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珊瑚砂地基建设场地在吹填过程中形成的软弱夹层工程性能较差,导致珊瑚砂地基承载力较低、沉降较大。通过物理试验对软弱夹层进行土性分析研究,采用4种不同工艺参数的振冲密实施工方法。结果表明工艺3效果较好。因此,合理布置振冲点位,选择较粗的吹填料进行回填置换,可使软弱夹层较密实、珊瑚砂地基的承载力明显提高,最终满足设计使用要求。 相似文献
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《港口科技》2020,(1)
为合理确定重力式码头结构基础尺度,对重力式码头结构地基承载力变化与地基土体抗剪指标(黏聚力和内摩擦角)、基床厚度等参数变化之间的敏感程度进行分析。结合大连港太平湾港区某码头工程实例,采用《水运工程地基设计规范》中的方法计算地基承载力抗力分项系数,并绘制地基承载力抗力分项系数与地基土体抗剪指标、基床厚度之间的关系曲线。结果显示:黏土内摩擦角、黏聚力数值的增加可持续提高地基承载力;黏土内摩擦角的数值越大,对地基承载力的提高作用越显著;当基床厚度增加时,对地基承载力的提高作用逐渐减弱。在以地基承载力确定重力式码头结构地基尺度时,可以通过改善土体指标或增加基床厚度提高地基承载力,但应避免一味地增加基床厚度。 相似文献
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目前国家标准和水运工程相关检测规范中,未明确十字板抗剪强度和地基承载力的换算关系,导致利用十字板剪切试验检测地基承载力的评价标准不统一。通过对岩土勘察、公路、铁路基础设计规范中十字板抗剪强度换算地基承载力的公式进行对比,并以某软基加固检测工程为例,运用多种公式进行承载力的计算和验证。结果表明,根据《建筑地基基础设计规范》推导的简化公式更适用于软基处理加固效果的评价,可作为十字板剪切试验检测软基加固承载力的验收依据。 相似文献
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桩靴/地基承载力的准确预报是确保自升式平台进行海上插桩作业安全性的重要前提,常规的规范算法在处理复杂地基条件时存在困难。基于非线性数值分析方法,在对加载点位置、网格尺寸、地基边界等关键技术进行研究的基础上,以某400ft水深自升式平台为例,分别对海底均质土和成层土的承载力进行了研究。同时,对各土层参数的影响进行了详细分析,为探索插桩过程中地基破坏原理和承载力计算提供了一些参考。 相似文献
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介绍了我国港口资源的整合现状,指出港口整合可以提升港口的形象和地位,也为区域经济和城市的发展注入强大的动力。最后指出在港口资源整合中要避免的几个问题。 相似文献
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广州集装箱码头的轮胎式场桥小车制动器使用10多年后,出现了许多问题,故进行了改造.分析了轮胎式集装箱龙门起重机小车制动器的主要故障现象,提出了改造方案,并加以实施. 相似文献
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本文对现有的选定球面轴承的三种工程方法进行了分析比较.引入了“合力系数”,并给出了合力方向上投影面积的精确解. 相似文献
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分析柴油机故障中常见的机体裂纹故障原因,认为由于设计缺陷和管理及操作不当,易造成船舶柴油机缸体上的裂纹多发生在气缸套凸肩处。如不及时处理这些裂纹和故障,就会造成缸套的裂纹直至出现缸套漏水等严重后果,针对NANTAIQUEEN轮柴油机对该类型故障的检修提出具体措施。 相似文献
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The hydrophysical and hydrochemical structure of the Sea of Azov, with developed bottom anoxia, was studied during the RV “Akvanavt” cruise from July 31 to August 03, 2001. The anoxic zone with a thickness from 0.5 to 4 m above the bottom was found in all deep regions of the Sea. Concentrations of hydrochemical parameters were similar to the pronounced anoxic conditions (about 90 mmol m− 3 of hydrogen sulfide, 17 mmol m− 3 of ammonia, 6 mmol m− 3 of phosphate, 7 mmol m− 3 of total manganese). The hydrophysical structure was characterized by the uniform distribution of temperature in the upper 6–7 m mixed layer (UML). Below this a thin (0.4–0.8 m) thermocline layer was observed, just above the anoxic waters. Formation of this phenomenon was connected with that summer weather conditions. Intensive rains led to increased influx of river waters in June. That resulted in large input of allochtonous organic matter (OM) and inorganic nutrients; the latter were consumed on the additional autochthonous organic matter production. In July the weather was characterized by a significant rise in the daily averaged air temperature and large oscillations of temperature during the day. In this period a wind of constant direction was absent, but wind bursts were observed. The completed analyses showed that the formation of such a structure could be connected with the following factors: (i) positive growth trends of the daily averaged temperature and the daily oscillations of temperature, (ii) presence of wind bursts. The joint action of these factors resulted in the formation of the UML. The amplitude of wind bursts determined the depth of UML, and the value of trend determined the value of the temperature change in the thermocline. An initial presence of bottom halocline (caused by the Black Sea water influx to the bottom of the Sea of Azov) prevented the heating of the bottom layer and therefore led to an increase of vertical gradient of temperature in the thermocline. The spatial distribution of the turbulent exchange coefficient confirmed the existence of a “stagnation” area located above the anoxia zone, which is also, apparently, the reason for its occurrence. 相似文献