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학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
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연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
이용수
초록· 키워드
오류제보하기
Soils exhibit creep behavior in which deformation and movement proceed under a state of constant stress or load. In Korea, weathered soil is abundant and occupies around one-third of the country. Weathered soil is visually described as a sandy or gravelley soil, but the behavior is quite different from the behavior of usual sand and gravel. In particular, the permeability of weathered soil is similar to sand, but the durability of settlement is similar to clay. Therefore analysis of time-dependent behavior of weathered soil is very important. In this study, Creep tests with weathered soils were carried out under constant principal stress differences of various stress levels which were experimentally obtained by triaxial compression test. The results of these tests showed the creep behavior for which the deformation increased with time, and the results are consistent with phenomenological model by creep equation of Singh-Mitchell.
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참고문헌 (16)
참고문헌 신청
Casagrande, A. / 1951 / Effect of rate of load on the strength of clays at constant water content / Geotechnique 2 (3) : 251 ~ 263
Chung, H. S. / 1991 / A Study on the Creep Characteristics of Marine Clay / Journal of Korean Geotechnical Society 7 (4) : 65 ~ 73
Edward Kavazanjian, Jr. / 1980 / Time-Dependent Deformation Behavior of Clays / Journal of the Geotechnical Engineering Division 106 (6) : 611 ~ 630
G.R. McDowell / 2003 / Creep of granular materials / Granular Matter 5 : 115 ~ 120
Jarosav Fesa / 1992 / Creep of soils and related phenomena / ELSEVIER
Chung, H. S. / 1991 / A Study on the Creep Characteristics of Marine Clay / Journal of Korean Geotechnical Society 7 (4) : 65 ~ 73
Edward Kavazanjian, Jr. / 1980 / Time-Dependent Deformation Behavior of Clays / Journal of the Geotechnical Engineering Division 106 (6) : 611 ~ 630
G.R. McDowell / 2003 / Creep of granular materials / Granular Matter 5 : 115 ~ 120
Jarosav Fesa / 1992 / Creep of soils and related phenomena / ELSEVIER
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