• 한국농공학회논문집
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• 제53권4호
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• pp.21-27
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• 2011

Soil stress distribution under loading is one of the important problems in civil engineering. Many models have been proposed to interpret the stress distribution in soil and most models assume that the soil is homogeneous and isotropic. Therefore, the actual stress distribution may be different. In addition, With the increase of the top load, soil stress does not increase linearly. In this study, vertical stress changes in sandy soil according to top load increase were measured through experiments. Experimental results, vertical soil stress due to top load increase showed an initial nonlinear behavior and when the load increases to some extent, vertical soil stress showed a linear behavior. ${\alpha}$ value obtained by existing theories always 1.00. But, ${\alpha}$ value by experiment was observed from 0.91 to 1.22 and ${\alpha}$ value was increased with increasing distance from the loading plate.

• 한국환경생태학회지
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• 제14권1호
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• pp.38-45
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• 2000

강원도 고성군 죽왕면과 토성면 일대의 소나무군락을 대상으로 1996년 4월에 발생한 산화에 따른 산림환경변화가 토양의 이화학성에 미치는 영향을 구명하기 위하여 비산화지역(NF) 산화후 비벌채지역(FNC), 산화후 벌채지역(FC) 및 산화후 조림지역(FCP)으로 분류하여 토양의 특성을 분석하였다. 전조사지역의 토성은 사질식양토이었고, 토양의 입경조성을 비교하면 비산화지역은 표토의 모래함량이 심토보다 낮았고, 점토함량은 높았지만 산화지역은 모두 표토의 모래함량이 점토에 비해 높았다. 토양공극 분포 중 전공극량은 지역별로 큰 차이가 없었으나, 조공극량과 투수성은 비산화지역 ＞ 산화후 비벌채지역 ＞ 산화후 조림지역 ＞ 산화후 벌채지역 순이었고, 세공극량과 가비중은 반대의 경향을 나타내었다. 이는 산화에 따른 산림환경변화로 지피식생이 제거되어 토양침식이 가속화되면서 토양 내 수분함유능력의 지표인 토양공극과 투수성에 큰 영향을 주면서 토양물리성을 악화시키고 있는 것으로 판단된다. 토양 pH는 비산화지역과 산화후 비벌채지역이 산화후 벌채지역과 조림지역보다 표토 및 심토 모두 높게 나타났다. 유기물함량 및 전질소함량 변화는 표토와 심토 모두 비산화지역＞ 산화후 비벌채지역＞ 산화후 조림지역＞ 산화후 벌채지역 순이었다. 양이온치환용량 및 치환성 양이온($K^{+}$ , $Na^{+}$ /, $Ca^{2+}$, $Mg^{2+}$)함량 변화는 모두 표토가 심토보다 높았으며, 지역별로는 비산화지역＞ 산화후 비벌채지역＞ 산화후 조림지역＞ 산화후 벌채지역 순으로, 이는 산화후 표토층의 침식으로 지력이 악화된 결과로 사료된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1997년도 가을 학술발표회 논문집
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• pp.189-196
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• 1997

• 한국유기농업학회지
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• 제24권4호
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• pp.719-733
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• 2016

본 논문은 앞그루작물 재배 시 형성된 이랑을 재활용하여 다음 뒷그루작물을 무경운으로 재배할 경우 토양의 이화학성과 생육 및 수량에 미치는 영향을 구명하고자 추진한 연구 결과의 일부이다. 토양에서 경운 후 시간의 경과에 따른 토양 입자 크기의 분포를 조사한 결과 관행경운과 무경운 토양 입자는 공히 입상구조(granular structure)를 이루고 있었다. 무경운 토양의 입자 크기 2 mm 이상의 분포는 무경운 토양이 경운 토양에 비하여 표토와 심토 공히 증가 되었다. 그리고 내수성입단 0.25 mm 이상 0.5 mm 이하와 0.5 mm 이상 1 mm 이하, 1 mm 이상의 대입단 분포는 경운과 무경운 1년차 토양에서 유의적인 차이가 없었으나, 무경운 2년차에서는 입단의 크기별로 각각 8.2%, 4.5%, 1.7%로 경운과 무경운 1년차에 비하여 유의적인 증가를 보였다. 관행 경운 토양 표토의 용적밀도 $1.10MG\;m^3$이 무경운 1년차에서 $1.30MG\;m^3$으로 증가 되었으나, 무경운 2년차는 $1.14MG\;m^3$, 무경운 3년차는 $1.03MG\;m^3$으로 용적밀도가 감소되었으며, 심토도 같은 경향이었다. 따라서 용적밀도와 정(+)의 상관이 있는 고상율은 표토와 심토 공히 무경운 1년차에서 관행 경운 토양에 비하여 증가되었으나, 무경운 2년차와 3년차는 감소되었다. 용적밀도 및 고상율과 부(-)의 상관관계가 있는 공극율은 경운 토양 58.5%가 무경운 1년차는 51%로 8.5% 감소되었으나, 무경운 2년차는 56.9%, 무경운 3년차는 61.2%로 증가되었으며, 심토도 같은 경향이었다. 공극율과 정(+)의 상관관계가 있는 기상율은 관행경운 토양에 비하여 무경운 1년차는 감소되었으나, 무경운 2년차와 3년차에서는 증가되었다. 그리고 기상과 함께 공극율을 결정하는 액상율은 경운 표토 24.2%가 무경운 1년차는 28.3%로 증가되었으나, 무경운 2년차는 23.4%, 무경운 3년차는 18.3%로 현저하게 감소되었으며, 심토도 같은 경향이었으나, 심토의 액상율은 표토에 비하여 증가되었다.

