• Title/Summary/Keyword: 유구천

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The feasibility analysis of restoring the ecological integrity of the Namyang and Yugu streams (생태하천 복원사업의 경제적 편익 분석 - 남양천 및 유구천을 중심으로 -)

  • Lim, Seul-Ye;Yoo, Seung-Hoon
    • Journal of the Korean Regional Science Association
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    • v.31 no.4
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    • pp.25-45
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    • 2015
  • The government has implemented the projects of restoring the ecological integrity of streams to improve its water quality and provide resting places with local residents. Because the projects require huge public investments, their economic feasibility should be investigated through ex-post examination of their benefits. This study attempts to analyze the economic feasibility of restoring the ecological integrity using specific cases of Namyang stream in Hwaseong, Gyeonggi and Yugu stream in Gongju, Chungnam. The contingent valuation (CV) method is employed to measure the benefits. To this end, a professional polling firm conducted two CV surveys of 210 and 209 households for Hwaseong and Gongju, respectively. The willingness to pay (WTP) model used in the study is based on utility difference approach and the single-bounded dichotomous choice spike model. The results reveal that the WTP for restoring ecological integrity of the Namyang and Yugu streams are estimated to be 3,140 and 10,121 won per household per year. Interestingly, the latter is about three times greater than the former. The quantitative information can be used in economic feasibility analysis of the projects of restoring the ecological integrity of the Namyang and Yugu streams.

The Analysis of the Plant Distributional Pattern in Yugu Stream (Gongju, Chungnam) (유구천(충남, 공주)의 식물 분포 현황분석)

  • Moon, Ae-Ra;Lee, Youl-Kyong;Park, Jeong-Mi;Jang, Chang-Gee
    • Korean Journal of Environmental Biology
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    • v.30 no.2
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    • pp.107-120
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    • 2012
  • This study was carried out to illiminate the diversity of vascular plants by making list of rheophyte and hydorphyte plants at Yugu stream. This study was conducted from Aug., 2009 to Sept. 2010 at 7 points. Based on the voucher specimens, vascular plants from investigated areas were 88 families 229 genera 290 species 3 subspecies 30 varieties 5 forms, totally 328 taxa. Korean endemic plants were 3 species such as Forsythia koreana (Rehder) Nakai (planted) and Paulownia coreana Uyeki (planted), and Weigela subsessilis (Nakai) L.H. Bailey. The rare and endangered plants were designated by Korea Forest Service were 4 taxa, such as Penthorum chinense Pursh, Acorus calamus L., Lilium callosum Siebold & Zucc. and Iris ensata var. spontanea (Makino) Nakai. Floristic special plants were totally 26 taxa, which were grade V of 2 taxa, grade IV of 2 taxa and grade III of 9 taxa. Naturalized plants were 27 taxa, that was 8.3% of whole discovered vascular plants in this area. Even naturalized plants has not influence on the vegetation of Yugu stream. Since village was composed along the stream and the roads and banks were linked, naturalized plants were flowed continuously into this region. So, strategy of the conservation for this region should be designed. Based on flora, 3 types of group were discriminated such as main stream type (4 points), branch stream type (2 points) and reservior type (1 point). Each group has difference in composition of plants.

Ecological Health Assessments of Yoogu Stream Using a Fish Community Metric Model (어류의 군집 메트릭 모델을 이용한 유구천의 생태 건강도 평가)

  • Lee, Eui-Haeng;An, Kwang-Guk
    • Korean Journal of Ecology and Environment
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    • v.39 no.3 s.117
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    • pp.310-319
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    • 2006
  • The objective of study was to evaluate ecological health from seven sampling locations of Yoogu Stream, one of the tributaries of Guem River, July and September 2005. The research approach was based on the Index of Biological Integrity (IBI) using fish assemblage and Qualitative Habitat Evaluation Index (QHEI) using fish assemblage. The models of IBI and QHEI were modified as 10 metric model and 11 metric model, respectively, for the regional applications. In Yoogu Stream, value of IBI were averaged 29.5 (n=7) which is judged as a 'fair condition'. The IBI model scores, at the site 3 and 7, were estimated as 23 and 24, indicating a 'poor${\sim}$fair condition' while, site 5 was estimated as 28, 'fair condition'. The remaining sites were between 31 and 34, indicating 'fair${\sim}$good condition'. According to the analysis of QHEI, the average was estimated as 136, 'fair${\sim}$good condition'. Spatial variation the QHEI were evident; site 1 and site 4 were 186 and 120 respectively, indicating an 'excellent and fair${\sim}$good conditions'. Site 3 was 69, fair condition while the other sites were 128${\sim}$156, good condition.

