental Fluid Dynamics Code (EFDC) were adapted to predict the water quality before and after the dam construction in the proposed reservoir. The non-point pollutant delivery load from the river basin was estimated using the HSPF, and the EFDC was used to predict the water quality using the provided watershed boundary conditions from the HSPF. As a result of water quality simulation, it is predicted that the water quality will be improved due to the decrease of pollution source due to submergence after dam construction and temporary storage during rainfall. There would be no major water quality issues such as the eutrophication in the reservoir since the dam would impound the floodwater for a short time (2~3 days). In the environmental impact assessment stage of a planned dam, there may be some limitations to the exact simulation because the model can not be sufficiently calibrated. However, if the reliability of the model is improved through the acquisition of actual data in the future, it will be possible to examine the influence of the water environment according to various operating conditions in the environmental impact assessment of the new flood control dam.

A Study on the Correlation between Odorous Compounds, Actinomycetes and Algae in Drinking Water Source of Nakdong River (낙동강 상수원수 중 이취물질과 방선균 및 조류의 상관관계 연구)

  • Kim, Jeong-A;Kim, Gyeong-A;Yun, Churl-Jong;Park, Hong-Gi;Jung, Eun-Young;Cha, Dong-Jin;Choi, Jin-Taek;Son, Hee-Jong
    • Journal of Korean Society of Environmental Engineers
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    • v.35 no.3
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    • pp.213-219
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    • 2013
  • We have investigated the correlation between odorous compounds and actinomycetes in drinking water source of Nakdong River in 2011. Geosmin was mainly detected in the spring and summer seasons (Mar, Aug, and Sep) and 2-MIB was mainly detected in the winter and spring seasons (Feb, Mar and May). The odorous compounds concentrations were highest on March which also overlapped with the peak of actinomycetes, geosmin and 2-MIB were detected highly in the diluted culture solution of isolated actinomycetes strains from Nakdong River. For these reasons we could confirm that odorous compounds on March and August are closely related with actinomycetes. Meanwhile, geosmin increase on September supposed to relate with Microcystis.

Development of Web-based Research Network and Watershed Environment Information System for YeongSan River Basin (웹기반 물관리 연구네트워크 구축에 관한 연구 영산강 웹기반 연구 네트워크 구축 및 유역환경정보시스템 개발)

  • Lee, Kyonge-Eun;Lee, Jong-Chul;Kim, Dong-Ho;Hong, Jung-Jin;Choi, Yu-Jin
    • Proceedings of the Korea Water Resources Association Conference
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    • 2009.05a
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    • pp.1673-1677
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    • 2009
  • 영산강 수계내의 연구기관 및 지자체 등 유관기관에서는 각종 연구사업 및 조사사업이 활발하게 진행되고 있으며, 지속해 매년 많은 예산과 전문 인력이 투입되고 있다. 또한 수행된 사업에서 산출된 연구결과나 조사결과 등의 자료는 영산강 수계내의 유역특성, 수계특성, 하천특성, 호소특성 등을 분석하고 평가하는데 매우 유용한 자료로 활용된다. 이러한 관점에서 유역내의 전문가, 민간단체, 정부기관, 학계 등의 유기적인 교류를 통해 정보의 합리적 관리 및 공유가 필요하며, 서로의 이해관계를 유기적으로 결합하여, 더 나아가 TFT(Task Force Team) 운영 등의 방안도 제시할 수 있는 여건의 필요성이 있다. 따라서 본 연구에서는 영산강 웹기반 연구 네트워크 및 유역환경정보시스템을 통해 영산강 유역내의 물환경 인프라를 확충에 그 목적이 있다. 수계내의 기상, 수문 및 수질관련 자료를 구축하여 제공하며, 수질, 오염원, 생태조사 등의 현장조사에 의한 성과자료의 정보 활용을 위한 시스템을 구축하여, 조사연구사업 지원 및 환경정책결정 기초자료로 활용함으로써 관계기관과 전문가단체 등의 정보 교류의 장으로 활용하고자 한다. 또한 기존의 영산강 수계통합관리시스템의 연계를 통한 측정망자료 및 환경기초시설 현황 등의 자료의 접근을 강화하고자 한다.

