陆浑水库坝基断层破碎带渗透稳定性评价

陆浑水库位于河南省洛阳市嵩县境内。为了论证大坝在水库投入正常高水位（319．5m,327.5m,331.8m)运行时的安全,经过对30余年的水位观测资料的整理和分析,在厘定水文地质模型的定性分析基础上,运用现代数理统计原理,成功地解决了困扰水库正常运行的坝基渗流问题,获得了善于坝基渗透稳定状况及其变化趋势的认识。结果表明：目前大坝的运行状况是正常的;水库在缓慢蓄水过程中,截水槽的薄弱部位可以得到渗透中固,截水槽中的填土与岩石结合面的抗渗比降可达45以上;上游铺盖与截水槽结合下游排水的防渗体系有效地控制了坝基渗流。同时,预测了高水位时坝基渗流是稳定的,水库完全可以投入高水位运行。这为病险水库的论证提供了一个案例。     

基于三维平差的基坑监测数据处理方法探讨

在基坑监测自由测站边角交会构网监测方法的基础上,提出基于全站仪观测数据的三维平差数据处理方法。通过结合工程实例,对监测数据进行精度分析,并比较三维平差与传统平差方法的计算结果,验证文中方法可满足二级基坑的监测精度要求,能准确、高效地监测基坑形变。     

考虑桩底沉渣的随钻跟管桩竖向承载特性模型试验研究

随钻跟管桩施工不能完全清除桩底岩土沉渣,从而影响桩基端承力。为揭示桩底沉渣对随钻跟管桩承载力的影响机制,开展了考虑桩底沉渣影响的随钻跟管桩竖向承载特性模型试验研究。试验结果表明:在密砂地层中,具有桩端水泥土扩大头的随钻跟管桩,其桩顶荷载-沉降曲线为缓降型,而模拟试验的其他管桩均为陡降型;桩底沉渣降低随钻跟管桩的极限承载力在22%以内,且其桩顶荷载主要由桩侧摩阻力承担,承担占比超过90%;与存在一定厚度沉渣的钻孔灌注桩相比,随钻跟管桩的桩底沉渣对降低承载力的影响相对较小;靠近桩端的轴力随着沉渣厚度的增加而减小,沉渣越厚,减少的幅度越明显;桩端水泥土扩大头施工可提高随钻跟管桩约37%的承载力,且桩端阻比均小于15%。现场原位测试(桩长为15.5 m,长径比为15.50)和室内模型试验(桩长为1 m,长径比为15.87)结果均表明:存在桩底沉渣时,随钻跟管桩是以发挥侧摩阻力为主的端承摩擦型桩。研究成果有助于进一步加深对随钻跟管桩承载性状的认识。     

平面应变条件下土工格室加筋垫层的变形分析

将铺设在软土地基上的土工格室加筋垫层看作具有一定刚度的梁板。地基上梁板的变形计算一般以弹理论的文克尔假定为基础。针对文克尔假定中不考虑水平抗力影响的问题,提出了考虑水平抗力的双参数法,并以该法应用于土工格室加筋垫层工法的变形分析。     

碎石桩复合地基设计方法的探讨

通过对碎石桩复合地基承载力和抗震液化设计的对比和分析,提出了以承载力和抗震液化相互综合考虑的设计方法。     

风积沙地基装配式偏心基础抗拔试验研究

在毛乌素沙漠中开展装配式偏心基础在上拔、上拔+水平力组合荷载作用下的现场试验研究。根据试验加载过程中监测的基础顶部位移、地表竖向位移及基础底板土压力数据,分析基础顶部的荷载-位移特性,研究装配式偏心基础的抗拔承载机制。结果表明,（1）在上拔、上拔和水平力组合作用下,基础顶部上拔和水平位移曲线均呈二阶段的承载特性;（2）当仅受上拔荷载作用时,基础偏心引起的附加弯矩,使得基础底板产生偏转,基础及底板上覆部分沙土自重抵抗上拔荷载,而在上拔和水平力组合荷载工况下,基础偏心引起的附加弯矩小,与上拔荷载工况相比,基础极限抗拔承载力提高8.7％,即在组合荷载工况下装配式偏心基础能够发挥更多的沙土来抵抗上拔荷载;（3）根据装配式偏心基础的抗拔承载机制,引入外荷载合力作用线与支架作用线之间的夹角δ来反映水平荷载对装配式基础抗拔破坏因子的影响,其影响规律为装配式基础的抗拔破坏因子随δ增加而降低。     

弹性地基中厚板弯曲问题的无网格LRPIM分析

无网格局部径向点插值方法（LRPIM）的形状函数具有Kronecker delta函数的特性,便于施加位移边界条件,不需要进行特殊地处理。采用局部加权残值法推导了双参数弹性地基中厚板的离散系统方程,利用无网格LRPIM对四边简支和四边固支以及筏式双参数弹性地基中厚板的弯曲问题进行了分析和计算。算例表明,用无网格LRPIM分析弹性地基中厚板问题具有非常灵活和易于实现等优点。     

