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1.
能否对砂土液化进行准确的判断评价,与工程的安全性、经济效益和社会效应关系密切。目前,勘察规范和抗震规范中均没有专门针对海底岩土层饱和砂土液化判别方法的规定和要求。文章对目前饱和砂土可液化性判别方法进行了分析总结,给出了海域工程场地可液化土的液化判别方法及存在的问题,提出海域工程建设场地饱和砂土层的判别宜采用标准贯入试验法和室内液化振动三轴试验抗液化剪应力判别法相结合的方式进行综合评价。  相似文献   

2.
王虎刚  贾魏 《海岸工程》2020,39(2):124-129
内摩擦角作为砂土的抗剪强度指标之一,是工程设计的重要参数。常规海洋工程勘察中主要依据室内土工试验确定,如三轴压缩试验、直接剪切试验、颗粒粒径、级配和密实度等。随着孔压静力触探(Piezocone Penetration Test, PCPT)在海洋工程勘察中广泛开展,利用孔压静力触探测试的锥尖阻力、侧壁摩阻力和孔隙水压力等参数确定砂土内摩擦角具有无需取样、快速、合理、可靠的优点,在桩基础、管线路由、水下基础等海洋工程勘察中具有越来越重要的工程意义。本文总结了3种利用PCPT资料确定砂土内摩擦角的方法即Mayne提出的内摩擦角评估经验公式、砂土最大最小经验公式和Senneset等提出的计算砂土内摩擦角经验公式,在中国广东沿海某风电场开展了3个钻孔的应用实践。对结果进行对比分析后认为,在熟练掌握PCPT测试方法、资料采集、数据处理和成果解释的基础上,依据Senneset等提出的计算方法,用PCPT资料确定砂土内摩擦角,具有一定的可靠性与适用性。  相似文献   

3.
胜利油田浅海区域海底土层的液化判别方法分析   总被引:2,自引:0,他引:2  
针对胜利油田海上石油勘探开发区(埕岛油田)的海底饱和粉土(砂土)液化判别问题,结合工程研究实例,对土层液化判别的各种方法进行对比分析,指出了当前各种方法的局限性和不足,为海底土层的液化判别分析提供了新思路。  相似文献   

4.
海底土体在波浪作用下能否产生液化是海岸工程所关心的问题。借鉴地震液化判别使用的砂土液化判别方法,将海底粉质土波致液化的判别分为初判和复判2个阶段。初判以所致海床土体发生破坏的临界循环应力比界限指标来判别,以土质基本特征和波浪条件为参数,对某海域海底液化形成判断;复判以波致海床土体中剪应力与实际土体的动剪切强度比较来判别。结合已有研究成果给出了波致土体液化判别的具体方法。  相似文献   

5.
根据杭州湾近年来工程地质勘察和地球物理探测所获得的资料,将杭州湾常见的地质灾害分为活动性地质灾害和限制性地质灾害.对杭州湾常见的地质灾害因素作了比较深入的分析,特别是潮流冲刷槽、古河道、软土、滑坡、砂土液化、浅层气等与海洋工程密切相关的地质灾害类型及其分布特征、形成机制及危害性等,为本区海洋工程建设和海洋开发提供基础资...  相似文献   

6.
辽东湾北部浅海区海洋工程地质特征   总被引:2,自引:0,他引:2  
通过对浅地层剖面仪、侧扫声纳和海底取样等实测资料的详细分析,揭示了辽东湾北部浅海区的自然地质状况和复杂的海洋工程地质特征。该海区海底地形地貌较为复杂,存在海底冲刷深槽、埋藏古河道、浅层气、潮流沙脊与潮沟、埋藏古陡坡、软弱土层及可能的砂土液化层等潜在灾害地质因素,对海上构筑物存在直接或潜在的危险性,应引起高度重视。  相似文献   

