• 한국방재안전학회논문집
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• 제12권2호
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• pp.57-63
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• 2019

서울시에서 2010년부터 2016년까지 발생한 도로함몰 발생 건수는 총 4,737건으로 매년 증가하여 사회문제도 대두되고 있다. 특히 도로함몰은 충적층이 두껍게 분포하는 송파구와 구로구에 집중되어 나타나는데 이는 하수관로 또는 지하철이 통과하는 지역의 지반특성이 큰 영향을 미치기 때문이다. 도로함몰에 대한 대책방안을 수립하기 위해서는 누수가 발생하는 구간에서의 지반특성과 지반거동의 관계를 정확하게 규명하는 것이 필요하다. 이 논문에서는 충적층에 가장 흔하게 나타나는 사질토와 점성토를 대상으로 개별요소법 프로그램 중 하나인 EDEM 프로그램을 이용하여 지층 내 공동의 위치 및 크기를 달리하여 시뮬레이션을 수행하였다. 그 결과 점성토 지반보다 사질토 지반에서 함몰 규모가 크게 발생한 것으로 나타났으며, 점착력이 없는 사질토 지반에서는 지하 공동의 깊이가 깊고 지하 공동의 규모가 증가할수록 도로함몰이 쉽게 발생하는 양상을 보인 반면, 점착력이 있는 점성토 모델에서는 지하 공동의 깊이가 얕을수록 도로함몰이 쉽게 발생하는 양상을 보였다.

• 한국토양비료학회지
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• 제50권2호
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• pp.81-92
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• 2017

Recently, agricultural lands have decreased sharply, which was caused by huge housing site, urbanization, land consolidation, and road construction etc. In particular, Yangju city near Seoul city has the most severe land use change in Korea. Therefore, we analyzed changes of land use, soil properties, and soil information in order to provide the basic soil information and soil management practices in this city. The area of crop cultivated land in Korea (2015) reduced by 12,090 ha compared to ones from the previous year (2014). The paddy field decreased by 25,421 ha but, upland field increased by 13,331 ha. One of the reasons for the reduction of the paddy field was converting paddy field to upland (20,916 ha) > others (3,056) > building (2,571) > public facilities (847) > idle land (217). But, reasons for increase of upland field were switching paddy to upland (20,916 ha) > land developed (634). The main reason of converting paddy field to upland was changing from rice to more profitable speciality crops or pulses. The cropland area (paddy fields, upland, orchard) of Yangju city reduced by 1,412 ha (2015/2014). The ratio of cropland area in each city reduced by 22.9% dramatically compared 2015 to 1999. The paddy fields located in alluvial plains in Yangju city were changed into upland or green house. The drainage classes of soil have been deteriorated because the flows of water were intercepted by road construction and other disturbance to water flows. In particular, paddy fields have been changed to not only upland, orchard, greenhouse cultivation but also to fallow and soil dressing on paddy in Yangju city. To analyze result of soil survey of Yangju city, 858 soil codes (soil phases) were used and the area was 105.17ha. The number of soil series increased from 60 to 65, and that of soil phase increased from 105 to 124. The largest increased area was Noegog soil series. 125.7ha of Neogog soil series was incorporated from the existing Sachon, Yecheon and Eungog soil series. The soil suitability class of paddy field in Ogjung huge housing site of Yangju city was the 4th grade for 32.6% of the area. The soil suitability classes of upland were 2nd and 3rd grade for 72.4% of the area. Farm land with high quality should be conserved by related law.

• 한국농공학회논문집
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• 제59권5호
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• pp.25-30
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• 2017

Hydrologic soil group is one of the important factors to determine runoff potential and curve number. This study was conducted to classify the hydrologic soil groups of Korean soils by considering saturated hydraulic conductivity and depth of impermeable layer. Saturated hydraulic conductivity of Korean soils was estimated by pedotransfer functions developed in the previous studies. Most of paddy soils were classified as D type due to shallow impermeable layer and low saturated hydraulic conductivity in B soil horizon. For upland and forest, soils classified to A and D types increased compared with former classification method because underestimated permeabilities and overestimated drainages were corrected and rock horizon in shallow depth was regarded as impermeable layer. Soils in mountainous land showed the highest distribution in A type, followed by D type. More than 60 % of soils in mountain foot-slope, fan and valley, alluvial plains, and fluvio-marine deposits were classified to D type because of land use such as paddy and upland.

