岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2014年
4期
849-856
,共8页
王虎%刘红军%张民生
王虎%劉紅軍%張民生
왕호%류홍군%장민생
土力学%粉土%低应力条件%不排水强度%波浪%海底滑坡%黄河三角洲
土力學%粉土%低應力條件%不排水彊度%波浪%海底滑坡%黃河三角洲
토역학%분토%저응력조건%불배수강도%파랑%해저활파%황하삼각주
soil mechanics%silt%low stress condition%undrained shear strength%wave%submarine landslide%Yellow River delta
针对浅层滑坡等海底地质灾害,设计并实施一系列的十字板试验和三轴试验,对低应力条件下典型海洋粉土的不排水强度特性进行研究探讨。试验结果显示:固结度对粉土的十字板强度有明显影响,十字板强度随着超孔隙水压力的升高而降低。剪切应变速率对粉土的固结不排水三轴强度影响很小,而超固结比和剪切围压则影响较大;三轴试验中各个试样都能够达到临界状态,临界状态强度随着超固结比和剪切围压的增大而增大。分析波浪作用下海床土剪切滑动的渐进特性,指出临界状态是滑坡发生时滑带土所能达到的最终状态。采用平均有效应力,对十字板强度和三轴临界状态强度进行归一化处理,两种强度显示较好的一致性,得到低应力条件下海洋粉土的临界强度线。最后,应用所得的临界强度线,对风暴潮作用下黄河水下三角洲粉土海床浅层滑坡及“复活”进行很好地分析和解释。
針對淺層滑坡等海底地質災害,設計併實施一繫列的十字闆試驗和三軸試驗,對低應力條件下典型海洋粉土的不排水彊度特性進行研究探討。試驗結果顯示:固結度對粉土的十字闆彊度有明顯影響,十字闆彊度隨著超孔隙水壓力的升高而降低。剪切應變速率對粉土的固結不排水三軸彊度影響很小,而超固結比和剪切圍壓則影響較大;三軸試驗中各箇試樣都能夠達到臨界狀態,臨界狀態彊度隨著超固結比和剪切圍壓的增大而增大。分析波浪作用下海床土剪切滑動的漸進特性,指齣臨界狀態是滑坡髮生時滑帶土所能達到的最終狀態。採用平均有效應力,對十字闆彊度和三軸臨界狀態彊度進行歸一化處理,兩種彊度顯示較好的一緻性,得到低應力條件下海洋粉土的臨界彊度線。最後,應用所得的臨界彊度線,對風暴潮作用下黃河水下三角洲粉土海床淺層滑坡及“複活”進行很好地分析和解釋。
침대천층활파등해저지질재해,설계병실시일계렬적십자판시험화삼축시험,대저응력조건하전형해양분토적불배수강도특성진행연구탐토。시험결과현시:고결도대분토적십자판강도유명현영향,십자판강도수착초공극수압력적승고이강저。전절응변속솔대분토적고결불배수삼축강도영향흔소,이초고결비화전절위압칙영향교대;삼축시험중각개시양도능구체도림계상태,림계상태강도수착초고결비화전절위압적증대이증대。분석파랑작용하해상토전절활동적점진특성,지출림계상태시활파발생시활대토소능체도적최종상태。채용평균유효응력,대십자판강도화삼축림계상태강도진행귀일화처리,량충강도현시교호적일치성,득도저응력조건하해양분토적림계강도선。최후,응용소득적림계강도선,대풍폭조작용하황하수하삼각주분토해상천층활파급“복활”진행흔호지분석화해석。
A series of the vane shear tests and the triaxial tests investigating the undrained shear strength of typical ocean silt under low stress conditions were carried out to understand the submarine geological hazards such as shallow landslide. It was found that the degree of consolidation affected the vane shear strength of silt and the vane shear strength decreased as the excess pore pressure increased. The triaxial undrained shear strength of silt is affected by the over consolidation ratio and the confining stress level but not by the shear strain rate. All samples reached the critical state in the triaxial tests and the shear strength at the critical state increased with the increase of the over consolidation ratio and the confining pressure. The vane shear strength and the triaxial undrained shear strength at critical state were normalized using the mean effective stress and the good consistency was found between them. The critical strength line of marine silt under low stress condition was obtained,which explained the reactivation of the submarine landslide by the storm wave in the Yellow River delta.