7.
黄河三角洲埋藏古河道对工程建设和第四纪环境的研究有重要意义.结合前人的钻孔资料,通过对新老黄河口间近300 km的浅层剖面资料,尤其0~50 m的浅层剖面资料进行分析,发现研究区内古河道属于古黄河水系,断面多呈对称性型,各层位古河道断面在空间上分布具有分区性.河道充填物多为河流溯源堆积,呈发散或上超型反射,工程地质条件差,易造成不均匀沉降、局部塌陷、砂土液化等地质灾害.研究区从约38 kaBP至今共发生3次海退和3次海进,其中1次海退规模较小.  相似文献   

8.
本文阐述了近海重力式建筑物地基在风浪荷载作用下的特性,以及相应的一些考虑。鉴于目前判断土体液化势的应力分析法存在着某些缺点,以及为便于研究复杂的振动问题,文中介绍了笔者曾建议的能量分析法。由于作用在地基上的荷载为随机过程,故文中亦探讨了根据砂土在常幅谐振下的液化势,来估计随机振动下液化势的方法。对于排水条件较好和振动时间较长的情况来说,考虑孔隙水压力在振动期及其后的消散和再分布很为重要。因为事实上在这些情况下,孔隙水压力的消散与再分布很可能阻止地基的液化。  相似文献   

9.
1 前言自先进的电子计算机和计算机处理技术引入地震勘探领域,无论是地震资料的采集,还是资料的处理解释都日趋于自动化。极大地提高了勘探精度和可靠程度。但这仅限于反射波法地震勘探。而对于折射波法发展较慢,尤其是在资料处理解释方面更是如此。对于浅层初至折射波法,由于数据量较少,其资料处理解释工作仍用人工来完成。本文根据这一情况,讨论在IBM-PC机上对浅层初至折射波地震资料进行自动解释并在绘图仪上绘制解释成果图件的实现原理与方法。并对实际资料进行了处理,经与人工解释的成果资料对比,两者非常接近。因此,用微机对初至折射资料进行自动解释代替人工解释是可行的,  相似文献   

10.
南海北部湾海洋工程地质特征   总被引:8,自引:0,他引:8  
根据地球物理、声学探测及海底取样等实测资料详细分析,发现北部湾油气勘探开发区具有近岸、水浅等优越自然条件以及复杂的海洋工程地质特征。海底地形地貌较为复杂,存在潮流沙脊与潮沟、海底沙坡、埋藏古河道、浅层气、埋藏古陡坡、滑塌断层及可能的砂土液化层等潜在灾害地质因素,对海上构筑物存在直接或潜在的危险性。尤其在东部,海底坎坷不平,活动性的潮流消脊、侵蚀沟槽、海底沙波及浅层气等很发育,是海底工程建设的危险区,应引起高度重视。  相似文献   

11.
成层海床波浪响应的状态空间解及其应用   总被引:1,自引:0,他引:1  
针对成层海床的波浪响应问题,采用Laplace-Fourier变换和状态空间法求解控制方程,得到表征该问题基本状态量之间的传递矩阵。利用矩阵递推规律、边界条件及逆变换技术实现成层海床波浪响应的计算。以北海和密西西比三角洲的波浪和海床特征为参数进行算例分析,结果表明该方法具有较高的效率和精度。结合北海的工况指出在砂质海床的表面铺设一层砾石土可以增强海床的抗液化能力,起到保护海床的作用。  相似文献   

12.
海床式静力触探设备工作效率高,能够实现从垂向上对地层的连续探测,数据分辨率较好。通过对黄河口海域3个静力触探孔和1个地质钻孔的分析,将研究区20m以浅地层自上而下划分为粉土、粉质黏土、粉土夹粉砂或粉砂、粉质黏土、粉土五层,静力触探曲线对粉土层中的硬壳层和粉质黏土层中的贝壳夹层等特殊地质现象有很好的反映。对粉质黏土的静力触探参数与物理力学参数进行相关性分析,得到适合该区域的回归方程。采用基于CPT数据的液化判别法,对研究区表层粉土液化可能性进行评判,通过Seed简化法计算的周期应力比(CSR)与Olsen法计算的周期阻力比(CRR)的大小比较,得出当抗震设防烈度为7度时,研究区表层粉土不会液化,当抗震设防烈度为8度时,粉土层将发生液化,计算最大液化深度3.7m。  相似文献   

