• 한국습지학회지
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• 제16권2호
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• pp.251-259
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• 2014

최근들어 세계환경의 화두는 습지와 더불어 논습지 그리고 습지의 생태계서비스 기능에 집중 조명되고 있지만, 논습지의 생태계서비스를 평가 할 수 있는 연구체계가 부족한 실정이다. 따라서 본 연구는 기존의 습지평가체계를 논습지에 적용하여 습지로서 논의 가치를 평가해보는 동시에 논습지 중심의 평가체계를 구축하는 기초자료로 활용하고자 연구를 진행하였다. 연구 대상지는 고도와 토양을 기준으로 16곳을 선정하였다. 습지평가 결과 연구대상지 16곳은 총점 110점~118점, 평균 2.17~2.50으로 선행연구 사례지인 호수형습지, 소택형습지, 하천형습지와 비교해도 습지로서 가치가 인정되었다고 할 수 있다. 하지만 고도, 토성에 따라서는 평가결과의 차이는 없었으며, 보전가치는 모두 같게 나타났다. Pearson 상관분석을 통해 보전가치에 가장 밀접하게 작용하는 요인을 찾아본 결과, 면적이 상관관계가 있는 것으로 나타났다. 그러나 기존의 습지평가체계로 논습지에 적용하기에는 한계가 있는 것으로 사료되어 논습지 평가를 위해서는 재배유형, 지형적 특성, 식생특성, 생육환경, 생물다양성 등의 다양한 후속 연구를 통해 습지평가체계를 보완할 필요가 있는 것으로 판단하였다.

• 한국환경복원기술학회지
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• 제11권3호
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• pp.50-61
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• 2008

Environmental factors and phragmites growth properties at various habitats in Eulsukdo ecological park were investigated to understand major factors affecting phragmites distribution in constructed wetlands. Although phragmites is very important species in wetland ecosystem, it should be controlled to prevent excessive expansion within the restricted park area. The results showed that phragmites dominant sites have the highest LAI among other emerged plants habitats and could adversely affect for waders habitats. Phragmites were also found at the areas with wide ranges of water-depth than other plants, and showed phragmites could be favored for occupying the newly constructed wetlands like Eulsukdo ecological park. The results showed difference in soil redox potential between phragmites dominant and non-dominant sites. Because soil redox potential is affected by wetland hydrology like flooding duration, control of wetland hydrology should be considered for creation and management of constructed wetlands. The results also showed that differences in soil cation exchange capacity, soil salinity, soil organic matter content and site inclination between phragmites dominant and non-dominant sites as well as brackish and freshwater areas. Those abiotic factors can be important considerations for the sustainable wetland management especially for the phragmitest managements in the ecological park.

• 한국습지학회지
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• 제17권2호
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• pp.184-192
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• 2015

습지 토양으로 인한 수질 악화를 저감할 수 있는 저관리형 습지 조성을 위한 기초연구로써 진행된 본 연구의 목적은 인공지반 위에 습지 조성 시 수체와 토양의 분리가 가능한 플랜터형 호안구조물이 설치된 습지의 수질 제어 기작을 연구하는 것이다. 실험구는 고무수조에 마사토를 채운 플랜터형 호안구조물을 적용하여 수체와 토양을 분리하였으며, 대조구는 고무수조에 마사토를 포설하여 수체에 직접 노출시켰다. 실험구와 대조구의 수질을 Kolmogorov-Smirnov Z 검정으로 분석한 결과, pH, BOD, SS, Chl-a, T-P, T-N에서 통계적으로 유의한 차이가 있는 것으로 나타나 플랜터형 호안구조물 적용 여부에 따른 수질 제어의 효과 차이를 입증하였다. 환경정책기본법에 근거한 수질 분석결과 수온과 EC는 실험구와 대조구가 비슷한 양상으로 나타났으며, pH와 DO는 두 메조코즘이 같은 등급에 속하였다. BOD, SS, Chl-a, T-P는 실험구가 더 높은 등급을 상회하는 것으로 평가되었으며, T-N은 대조구가 더 낮은 수치를 나타냈지만 수질의 등급이 같은 것으로 나타나 미미한 차이임을 알 수 있었다. 본 연구는 습지 조성 방식에 있어 플랜터형 호안구조물을 활용해 토양과 수체를 분리하여 습지를 조성하면 문제시 되어 오던 사면 침식으로 인한 육화 및 건조화 현상과 영양염류로 인한 녹조나 부영양화 현상 등을 예방하고, 식생대를 제어할 수 있음을 시사하였고, 특히 플랜터형 호안구조물을 활용한 습지 조성 시 수질 제어 기작을 통해 습지의 심미적, 생태적, 사회적, 경제적 가치를 증진시킬 수 있는 것에 대해 증명하였다. 따라서 본 연구의 결과는 향후 효율적인 수질 유지가 가능하여 관리조방적인 인공습지를 계획하고 조성하는데 기초 자료로 활용될 수 있을 것이다.

