• 한국농업기계학회:학술대회논문집
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• 한국농업기계학회 1993년도 Proceedings of International Conference for Agricultural Machinery and Process Engineering
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• pp.556-564
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• 1993

The response of salt affected rice soils to salinity reclaimation by flushings and chemical amelioration by lime and gypsum were evaluated . Soils with good drainage system responded well to simple reclimation . The effects of seawater intrusion were reduced efficiently in a very short time. Yields of rice crops recovered to their potential level within one to two seasons of cropping. Soil profile strength was also improved under well drained areas. However, when drainage system was ineffective the problems of salinity and soil strength remained unsolved. Under both condition, water depth management played important role in the survival of rice crop under the sline soil conditions.

• 한국자원리싸이클링학회:학술대회논문집
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• 한국자원리싸이클링학회 2003년도 추계정기총회 및 국제심포지엄
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• pp.44-48
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• 2003

• 한국주조공학회지
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• 제22권3호
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• pp.121-129
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• 2002

According to the investigation of waste $CO_2$ molding sand in the 15 steel foundries in Busan and Gyeong area, about 1 ton of waste $CO_2$ molding sand per ton of steel castings production was produced In order to reduce amount of $Na_2O$, Loss of Boiling (L.O.B), Loss of Ignition (L.O.I), Conductivity and PH which are present in the waste $CO_2$ molding sand below the reclamation effect, more than 50% of elimination for reclamation was required. It was found that the waste $CO_2$ molding sand does not contain a harmful component designated by industrial waste materials. Reclamation of the waste $CO_2$ molding sand was practically achieved by an abrasive-dry reclamation process. According to bench time of the sodium silicate-bonded $CO_2$ molding sand, reduction of compressive strength and surface stability index(S.S.I) become slowdown. Therefore, the reclaimed sand could be allowed the reuse of molding sand in $CO_2$ molding process including core sand.

• 한국토양비료학회지
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• 제23권4호
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• pp.259-267
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• 1990

본(本) 연구는 간척지토양(干拓地土壤)의 숙성화정도(熟成化程度)에 따른 토양(土壤)의 이화학성(理化學性) 변화(變化) 양상(樣相)을 구명(究明)하여 벼 수량증대(收量增大)를 위(爲)한 토양개량(土壤改良)과 관리자료(管理資料)를 얻고져 실시하였다. 1. 광활통의 이앙전(移秧前) 토양(土壤) 및 지하수(地下水) 염농도는 간척(干拓)21년차(年次)에서 각각(各各) 0.29, 1.02%로 염해가 우려(憂慮)되나 33년차(年次)부터는 수도재배(水滔栽培)가 가능(可能)한 함량(含量)이었고, 포승통(浦升統)은 33년차(年次)까지 염해우려와 그 이후(以後)부터는 벼안전재배(安全栽培)가 가능(可能)한 함량(含量)이었다. 2. 토양(土壤)이 숙성화(熟成化) 됨에 따라 입경중(粒徑中) 점토함량(粘土含量), Atterberg limits, 점토활성도(粘土活性度)는 양토양(兩土壤) 공(共)히 부(負)의 상관(相關), 모래함량 및 N-계수(係數)는 정(正)의 상관(相關)을 보였다. 3. 토심별(土深別) 원추저항(圓錐抵抗)은 양토양(兩土壤) 공(共)히 간척(干拓)5년차(年次)까지는 원추관입지수(圓錐貫入指數) $3kg/cm^2$이하(以下)를 보인 반면(反面) 경반시생성(硬盤尸生成)은 광활통 33년차(年次), 포승통(浦升統)은 49년차(年次)부터 나타났으며 그 정도(程度)는 포승통(浦升統)에서 두껍게 생성(生成)되고 있었다. 4. 전단저항(剪斷抵抗)은 경작년수(耕作年數)가 경과(經過)할수록 양토양(兩土壤) 공(共)히 낮아지는 경향(傾向)이며, 마찰저항(摩擦抵抗)은 포승통(浦升統)보다 광활통에서 높아지는 경향(傾向)이었다. 5. 경작년수(耕作年數)가 경과(經過)할수록 양토양(兩土壤) 공(共)히 토양산도(土壤酸度), 유효규산(有效珪酸), 고토(苦土), 가리(加里), 소다, 양(陽)이온 치환용량(置換容量)은 부(負)와 상관(相關), 유기물(有機物), 유효인산(有效燐酸), 석회(石灰), 전질소함량(全窒素含量)은 정(正)의 상관(相關)을 보였다. 또 유기물(有機物) 및 석회함량(石灰含量)은 광활통에서 높았으며 양(陽)이온 치환용량(置換容量)은 포승통(浦升統)에서 매우 높았다.

