• 상하수도학회지
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• 제23권1호
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• pp.97-105
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• 2009

Analysis was done on the particle size distribution of sediments flown into Saemangeum from the Mankyung and Dongjin River. The organic pollutants and heavy metal existing in the sediments were analyzed, which was further used to study the properties of pollution in the sediments according to the particle size distribution. Conclusions shown below were made from these analyses. The particle size distribution showed a big difference between the upriver areas of Mankyung and Dongjin River. Particles under $75{\mu}m$ showed to be around 85% at Dongjin River, while it showed to be around 70% at Mankyung River. This kind of distribution in particle size concluded in greatly affecting the contamination density of the sediments. From the analysis done on the soil type of sediments, deposition in Mankyung River categorized into Silty loam and Sandy loam, where Silty loam covered most of area and deposition in Dongjin River categorized into Sand, Loamy sand, Silty loam, Sandy loam. Considering the weight ratio, the density of contamination of the sediments by particle size at Dongjin and Mankyung River has been analyzed to show that organic pollutants and heavy metals occupy more than 70% of the whole contamination in the range under the particle size of $75{\mu}m$.

• 한국조경학회지
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• 제27권5호
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• pp.170-180
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• 2000

The surface-drainage system, which consists of bio-swale and detention-infiltration Basins and carries out the function of temporary detention-infiltration of runoff, is defined as the "natural drainage system". It is an environmentally sound and economically beneficial practice to reduce run-off by retaining it in swales as much as possible and letting run-off infiltrate into the ground. In order to estimate appropriate capacity of swales, it is necessary to know how long will it take for certain depths of water to infiltrate. The ponding times, or infiltration times, of various depths and of various soil textures, could be estimated with the Green-Ampt Infiltration Model. Included soil textures are loamy sand, sandy loam, loam, silty loam, sandy clay loam and clay loam. Ponding depths are from 10cm to 100cm intervals. Newton-Raphson method is used for the solution of the Green-Ampt equation by a computer program. The computer program was written with the FORTRAN Developer 4.0 v.. Selected ponding depth is acceptable when the sum of the ponding time and the breeding time of mosquitoes is less than the tolerance period of innundation of grasses and trees.and trees.

• 한국작물학회지
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• 제38권3호
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• pp.290-295
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• 1993

수도 무경기 기계이앙 재배시 수도수량과 토양특성 변화를 구명하기 위하여 무경운을 포함한 논토양 특성에 맞는 최소경운 방법을 확립코자 미사 질식토, 사양토, 미사질양토의 3개 포장에서 경운방법을 달리하여 화성벼를 재배하면서 수도 수량과 토양특성을 조사, 분석한 결과는 다음과 같다. 1. 무경기구의 수온과 지온은 제 일 낮았으나 처리간에 온도차이는 크지 않았다. 2. 토성별 평균감수심은 사양토에서 가장 많았고 미사질식토에서 가장 적었는데 무경윤구의 감수심이 다른 처리구보다 1.4～2.2mm/일 많았다. 3. 수확기때 수도체의 무기함량은 무경기시 다른 처리구에 비하여 미사질식토에서는 $Na_2$O 함량을 제외하고는 가장 높았다. 4. 무경운구의 수양감수는 경운기 경운+로타리구에 비하여 사양토에서 18%, 미사질식토에서 7%, 미사질양토에서 1%감수되었다.

• 한국토양비료학회지
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• 제44권1호
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• pp.22-28
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• 2011

With the increasing cultivation of acid-loving plants such as blueberries, the artificial acidification of soils is frequently required. This research was conducted to determine the application rates of elemental sulfur (S) required in the soil acidification for blueberry cultivation. Laboratory incubation experiment was conducted to acidify three arable soils (pH 6-7) of different texture to pH 4.5-5.0 by the addition of varying amounts of elemental S. All rates of elemental S addition reduced soil pH, although the efficacy of acidification was related to the application rate and soil characteristics. pH reduction was slow in sandy loam soil, and the final equilibrium pH was obtained after 60, 43, and 30 days of incubation in sandy loam, loam, and silty clay, respectively. Although the final pHs obtained after 93 days of incubation were not significantly different among the three soils, the equilibrium pH was relatively higher in soil of higher clay content in the application rates of 1.5-2.0 g S $kg^{-1}$ soil. The estimated amounts of elemental S required in lowering pH to 4.5-5.0 were 0.59-1.01, 0.67-1.03, and 0.53-0.88 g S $kg^{-1}$ for sandy loam, loam, and silty clay, respectively. The lowest estimated amount of elemental S in the acidification of silty clay soil was attributable to the low organic matter content. For clay soils containing optimum level of organic matter, the application rates of elemental S should be much higher than those values estimated in this research. Soil acidification did not significantly increase the available concentrations of Ca, Mg and K. Extractable Cu and Zn was not greatly affected by the acidification, but extractable Fe, Mn, and Al in the acidified soils were higher than those found in non-acidified soils. Such increases in solubility are attributable to the dissolution of oxides and hydroxides of the elements.

