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目前,我国大部分声学测试试验在浅海海域进行,浅海声波导的多途效应、声速梯度的变化对声传播产生直接的影响。通过射线声学模型对不同频率的声源在浅海等声速梯度和温跃层声速梯度环境下辐射声场和声传播衰减特性进行仿真研究,给出声场分布图和传播损失变化曲线图,得到声场分布和传播损失随声源频率的变化规律。 相似文献
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为考察吸声尖劈对船舶声纳平台水下声学环境的影响,开展了吸声尖劈对板柱组合结构水下声学特性影响的模型试验研究。通过对板柱组合结构0%、36%、60%、100%敷设吸声尖劈材料,在声波以0°、90°、180°方向入射板柱组合结构时,研究了尖劈敷设方式、声波入射角度对板柱组合结构水下声场及散射声场的影响,得到了不同工况下板柱组合结构典型部位的声场分布。研究表明:吸声尖劈可明显改变板柱组合结构的声场分布,降低板柱组合结构的自噪声;但其抑制效果随考核位置、声波频率、敷设密度的不同而各有变化。 相似文献
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海洋声场预报及战术应用 总被引:1,自引:0,他引:1
随着科学技术的飞速发展,对海洋声场做出合乎要求的快速精确预报显得尤为重要。射线模型、抛物线模型、简正波等模型适合于不同具体的海洋声场环境,这些传播模型可以实现声场数值预报的实时性。基于上述模型建立的海洋声场预报系统及对其战术应用进行的研究,对声呐的设计、使用及舰艇作战有着重要的意义。本文在上述模型基础上利用Matlab和Fortran Powerstation工具建立了海洋声场预报系统,使用声场预报系统对典型的海洋环境,即海洋锋、涡漩的声场能量传播规律进行了研究,并提出了在反潜作战中对海洋锋、涡漩、深海会聚区和影区等海洋环境的战术应用。 相似文献
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本文结合海洋声学结构、多波束测深原理,分析声波折射对测深的影响,提出实际水层声速、调和平均声速与水深之间的变化关系,以及表层声速对水深测量的重大影响并进行模拟验证。最后,结合工作实例提出解决问题的校正方法,使其达到正确水深数值,满足多波束测深精度的要求。 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