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湛江地区结构性软土的赋存规律及其工程特性

Occurrence and engineering properties of structural soft clay in Zhanjiang area

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【作者】 拓勇飞孔令伟郭爱国谭罗荣

【Author】 TUO Yong-fei,KONG Ling-wei,GUO Ai-guo,TAN Luo-rong (Key Laboratory of Rock and Soil Mechanics, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 430071, China )

【机构】 中国科学院武汉岩土力学研究所岩土力学重点实验室中国科学院武汉岩土力学研究所岩土力学重点实验室 湖北武汉430071湖北武汉430071湖北武汉430071

【摘要】 立足于土体演化的地质背景,以湛江地区第四系下更新统湛江组强结构性软土地层为依托,开展了宏观与微观土工试验研究,探求该区软土赋存规律与其强结构性的内在联系。研究表明,湛江软土是以陆相沉积为主的河控三角洲相(即海陆交互相)沉积层,由于受该区构造运动的强烈影响,该土集多种地质营力的复杂耦合作用而呈现出特殊的沉积特征;胶结作用是该土具有较高的结构强度的根本原因,其强结构性形成机理与当地广泛发育的红土极为相似。

【Abstract】 Based upon geologic background of solum evolvement, aimed to strong structural soft clay strata Zhanjiang Formation lower Pleistocene series the Quaternary system in Zhanjiang area, the research on soil properties, which combines macroscopical mechanics test and microanalysis, has been made, so as to disclose internal relations between occurrence and strong structural characteristic of soft clay in this area. It is shown that Zhanjiang Formation is the deltaic-facies strata controlled by river(interactive marine & continental sedimentation); and its special sedimentation characteristic result from multi-geologic-agent coupling action with strong tectonic movement working on. Fundamentally, agglutination among particles result in the characteristic strong structural strength of this soft clay, and its pedogenic mechanism is extraordinarily similar to that of indigenous laterite.

【基金】 中国科学院武汉岩土力学研究所知识新工程项目(批准号:Q110201)
  • 【文献出处】 岩土力学 ,Rock and Soil Mechanics , 编辑部邮箱 ,2004年12期
  • 【分类号】TU411
  • 【被引频次】67
  • 【下载频次】644
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