• Korean Journal of Environment and Ecology
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• v.30 no.4
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• pp.745-750
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• 2016

Morphological characteristics and population characteristics of the Rhynchocypris kumgangensis were investigated at Taehwa River from April 2014 to April 2015. This is the first record on R. kumgangensis not only from Guksu stream (the upstream region of Taehwa River, Ulsan-si Ulchu-gun Beomseo-eup Kuksu-ri) but also from the stream flowing into the Gangneungnamdae stream, in the southern part of East Sea, Korea. The morphometric characteristics of R. kumgangensis in the Taehwa River and the Han River are very similar except that the population at Taehwa River showed shorter caudal peduncle length than caudal peduncle depth when compared with the population at Han River. In terms of meristic character the population at Taehwa River showed fewer numbers of scales at the lateral line, above the lateral line and below the lateral line. Other than that, the two populations showed the same meristic characters. The fish cohabiting with R. kumgangensis mainly composed of Zacco platypus (25.2%), Rhynchocypris oxycephalus (24.1%) and Zacco koreanus (21.8%). Length frequency distribution analysis indicated that the length of the group ranged between 45~65 mm and the average length was 54.3 mm. Calculation of the length-weight relation of R. kumgangensis showed the value of constant a as 0.000002 and b as 3.34, and the Condition factor (K) was 1.10 an on average.

• Journal of The Geomorphological Association of Korea
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• v.23 no.2
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• pp.1-13
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• 2016

This study analyzed pollen compositions in archaeological site on alluvial plain of Taehwa River, Taehwa-dong, Ulsan-si vegetational and environmental change during 6,200~3,000 yr BP. The results consist upward of Pollen Zone I (Inner Bay environment), Pollen Zone II (Quercus-Alnus stage) and Pollen Zone III (Alnus stage). The pollen grains of Fagopyrum and reddish gray silty horizon including artifacts of the Bronze Age suggest that there was cultivation on dry-field around the study site, although it is not sure that there was paddy-field cultivation.

• Water for future
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• v.39 no.8 s.157
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• pp.90-101
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• 2006

• Water for future
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• v.41 no.12
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• pp.48-57
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• 2008

• Journal of Wetlands Research
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• v.13 no.2
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• pp.363-375
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• 2011

Recently, Water quiality of urban river largely have gotten better by virtue of sewer pipe laying and sewage treatment plants construction. or the various contaminants which is flowed in into river have generated underwater ecosystem disturbance and red tide by lack of sewage and waste water disposal facilities. With tidal river, taehwa river of ulsan metropolitan city has large river width and gradual stream bed gradient at the dry and storage period. Moreover, the flow is paralyzed due to the bridge pier protection work, consist of the mat foundation which is about 1.2km from two bridge and the contaminant is accumulated. it is caused by of the red tide generated from the several years or it activates. In this study, When flow area is largest by changing independent footing of bridge pier of two bridges and using RMA2 model, we hydraulically analyzed a variable breadth of velocity and discharge. Consequently, flow rate increased the maximum 103%, discharge was exposed to increase the maximum 61%. Directly this cannot extinguish the red tide but suppresses the red tide occurrence or can reduce. And it is determined to prevent the depositioning of the contaminant and can control fundamentally the red tide occurrence cause.

• Journal of Korea Water Resources Association
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• v.47 no.1
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• pp.1-10
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• 2014

This study aimed to analyze water cycle at Taehwa river, Dongcheon, Hoiya river and Cheongryang cheon in Ulsan city using CAT model developed by Korea Institute of construction technology. To apply CAT model, we separated Teahwa river into 25, Dongcheon into 11, Hoiya river into 17 and Cheongryangcheon into 5 subbasins and discriminated between contribution runoff basins and source basins. The results of water cycle analysis performed using rainfall datas measured from 1975 and 2008 and hydrologic datas of change of land use etc. were that surface runoff increase and interflow decrease, caused by the increase of impervious area. The increases of surface runoff at the basin of Taehwa river and Dongcheon which is a tributary of Taehwa river were small and similar to each other respectively as 1.7% and 2.4%, and increased high rate of 3.2% and 7.7% in Hoiya river and Cheongryangcheon including subbasins which are having high rate of urbanization.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.390-390
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• 2020

