• Proceedings of the Zoological Society Korea Conference
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• 1999.10b
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• pp.108.1-108
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• 1999

• Journal of Korea Water Resources Association
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• v.37 no.5
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• pp.407-424
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• 2004

Using geomorphoclimatic unit hydrograph(GCUH), we estimated the fitness to calculate the mountainous area discharge and flash flood trigger rainfall(FFTR). First, we compared the GCUH peak discharge with the existing report using the design storm at the Dukcheon basin. Second, we compared the HEC-HMS(Hydrologic Engineering Center-Hydrologic Modeling System) model and GCUH with the observed discharge using the real rainfall events at the Taesu stage gage. Third, GCUH and NRCS(Natural Resources Conservation Service) were used for calculating FFTR and proper calculation method was shown. At the Dukcheon basin, the comparison result of using design storm was shown in Table 11, and it was not in excess of 1.1, except for the 30 year return period. In case of real rainfall events, the result was shown in Table 12, and GCUH discharges were all larger than the HEC-HMS model discharges, and they were very similar to the observed data at the Taesu stage gage. In this study, we found that GCUH was a very proper method in the calculation of mountainous discharge. At the Dukcheon basin, FFTR was 12.96 mm in the first 10 minutes when the threshold discharge was 95.59 $m^3$/sec.

• Journal of Korea Water Resources Association
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• v.52 no.spc2
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• pp.855-863
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• 2019

The efficiency of fishway installed in rivers can be directly evaluated by means of fish monitoring. On the other hand, when it is difficult to monitor the fish in certain conditions, or when planning a fishway, the efficiency can be evaluated indirectly through the hydraulic analysis. In this study, the hydraulic analysis technique for evaluating the efficiency of a fishway was presented. The River-2D model with the fish physical habitat module was used for the analysis of the attraction efficiency, and the weighted usable area was proposed as an index of the efficiency. In the analysis of passage efficiency, the three-dimensional model, Flow-3D, was used as an evaluation tool to describe the fluid behavior on a hydraulic structure with free surface. The ice-harbor type fishway at Baekgok weir in the Deokcheon River was selected as a test-site, and the efficiency was estimated using the hydraulic analysis. And then it was compared with fish monitoring data acquired from the river. As a result, it is difficult to replace the hydraulic analysis results with the efficiency quantitatively, but it can help to grasp the general tendency.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.1094-1097
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• 2007

낙동강 유역의 가용한 최장기 수량 및 수질자료를 획득하여 자료의 적합성 및 QC과정을 통하여 분석 가능한 자료를 생산하고 자료의 분석에 적합한 통계기법을 선정 각 변수의 변동특성과 변동 상관성을 정밀 분석하였다. 본 연구에서는 낙동강 수질자료의 변동특성을 분석하고 수질개선 필요성을 파악하기 위하여 Mann-Kendall 검정을 사용하여 수질변화의 경향성을 분석하였다. 낙동강 수계의 수질변화 특성을 분석하기 위하여 수온$(^{\circ}C)$, $DO(mg/{\ell}),\;BOD(mg/{\ell}),\;COD(mg/{\ell}),\;SS(mg/{\ell}),\;TN(mg/{\ell}),\;TP(mg/{\ell})$ 이상 7가지의 가용자료를 선택하였다. 수질자료는 환경부에서 운영하는 물 환경 정보 시스템의 수질측정망 자료인 월 단위 자료를 대상으로 Mann-Kendall 검정을 수행하였다. 분석에 사용된 자료 기간은 강우량자료와 유출량자료의 동기간인 1989년${\sim}$2000년까지이다. BOD의 변화를 살펴보면 전반적으로 감소하는 것을 알 수 있다. 가장 큰 감소 경향을 보인 지점은 금호강6 지점으로 $-39.1mg/{\ell}/20yr$로 나타났다. 증가지점으로는 안동과, 구미, 달성, 반변천 등이고 증가량은 약 $1.1mg/{\ell}{\sim}0.03mg/{\ell}/20yr$ 정도이다. COD의 변화를 살펴보면 대부분 지점에서 증가하는 것을 알 수 있다. 감소하는 지역은 고령과 현동, 대암, 금호강3${\sim}$6등이다. 특이사항은 금호강6의 감소분이 $-30.2mg/{\ell}$로 타 지점에 비해 상당히 크다는 것이다. DO의 경우는 증가지점과 감소지점의 수가 비슷하였고 주로 상류쪽이 감소하고 하류로 오면서 증가함을 알 수 있다. DO 또한 금호강6 지점이 가장 큰 폭으로 증가하고 있는 것을 볼 수 있다. pH는 함양위천과 덕천강1을 제외한 모든 지역이 증가 하였다. SS 또한 금호강5, 6, 거창 위천2를 제외한 모든 지역에서 증가하였다. SS항목도 금호강6 지점이 가장 큰 폭으로 감소하였다. 샘플지점(금호강6)의 BOD/COD/DO/pH/SS/TEMP/TN/TP 시계열을 통해 자료분석기간 동안 수처리시설 등의 확장으로 인한 금호강유역의 급격한 수질개선을 알 수 있다.