• 한국조경학회지
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• 제27권5호
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• pp.107-113
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• 2000

The purpose of this study is to investigate the effects of soil amendments for reducing soil compaction at heavy traffic area in golf course. Major results of this research are summarized at follows: 1. In the Lab. experiment, the porosity was improved significantly when the materials, such as peatmoss, charcoal, and tire chip mixtures were used respectively. Especially mixture of sand and 20% peatmoss showed higher effectiveness (10%) in porosity, comparing with ordinary sand. This soil mixture(sand 80%+peatmoss 20%) was observed the best in water retention, soil hardness and hydrauric conductivity. 2. In the greenhouse experiment, traffic pressure was given 7 times a day on several combination of mixture treatments to see the top dry weight. The soil mixture of 20% peatmoss showed the highest in the top dry weight. When the more traffic pressure(15 time/day) were given on the different treatment, the top dry weight was significantly reduced. However, the mixture of 20% peatmoss also had the least influence on this type of heavy traffic. 3. In the field experiment, the soil amendments were treated in traffic area f golf course, and observed at 30days, 60days, 90days, 120days after treatment. Visual turf quality(color), root length and soil compaction were compared to those of control. As a result, overall treatments with soil amendments were effective, which showed better turf quality and less soil compaction. 4. In the field test, physical characters of soil (such as soil hardness and hydrauric conductivity) in sand+tire chip+peatmoss(60:20:20, %, v/v) treatment was significantly improved. Also in the slow increasing of traffic, the soil compaction was the most effective in reducing soil hardness.

• 한국토양비료학회지
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• 제48권3호
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• pp.194-204
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• 2015

Six study sites in Gumi, Goryeong in Gyeongbuk province and Naju in Jeonnam province were selected to investigate soil properties of poorly drained horizons in paddy soils. The horizons were re-established layers which were parent material layers originated from fluvial deposits. Topsoil layers were differentiated from piled parent materials while soil structure of the topsoil layer was massive with striated microstructure. Compaction at soil re-establishment and a lack of structure and aggregate development in these soils may cause the limitation of vertical water movement and result in poorly drained horizons. Soil samples were taken from paddy fields with top soils of sandy loam, silt loam and silty clay loam and re-established soils of coarse and fine texture. The samples were taken from each horizon for the analyses of soil chemical and mineral properties. Soils with re-established soils of coarse texture had greater amounts of sands from top soil texture distributions, while soils with fine texture had greater amounts of silts. Chemical properties of top soils were analyzed from rice cultivated soils at the time of re-establishments and one year after the re-establishments. The coarse texture of the re-established horizons decreased in EC values from 0.23 to $0.11(dS\;m^{-1})$, available phosphate values from 112 to $54(mg\;kg^{-1})$, and exchangeable Ca values from 6.6 to $4.9(cmol_c\;kg^{-1})$. On the other hand, soils with fine texture showed decrease only in pH and exchangeable Ca values. Especially, organic matter and available phosphate contents showed heterogeneous distributions from each horizon. This result may be caused by mixture of plough layer and subsurface layer during and consolidation. Hydraulic conductivity values were low at the boundaries of top soil and parent material layers except SL/coarse soil. Soil microstructure was massive structure without soil clods or pores and showed striated structure. Therefore, re-established paddy fields with fluvial deposits as parent material layers showed limited vertical movements of soil water because of occurrence of compacted layers and less-development of soil clods and aggregates.

