포화점토가 보오링공에서 불교란시료로써 채취되면, 부의 간극수압이 체적팽창을 억제한다. 이 점토시료에는 지반중에서 작용한 평균주응력이 등방적으로 작용하며, 이 평균주응력은 수직응력보다 작고, 수평응력보다 크다. 그러므로 시료는 비배수조건하에서 수직으로 늘어나고, 수평으로 수축하게 된다. 통상적인 압밀시험은 이와 같이 변형된 시료를 그대로 사용하여 압밀링 크기와 똑같이 성형한 후 수행한다. 따라서 지반중의 유효상재압이 재하되면, 이 압력이 수평응력보다 크기 때문에 압밀량이 늘어나게 된다. 즉 압밀시험공시체는 현장의 압밀거동을 정확하게 나타내지 못하고 항상 아래에 위치하게 된다. 이 논문에서는 상기와 같은 시료변형의 영향을 고려하여, 압밀시험 공시체에 유효상재압이 재하되었을때 수평방향으로 비배수 변형하여 압밀링 내경에 밀착해도록 하였다. 그리고 제안하는 시험법의 적용성과 결과를 통상적인 압밀시험결과와 검토하였다.
포화점토가 보오링공에서 불교란시료로써 채취되면, 부의 간극수압이 체적팽창을 억제한다. 이 점토시료에는 지반중에서 작용한 평균주응력이 등방적으로 작용하며, 이 평균주응력은 수직응력보다 작고, 수평응력보다 크다. 그러므로 시료는 비배수조건하에서 수직으로 늘어나고, 수평으로 수축하게 된다. 통상적인 압밀시험은 이와 같이 변형된 시료를 그대로 사용하여 압밀링 크기와 똑같이 성형한 후 수행한다. 따라서 지반중의 유효상재압이 재하되면, 이 압력이 수평응력보다 크기 때문에 압밀량이 늘어나게 된다. 즉 압밀시험공시체는 현장의 압밀거동을 정확하게 나타내지 못하고 항상 아래에 위치하게 된다. 이 논문에서는 상기와 같은 시료변형의 영향을 고려하여, 압밀시험 공시체에 유효상재압이 재하되었을때 수평방향으로 비배수 변형하여 압밀링 내경에 밀착해도록 하였다. 그리고 제안하는 시험법의 적용성과 결과를 통상적인 압밀시험결과와 검토하였다.
When a saturated clay is sampled from a borehole in an undisturbed manner, the exerted negative pore water pressure restricts the volume expansion. The vertical and horizontal stresses to which the clay was subjected in the ground are smaller and larger than this isotropically confining stress equiv...
When a saturated clay is sampled from a borehole in an undisturbed manner, the exerted negative pore water pressure restricts the volume expansion. The vertical and horizontal stresses to which the clay was subjected in the ground are smaller and larger than this isotropically confining stress equivalent to the mean principal stress in the ground, respectively. Therefore the sample expands vertically and shrinks laterally under an undrained condition. In the ordinary consolidation test, the sample thus deformed is trimmed to fit the inside of the consolidometer ring. Thus, the specimen generates larger consolidation displacement due to confining larger horizontal stress when in-situ effective pressure is loaded. The specimen does not reproduce the in-situ consolidation behavior, In this paper, considering sample deformation, the test specimen is made to expand laterally to fit the inside of the ring in the undrained manner when the in-situ effective pressure is loaded. And applicability of this proposed test procedure was verified; results from the conventional consolidation test procedure are also discussed.
When a saturated clay is sampled from a borehole in an undisturbed manner, the exerted negative pore water pressure restricts the volume expansion. The vertical and horizontal stresses to which the clay was subjected in the ground are smaller and larger than this isotropically confining stress equivalent to the mean principal stress in the ground, respectively. Therefore the sample expands vertically and shrinks laterally under an undrained condition. In the ordinary consolidation test, the sample thus deformed is trimmed to fit the inside of the consolidometer ring. Thus, the specimen generates larger consolidation displacement due to confining larger horizontal stress when in-situ effective pressure is loaded. The specimen does not reproduce the in-situ consolidation behavior, In this paper, considering sample deformation, the test specimen is made to expand laterally to fit the inside of the ring in the undrained manner when the in-situ effective pressure is loaded. And applicability of this proposed test procedure was verified; results from the conventional consolidation test procedure are also discussed.
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제안 방법
The measurement of the extension strain was also made for laboratory constituted clay samples with different plasticities consolidated from slurry in a cylindrical mold when they were removed from the mold. Based on this measurement, several series of consolidation tests using specimens with smaller diameter than the inside diameter of consolidometer ring trimmed from these laboratory constituted samples were conducted. Test results were compared with the ordinary standard consolidation test results.
대상 데이터
5 cm high. Five specimens were prepared and were loaded in the consolidometer ring of 10 cm of inside diameter from the preconsolidation pressure of 39.2 kPa to 156.9 kPa (1.6 kgfecm2) at the load increment ratio of unity.
01 mm. Measurements were made at Obiraki, northwest region in Osaka city, and Neyagawa alluvium plain, Osaka prefecture. Results are shown in Table 1, in which data previously obtained by one of the authors (Takada and Hamada, 1993) at Suminoe, south-west region in Osaka city, are also presented for reference.
Clay samples were prepared by consolidating slurry clays remolded with water so that the water content was around twice the liquid limit. Two seabed clays passing the 0.425 mm sieve collected from Osaka bay area, N105 and H77, and the mixture of H77 and kaolinite clay powder, HK57, were used. Their liquid limits and plastic limits are shown in Table 2.
참고문헌 (5)
lnterpItation and application ofground survey and soil test results (1998), Japanese Geotechinical Society, pp.229-233 (in Japanese)
Kim J. and Takada N. (2001), 'Consolidation test method to reflect sample deformation due to stress release', Journal of JSCE, No. 680 / III-55, pp.263-268 (in Japanese).
Kim J. (2003), Q&A. Korean Geotechinical Society, Vol.19, No.5, pp.55-58
Takada N. and Hamada T. (1993), 'Measurement of deformation of clay sample after sampling', Proc. of annual convention of JSCE, IIl-456 (in Japanese)
Recommendation Design of Building Foundation (1988), Architectural Institute of Japan, pp.137-138 (in Japanese)
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