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基于Star-CD的某船机舱火灾烟气流动计算与分析 总被引:1,自引:1,他引:0
为了探究机舱火灾的烟气流动情况,减少火灾烟气带来的危害,基于Star-CD平台,采用场模拟方法,模拟某船舶机舱火灾发生时的温度场、速度场、压力场及烟气的分布情况,结果显示了机舱空间在不同截面和时刻机舱的温度、速度、压力和烟气的分布,在火源正上方的温度、速度、压力和烟气浓度比周围的高,压力最高值出现在机舱的顶部,机舱上部的烟气平均浓度、温度明显高于下部的浓度,并给出了不同高度的烟气浓度和温度曲线.根据计算结果和该船现有的消防体系,建议在机舱内安装一套固定灭火系统,计算结果符合室内火灾的基本规律. 相似文献
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船舶火灾往往造成严重的人员伤亡和财产损失,究其原因主要是,船员缺乏船舶的防火与灭火知识,在灭火中采取的措施不当,忽视了对火场通风的控制.导致小火成大灾的严重事故。因此.如何采取正确的灭火措施,以求尽快控制火势,直至最终扑灭火灾,就显得十分重要.而对火场的通风控制则是一个不容忽视的重要环节。 相似文献
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舱室消防预案数值模拟设计及实现 总被引:1,自引:0,他引:1
《舰船科学技术》2015,(7):93-98
为提高水面舰船消防预案的有效性,针对制定舰船消防预案的需求,设计了具有工程实用性的数值模拟方案,并以某一主机舱所处防火主竖区为典型案例,采用火灾动力学场模拟方法,模拟起火舱室及相邻舱室采取灭火措施后的舱内烟气温度、舱壁和顶壁温度、CO气体浓度、能见度等参数随时间的变化,并分析火灾对扑救人员的威胁以及灭火措施对火灾控制的影响。实例计算表明,及早发现初火并正确操作至关重要,没有控制住且进一步发展的火灾,机械通风状态对舱内火灾早期烟气运动的影响较大,舱壁喷水冷却对降低舱壁温度效果明显,但封舱灭火后需要较长时间才能达到安全状态等。数值模拟结果对进一步细化消防预案具有重要意义。 相似文献
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以船舶机舱为研究对象,采用大涡模拟方法,以FDS软件为平台,计算了不同火灾功率、风机启动时间、风机流速和补风口面积条件下的火场温度变化过程。以FDS的数值模拟数据为样本建立了船舶机舱火灾温度的支持向量机计算模型,为提高模型预测的精确度,利用遗传算法对参数进行寻优。实验表明:应用本文模型预测结果与FDS计算结果基本一致,优于SVM模型以及BP神经网络的预测结果,提出一种快速预测火场温度的工程计算方法。 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
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