• 한국토양비료학회지
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• 제46권6호
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• pp.417-425
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• 2013

This study investigated the runoff from rice paddy located on reclaimed fine sandy loam soil to provide data for the development of policies to protect water quality of estuaries. Total N (TN), Total P (TP) concentrations and runoff loads at outlet were monitored from 2006 to 2008. Soil phosphate adsorptivity was measured and compared with typical paddy soil in watersheds. TP concentration of the paddy water and TP runoff loads were much greater than those of typical paddy field in watershed because phosphate adsoptivity in reclaimed paddy field of fine sandy loam appeared to be a third of those of typical paddy soils by relatively low soil OM and high sand content of the reclaimed soil. Thus, nutrient runoff, particularly phosphate from the reclaimed paddy field needs to be managed more thoroughly to protect estuarine water quality.

• 환경영향평가
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• 제17권6호
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• pp.321-333
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• 2008

Considering risks and artificial enrichments of metals in the soils of the study area, the study aims to analyze geology, grain size and geochemistry. Geology is mainly composed of gneisses and phyllites of metamorphic rocks, sandstones, siltstones, shales, tuffs of sedimentary ones and granites and andesites of igneous ones in the area. In the area, mean contents of metals are not meaningful in accordance with petrogenesis. The soil textures of the area are of S, lS and sL of sandy soil, L, scL, cL of loam and C, zC and sC of clayey soil. Mean contents of Ni, Cr, Co and Cu are meaningfully high in loam and clayey soil relative to sandy soil, whereas Ni, Zn, Cd contents are higher in clayey soil than in loam. Those differences imply the metallic contents are dependent to grain size. Based on the metal contents in the soils of the study area, Cu and Zn in loams and Pb in sandy soils are corresponded to soil contamination warning standards, and As showing 75mg/kg of maximum content in loams is assigned to soil contamination countermeasure standards, respectively. Artificial enrichment factor minimized wall rock and grain size relations is over 1 in Cr, Ni and Cu, but the factor is below 1 in average of other metals.

• 유기물자원화
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• 제25권4호
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• pp.15-22
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• 2017

농경지에 유기물 자원을 시용하면 지력이 높아져서 작물의 수량이 높아진다. 본 연구의 목적은 유기물 자원을 밭 토양에 시용하였을 때 작물 수량 및 토양 물리성에 미치는 영향을 유기물 자원별로 비교하고자 하였다. 콩을 평야지인 수원의 사양토와 식양토 포장에서 재배하였으며, 온도 영향을 살펴보기 위하여 고랭지 평창의 사양토 포장에서도 수행하였다. 시험에 쓰인 유기물 자원은 볏짚퇴비, 돈분톱밥퇴비, 계분톱밥퇴비, 코코피트였으며, 콩 파종 전에 탄소 기준으로 동등한 수준으로 시용하였다. 무기질비료의 시용량은 토양검정한 분석치를 고려하여 결정하였다. 유기물 자원의 분해 특성을 살펴보기 위하여 항온배양실험을 실내에서 사양토를 대상으로 수행하였다. 분해 속도는 볏짚퇴비가 가장 높았으며, 돈분톱밥퇴비, 코코피트 순이었다. 유기물 자원의 시용에 따른 콩 수량의 증가 효과는 사양토에 비해서 식양토에서 높았다. 기상 비율의 증가 효과도 식양토에서 뚜렷하였다. 반면에 토양 입단 안정성의 증가 효과는 사양토에서 비교적 높았다. 볏짚퇴비가 모든 토양에서 콩 수량의 증가 효과가 가장 높았다. 코코피트의 콩 수량 증가 및 토양 물리성 개선 효과는 다른 유기물 자원에 비해서 높지 않았다. 따라서 밭작물 수량의 증대 및 토양 물리성의 개선을 위해서는 축분퇴비 등 다른 유기물 자원에 비해서 볏짚퇴비가 적합하였다.

