河南城建学院学报
河南城建學院學報
하남성건학원학보
JOURNAL OF PINGDINGSHAN INSTITUTE OF TECHNOLOGY
2014年
5期
9-11
,共3页
膨胀土%蠕变%非线性%应变%应力
膨脹土%蠕變%非線性%應變%應力
팽창토%연변%비선성%응변%응력
expansive soil%creep%non-linear%strain%stress
针对合肥地区非饱和膨胀土进行单轴压缩蠕变试验,根据应变-时间关系曲线,探讨该区非饱和膨胀土的蠕变特性。试验结果显示:非饱和膨胀土蠕变经历两个阶段,即瞬时弹性蠕变阶段和稳定蠕变阶段。瞬时弹性阶段时间比较短,蠕变快,很快进入蠕变稳定阶段,蠕变稳定阶段持续时间很长。在相同含水率情况下,应力作用值越大,瞬时弹性蠕变量越大,稳定蠕变阶段时间越久;在相同应力作用下,含水率越大,瞬时弹性蠕变量越大。在40 kPa的小应力作用下,应变-时间呈线性关系;在100 kPa、200 kPa的较大应力作用下,应变-时间呈非线性关系,拟合函数为对数函数。
針對閤肥地區非飽和膨脹土進行單軸壓縮蠕變試驗,根據應變-時間關繫麯線,探討該區非飽和膨脹土的蠕變特性。試驗結果顯示:非飽和膨脹土蠕變經歷兩箇階段,即瞬時彈性蠕變階段和穩定蠕變階段。瞬時彈性階段時間比較短,蠕變快,很快進入蠕變穩定階段,蠕變穩定階段持續時間很長。在相同含水率情況下,應力作用值越大,瞬時彈性蠕變量越大,穩定蠕變階段時間越久;在相同應力作用下,含水率越大,瞬時彈性蠕變量越大。在40 kPa的小應力作用下,應變-時間呈線性關繫;在100 kPa、200 kPa的較大應力作用下,應變-時間呈非線性關繫,擬閤函數為對數函數。
침대합비지구비포화팽창토진행단축압축연변시험,근거응변-시간관계곡선,탐토해구비포화팽창토적연변특성。시험결과현시:비포화팽창토연변경력량개계단,즉순시탄성연변계단화은정연변계단。순시탄성계단시간비교단,연변쾌,흔쾌진입연변은정계단,연변은정계단지속시간흔장。재상동함수솔정황하,응력작용치월대,순시탄성연변량월대,은정연변계단시간월구;재상동응력작용하,함수솔월대,순시탄성연변량월대。재40 kPa적소응력작용하,응변-시간정선성관계;재100 kPa、200 kPa적교대응력작용하,응변-시간정비선성관계,의합함수위대수함수。
The expansive soil’ s creep characteristics are explored based on the uniaxial compression creep test of unsaturated expansive soil in Hefei area, combining the strain-time curve. The test results show that the ex-pansive soil creep undergoes two different stages: the instantaneous elastic creep stage and the steady creep stage. At the same moisture content, stress is greater, the greater the instantaneous elastic creep lasts, the longer steady creep stage time is;under the same stress, the higher the moisture content, the greater the in-stantaneous elastic creep is. In the same moisture content condition, when stress is greater, the instantaneous elastic creep is greater, steady creep stage time is longer;in the same stress condition, when moisture content is higher, the instantaneous elastic creep is higher. Under the action of stress such as 40 kPa, strain-time is linear;under the action of stress such as 100 kPa or even 120 kPa, strain-time relationship is non-linear, the fitting function is logarithmic function.