13.
For South Korea, liquefaction potential along the western coast has not been widely assessed because South Korea is considered to be a low seismic hazard. However, recent earthquake events and historical records indicate that the seismic hazard of South Korea should not be ignored. Moreover, as artificial fills are extensively used along the western coast for development, liquefaction evaluation of the soils in this area is necessary. In this paper, we present: (1) the seismic characteristics of the study area; (2) procedures for evaluating liquefaction potential, focusing on the liquefaction potential index (LPI) approach; and (3) LPI distributions at several representative locations along the western coast of South Korea under various seismic scenarios. The liquefaction potential index represents the liquefaction potential over the upper 20 m of a boring or sounding. Using cone penetration test (CPT) and standard penetration test (SPT) data from two coastal sites, we compare and discuss CPT-based and SPT-based LPI values, particularly values computed in nonplastic, silt-rich soils. In these soils, it appears that the CPT yields lower liquefaction resistance, resulting in large LPI values. Finally, discussion and suggestions are provided for CPT- and SPT-based liquefaction assessment of low plasticity and high fines content soils.  相似文献   

14.
浅地层剖面交互拾取解释技术研究   总被引:6,自引:0,他引:6       下载免费PDF全文
浅地层剖面探测在海洋学研究与海洋工程调查中使用愈来愈频繁,剖面资料的解释工作变得越来越繁重。因浅地层剖面实际解释工作的需要,结合浅地层剖面资料的特点,研究并实现了剖面反射层位的自动拾取、利用Event号交互拾取特征点、等Ping间隔拾取、求取海底下反射层位厚度等解释功能,这些解释功能的实现加快了剖面解释工作的进度,提高了解释结果的精度,并在实际浅地层剖面资料解释工作中取得了良好的应用效果。  相似文献   

15.
Soils are classified as sandy soils and clayey soils in most soil classification systems, and appropriate equations are used for practical design, depending on soil type, to represent each soil behavior. Sand-clay mixtures, however, need a special standard to evaluate their specific behaviors since they are categorized as intermediate soils or transitional soils and typically show intermediate properties. In this article, a series of cyclic triaxial tests were conducted on specific sand-fines mixtures with three fine types and various fine contents. The behaviors of various soil mixtures (silica sand with Iwakuni natural clay, Tottori silt, and Kaolin clay) were investigated by considering a concept of granular void ratio expressed in terms of sand structure. The cyclic shear strengths of the soil mixtures were also evaluated by increasing the fine content but no more than the threshold fine content. In the results, the cyclic deviator stress ratio decreased in dense soils whereas it increased in loose soils by increasing the fine content. In addition, a simple equation was proposed to predict the liquefaction resistance of sandy soils by evaluating the cyclic deviator stress ratio with a concept of equivalent granular void ratio.  相似文献   

16.
A remote sediment classification technique based on attenuation measurements from Chirp sub-bottom profiler data is described. This differs from previously published work in that attenuation measurements are obtained for each stratigraphic unit within a complex, thinly interbedded sedimentary sequence. Compressional wave attenuation measurements are obtained for a wide variety of lithologies, including muds, silts, sands, clayey sands, silty clays and gravel lags, with grain sizes ranging from 8 Phi to -4 Phi. In addition, attenuation measurements from sub-bottom profiler data were calibrated against laboratory acoustic measurements of vibracores and seabed samples from corresponding geographic locations, under simulated in-situ conditions using a Pulse Tube method. We adapt an instantaneous frequency matching method using a causal attenuation filter to model the decay of the Chirp transmitted waveform. From this modelling, a relationship between t* (a causal attenuation operator) and change in instantaneous frequency is established. The Hilbert transform is used to extract instantaneous frequency information from Chirp seismic, which is used to derive attenuation information for selected individual stratigraphic layers imaged by the sub-bottom profiler. This paper draws attention to the limitations in comparing attenuation measurements derived from Chirp sub-bottom profiler data against previously published literature on experimental attenuation measurements, which are limited by the wide variance of these data, and the difficulty in finding a meaningful best fit to these data. This demonstrates the importance of calibrating remote sediment classification observations using complimentary acoustic analysis of seabed samples to generate a site-specific geoacoustic database. A positive correlation between laboratory and sub-bottom profiler attenuation measurements was obtained, with a correlation coefficient of 0.885. Poorly sorted gravels with a mixed lithic and biogenic pebble component are characterised by very high attenuation with values of Q from 4 to 19. These sediments are considerably coarser-grained than those typically described in previously published experimental studies.  相似文献   