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The Present Condition Of Free Water Surface Wetland In Tandong-River And The design Of It's Water Quality Improvement (탄동천의 현황 및 수질개선을 위한 인공습지 설계방안)

  • Yoon, Jin-Ho;Seo, Dong-Il;Seo, Mi-Jin;Lee, Yong-Sung
    • Proceedings of the Korea Water Resources Association Conference
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    • 2008.05a
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    • pp.1957-1961
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    • 2008
  • 대전광역시는 대전시의 3대 하천 살리기 사업 중 하나로 갑천을 2009년까지 수영이 가능한 하천으로 개선하는 '갑천 수질개선 기본계획'을 추진하고 있다. 이러한 계획이 성공적으로 수행되기 위해서는 오염물질을 포함하는 지류의 수질을 개선하는 것이 우선되어야 한다. 대전의 탄동천은 상류에 군부대 시설이 밀집해 있고 하수처리장이 운영되고 있는 관계로 하천 수질은 일반적인 하천에 비하여 높은 오염도를 나태내고 있다. 또한 중류지역의 주거시설에서 하수시스템으로 완벽하게 연결되지 못한 부분에서 오염물질이 유출되는 것으로 추정되며, 연구단지등에서 강우시 유출되는 비점오염물질 등이 하천의 수질에 영향을 미치고 있다. 본 연구에서는 탄동천의 상류 자운동의 자운1교부터 갑천과 합류되기 전의 국립중앙과학관 앞까지의 7.4km 구간의 6개 지점과 하수처리장 방류수, 우수 관거 및 지류인 삼성천 등 6개 점오염원 지점의 총 12개 지점에 대하여 현장조사 및 수질측정 을 진행하였다. 본 연구에서는 하수처리장으로 더 이상 제어하기 어려운 오염물질 농도를 추가로 저감하기 위하여 지표형 인공습지 운영 및 설계방안을 연구하였다. 인공습지를 합리적으로 설계하는 경우 결과 탄동천의 수질을 개선할 수 있을 뿐만 아니라 하천 환경을 개선하고 경관을 개선하는 효과가 있을 것으로 기대되며 도시형 소하천들의 수질 개선에 긍정적인 영향을 미칠 것으로 기대된다.

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A study on the Hydrological Property with Hydraulic Model and Numerical analysis of the Bight River (만곡부 하천의 수리모형과 수치해석을 통한 수리학적 특성 연구)

  • Park, Soo-Jin;Seo, Dong-Il;Lee, Jin-Tae;Choi, Han-Kuyl
    • Proceedings of the Korea Water Resources Association Conference
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    • 2007.05a
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    • pp.1297-1301
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    • 2007
  • 홍수위 산정을 위하여 이용되는 기법은 평균적인 홍수위 산정이 가능한 1차원모형과 하천 좌우의 수심 편차까지 해석이 가능한 2차원 모형 및 수심에 대한 변동까지 해석이 가능한 3차원 모형으로 구분된다. 이중에서 기본계획 수립시 사용되는 모형은 1차원 수치해석 모형으로 하천 단면별로 평균홍수위 만을 산정하므로 만곡부하천의 특성의 영향이 반영되지 않고 있는 실정이다. 따라서 본 연구는 만곡부 하천을 선정하여 총2.4Km구간의 모형을 제작하였으며, 수리모형 실험을 통하여 일차원 및 이차원 수치해석을 실시하여 모형실험값과 비교 고찰하였다. 본 연구를 위하여 일차원 수치해석은 HEC-RAS모형을, 이차원 수치해석에서는 SMS모형을 사용 하였다. 연구결과, 유속의 경우 우안지점의 평균 유속은 모형실험은 8.33m/s, 일차원 및 이차원 수치해석은 각각 3.08m/s, 8.57m/s로 나타남을 확인 하였으며, 평균유속은 이차원 수치해석이 모형실험과 유사한 값을 보였다. 또한 수위경우는 모형실험의 좌안과 우안에 대한 일차원 및 이차원 수치해석의 최대 오차는 각각 0.66m, 0.84m와 0.28m, 0.48m로 수위 또한 이차원 수치해석이 수리모형실험과 유사한 결과를 보였다. 따라서 본 연구를 통하여 알 수 있듯이 만곡부 하천의 경우 일차원 수치해석보다는 2차원수치해석을 실시하여 기본계획을 수립하는 것이 바람직할 것으로 판단된다.