A study on the relations between river bed and biological health (하상 변화와 수생태계 건강성과의 관계 분석)

  • Choi, Mikyoung;Felix, Micah Lourdes;Zhang, Ning;Jung, Kwansue
    • Proceedings of the Korea Water Resources Association Conference
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    • 2021.06a
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    • pp.456-456
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    • 2021
  • 하상 변화는 유량이나 유사의 흐름에 따라 침식, 운반, 퇴적되어 변화하며, 하상변동에 의한 결과는 하천의 형태 (직렬,복렬, 곡렬 등)나 서식처의 구조 (여울과 소, 웅덩이, 습지 등) 형성 로 나타난다. 이어서 서식처 구조의 다양성은 생물다양성에 긍정적인 영향을 미친다. 본 연구에서는 수리 (유량이나 유사량)-지형(서식처 구조)-생태 (생물다양성)을 연계하여 관리하기 위한 생태적인 하천관리 프레임을 제시하기 위하여, 지형과 생물상의 관계를 우선 파악하고자 한다. 국내 하천은 수생태 건강성 평가 중 서식 및 수변환경 지수(HRI, Habitat and Riparian Index)를 활용하여 하천의 형상 및 자연성을 평가한다. 해당 지수는 하천의 자연성을 판단할 수 있으나 유량이나 유사량 등과 같이 수리적 조건과 연계하여 하천환경 변화를 예측하기 어렵기 때문에, 본 연구에서는 하천의 자연성을 판단하는 지형변수들을 제안하고, 생물상과 상관관계를 분석한다. 수질 변화가 급격하지 않는(년간 변화폭이 일정한) 금강 유역의 지천 (갑천, 미호천, 논산천, 유구천 등) 중 생태계 건강성 평가 지수가 산정되어 있는 지점을 기준으로 상·하류 약 5 km 구간들을 대상으로 한다. 지형 변수로는 (항공사진을 이용한)사주 비율(사주면적/제방 내 홍수터 면적), 사주 식생비율(식생면적/사주면적)과 사주 변동량(연간 사주 이동량), 서식처 구조의 다양성(여울, 소, 웅덩이 등), 기존의 서식 및 수변환경 지수 등을 활용하고, 생물 변수로는 저서동물지수(BMI, Benthic Macroinvertebrate Index), 저서동물의 우점도, 어류생물지수(FAI, Fish Assessment Index), 어류생물지수에 활용하는 국내종의 총 종수, 여울성 저서종수, 민감종수 등을 활용한다.

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Examination of Modified Larinier pass Fishway in Korea (수정 라리니에식 어도의 국내 적용성 검토)

  • Kim, Sun-Joo;An, Min-Woo;Choi, Young-Kyoung;Kyoung, Min-Su
    • Proceedings of the Korea Water Resources Association Conference
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    • 2006.05a
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    • pp.452-456
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    • 2006
  • 본 연구는 수정 라리니에식 어도를 조립식으로 개발하여 실제 현장에 적용하기에 앞서 수리모형을 통해 어도 경사와 어도내 조류제 형태(평면형, 경사형, 역경사형)를 3가지로 달리하여 각 형태별 유속을 조사하고 실제 우리 나라 토착 민물고기인 갈겨니, 쉬리, 피라미, 금강모치의 소상능력을 시험하였다. 또한 실제 크기의 목재로 만든 조립식 수정 라리니에식 어도를 제작하여 충청남도 공주시 유구천의 농업용 보에 적용하였으며, 2005년 6월부터 10월까지 모니터링을 하여 수정 라리니에식 어도의 국내 하천 적용성에 대해서 검토하였다. 모형실험결과 수심은 6cm(현장 30cm)일때, 조류재의 형태는 평면형과 경사형, 경사는 1/20, 유속은 0.3-0.4m/s에서 어류가 원활하게 소상하는 것으로 나타났고, 어도내 마련된 휴식부에서는 실제 물고기들의 휴식하는 모습이 관찰되었다. 또한 휴식부의 잠공은 하천 유량 조건이 좋을 때보다 갈수기나 홍수기에 어류가 소상하는 통로의 역할뿐만아니라 저서 생물의 이동통로 역할을 할 수 있을 것으로 생각된다. 따라서 본 어도는 조류재의 형태에 따른 다양한 유속대를 제공하여 다양한 어종이 이용할 수 있을 것으로 판단되며, 조립식으로 되어 시공 및 유지관리가 용이하여 우리나라 하천 상황에 적절한 어도로 판단된다.

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Origin, Age and Sedimentation Rate of Mid-Geum River Sediments (금강 중류 하상 퇴적층의 기원과 형성시기 및 퇴적율)

  • Oh, Keun-Chang;Kim, Ju-Yong;Yang, Dong-Yoon;Hong, Sei-Sun;Lee, Jin-Young;Lim, Jae-Soo
    • Economic and Environmental Geology
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    • v.43 no.4
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    • pp.333-341
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    • 2010
  • Fluvial sediments are widely distributed in present and old river-beds of the mid-Keum River, the tributaries of which are the Yugu and Jeongan Rivers. The basement of the mid-Keum River area consists of Mesozoic granites which are easily eroded compared to Precambrian gneisses, which are exposed in the upper-Keum River area. The provenance of the fluvial sediments includes both the Precambrian gneisses and Mesozoic granites, which occur in the catchment of the mid-Keum River. The coarse-grained sediments were probably transported from the river-beds and the overbank floodings of the main Keum River and its tributaries when the climate was warm and wet. The oldest mud deposits were dated at ca. 9,400 yr BP by the radiocarbon method. It has been estimated that the sand deposits below the dated muds were formed in a period from the Late Pleistocene to the Early Holocene. However we have revealed that the major part of the present river-bed sediments was formed at ca. 3,000-6,000 yr BP, i.e., in the mid- to late Holocene, when summer monsoon was very strong due to climatic changes. We have calculated fluvial sedimentation rates of 0.12-0.16 cm/yr and 0.02-0.09 cm/yr for borehole KJ-29 river-bed sediments and borehole KJ-28 floodplain deposits, respectively. We conclude that the sedimentation rate is higher near the present stream channel than near the floodplain.