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《水道港口》2018,(6)
三峡水库运行后下荆江河段冲刷下切,局部失稳崩岸频繁发生。针对下荆江河段概化的上粘下砂二元岸坡,文章推导了崩塌土体坡脚堆积掩护公式,结合下部砂土层冲刷计算与上部悬空粘土层稳定性分析,同时考虑水位、土体性质、岸坡形态等随时间的耦合变化,利用Matlab编程建立了岸坡崩塌分析模型;应用该模型动态模拟了下荆江二元河岸崩退过程,与现场实测符合良好;在此基础上,探讨了不同水位变化模式对二元河岸崩塌过程的影响。研究结果表明:水位下降期较之水位上升期上部粘土层更易发生绕轴崩塌;水位变化至两土层交界面附近时是岸坡崩塌的最危险时期;与未考虑坡脚掩护相比,考虑掩护后落、涨水期的坡脚累计冲刷距离分别减少约45%和17%。 相似文献
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岸坡稳定问题在航道整治工程中经常遇到但尚未很好的解决。文章对虎跳门航道整治工程中堤岸滑坡的原因进行了分析,对治理措施进行了总结,也对岸坡失稳的预防提出了几项具体建议。 相似文献
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实体斜坡式结构是天然岸坡起伏不大、坡脚水深较深、大水位差河港码头的常用结构形式.在实体斜坡码头施工时,常因施工期水位低、水流急或施工顺序不当等原因发生局部塌方的岸坡失稳情况.文中对黄石某码头上游段施工期局部塌方引起的岸坡失稳情况进行了分析并提出了处理方案,供其它类似工程设计参考. 相似文献
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以一座向家坝库区码头的加筋岸坡稳定性为研究对象,根据简化Bishop理论,建立了加筋岸坡的稳定性极限状态函数,并采用Monte Carlo模拟法对土体密度ρ、抗剪强度c和φ值、加筋材料强度及水位等参数进行随机抽样和岸坡的可靠度分析,最后分析了土体抗剪强度c、φ值的相关系数对岸坡安全系数均值和可靠度指标的影响,得出了一些有益的结论。 相似文献
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通过对长江上游大水位差港口散货码头自然条件的分析,提出了一种用于山区河流大水位差码头特殊条件下能适应水位变化、移动的大倾角输送设备.它的使用将使散货连续输送设备对岸坡坡度要求的适应性更强,并能大幅度降低工程造价,节省岸线资源. 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