자연재해 중 홍수의 경우 단기간에 발생하며, 큰 인명 및 금전적 피해를 가져오는 재해이다. 1970년~2017년 국내 홍수 피해 분석결과 사상자(총 8,152명)는 점차 줄어드는 추세를 보이지만, 반대로 피해액(총 17조5,000억원)은 증가하는 것으로 나타났다(wamis, 국가수자원관리종합정보시스템). 이러한 국내 홍수 피해를 최소화하기 위해서는 각 유역 또는 지역별 특성을 고려한 홍수 취약성 평가가 필요하다. 홍수 취약성은 대상 지역의 기상, 지형, 인문학적 상황에 따라 상이하게 나타나며, 홍수 취약성을 평가하는 인자의 선정 또한 매우 중요하다. 따라서 본 연구에서는 홍수 피해 자료와 홍수 인자간의 인과관계를 분석하여 홍수 취약성 지표 선정 및 취약성 평가를 실시하였다. 홍수 취약성 평가를 위해 홍수 피해 자료와 대상 인자간의 상관성 분석을 통해 상관계수 값이 상대적으로 높게 나온 인자를 선정하였다. 대상 인자는 크게 기상학적 인자, 지형학적 인자, 사회·인문학적 인자로 구분하였다 선정된 인자 간 서로 높은 상관성을 보일 시 공선성이 존재함을 의미하며, 이러한 공선성을 방지하기 위해 VIF (Variance Inflation Factor, 분산팽창계수)를 통한 공선성 검토를 적용하였다. 또한 각 인자 간 에는 서로 다른 단위 및 범위를 가진다. 이러한 경우 특정 인자들의 증감을 취약성 평가에 반영하기에 어려움이 있으며, 유역별 평가 시 신뢰성이 낮아진다. 따라서 Re-scaling 방법을 통해 각 인자의 단위 및 범위를 표준화 후 동일가중치 법을 적용하였다. 본 연구에서는 전체 유역 중 홍수피해가 가장 크게 발생하는 낙동강 태화강 유역을 연구 대상 지역으로 선정하였다. 태화강은 도심지의 중심부를 흐르는 하천이며, 산지의 고도가 높은 지형적 특성을 가지고 있어 홍수에 대한 취약성이 높은 것으로 나타났다(wamis, 국가수자원관리종합정보시스템). 태화강 유역 홍수 취약성 평가결과 유역별 기상, 지형, 인문학적 특성에 따라 홍수 취약성이 높게 나타나는 결과를 보였다. 이와 같은 결과는 유역 내 도심지 비율, 인구밀도, 토지피복 특성에 의한 것으로 주로 지형학적 인자로 인해 취약성이 높게 나타났다. 본 연구에서 활용한 홍수 취약성 평가 방법은 향후 홍수피해 대책 수립에 사용될 수 있을 것으로 판단된다.

• Journal of Korea Water Resources Association
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• v.48 no.8
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• pp.647-657
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• 2015

This study assessed the water use vulnerability for 12 basins of South Korea. The annual runoff of 12 basins are derived using a Soil and Water Assessment Tool (SWAT) and the calculated runoff per unit area and population are compared with each basin. The 18 indicators are selected in order to assess the vulnerability. Those are classified by aspects of demand, loss and supply of water use. Their weighting values used Entropy method to determine objective weights. To quantitatively assess the water use vulnerability, the Technique for Order of Preference by Similarity to Ideal Solution (TOPSIS) based on multi-criteria decision making are applied. The results show that the water availability vulnerability of Hyeongsan River has the highest value followed by Sapgyo River; Dongjin River; Seomjin River; Anseong River; Mangyung River; Nakdong River; Tamjin River; Youngsan River, Geum River; Taehwa River; and Han River. The result of this study has a capability to provide references for the index deveopment of climate change vulnerability assessment.

• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.206-210
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• 2011

하상재료 조사 결과는 하천 계획과 개발의 기초 자료로 사용한다. 그러나 우리나라에는 하천 특성을 반영한 적절한 하상재료 조사 및 분석 방법을 제시하지 못하고 있다. 따라서 태화강 도시하천 연장 5km 구간에서 높은 밀도로 시료채취를 시행한 후 하상재료의 분석 결과를 토대로 국내 하천 실정에 맞는 하상 재료 조사 및 분석 방법을 제안하고자 한다. 대상구간 5km에 대하여 250m 간격으로 시료 채취 간격을 설정하고, 하천의 중심 및 좌 우안의 시료를 채취하였으며, 심도별로 시료를 분리하여, 시료의 공간적 분포 특성을 판별할 수 있도록 하였다. 한편, 시료의 입도 분포와 유기물질 함량과의 관계, 입도 분포와 거리와의 상관관계를 분석하였다. 분석결과로부터 향후 시료채취의 적절한 간격과 시료채취의 적절한 깊이를 제안할 수 있다. 연구 성과는 하천 관련 계획이나 개발에서 실용적인 방법으로 활용할 수 있다.

• Journal of Korean Society of Water and Wastewater
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• v.25 no.4
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• pp.453-462
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• 2011

This study was analyzed to determine the cause of red tide at 10 and 30 days antecedental rainfall, stage and discharge in the Taehwa River, tidal data of Ulsan port, also, it was analyzed variation of red tide population, salinity, BOD, COD, T-N, T-P at S1, S2 each point. Most of the red tide in the Taehwa River occurred by provision of proper nutrients with antecedent, the proximity between discharge and low-flow capacity, and stage and discharge of stabilized condition after the sea water was inflowed by maximum tide difference. Red tide population is not nearly related to the change of salinity, the Taehwa River seems specific features of Non-coastal rivers downstream, because red tide was occurred when salinity quite low-end condition.