• Proceedings of the Korea Air Pollution Research Association Conference
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• 2000.04a
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• pp.134-135
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• 2000

에어로졸은 인위적으로 발생하거나 자연적으로 발생하는 먼지(토양 발생인 먼지, 생물학적 비해염입자, 유기입자 둥)로 나뉘어지는 데 자연적으로 발생하는 먼지의 대표적인 사례로 황사를 들 수 있다. 이는 시정악화나 해수성분의 변화, 강수의 pH 변화 등 여러 가지 방면에서 영향을 주고 있는 것으로 나타나고 있다(Parungo et al., 1995). 동북아시아 지역의 지역적인 특수성으로 인해 미네랄 에어로졸 표면에서의 화학반응 활성화가 황산염이나 질산염의 생성을 유발한다는 여러 가지 보고가 있다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.129-130
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• 2002

최근 황사는 지구온난화와 토양의 사막화 등에 의해 발원지가 계속 확대되고 발생빈도 역시 증가하고 있으며 서해안에 인접한 중국의 북동부 공업지역에서 방출되는 오염물질까지 황사에 실려와 심각한 국내의 오염 문제 및 국제 문제로 부각되고 있다. 이들 대기오염물질은 가스상과 입자상으로 구분할 수 있는데, 요즘 입자상 물질의 건성침적량에 관한 연구가 서서히 활기를 띄어가고 있다. 입자의 크기가 0.1-10$\mu\textrm{m}$에 달하면 장거리 이동이 가능하며, 시정악화는 물론 흑비를 내리고, 인체에는 기관지 질환을 유발하기도 한다. (중략)

• Korean Journal of Soil Science and Fertilizer
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• v.18 no.3
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• pp.240-246
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• 1985

This study was conducted to estimate the proper particle size of Zeolite particle as the soil conditioner for sandy soil. On sand columns filled with different size of sand fractions, Zeolite particles of different size were applied. Tap water was percolated through those columns under the same water level as paddy soil during rice growth. The > 0.1mm fraction of Zeolite was not vertically moved although the water was percolated for 96 hours. The < 0.1mm fraction of Zeolite was moved out 85.7% in 2-1mm, 32.64% in 1-0.5mm, and 24.5% in 0.5-0.25mm sand column, respectively. The proper diameter of Zeolite particle for amelioration of sandy soils widely distributed around river side in Korea was estimated as 0.25-0.1mm fraction in consideration of its pore size.

• KOREAN JOURNAL OF CROP SCIENCE
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• v.59 no.4
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• pp.532-538
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• 2014

Arsenic (As) is nonessential element toxic to plants. In Korea little is not only known about the extent of actual anthropogenic sources and inputs of arsenic to the agricultural land which plays a active role as a sink, but also systematic research on arsenic as an toxic element entering the food chain via the soil-plant pathway has not been investigated in the fields and greenhouses besides in few places of abandoned mining sites. Therefore, it is important to focus on the effect of As-contaminated soils on As uptake and biomass production of lettuce plants. In this study, As concentrations in the soil and accumulation of As in lettuce transferred by As uptake from soils were investigated. To do this, soil which was mixed with various rates of arsenopyrite gravels containing arsenic from 0 to 100% was packed into a round plastic pot. Then, 10 days old vegetable crops of chinese cabbage and lettuce after germination were transplanted into a pot. Growth of lettuce was observed for four weeks with one week interval. All experiments were done by triplicate. The results showed that the growth rates for number of leaves, width and length of the crop plants were retarded with increasing amount of gravel mixed due to increasing bioavailable amount of arsenate with increasing rate of gravel in soils. With these results, we conclude that the bioavailable amount of arsenate can influence the growth of lettuce.

