• Magazine of korean Tunnelling and Underground Space Association
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• v.3 no.1
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• pp.6-17
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• 2001

• Proceedings of the Mineralogical Society of Korea Conference
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• 2005.05a
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• pp.103-105
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• 2005

• Water for future
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• v.9 no.1
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• pp.9-23
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• 1976

• Proceedings of the Korean Society for Environmental Edudation Conference
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• 2005.08a
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• pp.49-70
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• 2005

• Proceedings of the Korean Environmental Sciences Society Conference
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• 1995.04a
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• pp.0-0
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• 1995

• Magazine of korean Tunnelling and Underground Space Association
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• v.2 no.2
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• pp.44-58
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• 2000

• Proceedings of the Korea Water Resources Association Conference
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• 2003.05b
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• pp.907-909
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• 2003

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2004.04a
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• pp.173-178
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• 2004

Due to the development of Yongsan river estuary weir and Yongam-Kumho sea dike, Mokop coastal area is changed. Especially, Discharged water through Yongsan river estuary weir and Yongam-Kumho sea dike, may cause the environmental influences such as the changes of currents pattern and sedimentation in the vicinity of semi-closed Mokpo harbor. This study deals with the collection and analysis of discharge through estuary weir and sea dike, based on that, we analyzed a characteristics of a sea area from simulation. As the results of this study, it is known that discharge causes the changes of a tidal currents pattern and calculated depth variations showed close relation with tidal circulation.

• Korean Journal of Environmental Agriculture
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• v.18 no.2
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• pp.126-134
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• 1999

To provide the basic information for the water improvement and control of water resource in Nakdong river districts, the physico-chemical characteristics of water in four main streams and three branch streams of the river were investigated through 36 times totally, one time per each month from January in 1995 to November in 1997. The pH values of each sites in main or branch stream of Nakdong river was pH $6.3{\sim}9.3$ range, pH range of Jukpo and Namji area at spring and fall was almost over pH 8.5, which was exceeded the water quality standard for agriculture. DO values of Nakdong river was almost $8.0{\sim}13mg/l$, except for Kangchang area in downstream of Kumho river. BOD values in Dasa area where was prior to mixing of Kumho river was $1.5{\sim}4.8mg/l$, which was under the water quality standard for agriculture(8mg/l), but BOD values followed mixing of Kumho river was over the permit standard of agricultural water as $3.8{\sim}8.9mg/l$ in Koryung, $3.4{\sim}8.4mg/l$ in Jukpo and $3.3{\sim}7.8mg/l$ in Namji according to time or season. Especially, BOD values at Gangchang area in Kumho river were $7.6{\sim}18.5mg/l$, which was over the water quality standard for agriculture and so Kumho river was a main pollutant: source of Nakdong river. COD values of main stream of Nakdong river was over the permit standard of agriculture(8mg/l) as $5.2{\sim}13.5mg/l$ in Koryvng, $5.0{\sim}12.7mg/l$ in Jukpo and $5.0{\sim}12.2mg/l$ in Namji according to time or season. And COD values was much high rather than BOD values and its gap of concentration was increased along with downstream. $NH_4-N$ of main stream of Nakdong river followed mixing of Kumho river($0.5{\sim}13.1mg/l$) was the highest affected in Koryung($0.18{\sim}5.0mg/l$) and detected much more in winter than in summer. T-N in Koryung($4.96{\sim}12.06mg/l$) followed mixing of Kumho river was significantly high rather than $2.86{\sim}4.86mg/l$ in Dasa, $4.20{\sim}8.20mg/l$ in Jukpo and $3.18{\sim}8.64mg/l$ in Namji, which was almost over the permit standard of agricultural water(1.0mg/l). T-P in Koryung($0.10{\sim}0.58mg/l$) also was significantly high rather than those $0.07{\sim}0.36mg/l$ in Jukpo and $0.08{\sim}0.4mg/l$ in Namji as over the standard of agricultural water(0.1mg/l). The concentration of T-N or T-P in Nakdong districts was trended of increasing in every year.

• Korean Journal of Environmental Agriculture
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• v.1 no.1
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• pp.39-47
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• 1982

Dissolved oxygen, BOD and flow pattern of the Nakdong River stream were measured for 3 years from 1978 to 1980 at quarterly intervals of January, April, June and October at 12 sites along the main stream from Sangju to Imhaejin and at 2 sites of Geumho and Nam River tributaries. With these data, the self-purification factors of the river were computed to obtain the following results: 1) The average BOD loads per day at the tributary of Geumho River were 94 tons in January, 39 tons in April, 60 tons in July and 54 tons in October, and these are considered to be the main source of water pollution toward the main stream of the Nakdong River. 2) Self-purification factors for the Hwawon-Hyunpung region of the main stream after receiving Geumho River water were computed to give $0.21{\sim}0.59$ of deoxygenation $constant(K_1)$ and $0.56{\sim}2.27$ of reaeration $constant(K_2)$. The oxygen-sag curves constructed for the main stream showed a remarkable decline at Hwawon and a quick recovery at Hyunpung, indicating a rapid decomposition of pollution loads received from the Geumho River. It was confirmed that the self-purification capacity of the Nakdong River was relatively high.