• 접착 및 계면
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• 제10권4호
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• pp.191-198
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• 2009

지방족 에폭시 수지인 glycerol diglycidyl ether (GDE)에 단관능성 아크릴 수지인 2-carboxyethyl acrylate (2-CEA) 또는 2-hydroxyethyl acrylate (2-HEA)를 반응시켜 지방족 에폭시 아크릴레이트를 제조하였다. FT-IR, $^1H$-NMR, 그리고 $^{13}C$-NMR를 사용하여 생성물을 확인하였고, 수율은 prep-LC를 사용하여 얻었다. 생성물의 자외선 경화거동은 photo-DSC를 사용하였고, 열경화 반응성은 DSC를 사용하여 얻었다. 2-CEA의 반응성이 2-HEA보다 월등히 높음을 알 수 있었고, 2-CEA로부터 제조한 지방족 에폭시 아크릴레이트(GEA-C)의 수율은 약 83%이었다. 촉매를 제거한 GEA-C 생성물의 자외선 경화반응($T_{max}$)은 약 10 s로 빠르게 진행되었다. GEA-C는 투명하고, 내열성이 우수하며 저점도를 갖고 있음을 확인할 수 있었다. ${\Delta}E^*$는 2.51, 점도는 192 cps, 5% 중량감소 때의 온도는 $299^{\circ}C$이었다. Kissinger와 Ozawa-Flynn-Wall 식으로 얻은 GEA-C의 열경화 반응의 활성화에너지($E_a$)는 91~92 kJ/mol이었다.

• 한국물환경학회지
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• 제24권2호
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• pp.185-194
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• 2008

There is increased soil erosion potential at highland agricultural crop fields because of its topographic characteristics and site-specific agricultural management practices performed at these areas. The agricultural upland fields are usually located at the sloping areas, resulting in higher soil loss, pesticides, and nutrients in case of torrential rainfall events or typhoon, such as 2002 Rusa and 2003 MaeMi. At the highland agricultural fields, the soil reconditioning have been performed every year to decrease damage by continuous cropping and pests. Also it has been done to increase crop productivity and soil fertility. The increased amounts of soil used for soil reconditioning are increasing over the years, causing significant impacts on water quality at the receiving water bodies. In this study, the field investigation was done to check soil reconditioning status for potato, carrot, and cabbage at the Doam-dam watershed. With these data obtained from the field investigation, the Soil and Water Assesment Tool (SWAT) model was used to simulate the soil loss reduction with environment-friendly and agronomically enough soil reconditioning. The average soil reconditioning depth for potato was 34.3 cm, 48.3 cm for carrot, and 31.2 cm for cabbage at the Doam-dam watershed. These data were used for SWAT model runs. Before the SWAT simulation, the SWAT ArcView GIS Patch, developed by the Kangwon National University, was applied because of proper simulation of soil erosion and sediment yield at the sloping watershed, such as the Doam-dam watershed. With this patch applied, the Coefficient of Determination ($R^2$) value was 0.85 and the Nash-Sutcliffe Model Efficiency (EI) was 0.75 for flow calibration. The $R^2$ value was 0.87 and the EI was 0.85 for flow validation. For sediment simulation, the $R^2$ value was 0.91 and the EI was 0.70, indicating the SWAT model predicts the soil erosion processes and sediment yield at the Doam-dam watershed. With the calibrated and validated SWAT for the Doam-dam watershed, the soil erosion reduction was investigated for potato, carrot, and cabbage. For potato, around 19.3 cm of soil were over applied to the agricultural field, causing 146% of more soil erosion rate, approximately 33.3 cm, causing 146% of more soil erosion for carrot, and approximately 16.2 cm, causing 44% of more soil erosion. The results obtained in this study showed that excessive soil reconditioning are performed at the highland agricultural fields, causing severe muddy water issues and water quality degradation at the Doam-water watershed. The results can be used to develop soil reconditioning standard policy for various crops at the highland agricultural fields, without causing problems agronomically and environmentally.