• Applied Biological Chemistry
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• v.29 no.3
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• pp.311-317
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• 1986

This experiment was conducted to find out the minimum size of pores through that Zeolite particles moved vertically out with percolated solution in the sand column and to estimate whether they were lost through the pores in the field sandy soil. The results were as follows. 1. The amount of Zeolite loss through sand columns was increased in the order of the columns filled with $2{\sim}1>1{\sim}0.5>0.5>0.25mm$ sand particles. 2. The Zeolite particles lost through columns filled with $1{\sim}0.5$ and $0.5{\sim}0.25mm$ sand were clay fraction. 3. The pore sire that clay fraction of Zeolite mineral could migrate through was determined to be above $150{\mu}m$ and Jangchon subsoil was presumed to have possibility of Zeolite loss in consideration of its pore size distribution. 4. The suitable particle size of Zeolite for application in sandy soil was presumed to be above $2{\mu}m$.

• Korean Journal of Soil Science and Fertilizer
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• v.28 no.4
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• pp.340-349
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• 1995

Effects of the zeolite particle size on the soil chemical properties and on rice growth was investigated on the pot with the loamy sand (Sadu series) and silty clay loam(Paju series) soils. All the zeolite treatments brought the increase of unhulled grain yield on the both loamy sand and silty clay loam soils. Unhulled grain yield increased with increasing the amount of zeolite applied and with decreasing the amount of particle size of zeolite applied on both soils. Unhulled grain yield increased significantly by 11.1% (22.79g/head) with 2ton/10a of smaller than $106{\mu}m$ size zeolite on the loamy sand soil and on the silty clay loam soil, yield increased by 9.3% (24.98g/head) with 1.5ton/10a of smaller than $106{\mu}m$ size zeolite. CEC, pH and contents of exchangeable cations of the soil after experiment were raised by increasing the amount of zeolite and also by decreasing the particle size of zeolite at both soil. At the heading stage, the zeolite treatments improved the growth of rice plant compared to control. The nutrient contents(T-N, Ca, Mg, K, Na), except phosphorus, in the rice plant grown on the zeolite treated soils were higher than control plot.

• Proceedings of the Korean Quaternary Association Conference
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• 2004.11a
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• pp.4-13
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• 2004

제주도 북제주군 한림읍 협재리에는 대부분 탄산염퇴적물로 이루어진 해안사구가 분포하고 있다. 사구를 이루는 탄산염퇴적물은 연체동물과 홍조류의 조각이 약 80% 이상을 차지하며 그 외에 저서성 유공충, 성게류와 태선동물의 조각, 그리고 화산암편으로 이루어져 있어, 제주도에 분포하는 여러 탄산염 해빈퇴적물의 입자조성과 매우 유사한 경향을 나타낸다. 이러한 탄산염 입자들은 천해에 서식하던 해양생물들에 의해 생성되며, 그 각질이 해빈으로 운반되고 바람에 의해 재동되어 사구를 형성하였다. 특히 이 연구지역의 사구가 분포하는 지점에서 북쪽으로 약 1km 떨어져 있는 협재 해수욕장에는 현재에도 천해에서 생성된 많은 양의 탄산염 해빈퇴적물이 퇴적되어 있으며, 제주도의 타 지역에 비해 매우 빠른 북동${\sim}$북서방향의 바람이 불고 있어, 퇴적물을 해빈에서부터 사구형성지점으로 운반시키는 데 효과적인 역할을 했을 것으로 판단된다. 사구를 절개하여 그 단면을 관찰한 결과, 전반적으로 희미한 수평층리와 사층리가 발달하고 있으며, 그 외의 다른 뚜렷한 퇴적구조는 관찰되지 않는다. 퇴적물의 입자들은 주로 직경이 $0.27{\sim}0.40mm$로 중립질 모래에 해당한다. 이 크기의 입자들은 가장 침식이 잘 될 수 있는 입자크기에 해당하는 것으로 알려져 있으며, 따라서 해빈으로부터 퇴적물이 운반될 때에 특히 이 크기의 입자들이 차별적으로 더 많이 운반되었을 것이라고 생각된다. 또한 퇴적물 입자의 크기와 구성성분의 함량은 각 사구의 전 층준에서 크게 변화하지 않는 것으로 나타나며, 이는 사구가 형성되는 기간 동안 탄산염퇴적물을 운반한 바람의 세기가 어느 정도 일정하였음을 지시한다. 해안사구의 형성시기를 알아보기 위하여 사구의 기반을 이루는 고토양층과 사구 최하부와 최상부의 탄산염퇴적물에 대해 방사성탄소연대측정을 실시하였다. 그 결과, 사구의 형성시기를 지시하는 고토양의 연령은 $680{\sim}720\;BP\;(1,200{\sim}1,300\;AD)$로 측정되었으며, 사구를 이루는 탄산염퇴적물의 연령은 전 층준에서 모두 약 3,500 BP로 측정되었다. 따라서 약 3,500 BP에 천해에서 생성된 탄산염퇴적물이 해빈에 분포하다가 $1,200{\sim}1,300\;AD$에 바람에 의해 재동되고 현재의 위치에 쌓여 사구를 형성한 것이라고 해석할 수 있다. 사구가 형성되기 시작하던 시기는 전세계적으로 춥고 바람이 세었던 Little Ice Age ($1,300{\sim}1,820\;AD$)에 해당하며, 따라서 해빈에 분포하던 많은 양의 탄산염퇴적물이 이 시기에 집중적으로 운반된 것으로 사료된다.