• Journal of Ecology and Environment
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• 제30권2호
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• pp.151-159
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• 2007

We studied the optimal ranges of water and soil characteristics for wetland plants, particularly Scirpus tabernaemontani (softstem bulrush) and Typha latifolia (broadleaf cattail), which are dominant species with potential for restoration of Korean wetlands. We observed vegetation in S. tabernaemontani and T. latifolia communities from the mid to late June, 2005, and measured characteristics of water environments such as water depth (WD), temperature (WT), conductivity (WC), and concentration of several ions $(NO_3{^-}-N,\;Ca^{2+},\;Na^+,\;Mg^{2+},\;and\;K^+)$, and characteristics of soil environments such as soil texture, organic matter (loss on ignition, LOI), conductivity, and pH. The S. tabernaemontani community was accompanied by Zizania latifolia (Manchurian wildrice), Persicaria thunbergii (Korean persicary), Actinostemma lobatum (lobed actinostemma), and Beckmannia syzigachne (American slough grass), while the T. latifolia community was accompanied by P. thunbergii, T. angustifolia (narrowleaf cattail), and Glycine soja (wild soybean). We defined the optimal range for distribution (ORD) as the range that each plant was crowded. The optimal range of water characteristics for the S. tabernaemontani community was a $WD\;10{\sim}50cm,\;WT\;24.0{\sim}32.0^{\circ}C,\;WC\;100{\sim}500{\mu}S/cm,\;{NO_3}{^-}-N\;0{\sim}60ppb,\;K^+\;0.00{\sim}1.50ppm,\;Ca^{2+}\;7.50{\sim}17.50ppm,\; Na^+\;2.50{\sim}12.50ppm,\;and\;Mg^{2+}\;3.00{\sim}7.00ppm$. In addition, the optimal range of soil characteristics for the S. tabernaemontani community was a soil texture of loam, silty loam, and loamy sand, $LOI\;8.0{\sim}16.0%,\;pH\;5.25{\sim}6.25$, and conductivity $10{\sim}70{\mu}S/cm$. The optimal range of water characteristics for the T. latifolia community was a $WD\;10{\sim}30cm,\;WT\;22.5{\sim}27.5^{\circ}C,\;WC\;100{\sim}400{\mu}S/cm,\;{NO_3}{^-}-N\;0{\sim}60ppb,\;K^+\;0.00{\sim}1.50ppm,\;Ca^{2+}\;0.00{\sim}17.50ppm,\;Na^+\;0.00{\sim}12.50ppm,\;and\;Mg^{2+}\;0.00{\sim}5.00ppm$, and the optimal range of soil characteristics for the T. fatifolia community was a soil texture of loam, sandy loam, and silty loam, LOI $3.0{\sim}9.0%,\;pH\;5.25{\sim}7.25$, and conductivity $0{\sim}70{\mu}S/cm$.

• 한국농공학회논문집
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• 제53권6호
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• pp.121-128
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• 2011

Long-term water treatment performance analysis was conducted for the constructed wetland treating agricultural tailwater. Studied wetland was established in 2001 and operated from June, 2002 to November, 2010. Wetland vegetation cover was shown over 90 % coverage after 2005. According to vegetation development, accumulation of sediment nutrient was observed; Organic Carbon, T-P and T-N. In addition, DO concentration and temperature was decreased in the constructed wetland output. An infiltration rate also significantly decreased due to compaction of wetland soil. A runoff coefficient was increased due to the low infiltration rate after 2005. A T-N, TSS and Chl.a removal rate was maintained constantly. However, the T-P removal rate was slightly decreased along to wetland operation because low DO concentration could increase elution of phosphorus from sediment. After constructing open water, the T-P removal rate was increased. This is because open water could accelerate the reaearation process. Consequently, over three years of vegetation development could be helpful for wetland performance. In addition, DO concentration is important factor to maintain the T-P treatment.

• 한국환경복원기술학회지
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• 제6권3호
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• pp.69-78
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• 2003

The main purpose of this study was to verify the shore margin protection effect of the root system of Salix gracilistyla Miq. developed from direct sticking cuttings on wetland, focusing on the effect of the root system reducing soil particle dissociation rate in water. The soil dissociation rate was examined through slaking tests with cylindric pure soil column at maximum particle density and the same size column of root reinforced soil. The dry weight of remained soil was measured after 5, 10, 15, 30minutes and 1, 6, 12, 24, 48hours inundation. As results, the soil particles began to dissociate severely at 10 minutes and only 10% of soil particles were left after 25minutes inundation. The stable slope angle of pure soil was $36^{\circ}$after 24 hours. On the other hand, the columns of root reinforced soil were stable even after 24hours, being dissociated only 7.2% of soil particles. So, it was revealed that the root system was very effective materials protecting more than 80% of soil particle from dissociation in inundation.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2004년도 학술발표회
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• pp.72-76
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• 2004

