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根据天津港航道的现状,天津港存在单向通航情况,尤其是随着大型船舶进出主航道艘次的增加,在现有航道宽度不发生变化的情况下,同时考虑单向通航和双向通航的情况,包括单向通航到双向通航的转换及双向通航到单向通航的转换过程。本文给出了天津港航道通航能力的理论计算模型,并运用该模型进行了计算分析。 相似文献
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随着天津港主航道通航标准的提高,通航环境得到极大改善,但同时主航道上航行船舶的密度大量增加,航行过程中面临更多的“对驶”、“追越”等局面。因此,驾引人员应按照《避碰规则》和港章的规定,采用“良好船艺”安全操纵船舶。 相似文献
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通过对天津港10万t级大沽沙航道自然条件的调查,根据进出港船型需求及相关理论计算,论证不同海况下设计宽度为375m的10万t级大沽沙航道所能允许双向通航的船舶尺度,对即将开通的天津港10万t级大沽沙航道的通航管理具有一定的参考意义。 相似文献
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日前,天津海事局召开新闻发布会宣布,为助力港航企业应对金融危机,自12月11日起,海事部门将实施“放宽天津港主航道通航标准”、“推荐天津港砂石运输船舶专用航路”等10项新举措。这些措施将大大提高天津港水域的船舶通行效率和安全性,缩短船舶锚泊等候时间,降低港航企业的营运成本, 相似文献
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拟建的海河开启桥水文情况较为复杂,大桥的建设客观上改变了该水域原有的通航环境和通航条件,对船舶航行安全带来一定的影响。通过对大桥通航尺度和通航方案的研究,能够保障桥区水域具有良好的通航环境和通航秩序,使桥区船舶航行更安全。 相似文献
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现有伶仃航道船舶双向通航能力的规定制约和限制了大型集装箱班轮进出广州港南沙港区的通航效率。为更好地服务地方经济建设和发展,海事部门有必要对伶仃航道的通航能力重新做科学评估,本文在此基础上,对不同吨级的集装箱船双向通航能力进行了分析和计算,得出适合目前通航环境下伶仃航道船舶双向通航能力的标准。 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