• 한국작물학회지
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• 제47권2호
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• pp.132-136
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• 2002

The rice straw managements are essential for maintaining soil fertility as well as reducing chemical fertilizer application in paddy field. A field experiment was conducted on moderately well draining alluvial paddy soil to investigate the decomposition pattern of rice straw. The mesh bags containing the rice straw harvested in the previous year were placed at soil surface and buried into around 10cm depth and recovered periodically for determining the straw decomposition. Pot experiments were conducted to investigate the fates of N released from $^{15}$ N-labeled rice straw under different levels of N fertilizer application. The overall decomposition patterns of rice straw were similar for the two incorporation depths in transplanted paddy field. The straw incorporated at transplanting date showed weight loss of about 50%, 70% and 90% after 2 months, 5 months, and 2 years, respectively. The decompositions of straw cell wall components showed somewhat different pattern. The decompositions of cellulose and silica were similar to that of dry weight while the decomposition of lignin was slower than that of cellulose and silica. N was released from rice straw 42% and 65 % of the initial N after one month and after five months, respectively. P release was faster than N release. Recoveries of rice straw-$^{15}$ N by rice plants were 10.2, 13.4 and 14.9% in 0, 120 and 240 mg N pot$^{-1}$ , respectively. Soil recoveries of rice straw $^{15}$ N were 17.3, 20.6 and 18.9% in 0, 120 and 240mg N pot$^{-1}$ , respectively.

• 한국토양비료학회지
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• 제30권1호
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• pp.35-40
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• 1997

담수된 논 토양에서는 산소공급의 차단으로 환원상태가 조장되어 메탄가스가 생성되는데, 생성된 메탄은 확산이나 벼 식물체를 통하여 대기로 배출되어 지구온난화 가스로 작용된다. 본 연구는 메탄가스 저감방법을 구명하고자 벼 재배양식별 메탄가스 배출특성을 조사한 결과를 요약하면 다음과 같다. 1. 벼 재배양식에 따른 메탄 배출량은 이앙재배, 담수직파, 건답직파순으로 많았으며 볏짚을 시용한 건답직파의 평균메탄 배출량($mg{\cdot}m^2{\cdot}h^{-1}$)은 10.27, 담수직파는 21.94, 그리고 이앙재배는 24.05였다. 2. 출수기의 시간별 메탄발생 양상은 오전 9시에서 오후7시까지 메탄배출량이 많았으며 밤에는 낮보다 메탄 배출량이 낮았다. 3. 메탄 배출량은 기온과 Eh와 높은 상관을 보였다. 4. 시기별 메탄 배출정점은 유수형성기와 출수기 무렵에 두번 보였다.

• 한국토양비료학회지
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• 제7권1호
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• pp.5-16
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• 1974

경사지(傾斜地) 및 산지(山地)의 특성(特性)과 현재(現在)의 토지이용상황(土地利用狀況)을 파악(把握)하고 그 토양조건(土壤條件)에 알맞는 토지이용(土地利用) 개발(開發)을 추천(推薦)하고져 3개부락(個部落)의 농가(農家)가 다양(多樣)하게 토지(土地)를 이용(利用)하고 있는 저구릉지(低丘陵地)를 중심(中心)으로 하여 조사(調査)한 결과(結果)는 다음과 같다. 1. 잔적토(殘積土) 및 홍적토(洪積土)에 재배(栽培)되고 있는 작물(作物)은 단순(單純)하였고 그 수량(收量)은 낮았으며 따라서 이 지역(地域)의 농민(農民)들은 빈곤(貧困)하였다. 2. 토지이용율(土地利用率)은 58.4%이었으나 이 중(中) 경사지(傾斜地) 경작(耕作)에서는 토양보존(土壤保存)에 대(對)한 고려(考慮)가 없었다. 전체(全體)의 37.2%에 달(達)하는 임지(林地에)는 입목(立木)이 적었으며 토지이용(土地利用) 계획(計劃) 및 관리(管理의) 소홀(疎忽)로 점차(漸次) 황폐화(荒廢化)되여 가고 있었다. 3. 조사지역(調査地域)에서 밝혀진 토양통(土壤統)은 12개(個)이다. 잔적토(殘積土)는 적갈(赤褐)~암갈색(暗褐色)의 양질(壤質)이고, 홍적토(洪積土)는 황적(黃赤)~갈색(褐色)의 식질(埴質)이었으며, 곡간충적토(谷間沖積土)는 암갈색(暗褐色)~회색(灰色)의 양질토(壤質土)로 다양(多樣)했다. 4. 토양반응(土壤反應)은 구릉지(丘陵地)가 pH 5.0~5.2로서 홍적대지(洪積臺地) 기경지(旣耕地) pH 4.7~4.8에 비(比)하여 pH가 높은 편(便)이었으나, 유기물함량(有機物含量)은 반대(反對)로 홍적토(洪積土)가 3.3~3.6%로 구릉지(丘陵地)의 2.6~2.8% 보다 높았다. 염기치환용량(鹽基置換容量)은 8~16me/100gr이며 이는 유기물함량(有機物含量), 점토(粘土) 및 미사함량(微砂含量)과 밀접(密接)한 관계(關係)를 가지고 있다. 5. 토양(土壤)의 특성(特性)에 따라 16개(個) 토지이용적성군(土地利用適性群)으로 나눌 수 있었다. 6. 조사전(調査前) 토지이용(土地利用)과 조사후(調査後) 추천(推薦)된 토양이용(土壤利用)에는 많은 차이(差異)가 보였다. 주(主)로 임지(林地)가 초지(草地), 유실수(有實樹), 과수(果樹) 및 상전(桑田)으로 추천(推薦)되었다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제22권5호
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• pp.1-12
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• 2017

