共查询到19条相似文献，搜索用时 734 毫秒
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低能量强夯法加固粉质黏土地基试验研究 总被引：5，自引：1，他引：4
结合上海某铁路集装箱中心站地基处理工程,针对其场区上部粉质黏土、下部砂质粉土的地基条件,对低能量强夯法加固此类地基的适用性进行了现场试验研究。通过对夯击过程中超静孔隙水压力随夯击次数、深度、距离的变化规律及在不同性质土层中的增长与消散规律的研究,提出了运用试验手段确定强夯夯击次数、夯点间距、有效加固深度及两遍强夯间隔时间等施工参数的方法。同时,用静力触探试验和标准贯入试验对地基加固的效果进行了检验,结果说明低能量强夯法加固粉质黏土地基的适用性,从而进一步拓宽了低能量强夯法的应用范围。 相似文献
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针对大型炼厂工程地基处理的复杂性,开展了振冲碎石桩的现场试验。利用静力触探试验检测桩体密实度和判别饱和砂土液化。基于旁压试验、标准贯入试验和重型动力触探试验结果,分析了施工前后地基承载力和土体工程特性变化情况。以单桩和复合地基载荷试验结果验证了桩间土、单桩及复合地基的承载性能。研究结果表明,振冲碎石桩对桩长范围的砂土具有明显的挤密效应,工程特性和场地的均匀性在处理后有了明显改善和提高,有效地消除了桩长范围内砂土的液化可能性。静载荷试验结果表明,振冲碎石桩复合地基承载力能达到设计要求;振冲碎石桩对砂土层下卧黏性土层的加固作用不明显,部分深度范围内土体强度降低;当地面以下10 m内不存在厚度大于5 m的软土夹层时,较薄的软土夹层状对挤密加固其余深度的砂土未产生明显影响,对地基承载力影响亦较小。 相似文献
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对长江下游河漫滩地新吹填的松散粉细砂,通过原位监测仪器和跟踪检测,进行了无填料振冲试验、施工技术开发和设计应用。研究了无填料振冲过程中桩周土的超静孔压变化与振冲有效范围,比较了振冲密实前、后桩周土强度变化。针对施工跟踪检测中发现的桩身土局部欠密实问题,分析了缺陷产生原因,提出了解决措施。结果表明,目前规范认为应加填料振冲处理的各种松散粉细砂,只要试验方法得当,及时发现振冲中可能出现的问题并予以解决,吹填粉细砂的无填料振冲密实法是可以大面积应用的。工程试验后提出的振冲设计参数、施工工艺参数和质量控制方法,最终检测显示,工程桩各项指标达到堆场使用要求。 相似文献
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Helical probe tests (HPT) are a quick and economical means for manual field testing of soils to depths of 1.5 m with readings taken at 0.15-m intervals in only 10 min. The equipment is lightweight (only 2 kg) and thus amenable to deploy on initial site reconnaissance explorations, shallow pavement projects, earth retention walls, and/or compaction of fills. Although suitable for use in a variety of geomaterials: sands, silts, clays, and mixed soils, the specific application to residual fine sandy silts and silty fine sands of the Appalachian Piedmont and Blue Ridge geologic provinces is shown here. Existing relationships for converting the measured HPT torque reading to equivalent cone penetration testing (CPT) tip resistances are reviewed, as well as other trends. 相似文献
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Examination of loose saturated sands impacted by a heavy tamper 总被引：1，自引：1，他引：0
This article examines the densification effects on the loose saturated sands impacted by a heavy steel tamper dropped from a great height (i.e., deep dynamic compaction, DDC). This examination was achieved by carrying out a series of piezocone penetration test (CPTu) soundings before and after the DDC impact. The depths at which densification took place ranged from 6.5 to 9.5 m below the ground surface (BGS) after one pass of DDC, and from 7.5 to 11.0 m BGS after two passes. The propagation of the surface waves generated in DDC disturbed the top 0.3–1.3 m soils. Directly below this disturbed layer, it was the most densified soil layer at the depths of 1.7–4.5 m BGS. The existence of the residual soft peat pockets reduced the densification effects substantially. Both the strength and the stiffness of the loose saturated sands were significantly improved after the DDC treatment. After two passes of impact, the liquefiable soils were densified to the level of unliquefiable along with dramatic reduction in liquefaction probabilities when subjected to earthquake motions. 相似文献
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随着海洋岛礁工程的大力推进,吹填珊瑚砂地基的密实加固问题开始备受关注。利用自主研发的室内振冲器开展了珊瑚砂饱和砂土地基的室内振冲模型试验研究,深入分析了振冲过程中动孔隙水压力、水平动土压力等动参量的响应规律,探讨了振冲后沉降变形、相对密实度的变化特征。结果表明：松散珊瑚砂地基的密实度在经过两次双点振冲反复加固后均提升至中密。其中相对密实度在振冲点位处的提升效果较其余位置更为明显,并且中层或深层区域的加固效果优于表层区域。在超孔隙水压力方面,其最大值出现在振冲珊瑚砂地基过程中的贯入阶段,并且在留振开始时出现衰减现象。珊瑚砂地基在振冲器上拔过程中超孔隙水压力发生断崖式下跌。在第2次贯入时,超孔隙水压力比的峰值较首次出现显著下降。超孔隙水压力比等值线云图表明,振冲过程中的超孔隙水压力比等值线呈现平行分布。珊瑚砂浅层水平土压力随振冲器的贯入与拔出均呈现增加态势,深层水平土压力则呈现减少态势。 相似文献
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Elastic modulus and Poisson’s ratio of soils are two important parameters required for safe design of various civil engineering
structures. The elastic modulus and shear modulus of the soils are generally obtained from the resonant column, torsional
shear tests and geophysical methods. Though, from these parameters the Poisson’s ratio can be determined, these tests are
quite elaborate, cumbersome, time consuming and require skilled manpower particularly for data interpretation. Moreover, direct
determination of the Poisson’s ratio by employing micro-strain gauges, which measure axial and lateral strains using Wheatstone
bridge circuits, is difficult for soils due to the problems associated with their fixing on the surface of the sample. Under
these circumstances, application of piezoceramic elements, which can generate shear and compression waves, seems to be an
excellent alternative. Using these wave velocities, the Poisson’s ratio can be computed easily and precisely. However, how
this (computed) value of the Poisson’s ratio compares vis-à-vis that obtained from the conventional triaxial tests (i.e.,
strain controlled uniaxial compression tests), which yield stress–strain relationship, needs to be established. With this
in view, investigations were conducted on soils of different types (clays and sands) in their disturbed and undisturbed forms
by resorting to piezoceramic tests and the triaxial tests. Details of the methodology are presented in this paper and it has
been demonstrated that application of piezoceramic elements yields the Poisson’s ratio and the elastic modulus of the soils
quite easily, particularly for the soft clays and sands. 相似文献