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本文介绍了NF3生产过程中静电产生、积聚和放电的过程,分析了NF3生产过程中静电爆炸危害,并提出了相应的防护措施。 相似文献
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高纯三氟化氮气体在电子工业中有着广阔的应用前景,在生产过程中常存在微粒子的污染问题,本文介绍了目前工业化生产三氟化氮(NF3)过程中微粒子产生的原因及几种不锈钢管路和阀门、附件的处理方法。 相似文献
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本文叙述了使用电解臭氧处理水的装置和方法。其组成是:在电解池的阳极室电解水产生含臭氧气体,含臭氧气体从阳极电解质中分离,用分离的含臭氧气体与处理的水接触。处理的水与电解的水是有区别的。 相似文献
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采用CFD方法对压缩空气吹除主压载水舱过程进行仿真,同时开展水舱吹除等比模型试验,验证了两种湍流模型的预报准确性。在此基础上,着重研究水舱气液两相流动过程以及舱内气体压力动态变化特性,分析气源压力、通海孔面积对吹除的影响。研究发现:两种湍流模型均可以较好地预测水舱吹除过程,其中,Realizable k-ε模型对气瓶气体压力的预测与试验吻合更好;SST k-ω模型对于水舱中气体压力的预测与试验相对较为接近。通海孔面积增加可以显著减弱水舱气体积压,在气源压力为2.16 MPa、5.04 MPa和8.16 MPa时,通海孔面积增大5.14倍,试验测得的水舱峰压分别减少51.13%、59.90%和64.82%,仿真得到的水舱峰压分别减少50.44%、57.30%和60.02%。在吹除后期,有压缩空气从通海孔溢出,舱内气体压力迅速下降,可以此作为解除吹除的判据。 相似文献
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由于Mie-Grüneisen状态方程形式比较复杂,给界面的处理带来很大难度.本文通过对Euler方程做分离变量和引入质量分数,完成了Mie-Grüneisen状态方程下的多介质可压缩流动的数值模拟,使计算过程得到简化,并通过算例验证了该方法的可靠性.在多项式形式的Mie-Grüneisen状态方程下,利用该方法模拟了球形炸药在水中爆炸后,气体和水相互作用的近场情况.在计算模型中引入的气体质量分数,很好反映了流场中不同区域内气体、水及水气并存3种不同的状态. 相似文献
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本文介绍了SPE水电解技术核心部分SPE电解槽中膜、膜电极组件、集电器、槽体结构的技术关键及解决途径,SPE水电解技术的发展趋势及对我所SPE水电解技术发展的分析。 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