This study reviewed the groundwater policies of USA as a benchmarking for the purpose of improving groundwater polices, regulations, and plans in Korea. Each state of the USA has its own unique groundwater policies. Recently, severe drought in the western parts of the USA resulted in the launch of the California Statewide Groundwater Elevation Monitoring (CASGEM) program. CASGEM classified a total of 515 alluvial groundwater basins of the California State to four prior groups (high, medium, low, and very low prioritization). In Texas, a total of 101 Groundwater Conservation Districts (GCDs) over the state has controlled groundwater pumping amounts in their own management areas and 16 Groundwater Management Areas (GMAs) over the state have directly managed groundwater aquifer. Direct management for aquifers by GMAs would be the most scientific method for groundwater management, which expected to provide water consumers the more advavnced groundwater service. These groundwater management strategies of the USA can be possibly considered in groundwater plans for national and local governmental authorities, which possibly results in more optimal groundwater management in Korea.

• 한국지하수토양환경학회지:지하수토양환경
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• 제22권3호
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• pp.18-26
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• 2017

The increasing frequency of droughts has been increasing the necessity of utilizing subsurface dams as reliable groundwater resources in areas where it is difficult to supply adequate agricultural water using only surface water. In this study, we analyzed the current status and actual conditions of five agricultural subsurface dams as well as the effect of obtaining additional groundwater from subsurface dams operated as one aspect of the sustainable integrated water management system. Based on the construction methods and functions of each subsurface dam, the five subsurface dams are classified into three types such as those that derive water from rivers, those that prevent seawater intrusion, and those that link to a main irrigation canal. The classification is based on various conditions including topography, reservoir location, irrigation facilities, and river and alluvial deposit distributions. Agricultural groundwater upstream of subsurface dams is obtained from four to five radial collector wells. From the study, the total amount of groundwater recovered from the subsurface dam is turned out to be about 29~44% of the total irrigation water demand, which is higher than that of general agricultural groundwater of about 4.6%.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.334-337
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• 2004

Groundwater chemistry in Namwon area, Korea, was investigated to understand the contribution of geochemical processes on groundwater chemistry. For this study, a total of 279 groundwater samples were collected from 93 wells distributed over the study area. Higher concentrations of major ions are generally encountered in the shallow alluvial wells, suggesting that these chemicals are originated from the surface contamination sources. Mass balance analysis based on reaction stoichiometry reveals that the water chemistry is regulated by three major chemical processes: weathering of silicate/ carbonate minerals, input of C1/SO$_4$ salts, and nitrate generating processes. The results show that mineral weathering is the most dominating factor regulating the groundwater chemistry. However, the groundwaters with the higher salt concentration indicate the larger mineral weathering effect, suggesting that some part of the mineral weathering effect is also associated with the anthropogenic activities such as limes applied to the cultivated lands, carbonates (CaCO$_3$) in the cement materials.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 추계 학술발표회
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• pp.1296-1305
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• 2008

In this study, the spatial distribution of depth between alluvial soil and weathered soil of Song-do new city is analyzed using geostatistics. From analysis results, the boundary depth of north-east region is deeper than that of south-west region, and average depth of north-east region is 27.14m and average depth of south-west region is 23.25m. The boundary depth is estimated by ordinary kriging and inverse distance method, and estimated results are almost similarity. So, in Song-do new city, these two method can be used to estimate the boundary depth. The ordinary kriging method is a very useful tool because the more exact analysis of spatial continuity and distribution characteristic is possible.