• 한국토양비료학회지
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• 제48권2호
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• pp.81-86
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• 2015

Soil management for orchard depends on the effects of soil microbial activities. The present study evaluated the soil microbial community of 25 orchard (5 sites for sandy loam, 7 sites for silt loam, and 13 sites for loam) in Gyeongnam Province by fatty acid methyl ester (FAME) method. The average values for 25 orchard soil samples were $270nmol\;g^{-1}$ of total FAMEs, $72nmol\;g^{-1}$ of total bacteria, $34nmol\;g^{-1}$ of Gram-negative bacteria, $34nmol\;g^{-1}$ of Gram-positive bacteria, $6nmol\;g^{-1}$ of actinomycetes, $49nmol\;g^{-1}$ of fungi, and $7nmol\;g^{-1}$ of arbuscular mycorrhizal fungi. In addition, silt loam soils had significantly low ratio of cy17:0 to $16:1{\omega}7c$ and cy19:0 to $18:1{\omega}7c$ compared with those of loam soils (p < 0.05), indicating that microbial activity increased. The average soil microbial communities in the orchard soils were 26.7% of bacteria, 17.9% of fungi, 12.6% of Gram-negative bacteria, 12.5% of Gram-positive bacteria, 2.5% of arbuscular mycorrhizal fungi, and 2.2% of actinomycetes. The soil microbial community of Gram-negative bacteria in silt loam soils was significantly higher than those of sandy loam and loam soils (p < 0.05).

• 한국토양비료학회지
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• 제29권4호
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• pp.336-341
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• 1996

경사지 토양에서 퇴비시용이 토양유실량과 토양의 이화학적 특성에 미치는 영향을 검토하기 위하여 1984년에 사양토, 양토, 식양토, 식토의 토양을 충진한 경사도 15%, 경사장 5m, 폭 2m, 길이 1.2m인 유저 Lysimeter를 설치하여 나지, 무토비, 퇴비구(1.5ton/10a)를 두고 보리-콩 작부체계로 경작해온 시험지에서 1990년과 1991년도에 조사한 2개년의 시험결과는 다음과 같다. 1. 토양유실량은 사양토, 식토, 양토, 식양토순으로 증가하였으며 물 유출량은 사양토, 양토, 식양토, 식토순으로 증가하였으나 침투수량은 이와 반대였다. 2. 퇴비 시용구와 무시용구의 토양유실량, 유출수량 및 침투수량의 증감비를 보면 토양유실량은 33.6~44.6%, 유출수량은 17.0~24.0% 감소하였고 침투수량은 17.1%~23.7% 증가하였다. 3. 토양유실량은 유출수량과 Y=-12.125 + 0.063 X(r = $0.970^{**}$)의 정 상관관계였고, 침투수량과는 Y = 43.415-0.096X(r = $0.917^{**}$)의 부의 상관관계였다. 4. 퇴비 시용으로 pH, OM, CEC, 유효인산, 치환성 염기함량, 공극율, 내수성 입단, 유효수분 함량이 증가하였다.

• 한국토양비료학회지
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• 제31권4호
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• pp.400-406
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• 1998

사양토, 양토, 식양토의 3 가지의 토양을 $2^{{\prime}{\prime}}{\times}30cm(D{\times}L)$ column에 충진한 후 인공 산성비(pH 2.0, 4.0, 6.0) 1,200mm를 처리하여 산성비의 토양내 침투수량에 따른 토양의 산성화 경향, 토양 중 무기양분의 용탈과 이동양상과 산성비 토양투입에 따른 석회 중화양을 비교검토한 결과, 산성비 처리에 따른 각 토양의 pH 변화는 산성비의 pH가 4.0과 6.0에서는 별 차이가 없었으나, pH 2.0에서는 토심별로 큰 차이를 보였으며 pH감소는 사양토>양토>식양토의 순이었고, 치환산도(치환성 Al+H)는 식양토>양토>사양토의 순위였다. 산성비에 따른 각 토양의 토심별 양분 용탈량은 산성비의 pH 2.0에서 많았으며, 사양토, 양토와 식양토의 경우, 각토양 공히 Ca>K>Mg 순위였다. 토양의 pH감소와 치환산도(치환성 Al+치환성 H)는 사양토 > 양토 > 식양토의 순위였으나, pH감소에 따라 증가되는 치환산도는 그 토양의 CEC범위내 이었다. 토양내의 치환성 Al는 토양의 pH가 5이하에서는 거의 없었다. pH 3.0인 산성비(황산:질산=2:1, $1,200mm\;year^{-1}$)의 유입에 따른 H이온의 유입은 $12kg\;ha^{-1}\;year^{-1}$, 산성비의 토양유입은 S와 N가 각각 128과 $56kg\;ha^{-1}{\cdot}year^{-1}$이었으며, 이를 중화할 수 있는 소석회의 양은 $444kg\;ha^{-1}\;year^{-1}$이지만 실제로 용탈된 염기는 소석회로 사양토 923, 양토 1,731, 식양토 $1,608kg\;ha^{-1}\;year^{-1}$로 추정되었다.