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Numerical Simulation for Dispersion of Anthropogenic Pollutant in Northern Masan Bay using Particle Tracking Model (입자추적모델을 이용한 마산만 북부 해역에서의 육상오염물질 확산 수치모의)

  • KIM, Jin-Ho;JUNG, Woo-Sung;HONG, Sok-Jin;LEE, Won-Chan;CHUNG, Yong-Hyun;KIM, Dong-Myung
    • Journal of Fisheries and Marine Sciences Education
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    • v.28 no.4
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    • pp.1143-1151
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    • 2016
  • To study the dispersion process and residence time of anthropogenic pollutant in Masan bay, a three-dimensional hydrodynamic model coupled to a particle tracking model, EFDC, is applied. Particle tracking model simulated the instantaneous release of particles emulating discharge from river and wastewater treatment plant to show the behaviour of pollutant in terms of water circulation and water exchange. Modelled outcomes for water circulation were in good agreement with tidal elevation and current data. The results of particle tracking model show that over half of particles released from northern Masan bay transport to out of area while the particles from Dukdong wastewater treatment plant transport to northern area. This meant pollution source from inside and outside of the northern area can affect water quality of northern Masan bay.

Hanseong Period of Baekje and Mahan (한성시대(漢城時代)의 백제(百濟)와 마한(馬韓))

  • Choi, Mong-Lyong
    • Korean Journal of Heritage: History & Science
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    • v.36
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    • pp.5-38
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    • 2003
  • The history of Baekje Kingdom, one of the Three kingdoms, is divided into three periods to the change of sociopolitical center, including its capital as follows: Hanseong Period (18 BC ~ AD 475), Ungjin Period (AD 475~538), and Sabi Period (AD 538~660). Though the Hanseong Period of Baekje Kingdom covers more than two thirds of the whole history of Baekje Kingdom (493 years), history and archaeological culture of the Hanseong Period is still unclear and even ambiguous comparing to the Ungjin and Sabi periods. Most of all, it is because of quite limited historical records and archaeological data available. In addition, negative attitude of the Korean academic circles to the early records of Samguksaki(三國史記) has been a critical obstacle to the study of early history of the Three kingdoms, including the Hanseong Period of Baekje kingdom. Author, who has attempted to combine historical records and archaeological data in order to reconstruct the history and archaeological culture of the early Baekje, specifically the Hanseong Period, has held positive attitude to the early records of the Samguksaki as far as possible. He(Author) came to realize that comprehensive understanding of Mahan (馬韓) society, one of the Three Han (三韓) Society was more than essential in the study of Baekje. According to historical records and archaeological data, Mahan Society represented by Mojiguk(目支國) ruled by King Jin(辰王) has been located in the middle and/or southwestern parts of the Korean peninsula from the 3rd~2nd century BC through the end of the 5th century or early 6th century AD. Mahan already occupied central portion of the Korean Peninsula, including the Han River Valley when King Onjo(溫祖王) first set up the capital of Baekje Kingdom at Wiryeseong (慰 禮城) considered to be modern Jungrang~Songpa-gu area of Han River Valley. From the beginning of the Baekje history, there had been quite close interrelationships between Baekje and Mahan, and the interrelationships had lasted for around 500 years. In other words, it is impossible to attempt to understand and study Hanseong period of Baekje, without considering the historical and archaeological identity of Mahan. According to the Samguksaki, Baekje moved its capital three times during the Hanseong Period (18 BC ~ AD 475) within the Han River Valley as follows: Wiryeseong at Jungrang-gu area of the Han River (河北慰禮城, 18 ~ 5 BC), Wiryeseong at Songpa-gu area of the Han River(河南慰禮城, 5 BC ~ AD 371), Hansan at Iseongsan fortress site(Historical site No. 422, 漢山, AD 371~391), and Hanseong at Chungung-dong of Hanam city(漢城, AD 391~475). Before 1990s, archaeological data of the Hanseong Period was quite limited, and archaeological culture of Mahan was not well defined. Only a few burial and fortress sites were reported to be archaeological remains of the early Baekje, and a few settlement and jar burial sites were assumed to be those of Mahan without clear definition of the Mahan Culture. Since 1990s, fortunately, a number of new archaeological sites of Hanseong Baekje and Mahan have been reported and investigated. Thanks to the new discoveries, there has been significant progress in the study of early Baekje and Mahan. In particular, a number of excavations of Pungnap-dong Fortress site(Historical site NO. 11, 1996~2003), considered to be the Wiryeseong at south of the Han River, the second capital of the Hanseong Baekje, provided critical archaeological evidence in the study of Hanseong Period of Baekje. Since the end of the 1990s, a number of sites have been reported in Gyeonggi, Chungcheong, and Jeolla provinces, as well. From these sites, archaeological features and artifacts representing distinctive cultural tradition of Mahan have been identified such as unstamped fortresses, pit houses cut into the rock, houses with lifted floor(掘立柱 건물), and potteries decorated with toothed wheel and bird's footprint designs. These cultural traditions reflected in the archaeological remains played a critical role to define and understand archaeological identity of the Mahan society. Moreover, archaeological data from these new sites reported in the middle and southwestern parts of the Korean Peninsular made it possible to postulate a hypothesis that the history of Mahan could be divided into three periods to the change of its sociopolitical center in relation with the Baekje Kingdom's political Situation as follows: Cheonan (天安) Period, Iksan(益山) Period, and Naju(羅州) Period. The change of Mahan's sociopolitical center is closely related to the sociopolitical expansion of the Hanseong Baekje.