Wetland is an important eco-system on the earth and can effectively control agricultural non-point source pollution. Reed is a typical wetland plant for land/inland water ecotone in north China. The studies indicated that reed had a underground rooted-stem, which formed a 'high speeded-connecting vessels' i.e. reed root channel (RRC) in Baiyangdian lake of Hebei province. It spread predominantly along horizontal direction underground and are mainly distributed at 18-75 cm. The results of field work from healthy reed-wetland (HRW) and regarded reed-wetland (RRW) showed that the reed, averagely, in HRW is 4.2 m height, 1 cm diameter, 65/m2 density; in RRW is 2.4 m height, 3 mm diameter, 86/m2 density. These results indicated the regradation of the function of RRC in RRW. The results of laboratory work of sewage purification from reed soil column (RSC) $(0\~100cm)$ and wheat soil column (WSC) showed that the efficiency of purification to sewage, in RSC, is high than in WSC, especially for phosphorus. The efficiency of purification, in RSC, is $92.6\%$ for total phosphorus, $43.5\%$ for total nitrogen, $54.1\%$ fur COD, respectively; in WSC, is $86.0\%$ for total phosphorus, $241.3\%$ for total nitrogen, $29.8\%$ for COD, respectively.

• 한국환경복원기술학회지
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• 제17권1호
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• pp.27-43
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• 2014

The purpose of this research is to assess potential area of mountainous wetland by GIS and AHP (Analytic Hierarchy Process). Mountainous wetland is topographically located at high altitude, so it's difficult to approach for researchers. And, it's difficult to investigate systematically because of the insufficient information of mountainous wetland. Therefore, it's necessary to study on potential area of mountainous wetland for systematic and efficient investigation. This research selected slope, wetting index, land-cover map and soil map as assessment items indicating environmental characteristics of mountainous wetland and established them by GIS DB. And, spatial value of mountainous wetland for each assessment item was drawn by existing investigation data and overlap analysis of mountainous wetland. Based on the numerical results of each assessment item, a survey was conducted and relative importance for each assessment item was decided by AHP. As the result, slope was the highest as 0.550 and ground coverage was the lowest as 0.083. The subject of this research was Yangsan-si and Ulsan of Gyeongnam and an analysis was conducted for mountainous wetland in those research areas. As the result, all of wetland was distributed in the range of potential area. And, field survey and literature search were conducted for the point that the distribution of mountainous wetland is expected. As the result, mountainous wetland was distributed. Therefore, mountainous wetland should be excavated through the results of this research and it should be helpful for effective investigation as providing information necessary to the following studies on mountainous wetland.

• 한국조경학회지
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• 제35권6호
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• pp.48-63
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• 2008

This research is to apply suitable natural ecosystem evaluation criteria in order to develop the ecosystem conservation, restoration and ways to build substitute habitats as a compensation plan for damaged soundly natural ecosystems in small-scale projects such as resource recovery facility, filtration, etc. The environmental ecology evaluation i.e. generally based on their actual vegetation, community structure, wildlife, water system survey were measured the primary plans for reflecting unique natural environment level of site. As a result, it is necessary to conserve the land in fallow type of wetland, good conservative condition of deciduous forest, wetlanded watercourse for amphibia and reptiles crossing. However, the plan of filtration plant was destroyed wetland(sound ecosystem), natural forest, asian toad spawning area. According to the result of it schemed to build alternative wetland and spawning area, plan to healthy ecosystem and surface soil transplantation as compensation plan. The alternative wetland and spawning area are not only created a various water levels like depth of water is $0{\sim}30cm,\;30{\sim}60cm$, more than 1.5m but also it leads to asian toad spawning and wildlife inhabitant. Moreover, the ecosystem and surface soil transplantation be applied to use the Quercus acutissima forest resources(114 upper trees, 71 canopy trees, 401 shrubs) and surface soil$(5,072m^3)$ in ecology creation sets.

• 동굴
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• 제67호
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• pp.43-51
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• 2005

본 연구는 수문지형학적 관점에서 고봉동습지를 연구하였다. 고봉산의 남서쪽에 위치한 습지는 산지의 개석과 심층풍화의 영향을 많이 받은 곳이다. 지질적으로는 호상편마암에 속하는 지역이다. 3개 사면으로 부터 지하수 및 지표수를 공급받으며, 습지수원의 대부분은 지하수이다. 습지 지역은 지하수면과 가까이 발달하고 있다. 토양적 조건은 습지 발달에 유리하다. 장석과 운모의 점토광물화로 인하여 습지수의 저류성을 높여주기 때문이다.