17.
根据天津永定新河口滩涂地层沙性土分布规律,采用现场标准贯入试验和室内动三轴试验两种方法进行了沙性土的液化判别。两种方法的判别结果基本一致,即在地震基本烈度为Ⅶ度的地震作用下,除第5层的沙性土不发生液化外,其余各层的沙性土均发生局部液化;在基本烈度为Ⅷ度的地震作用下,仅第5层的沙性土发生局部液化,其余各层的沙性土均完全液化;在基本烈度为Ⅸ度的地震作用下,所有地层中的沙性土均完全液化。  相似文献   

18.
With the presence of wind waves, the swaying of survey vessel may effect the quality of sub-bottom profiler records and, therefore, it is necessary to correct the distortions induced by wave action. A major issue is to distinguish wind wave effect and real bedforms such as sand waves. In this paper, a bandstop filter is designed according to the frequency features of wind wave effect to treat the distortion of seabed topography by wind waves. The technique is used to correct the sub-bottom profile in order to eliminate the wave-induced distortions for the sub-bottom profile records from the Yangtze Estuary. This study shows that the undulate seabed record is resulted from wave action, rather than the presence of sand waves, and the filtration technique helps to eliminate the wave effect and recover the real morphology of seabed and the sediment sequence underneath. In addition, a method for data processing is proposed for the case that the record indeed represents a combination of wave effects and real bedforms.  相似文献   

19.
现代黄河水下三角洲砂土液化模式   总被引:1,自引:1,他引:1  
根据实际勘探资料及室内土工试验结果,按极限平衡理论和线性波动理论等,分析了现代黄河水下三角洲砂土在地震和波浪动力因素的作用下发生液化的可能性,并根据其液化过程实质是孔隙水压力产生、发展和消散的过程,总结出砂土液化模式应包括四个阶段;(1)压密阶段:孔隙水压力升高至砂土本身强度,使颗粒产生相对位移;(2)初始液化阶段:孔隙水压力升至土层所受侧向压力,产生较大应变;(3)完全液化阶段:孔隙水压力升至土层上覆有效应力,产生喷水冒沙现象;(4)塌陷形成阶段:孔隙水压力消散。  相似文献   

20.
The liquefaction resistance of the soils used to be estimated through the in situ tests, such as standard penetration test and cone penetration test; or by means of cyclic triaxial test in laboratory. However, both in situ tests and cyclic triaxial test are time-consuming and costly; this study introduces a quick and cost-effective method to evaluate the liquefaction resistance of soils under certain confining pressure in laboratory. A particular device modified from the conventional triaxial compression test apparatus, namely “Triaxial Cone Penetration Test”, was developed to obtain the peak values of cone resistance in soils so as to correlate the liquefaction resistance of the reclaimed soils evaluated by cyclic triaxial tests. The test result indicates a good correlation between the peak value of cone resistance and the corresponding cyclic stress ratio (CSR) at the state of initial liquefaction, in which the correlation for loose samples is better than that for dense samples. Besides, both peak values of cone resistance and corresponding CSR increase with fine content of soils reaches 10% and decreased with fine content varying between 10% and 50%. By examining the compositions of the soils with scanning electron microscopy and X-ray diffraction, it is found that the proportion and characteristics of the fines plays an important role on the liquefaction resistance of the reclaimed soils.  相似文献   

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