IDENTIFICATION OF PALEO-EARTHQUAKES OF LUOYUNSHAN PIEDMONT FAULT BY QUANTITATIVE MORPHOLOGY OF LIMESTONE FAULT SURFACES

The quantitative analysis of morphologic characteristics of bedrock fault surface is a useful approach to study faulting history and identify paleo-earthquake. It is an effective complement to trenching technique, specially to identifying paleo-earthquakes in a bedrock area where the trenching technique cannot be applied. This paper focuses on the Luoyunshan piedmont fault, which is an active normal fault extending along the eastern boundary of the Shanxi Graben, China. There are a lot of fault scarps along the fault zone, which supply plentiful samples to be selected to our research, that is, to study faulting history and identify paleo-earthquakes in bedrock area by the quantitative analysis of morphologic characteristics of fault surfaces. In this paper, we calculate the 2D fractal dimension of two bedrock fault surfaces on the Luoyunshan piedmont fault in the Shanxi Graben, China using the isotropic empirical variance function, which is a popular method in fractal geometry. Results indicate that the fractal dimension varies systematically with height above the base of the fault surface exposures, indicating segmentation of the fault surface morphology. The 2D fractal dimension on a fault surface shows a ‘stair-like’ vertical segmentation, which is consistent with the weathering band and suggests that those fault surfaces are outcropped due to periodic faulting earthquakes. However, compared to the results of gneiss obtained by the former researchers, the characteristic fractal value of limestone shows an opposite evolution trend. 1)The paleo-earthquake study of the bedrock fault surface can be used as a supplementary method to study the activity history of faults in specific geomorphological regions. It can be used to fill the gaps in the exploration of the paleo-earthquake method in the bedrock area, and then broaden the study of active faults in space and scope. The quantitative analysis of bedrock fault surface morphology is an effective method to study faulting history and identify paleo-earthquake. The quantitative feature analysis method of the bedrock fault surface is a cost-effective method for the study of paleo-earthquakes in the bedrock fault surface. The number of weathered bands and band height can be identified by the segment number and segment height of the characteristic fractal dimension, and then the paleoearthquake events and the co-seismic displacement can be determined; 2)The exposure of the fault surface of the Luoyunshan bedrock is affected and controlled by both fault activity and erosion. A strong fault activity(ruptured earthquake)forms a segment of fault surface which is equivalent to the vertical co-seismic displacement of the earthquake. After the segment is cropped out, it suffers from the same effect of weathering and erosion, and thus this segment has approximately the same fractal dimension. Multiple severe fault activities(ruptured earthquake)form multiple fault surface topography. The long-term erosion under weak hydrodynamic conditions at the base of the fault cliff between two adjacent fault activities(intermittent period)will form a gradual slow-connect region where the fractal dimension gradually changes with the height of the fault surface. Based on the segmentation of quantitative morphology of the two fault surfaces on the Luoyunshan piedmont fault, we identified four earthquake events. Two sets of co-seismic displacement of about 3m and 1m on the fault are obtained; 3)The relationship between the fault surface morphology parameters and the time is described as follows:The fractal dimension of the limestone area decreases with the increase of the exposure time, which reflects the gradual smoothing characteristics after exposed. The phenomenon is opposite to the evolution of the geological features of gneiss faults acquired by the predecessors on the Huoshan piedmont fault; 4)Lithology plays an important role in morphology evolution of fault surface and the two opposite evolution trends of the characteristic fractal value on limestone and gneiss show that the weathering mechanism of limestone is different from that of the gneiss.     

Response of L-shaped rigid foundations embedded in a uniform half-space to traveling seismic waves

A simplified indirect boundary element method is applied to compute the impedance functions for L-shaped rigid foundations embedded in a homogeneous viscoelastic half-space. In this method, the waves generated by the 3D vibrating foundation are constructed from radiating sources located on the actual boundary of the foundation. The impedance functions together with the free-field displacements and tractions generated along the soil–foundation interface are used to calculate the foundation input motion for incident P, S and Rayleigh waves. This is accomplished by application of Iguchi's averaging method which, in turn, is verified by comparison with results obtained rigorously using the relation between the solutions of the basic radiation (impedance functions) and scattering (input motions) problems. Numerical results are presented for both surface-supported and embedded foundations. It is shown how the seismic response of L-shaped foundations with symmetrical wings differs from that of enveloping square foundations. The effects of inclination and azimuth of the earthquake excitation are examined as well. These results should be of use in analyses of soil–structure interaction to account for the traveling wave effects usually overlooked in practice.     

小波分析和RBF神经网络在地基沉降预测中的应用研究

地基沉降是一种危害很大的环境灾害。地基沉降的监测数据经常受降雨及工程施工等诸多外界因素的干扰,故而在沉降曲线中存在许多数据突变点。为此,提出基于小波分析与RBF神经网络相结合的新的地基沉降预测方法,首先采用小波分析对对原始监测数据进行数据去噪处理,进而得到反映实际变化的地基沉降曲线,然后采用径向基函数（RBF）神经网络方法对其进行预测,为工程设计提供依据。最后结合工程实例分析,通过多种小波去噪与预测结果的对比研究,表明3次B样条小波的去噪及预测效果最好,与实测值能较好地吻合,具有较好的工程应用前景。