• The Journal of the Petrological Society of Korea
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• v.22 no.2
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• pp.179-195
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• 2013

The study area, which is located in the southeastern part of the Jirisan province, Yeongnam massif, Korea, is mainly composed of the Precambrian Hadong southern anorthosite complex (HSAC), the Jirisan metamorphic rock complex (JMRC) and Cretaceous sedimentary rock which unconformably covers them. Lithofacies distribution of the Precambrian constituent rocks mainly shows NS and partly NE trends. This paper researched deformational phased structural characteristics of HSAC and JMRC based on the geometric and kinematic features and the forming sequence of multi-deformed rock structures, and suggests that the geological structures of this area was formed through at least three phases of ductile deformation. The first phase ($D_1$) of deformation happened due to the large-scale top-to-the SE shearing, and formed the sheath or "A"-type fold and the regional tectonic frame of NE trend in the HSAC and JMRC. The second phase ($D_2$) of deformation, like the $D_1$ deformation, regionally occurred under the EW-directed tectonic compression, and most of the NE-trending $D_1$ tectonic frame was reoriented into NS trend by the active and passive folding, and the persistent and extensive ductile shear zone (Hadong shear zone) with no less than 2.3~1.4 km width was formed along the eastern boundary of HSAC and JMRC through the mylonitization process. The third phase ($D_3$) of deformation occurred under the NS-directed tectonic compression, and partially reoriented the pre-$D_3$ structural elements into ENE or WNW direction. It means that the distribution of Precambrian lithofacies showing NE trend locally and NS trend widely in this area is closely associated with the $D_1$ and $D_2$ deformations, respectively, and the NS-trending Hadong shear zone in the eastern part of Hadong northern anorthosite complex, which is located in the north of Deokcheon River, also extends into the HSAC with continuity.

• Korean Journal of Ichthyology
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• v.18 no.4
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• pp.329-338
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• 2006

Phylogenetic relationships and DNA polymorphism among local populations of the Korean native catfish species, Liobagrus mediadiposalis, have been investigated based on mitochondrial cytochrome b DNA sequences. As a result, three genetically distinct groups of local populations were recognized based on the phylogenetic tree constructed. The first group was called "Nakdong-river group" that included the local populations from Geumho-river, Gyeongho-river, and Deokcheon-river; the second one was "Geum-river group"; the third one was represented as "Seomjin-river group" that included the samples from Seomjin-river, Dongjin-river and Geokum-do. The phylogeny also implied that the ancestral group of L. mediadiposalis have first evolved to Nakdong-river group, and later two local populations (Geum-river and Seomjinriver group) were diverged from the other lineage. DNA polymorphisms we observed were 4.4~4.7% between Geum-river group and Seomjin-river group, 5.1~5.5% between Seomjinriver group and Nakdong-river group, and 5.5~5.7% between Nakdong-river group and Geumriver group. These results indicated the long period of geographic isolation due to the river system in Korea caused such high degrees of DNA polymorphisms between local populations of L. mediadiposalis.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.9 no.3
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• pp.771-778
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• 2008

Effects of establishments of more sewer systems on water quality in Nam River, Deokchun River, and Jinyang Lake were analyzed for various scenarios using QUAL2E, WASP 7 water quality model. Three different scenarios were tested: 1) 20.8% of sewer diffusion rate which is same to the existing condition. 2) Expansion of sewer system to 65.2% which would emit less pollutants, BOD 2350.5 kg/d, TN 216.0 kg/d, TP 44.0kg/d. 3) Pollutants emission to maintain first grade water quality in Nam River, Jinyang Lake, BOD and TN in the case 2 were 7.69%, 2.10% lower than those in the case 1 in the Nam River. And in the Jinyang Lake, BOD, TN, and TP in the case 2 were 10.25%, 1.37%, 2.94% lower than those in the case 1. However the simulations showed that water quality could not hold down first grade water quality standard level with the establishments of more sewer systems. To satisfy the criteria in the Nam River and Jinyang Lake, BOD emission must be reduced 27.2%, 37.05% compared to those in the case 1.