• The Korean Journal of Ecology
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• 제20권4호
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• pp.275-283
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• 1997

Vertical and temporal characteristics of desalinized reclaimed soil were analyzed from reclaimed coastal land on the western coast of Korea. Of the vertical changes during desalting, pH valuse were the lowest at the topsoil without regard to reclaimation time. The content of C1 were designated as the early period (the first 2-4 years) which decreased exponentially and the later period(the last 5-7 years) which was almost constant, from top to down. In temporal changes of the soil attributes, pH values increased for 5 years and decreased at 6 year after reclamation. Chlorine leaches more rapidly than Na does, K and Ca are constant but Mg increases as time elapsed after reclamation. Sometimes the content of Ca and K in the reclaimed soil are of higher concentration than that of the seawater after reclamation. During desallinization as exemplified by decreasing EC of the soil, Cl and Na are rapidly leached, but K, Ca and Mg are somewhat enhanced. The ration of Na/Cl in the soil equals 1 when the EC registers 5 mmho and then increases dramatically as the EC decreases. Rapid leaching of $Cl^{-}$ elicits an increasing pH valus. The electrostatic balance of the soil is achived by replacement of $Cl^{-}$ with $OH^{-}$ until stationary or until a decreasing pH value is reached again.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2009년도 춘계 학술발표회
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• pp.640-648
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• 2009

Recently the truction of coastal reclaimation work has been extensively implemented in Korea. The Sondo New City is being established on the reclaimed land from the sea, construction companies of metro construction are planing to pull-out the sheet pile for saving the construction cost. In the case of soft marine clay, it is very difficult to pull-out the sheet pile by using the hydraulic hammer difficult. Therefore, the man of the field must be aware of vibration effect to the ground and the structure. For understanding the vibration effect to the ground during subway construction, the model was formulated with 1/25 braced-cut for subway construction. Scott and Iai(1989) proposed the law of the similarity for other experimental conditions. The laboratory model test was conducted under the vibration condition of sheet pile pulling out. The settlement on the ground surface was measured during the shaking table test. The pore water pressure was also monitored in the upper, middle, and lower layers of soil. The field settlement level and the pore water pressure can be predicted by using the results of the laboratory shaking table test.

• The Korean Journal of Ecology
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• 제21권5_3호
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• pp.603-631
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• 1998

Flora and distribution of vascular plants included introduced species of Mt. Nam park in Seoul were investigated from 1997 to 1998. The flora was composed of 112 families, 338 genera, 487 species, 1 subspecies, 60 varieties, 11 forma or 559 taca. Whole taxa of Mt. Nam calculated with the other reports were recorded 125 families, 461 genera, 832 species, 2 subspecies, 115 varieties, 14 forma or 963 taxa. Mt. nam area has lost its properties because of road and promenade construction, several park reclaimation, introduction of foreign species and exotic plants, and so on. The urbanized index (UI) was comparatively high at 18.3%. Eupatorium rugosum which shown high shade tolerance comparatively was occupied dominantly in road sides. The natural ecosystem and biodiversity of Mt. Nam were under threatened by introduced species. DBH mode of Pinus densiflora community was shown bell shape but that of Quercus mongolica was shown reverse J shape, therefore, it will be occupied in the future this area dominantly by Q. mongolica community. However the vegetation of Mt. nam park area are repressing by superior position in their growth of introduced species included R. pseudo-acacia, Ailanthus altissima and E. rugosum, etc.

• 한국농공학회지
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• 제40권6호
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• pp.70-78
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• 1998

The changes of tidal characteristics of Kyonggi-Bay Region after the Large Reclamations in the Inchon Coastal Area have been studied by the numerical modelling. The constructions of Inchon International Airport and Sihwa Seadike were considered as the main reclaimation projects in this region. A two dimensional hydrodynamic model was used for this study, and it was composed in relatively high resolution with curvilinear orthogonal coordinate. As the results, at the Inchon harbor and Palmido, where a deep channel is developed, the semi tidal ranges(Z$_0$) were decreased in 8 cm after the two reclamations. However, the Z$_0$ values in the outside of the deep channel were decreased only in 2~4 cm, so that the tidal changes in the deep channel were greater than in the outside of it. After the reclamations, the maxmum velocity was increased 17% at the Inchon harbor, however it was decreased from 1. 55 m/s to 1.10 m/s at the Palmido. This is because the available area in which the stream may spread out was largely reduced after the reclamations. An Asan-bay region, the Z$_0$ was decreased in 5 cm at the Punyang-man and Asan-man stations located after the reclamations in Inchon coastal area. However the changes of Z$_0$ were very little at the outside of Asan-bay. In Asan-bay, the current velocity and direction were little influenced by the reclamations in Inchon coastal area.