• Elastomers and Composites
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• 제40권4호
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• pp.266-271
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• 2005

실리콘 고무 (SR) 함량이 EPDM/SR 블랜드의 열안정성에 미치는 영향을 고찰하기 위하여 질소 분위기하에서 TGA 열분석을 수행하여 열분해온도, 열분해 활성화에너지 ($E_d$), 열분해 후 잔여량 등 열안정성 인자들을 알아보았다. 실험 결과, SR 첨가량이 10 wt%일 경우 블랜드의 열분해 곡선은 순수한 EPDM 고무와 비슷한 경향을 보였으나, SR 함량이 증가함에 따라 블랜드의 열분해는 더 높은 온도에서 진행되었다. 순수한 EPDM 고무인 경우 $E_d$ 값은 처음에는 서서히 감소하다가 분해분율이 20 wt%이상에서는 거의 일정한 값을 나타내었다. SR 함량이 10-20 wt%일 경우 블렌드의 $E_d$은 순수한 EPDM 고무의 경우보다 높은 값을 나타내었으며, 분해분율이 증가함에 따라 점차 감소하였다. 반면에 SR 첨가량이 30 wt%일 경우 블렌드의 $E_d$은 순수한 EPDM 고무의 경우보다 낮은 값을 나타내었으며, 분해분율이 증가함에 따라 서서히 감소하였다. 또한, $800^{\circ}C$에서의 열분해 후 잔여량은 SR 함량이 증가함에 따라 증가하였으며, 이는 분해된 실록산 그룹이 경화된 수지의 표면에 보호막을 형성하여 열전달 및 확산을 제한한 것으로 판단된다.

• 환경정책연구
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• 제8권1호
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• pp.73-95
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• 2009

댐 유역내 경작지나 산림에서의 가속화된 토양유실은 하류지역의 탁수문제를 야기시킨다. 토양유실은 탁수의 증가와 생태계 파괴의 원인으로서 사회적으로나 환경적으로 해결되어야만 하는 문제로 나타나고 있다. 또한 토양유실은 강우로 인하여 유출이 일어날 때 대부분의 경작지에서 발생하는데, 이는 수리 구조물을 불안정하게 만들고, 생태계를 파괴하며 취수를 악화 시키는 등 환경적 경제적 문제를 일으킨다. 이로 인해 수자원의 지속가능한 이용뿐만 아니라 하천생태계에도 많은 피해를 주고 있으나, 그동안 탁수문제는 저수지를 포함한 유역 물관리 운영에 적극적으로 고려되지는 않았다. 소양강댐 유역내 탁수의 주원인이 되는 탁수우선관리지역(우심지역) 세 개의 소유역 중 하나가 홍천에 위치한 자운리 지역이다. 특히 이 지역에서는 산림을 무허가로 밭으로 개간하여 소득작물을 재배하는 무허가 경작이 행해지고 있다. 본 연구의 목적은 Sediment Assessment Tool for Erosion Control(SATEEC) ArcView GIS를 기반으로 고해상도 위성사진과 지적도를 이용하여 현 상황을 보여주는 토지이용을 새롭게 구축하여 무허가 경작지를 산림으로 환원하였을 경우 토양유실저감을 평가하고자 함에 있다. 본 연구 결과에서 같이 무허가 경작지를 산림으로 환원한다면 17.42%의 토양유실 저감이 기대된다. 자운리 지역의 무허가 경작지는 경사도가 30%이상인 지역에서 47.48ha(30.83%), 경사도가 15%이상인 지역에서는 103.64ha(67.29%)를 차지하고 있다. 만약 모든 무허가 경작지를 산림으로 환원한다면 17.41%의 토양유실 및 유사량 감소가 기대되고, 경사도가 30%이상인 지역에서는 10.86%, 경사도가 15%이상인 지역에서는 16.15%의 감소가 기대된다. 따라서 자운리 유역에서 야기되는 토양유실과 이에 따른 학수발생을 저감시키기 위해서는 경사지에 위치한 무허가 경작지를 우선적으로 환원시켜야만 한다.

• 한국물환경학회지
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• 제23권4호
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• pp.467-473
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• 2007

