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灌注桩因其对各种土层的适应性强、桩基承载力高和施工时对附近建筑物及环境影响小等特点,在沿海桩基工程中得到广泛的应用。然而在厚度不均的抛石棱体层中进行冲孔灌注桩施工,在我国工程建设史上还不多见。文章介绍对海上抛石棱体层冲孔灌注桩成孔施工的工程实践经验和施工工艺方面的一些体会,供同行参考。 相似文献
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灌注桩因其对各种土层的适应性强、桩基承载力高和施工时对附近建筑物及环境影响小等特点,在沿海桩基工程中得到广泛的应用。然而在厚度不均的抛石棱体层中进行冲孔灌注桩施工,在我国工程建设史上还不多见。本文即是作者通过对海上抛石棱体层冲孔灌注桩成孔施工的工程实践经验结合自己的想法而形成的一篇应用性论文,供同行参考。 相似文献
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含有人工抛石层的地基有其独特的复杂性。本文就抛石地基上的冲孔灌注桩成孔施工特点及应采取的技术措施、常见的事故预防与处理作简要介绍。 相似文献
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本文主要介绍海上超厚抛石层冲孔灌注桩成孔施工工艺。水上平台的搭设、钢护筒跟进、泥浆配置等相关技术,是实现冲孔灌注桩穿透抛石层的主要技术难题。 相似文献
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斜向嵌岩复合桩为钢管桩与嵌岩灌注桩的组合体,其承载力高、抗拔及抗倾覆能力强,十分适用于大型高桩码头桩基工程,而其施工过程在所有类型码头桩基中最具复杂性与可变性,需要进行精细化施工管理和全过程细节控制才能取得良好的效果.文中针对该型桩基的冲孔浇砼施工进行循序渐进的讲解与剖析,希望能对类似工程施工提供借鉴. 相似文献
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本文叙述了庙岭三期工程冲孔灌注桩从平台装拆、开孔、成孔到砼施工的方法和工艺,同时对平台装拆、成孔过程中坍孔、护壁、砼灌注等施工过程中出现的问题及处理措施进行了讨论,重点介绍了平台搭设及大块石抛石层中成孔工艺,并就施工中应用情况进行了总结。 相似文献
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分析了冲孔灌注桩施工过程中出现卡锤事故的原因,介绍空心锤冲孔提锤法处理岩溶地区某桥桩基冲击成孔时埋卡锤事故的方法,提出了空心锤的加工制作要求、空心锤冲孔提锤的施工方法及要点。 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