• Journal of Plant Biology
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• 제33권4호
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• pp.285-292
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• 1990

In order to elucidate the formation of reaction tissues during the transition from primary to secondary growth, the developmental anatomy was conducted in the first internode of Ginkgo biloba seedling in horizontal position. The righting of the horizontal first internode took place at the middle portion and gradually proceeded to the base during the primary growth. Reaction tissues were formed corresponding to the righting movement in the horizontal first internode. During the transition from primary to secondary growth, compression wood was gradually developed on the lower side only. The anatomical features of compression wood also extended longitudinally to the lower side of the vertical portion where it coincided with the lower side of the horizontal first internode occurs acropetally from basal to apical portion. Eventually, some of the anatomical features of compression wood occurred at the primary growth. And the typical compression wood is gradually established during the secondary growth. On the other hand, the lower side tracheid and ray were longer and higher than those of the upper side in the horizontal first internode. However, difference in the width of ray was not observed between the lower and upper sides.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 기초기술위원회 워크샵
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• pp.53-80
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• 2002

Settlement in the Shallow Foundation are presented. Various practical methods to calculate immediate settlement, consolidation settlement, and secondary compression of the compressive soils under the shallow foundation are summerized. Especially the critical depth for settlement calculation, the contact pressure, the allowable settlement of the shallow foundation are recommended.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1999년도 봄 학술발표회 논문집
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• pp.373-380
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• 1999

Consolidation settlements of soft clay are often large and potentially damaging to the structures. Currently, large-scale construction projects for airport and harbor etc. are in progress in Korea and many of these structures will be constructed on thick and soft clay layers. For this kind of ground condition, evaluation of consolidation settlement is required at every design and construction stages, and the magnitude of secondary compression appears to be larger than expected. Generally, the magnitude of secondary compression is evaluated by laboratory and in-situ consolidation tests or by empirical $C_{a/}$ $C_{c}$, relationship. The use of empirical value $C_{a/}$ $C_{c}$ may be economical, fast and powerful tool in estimating secondary consolidation settlement. However, the databases of the $C_{a/}$ $C_{c}$, for typical soft clays in Korea are insufficient. The purpose of this study is to investigate the relationship of $C_{a/}$ $C_{c}$ on marine clay near the southern sea in Korea. A series of incremental loading consolidation tests with measurement of pore water pressure were performed. It was found that the $C_{a/}$ $C_{c}$ of undisturbed marine clay is 0.0397. This value is similar to that proposed by Mesri and Castro(1987) on inorganic clay and silt. and silt. and silt.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.1086-1093
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• 2005

In soft ground, consolidation settlement is mainly consider. The primary consolidation settlement which is the time when the excess pore water pressure is completely dispersed and the secondary consolidation settlement which follows. Recently as the depth of consolidation layer increases the consideration of not only the primary consolidation settlement but also of the secondary consolidation settlement becomes a very important element. But up to the present there were only a few in-depth study of the secondary consolidation settlement performed. At present there are a lot of methods available when it comes to the improvement of soft soil. In this study, Preloading Method which is the most commonly used soft soil improvement method locally was used in order to investigate the method for the reduction of secondary consolidation settlement. The objective of this study is to determine the amount of preloading required to reduce secondary consolidation settlement and to determine whether secondary consolidation settlement using standard consolidation test.

• Geomechanics and Engineering
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• 제16권2호
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• pp.125-140
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• 2018

Tianjin, which is located on the west shore of the Bohai Sea, is part of China's Circum-Bohai-Sea Region, where very weak clay is deposited. From the 1970s to the early $21^{st}$ century, Tianjin marine clay deposits have been the subject of numerous geotechnical investigations. Because of these deposits' geological complexity, great depositional thickness, high water content, large void ratio, excessive settlement, and low shear strength, the geotechnical properties of Tianjin marine clay need to be summarized and evaluated based on various in situ and laboratory tests so that Tianjin can safely and economically sustain more infrastructure in the coming decades. In this study, the properties of Tianjin marine clay, especially its consolidation properties, are summarized, evaluated and discussed. The focus is on establishing correlations between the geotechnical property indexes and mechanical parameters of Tianjin marine clay. These correlations include the correlations between the water content and the void ratio, the depth and the undrained shear strength, the liquid limit and the compression index, the tip resistance and the constrained modulus, the plasticity index and the ratio of undrained shear strength and the preconsolidation pressure. In addition, the primary consolidation properties of Tianjin marine clay, such as the intrinsic compression line (ICL), sedimentation compression line (SCL), compression index, $C_c$, coefficient of consolidation, $C_v$, and hydraulic conductivity change index, $C_{kv}$, are evaluated and discussed. A secondary consolidation property, i.e., the secondary compression index, $C_a$, is also investigated, and the results show that the ratio of $C_a/C_c$ for Tianjin marine clay can be used to calculate $C_a$ in secondary consolidation settlement predictions.

• 한국지반공학회지:지반
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• 제14권1호
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• pp.5-14
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• 1998

쓰레기 매립지의 장기 침하 메카니즘은 일반적인 홀의 거동과는 달리 생물학적인 분해에 의해서 크게 영향을 받는다. 본 논문에서는 쓰레기 매립지의 장기 침하량(역학적 이차침하량과 분해에 의한 이차침하량)을 예측하기 위하여 두 식이 사용되었다. 역학적 이차침하는 변형률-대수 시간에서 선형적인 관계를 갖는다고 가정하였다. 분해에 의한 침하를 평가하기 위하여, 분해 가능한 쓰레기 고형물의 용액화에 관련된 일차반응기작으로 모사되는 가수분해 과정을 고려한 모델을 숙성된 (aged) 쓰레기로 충진된 Lysimeter 침하자료에 적용하였다. 본 연구에서는 분해과정 가운데 쓰레기 고형물의 용액화로 말미암아 유발되는 침하를 효과적으로 모사할 수 있는 간단한 수학적 모델을 제안하고자 하였다.