Although the dominant land use at the Imha-dam watershed is forest areas, soil erosion has been increasing because of intensive agricultural activities performed at the fields located along the stream for easy-access to water supply and relatively favorable topography. In addition, steep topography at the Imha-dam watershed is also contributing increased soil erosion and sediment loads. At the Imha-dam watershed, outflow has increased sharply by the typhoons Rusa and Maemi in 2002, 2003 respectively. In this study, the Soil and Water Assessment Tool (SWAT) model was evaluated for simulation of flow and sediment behaviors with long-term temporal and spatial conditions. The precipitation data from eight precipitation observatories, located at Ilwol, Subi and etc., were used. There was no significant difference in monthly rainfall for 8 locations. However, there was slight differences in rainfall amounts and patterns in 2003 and 2004. The topographical map at 1:5000 scale from the National Geographic Information Institute was used to define watershed boundaries, the detailed soil map at 1:25,000 scale from the National Institute of Highland Agriculture and the land cover data from the Korea Institute of Water and Environment were used to simulate the hydrologic response and soil erosion and sediment behaviors. To evaluate hydrologic component of the SWAT model, calibration was performed for the period from Jan. 2002 to Dec. 2003, and validation for Jan. 2004 to Apr. 2005. The $R^2$ value and El value were 0.93 and 0.90 respectively for calibration period, and the $R^2$ value and El value for validation were 0.73 and 0.68 respectively. The $R^2$ value and El value of sediment yield data with the calibrated parameters was 0.89 and 0.84 respectively. The comparisons with the measured data showed that the SWAT model is applicable to simulate hydrology and sediment behaviors at Imha dam watershed. With proper representation of the Best Management Practices (BM Ps) in the SWAT model, the SWAT can be used for pre-evaluation of the cost-effective and sustainable soil erosion BMPs to solve sediment issues at the Imha-dam watershed. In Korea, the Universal Soil Loss Equation (USLE) has been used to estimate the soil loss for over 30 years. However, there are limitations in the field scale mdel, USLE when applied for watershed. Also, the soil loss changes temporarily and spatially, for example, the Imha-dam watershed. Thus, the SW AT model, capable of simulating hydrologic and soil erosion/sediment behaviors temporarily and spatially at watershed scale, should be used to solve the muddy water issues at the Imha-dam watershed to establish more effective muddy water reduction countermeasure.

• 농촌계획
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• 제11권4호
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• pp.67-74
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• 2005

The Doam watershed is located at alpine areas and the annual average precipitation, including snow accumulation, is significant higher than other areas. Thus, pollutant laden runoff and sediment discharge from the alpine agricultural fields are causing water quality degradation at the Doam watershed. To estimate soil erosion from the agricultural fields, the Universal Soil Loss Equation (USLE) has been widely used because of its simplicity to use. In the early spring at the Doam watershed, the stream flow increases because of snow melt, which results in erosion of loosened soil experiencing freezing and thaw during the winter. Also, extremely torrential rainfall, such as the typhoons 'RUSA' in 2002 and 'MAEMI' in 2003, caused significant amounts of soil erosion and sediment at the Doam watershed. However, the USLE model cannot simulate impacts on soil erosion of freezing and thaw of the soil. It cannot estimate sediment yield from a single torrential rainfall event. Also, it cannot simulate temporal changes in USLE input parameters. Thus, the Soil and Water Assessment Tool (SWAT) model was investigated for its applicability to estimate soil erosion at the Doam watershed, instead of the widely used USLE model. The SWAT hydrology and erosion/sediment components were validated after calibration of the hydrologic component. The R$^2$ and Nash-Sutcliffe coefficient values are higher enough, thus it is found the SWAT model can be efficiently used to simulate hydrology and sediment yield at the Doam watershed. The effects of snow melt on SWAT estimated stream flow and sediment were investigated using long-term precipitation and temperature data at the Doam watershed. It was found significant amount of flow and sediment in the spring are contributed by melting snow accumulated during the winter. Two typhoons in 2002 and 2003, MAEMI and RUSA, caused 33% and 22% of total sediment yields at the Doam watershed, respectively. Thus, it is recommended that the SWAT model, capable of simulating snow melt, sediment yield from a single storm event, and long-term weather data, needs to be used in estimating soil erosion at alpine agricultural areas to develop successful soil erosion management instead of the USLE.

• 식물병연구
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• 제9권2호
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• pp.57-63
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• 2003

Clubroot disease of curcifer crops caused by Plasmodiophora brassicae had been first reported in 1928 in Korea, and maintained mild occurrence until 1980s. Since 1990s the disease has become severe in alpine areas of Kyonggi and Kangwon, gradually spread to plain fields throughout the country, and remains as the great-est limiting factor for its production. Researches on the disease has begun in late 1990s after experiencing severe epidemics. Survey of occurrence and etiological studies have been carried out, particularly, on the pathogen physiology, race identification, quantification of soil pathogen population, and host spectrum of the pathogen. Ecology of gall formation and its decay, yield loss assessment associated with time of infection, and relationships between crop rotation and the disease incidence was also studied during late 1990s. In studies of its control, more than 200 crucifer cultivars were evaluated for their resistance to the disease. Lime applica-tion to field soil was also attempted to reduce the disease incidence. Resistant radish and welsh onion were recommended as rotation crops with crucifers after 3-year field experiments. However, so for, most studies on clubroot disease in Korea have been focused on chemical control. Two fungicides, fluazinam and flusulfamide, were selected and extensively studied on their application technologies and combination effects with lime application or other soil treatment. To develop environmentally-friendly control methods, solar-disinfection of soil, phosphoric acid as a nontoxic compound, and root-parasiting endophytes as biocontrol agents were examined for their effects on the disease in fields. In the future, more researches are needed to be done on development of resistant varieties effective to several races of the pathogen, establishment of economically-sound crop rotation system, and improvement of soil-disinfection technique applicable to Korean field condi-tion, and development of methodology of pretreatment of fungicides onto seeds and seedbeds.

