• Journal of the Korean hospital association
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• v.33 no.6 s.292
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• pp.7-14
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• 2004

• KOREAN POULTRY JOURNAL
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• v.34 no.6 s.392
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• pp.68-70
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• 2002

• The Korean Publising Journal, Monthly
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• s.206
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• pp.17-17
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• 1997

• KOREAN POULTRY JOURNAL
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• v.28 no.12 s.326
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• pp.99-103
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• 1996

• Monthly Korean Chicken
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• v.19 no.2
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• pp.49-53
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• 2013

• Water for future
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• v.5 no.1
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• pp.75-76
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• 1972

• Journal of the Korean association of regional geographers
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• v.14 no.1
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• pp.27-39
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• 2008

The propose of this research paper is to clarify the formative process of the lake-like swamps formed in channels of Nakdong-gang river and its tributary, Gumho-gang river. In order to understand the formative process of lake-like swamps, I compared topographical maps of three years(1918, 1962, 2005), analyzed the outline change of swamps, and draw their cross-sectional view and analyzed the horizontal distribution of particle size. Results of analysis are as follow. First, Saegang swamp and Geumgang swamps are residual swamps which are formed in abandoned distributary channels of braided reach. In braided reach, tributaries wind freely to create a new channel or to eliminate a old channel. Second, the Ssiksil swamp and Nat swamp are yazoo-type swamps. Their stream channels run parallel to the natural levees, as it blocks the waterway of a effluent tributary flowing from backward mountains to main stream. Third, the Secheon, Hochon and Jinchon swamps are backswamp behind natural levee. As main stream overflows, natural levee and back swamp are formed. Later flowing water of next bigger flood enter through natural levee into backswamp, create a channel following backswamp.

• Journal of Wetlands Research
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• v.9 no.3
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• pp.1-12
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• 2007

In this study, the correlation of organic content with particle size and type of sediment was found out.Particle size, stratigraphic section and organic content of sediments sampled from Dalpo wetland was analyzed. Dalpo wetland consists of three wetlands, and the area of Dalpo wetland is about $31,295m^2$. The particle size analyses for sampled sediments of 7 points (3 points in wetland A, 3 points in wetland B and 1 point in wetland C) were tested. As results of the particle size analyses, the sediment particle size becomes larger as to the edge of the wetland. It is revealed in order of wetland A > wetland C > wetland B. Borehole surveys with horizontal distance in the major and minor axes of wetland A, the major and minor axes of wetland B and the major axis of wetland C were accomplished. Clayey peat deposit is distributed at 10~90 cm depth below ground surface in the major axis of wetland A. The clayey peat deposit was the most thick at the center of wetland A that horizontal distance is 100 m. As the depth below ground surface of clayey peat deposit is less than 27 cm in the wetland B, we can infer that the life for the wetland B is being finished. Sediment composition of wetland C is simple because wetland C is small scale, and clayey peat deposit is distributed at 10~34 cm depth below ground surface. Sediment sampled by borehole survey in the Dalpo wetland was cut at interval of 10 cm, then organic content was analyzed. Organic content of wetland A sediment showed more than 40% until 70 cm depth below ground surface, also sediment of wetland B is similar to wetland A until 10 cm depth below ground surface, but is showed within 20 % above 30 cm depth below ground surface. Organic content of wetland B is showed the lowest as organic content near the ground surface is about 40%. All of the three wetlands, organic content is showed higher at clayey peat deposit near to ground surface. This is caused by finer particles of the clayey peat deposit, also organic materials were supplied from dead vegetation. Organic content of the Dalpo wetland showed in order of wetland A > wetland C > wetland B. This result is caused by thickness of clayey peat deposit in sediment. Through this study, it was verified that organic content of the Dalpo wetland sediment was dominated by particle size of sediment and vegetation of the upper part.

• Proceedings of the Korea Water Resources Association Conference
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• 2009.05a
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• pp.1250-1253
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• 2009

기후변화가 수자원에 미치는 영향을 평가하는데 있어서 주로 기후모형인 Global Climate Model (GCM)이 사용되고 있다. 그러나 이러한 기후모형의 공간적 해상도는 $3^{\circ}{\sim}4^{\circ}$ 정도로 한반도의 경우 바다로 묘사되기도 한다. 따라서 GCM을 이용해서 기후변화가 유역단위 수자원에 미치는 영향을 평가하기 위해서는 일반적으로 축소기법이 사용되고 있다. 현재까지 다양한 축소기법이 개발되었으며, 대표적인 모형으로는 SDSM(Statistical Down-Scaling Model)과 LARS-WG(The Long Ashton Research Station Weather Generator)이 있다. 이에 본 연구에서는 SDSM, LARS-WG와 함께 최근에 축소기법으로 사용되고 있는 인공신경망 기법을 이용해서 CCCMA(Canadian Centre for Climate Modeling and Analysis)에서 일 단위로 모의한 CGCM3 A2 시나리오를 기반으로 우포늪의 강우 및 온도시나리오를 구축하였다. 대상 지점인 우포늪은 경상남도 창녕군 우포늪(위도 $35^{\circ}$33', 경도 $128^{\circ}$25')에 위치하고 있으며, 모의 기간은 CASE1의 경우 현재, CASE2는 2050$^{\sim}$ 2080년, CASE3는 2080년$^{\sim}$2100년으로 각각 구분하여 축소기법을 적용하였다. 축소결과 축소기법에 따라 일정정도 차이를 보이기는 하였으나 강우와 온도 모두 증가하게 됨을 확인하였다.

• Journal of Wetlands Research
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• v.16 no.2
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• pp.187-192
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• 2014

This study is on the characteristics of habitat use of Pheasant-tailed Jacana Hydrophasianus chirurgus in Upo-wetland from June to August in 2013. The purpose is population management of Pheasant-tailed Jacana. Four nests were founded which are located in $56.2{\pm}16.37m$ from the waterside. Pheasant-tailed Jacana made their nests above Euryale ferox which consists with water plants such as Salvinia natans, Spirodela polyrhiza, Ceratophyllum demersum, Hydrocharis duvia and so on. Human beings seem to be the biggest obstacle of their breeding, according to this, Pheasant-tailed Jacana moved their eggs. Only two out of four nests, they moved their eggs and the distance was 1 to 2 meters from the nests. Since plant community of Euryale ferox is extensively distributed and water level also keep stable in Upo-wetland, the number of Pheasant-tailed Jacana coming to Upo-wetland is expected to increase every year. In the past, the number of Pheasant-tailed Jacana coming to Korea was too little to include management plan, but now, we need to manage them because of their population growth and the regular advent.