Occurrence of Pesticide Residues in Han River Basin in 2012 and 2014 (2012, 2014년 한강수계 하천수 중 잔류농약 검출 양상)

  • Kim, Chan-Sub;Lee, Hee-Dong;Son, Kyeong-Ae;Lee, Eun-Young;Oh, Jin-A
    • Korean Journal of Environmental Agriculture
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    • v.38 no.4
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    • pp.338-351
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    • 2019
  • BACKGROUND: To investigate distribution and seasonal variation of concentration and flux of pesticides in Han river basin, water samples were examined at 24 sites in 2012 and 2014. METHODS AND RESULTS: Water samples were collected four times per year and subjected to liquid-liquid partition extraction followed by GC-ECD/NPD analysis. Of fifteen pesticides detected, iprobenfos, diazinon, isoprothiolane, endosulfan sulfate and oxadiazon were detected in a higher frequency, while fenoxanil, carbofuran, fenitrothion, butachlor and metolachlor were only detected in a sample. Pesticides with high occurrences, iprobenfos, diazinon, isoprothiolane, endosulfan sulfate and oxadiazon were detected in residue level of 0.01-0.46, 0.01-0.24, 0.03-0.85, 0.02-0.06 and 0.05-0.24 ㎍/L, respectively. Carbofuran and acetanilide herbicides were found at lower frequencies, but their concentrations were one order of magnitude higher than those of the others. CONCLUSION: Discharge of pesticides in downstream area were mainly contributed from rice farming and suburban horticulture, while pesticide occurrences in upstream area, such as Donggang river basin were caused by highland agriculture for cabbage and potato production. Despite the influx of pesticides from tributaries through intensive agriculture areas, pesticide concentration in the main stream water was low due to the dilution effect from the upstream. Therefore, the water quality was considered to be good at the most downstream, the effluent of Paldang dam.

Occurrence of UV Filters in Nakdong River Basin : Mainstreams, Tributaries and STP Effluents (낙동강 수계에서의 자외선 차단제류 검출 특성 : 본류, 지류 및 하수처리장 방류수)

  • Seo, Chang-Dong;Son, Hee-Jong;Choi, Jin-Taek;Yoo, Pyung-Jong;Jang, Seong-Ho
    • Journal of Korean Society of Environmental Engineers
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    • v.37 no.8
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    • pp.472-479
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    • 2015
  • This study was investigated occurrence and distribution patterns of UV filters in Nakdong River basin (mainstream, tributaries and sewage treatment plant (STP) effluents). 5 (EHS, BP-3, 4-MBC, BZC and EHMC) out of 7 UV filters were detected in 5 out of 20 sampling sites (mainstream and tributaries), 7 UV filters were not detected in mainstream samples, and the EHS, BP-3, 4-MBC, BZC and EHMC concentration levels in tributary samples were ND~60.8 ng/L, ND~72.1 ng/L, ND~57.2 ng/L, ND~60.1 ng/L and ND~85.2 ng/L, respectively. 5 (EHS, BP-3, 4-MBC, BZC and EHMC) out of 7 UV filters were detected in effluents of 11 STPs around the Nakdong River basin. The EHS, BP-3, 4-MBC, BZC and EHMC concentration levels in 11 STP effluents were ND~89.3 ng/L, ND~90.8 ng/L, ND~88.1 ng/L, ND~118.5 ng/L and ND~104.4 ng/L, respectively. According to the sampling season, distribution patterns and detected concentrations of 5 UV filters were similar in June and September 2014, but change ranges of distribution patterns and detected concentrations of 5 UV filters were highly variable in April and November 2014.