• 한국철도학회논문집
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• 제19권2호
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• pp.195-203
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• 2016

최근 경부고속철도 2단계와 호남고속철도에 적용된 콘크리트궤도는 초기 건설비는 기존 자갈궤도에 비하여 불리하나, 유지관리비용은 유리한 것으로 검토되었다. 이와 같은 이유로 콘크리트궤도는 일반철도 신설구간을 중심으로 점점 더 적용구간이 늘어나고 있는 실정이다. 그러나 콘크리트궤도의 가장 큰 문제점 중의 하나는 침하로 인한 궤도 보수와 관계된 문제이다. 궤도의 하부 노반침하 및 이로 인한 궤도 안정성 저하는 콘크리트궤도의 가장 큰 단점이고, 고속철도 설계기준에는 허용잔류침하량을 25mm로 제시하고 있다. 콘크리트궤도의 안정성을 위해서는 2차 압축침하량을 기준치 이내로 관리하여야 한다. 본 연구에서는 2차 압축침하에 대한 이론을 토대로 연약지반의 2차 압축지수 및 연약지반 층의 두께 그리고 궤도수명에 따른 2차 압축침하량을 산정하여 궤도구조 선정에 활용하도록 제시하였다. 또한 국내 연약지반의 2차 압축계수의 확률분포 특성을 분석을 통하여, 콘크리트궤도 부설이 불가능한 지역이 10% 이상 나타남을 알 수 있었다.

• 한국지반공학회지:지반
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• 제10권4호
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• pp.167-180
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• 1994

사전압밀된 포화점토의 응력이력이 2차압밀특성에 미치는 영향 및 Bjerrum모델이 과압밀점토의 2차압밀침하추정에 적용가능한지를 실험적으로 파악하기 위하여 재성형점토를 이용하여 재하-제하 및 재하-제하-재재하 응력이력의 조건에서 일련의 장기압밀시험을 실시하였다. 실험결과에 의하면 과압밀점토의 2차압밀침하는 전반부에서 응력이력의 영향을 받고 전반부의 2차압밀계수 Cn은 OCR(선행 압밀하중 Pcy재재하하중 Pr), 최대 OCR(선행압밀하중 Pcy제 하시의 하중 Pu)과,제하시간에 의존하며 과압밀비 증가에 따라 감소한다. 또한 2차압밀후반부 의 2차압밀계수 C.2는 OCR의 영향을 받으며 과압밀비 증가에 따라 감소한다. 최종적으로 실험 결과와 Bjerrum모델을 비교분석한 결과 임의 응력이력범위를 벗어나면 과압밀점토에서 Bjerrum모델의 적용은 가능하다.

• 한국지반공학회논문집
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• 제15권6호
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• pp.87-98
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• 1999

연약지반에서의 압밀침하는 종종 구조물에 큰 피해를 미친다. 최근 국내에서는 대규모 프로젝트들이 계획 혹은 진행중인데, 이들 구조물들은 두꺼운 연약지반상에 건설되므로 설계나 시공에 있어서 각 단계별 정확한 압밀침하량 예측이 필요하다. 특히, 이러한 연약지반상의 이차압밀은 전체 압밀침하량에서 상당량을 차지하게 된다. 일반적으로 이차압밀은 실내 혹은 현장압밀시험을 통해 산정된다. 경험적인 $C_a/C_c$의 비는 이차압밀량을 예측하는데 있어서 경제적이고 효율적인 수단이 될 수 있을 것이나, 국내의 $C_a/C_c$는 그 데이터 베이스가 매우 부족한 실정이다. 본 연구에서는 간극수압을 측정하는 단계재하 압밀시험을 이용하여 남해안 해성점토에 대한 $C_a/C_c$의 비를 0.397로 제시하였다.

• Journal of the Korean Wood Science and Technology
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• 제9권1호
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• pp.1-12
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• 1981

The structure of spiral thickenings, particulary the appearance, arrangement and orientation of thickenings in compression wood of Torreya nucifera, were studied in detail by light and polarizing microscope, scanning and transmission electron microscope. The results obtained are as follows: (1) Using the inclined sections at an angle of 45 degrees to the fiber axis, it seems that we can not only observe the more accurate transverse view of the thickenings but also investigate the formation of their thickenings. (2) Generally 2-4 pieces of thickenings are projected to the cell lumen as nipple-like appearance in transverse section and are as frequent, well developed, forming pair and have the rope-like appearance in radial surface. (3) The secondary wall of early wood is composed of 3 layers (S1, S2, S3) and orientation of thickening appears S helix but that of late wood is of 2 layers (S1, S2) and that orientation shows Z helix. Above two regions are demaracted at several tracheid cells from the growth ring boundary. (4) Orientation of thickening seems to be a element showing the characteristics of compression wood in Torreya nucifera. (5) It believes that the thickenings of compression wood are integral part of the S3 in early wood tracheids and of the S2 in late wood and have the same orientations as the inner-most microfibrils in these layers. (6) Thickening and cavities seem to be not formed together in a secondary cell wall of same tracheids.