• Coupled systems mechanics
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• 제3권4호
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• pp.367-384
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• 2014

The study deals with the physical modeling of a typical single storeyed building frame resting on pile foundation and embedded in cohesive soil mass using the finite element based software SAP-IV. Two groups of piles comprising two and three piles, with series and parallel arrangement thereof, are considered. The slab provided at top and bottom of the frame along with the pile cap is idealized as four noded and two dimensional thin shell elements. The beams and columns of the frame, and piles are modeled using two noded one dimensional beam-column element. The soil is modeled using closely spaced discrete linear springs. A parametric study is carried out to investigate the effect of various parameters of the pile foundation, such as spacing in a group and number of piles in a group, on the response of superstructure. The response considered includes the displacement at the top of the frame and bending moment in columns. The soil-structure interaction effect is found to increase the displacement in the range of 38 -133% and to increase the absolute maximum positive and negative moments in the column in the range of 2-12% and 2-11%. The effect of the soil- structure interaction is observed to be significant for the type of foundation and soil considered in this study. The results obtained are compared further with those of Chore et al. (2010), wherein different idealizations were used for modeling the superstructure frame and sub-structure elements (foundation). While fair agreement is observed in the results in either study, the trend of the results obtained in both studies is also same.

• 한국농공학회:학술대회논문집
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• 한국농공학회 1999년도 Proceedings of the 1999 Annual Conference The Korean Society of Agricutural Engineers
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• pp.447-453
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• 1999

Salt accumulation is one of themajor problems in soils under protected cultivation . Since protected cultivation does not have rainfall or excessive irrigation, salt accumulaiton inthe soils is inevitable. In this study, characteristics of salt accumulation in soil column were ivestigated, and a salt-extracting method was tested to see its effectiveness. The results showed that the concentration of salt in top soil layers increased and electrical conductivity as thesalt concentration decreased especially in the top soil layer .When extraction medium was applied.

• 한국토양비료학회지
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• 제48권6호
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• pp.658-665
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• 2015

Temporal and spatial variation of soil moisture is important for understanding patterns of climate change, for developing and evaluating land surface models, for designing surface soil moisture observation networks, and for determining the appropriate resolution for satellite-based remote sensing instruments for soil moisture. In this study, we measured several soil moistures in upland soil using Advanced Microwave Scanning Radiometer 2 (AMSR2) Soil Moisture Content (SMC) during eight-month period in Chungbuk province. The upland soil moisture properties were expressed by simple statistical methods (average, standard deviation and coefficient of variation) from the monthly context. Supplementary studies were also performed about the effect of top soil texture on the soil moisture responses. If the results from this study were utilized well in specific cities and counties in Korea, it would be helpful to establish the countermeasures and action plans for preventing disasters because it was possible to compare with the relationship between soil moisture and top soil texture of each region. And it would be the fundamental data for estimating the effect of future agricultural plan.

• 원예과학기술지
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• 제32권2호
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• pp.133-141
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• 2014

Due to limited supplies and expensive importing costs, it is a goal to replace overseas peat with local soil amendments in turf industry of Korea. The study was initiated to compare the performances of five domestic and imported organic soil amendments (OSAs) on establishment characteristics and to provide basic information for root zone composition on sports turf design and construction. The study was conducted in Kentucky bluegrass (Poa pratensis L., KB) under greenhouse conditions from March to June in 2008. A total of 25 treatments of OSA + sand were prepared. These amendments were Berger Peat (OMA), Eco-Peat (OMB), G1-Soil (OMC), Premier Peat (OMD), and Supersoil I (OME). Significant differences were observed in establishment vigor, seedling emergence, and top growth. Results varied depending upon the type of OSAs and their rates in rootzone mixtures. OMA reached over 70% in establishment vigor in 5 WAS (weeks after seeding). OMC produced a maximum vigor of approximately 60% in 6 WAS. The OME amendment, however, showed poor performance lower than 30% in establishing KB turf until 8 WAS. There were considerable variations of top growth, being 3.8 to 14.5 cm. Greater differences in top growth resulted from OME mixtures. Shoot growth orientation in KB is also influenced by OSAs. In general, optimum mixing rate was considered as 10 to 20% for establishment vigor and 20 to 40% for top growth. Considering overall responses to establishment vigor, seedling emergence, and shoot growth, both local OMC and overseas OMD are considered as the useful soil amendments applicable for sports turfs. Domestic OME amendment would be applied for a low maintenance turfs such as rough and utility areas due to greater shoot growth. Information on these amendments would be of practical use for sports turf design and construction. Repeated experiments and field performance test are required to evaluate these OSA effect on other major turfgrass species and also to determine local OSA as imported peat substitute.