• 한국물환경학회지
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• 제26권4호
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• pp.637-647
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• 2010

The Universal Soil Loss Equation (USLE)-based modeling systems have been widely used to simulate soil erosion studies. However the GIS-based USLE modeling systems have limitation in gully erosion evaluation which is one of the most important factor in soil erosion estimation. In this study, the integrated soil erosion evaluation system using with Sediment Assessment Tool for Effective Erosion Control (SATEEC) system, nLS and Unit Stream Power-based Erosion/Deposition (USPED) model was developed to simulate gully erosion. Gully head location using nLS model, USPED for gully erosion, and the SATEEC estimated sheet and rill erosion were evaluated and combined together with the integrated soil erosion evaluation system. This system was applied to the Haean-myeon watershed, annual average sediment-yield considering sheet, rill and gully erosion was simulated as 101,933 ton/year at the study watershed. if the integrated soil erosion evaluation system is calibrated and validated with the measured data, this system could be efficiently used in developing site-specific soil erosion best management system to reduce soil erosion and muddy water inflow into the receiving waterbody.

• 식물병연구
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• 제21권1호
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• pp.6-11
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• 2015

고추 탄저병 요방제 수준을 설정하기 이하여 시험한 결과 노지 고추 수량에 영향을 주지 않는 수준의 탄저병 방제적기는 발생정도가 0.9% 이하이었으며, 노지고추 탄저병 발생정도와 수량과의 회귀식은 Y = -16.83X + 327.57, $R^2=0.83$ 성립하였다. 비가림 재배(무강우 조건) 고추의 수량에 영향을 주지 않는 수준의 탄저병 방제적기는 발생정도가 1.7% 이하이었으며, 고추탄저병 발생정도와 수량과의 회귀식은 Y = -4.92X + 361.02, $R^2=0.84$ 성립하였다. 비가림 재배(강우 조건) 고추의 수량에 영향을 주지 않는 수준의 탄저병 방제적기는 발생정도가 2.3% 이하이었으며, 고추 탄저병 발생정도와 수량과의 회귀식은 Y =-5.91X + 359.71, $R^2=0.76$ 성립하였다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1997년도 총회 및 춘계 학술발표회 논문집
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• pp.8-11
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• 1997

Current methods of evaluating soil contamination by heavy metals rely on analyzing samples for total contents of metals or quantities recovered in various chemical extracting solutions. Results from these approaches provide only an index for evaluation because these methodologies yield values not directly related to bioavailability of soil-borne metals. In addition, even though concentrations of metals may be less than those required to cause toxic effects to biota, they may cause substantial effects on soil chemical parameters that determine soil quality and sustainable productivity. The objective of this research was to characterize effects of Cu or Cd additions on soil solution chemistry of soil quality indices, such as pH, EC, nutrient cation distribution and quantity/intensity relations (buffer capacity). Metals were added at rates ranging from 0 to 400 mg/kg of soil. Soil solution was sequentially extracted from saturated pastes using vacuum. Concentrations of Cu or Cd remaining in soil solutions were very low as compared to those added to the soils, warranting that most of the added metals were recovered as nonavailable (strongly adsorbed) fractions. Adsorption of the added metals released cations into soil solution causing increases of soluble cation contents and thus ionic strength of soil solution. At metal additions of 200~400 mg/kg, EC of soil solution increased to as much as 2~4 dS/m; salinity levels considered high enough to cause detrimental effects on plant production. More divalent cations (Ca+Mg) than monovalent cations (K+Na) were exchanged by Cu or Cd adsorption. The loss of exchangeable nutrient cations decreased long-term nutrient supplying capacity or each soil. At 100 mg/kg or metal loading, the buffering capacity was decreased by 60%. pH of soil solution decreased linearly with increasing metal loading rates, with a decrement of up to 1.3 units at 400 mg Cu/kg addition. Influences of Cu on each of these soil quality parameters were consistently greater than those of Cd. These effects were of a detrimental nature and large enough in most cases to significantly impact soil productivity. It is clear that new protocols are needed for evaluating potential effects of heavy metal loading of soils.