• Journal of Korean Society of Environmental Engineers
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• v.37 no.2
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• pp.92-98
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• 2015

The physical effect induced by acoustic cavitation was investigated to accumulate basic data for the design of ultrasonic soil washing processes using aluminum foil erosion tests. A square aluminum foil was placed on the glass beads in the pyrex vessel submerged in the sonoreactor equipped with a 36 kHz ultrasound transducer module at the bottom. Cavitational erosion of foils was quantitatively analyzed for various glass bead diameter conditions (1, 2, and 4 mm), glass bead height conditions (5, 10, 15, and 20 mm), and water height conditions (5, 10, 15, and 20 mm). It was found that aluminum foil erosion significantly increased as the glass bead diameter increased and water height over the glass bead increased due to less attenuation of ultrasound and the optimization of sound field for cavitation. Moreover mechanical mixing was suggested to move constantly particles to the bottom area where the acoustic cavitation occurs most violently. It was because aluminium foil erosion by ultrasound transmitted through glass beads was relatively too weak.

• Journal of the Korean Magnetics Society
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• v.15 no.2
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• pp.76-80
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• 2005

It was evaluated whether magnetic beads able to add the functionality of environment purification can be employed in processing soil pollutants. In this study, the micro scale magnetic beads containing carboxyl groups were mixed with water and the soil $(<0.025{\cal}mm) filtered through a sieve, and then it was agitated before isolating the magnetic substances by the use of outer magnetic force. The factors considered at this step were the ratio of soil to magnetic beads, ratio of soil to water, size of the tube where the reaction occur, and intensity of the magnetic force. From the separation experiment between soil and magnetic beads, it was concluded that the magnetic beads and water quantity have an impact on the degree of separation, yet the size of the tube and magnetic force does not have a considerable effect upon that in this small-scaled experiment. Through this experiment, the reaction conditions were optimized to achieve $90\~100\%$ of separation. Therefore, it was concluded that when the functionalized magnetic beads is introduced to environmental processing, it is able to be adopted to the soil processing as well as the water processing.

• Journal of Korean Society of Environmental Engineers
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• v.39 no.7
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• pp.418-425
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• 2017

ZnO nanoparticles (ZnO NPs) are mainly used in semiconductors, solar cells, biosensors, and cosmetics (sunscreen). In this study, we investigated the behavior of ZnO NPs in aquatic and soil environments and their effects on plants (Artemisia annua L.) in hydroponic cultivation. It was confirmed that the ZnO NPs size increased and their dissolution decreased with increasing in pH. Leaching distance of ZnO NPs was less than 2.5 cm, indicating that ZnO NPs had a little potential to leach into deeper soil layers. When ZnO NPs were exposed to plant, the total weights of plants decreased. The effects on the length of root and shoot were not observed. In addition large amount of ZnO NPs were adsorbed on the surface of plant root and didn't translocate into shoot. These results suggest that ZnO NPs block the pores of the root cell wall and decrease the bioavailability of plant nutrients. Therefore it can be speculated that the particles increase in size and settle down in the water environment and may adversely affect the plant growth by firmly adhering to the root surface when the ZnO NPs are exposed to the environment.