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为便于分析水中目标在外部电磁场激励下的水下电磁场,本文以导电导磁球体为模型,分析其在无限大海水中谐变均匀磁场激发的水下磁场响应特征。从结果可知,响应磁场和响应电场与外部激励源磁场幅值成正比,即外场源幅值越大,产生的响应磁场幅值越大,越有利于探测;磁场x,z分量随着正横距的增加而减小,y分量随着正横距的增加是先增大后减小;磁场三分量随着频率的增加而减小,而10 Hz以下频率磁场三分量幅值衰减很小。 相似文献
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利用直流电偶极子阵列模型和时谐电偶极子分别计算了舰船稳恒电场和轴频电场随海洋环境电导率的变化情况。结果表明,舰船电场随着海水电导率增大而减小,低电导率海水的电场幅度要明显高于高电导率海水。高阻海床对电流具有排斥作用,导致深海环境下舰船电场水平分量要小于浅海环境下电场水平分量,垂直分量则大于浅海环境下垂直分量,并且水平分量幅度随着海床电导率的增大而减小,垂直分量幅度随海床电导率的增大而增大。因此,对实测数据进行处理时,必须考虑海洋环境电导率参数,采用空气—海水—海床3层模型研究舰船电场分布。 相似文献
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《舰船科学技术》2021,43(13)
根据海上实测海水电导率参数,建立空气—分层海水—海床5层海洋环境模型。基于传统的水平电偶极子空气-海水-海床3层介质模型中水下电场衰减规律和分布特性,通过对海水进一步分层的多层介质模型构建数学模型,进行理论推导和仿真计算,给出场源强度为1A·m,深度为4 m,频率为1 Hz时电场在不同水深处的空间分布及正下方Y=0测线上的水下电场分布。结果表明,随着水深的增加,电场X分量与电场Z分量之比是增加的;在海水-海床界面上,测线上电场Z分量最大值约为电场X分量最大值的1/4,电场Y分量最大值相对Y=0处有一定的偏移。从衰减曲线可以看出,在60~500 m范围内电场X分量和电场Z分量沿径向随距离呈3次方衰减。 相似文献
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将海水看作线形、均匀、各向同性的半无限大导体空间,建立点电极模型,然后利用矢量叠加方法可以推导出极低频时环形电流源产生的电场强度的解析分析式,运用文中推导的电场强度的解析分析式,可以计算海水中任意场点的电场值。 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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