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convective discharge相关的网络例句

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与 convective discharge 相关的网络例句 [注:此内容来源于网络,仅供参考]

It is the first time in the experiments of atmospheric pressure discharge using wire mesh electrode covered by PET film such fast images were obtained, which indicates that the homogeneous discharge is a Townsend discharge rather than a glow discharge.

在金属丝网电极覆盖PET薄膜的大气压气体放电实验中,这种放电图像被拍摄到,并说明大气压空气中的均匀放电只是汤森放电,而非辉光放电。

Further, a vapor discharge opening and a vapor discharge valve mechanism are provided in that part of the pump channel which is between the air discharge opening and an inlet section of the pump channel. The vapor discharge valve mechanism is closed in the start of the pump, preventing negative pressure at a fuel suction opening from being reduced, and the mechanism is opened in the start of fuel pressurization, discharging fuel containing vapor to the outside of the pump channel.

另外,在上述空气排出口和泵流路的入口部之间的泵流路上设置蒸汽排出口,此外设置蒸汽排出阀机构,其在燃料泵启动时闭阀而防止燃料吸入口的负压降低,如果燃料加压开始则开阀,从而将含有蒸汽的燃料向泵流路的外部排出。

Because the characteristic of the discharge could be strongly affected by the construction of the electrodes, three common used electrodes (direct discharge between two metal electrodes, silent discharge, surface discharge) were analyzed and compared in detail.

结合臭氧形成机理研究,比较了3 种放电形式在产生臭氧方面的特点。研制成功了产品化臭氧发生器,经检测,在使用未经处理的室内空气作为气源时,该发生器的臭氧生成效率为68.44 g/。

The experimental result shows that when the discharge time was more than 1.5μs, small crack emerged in the fuses due to mechanical force on the heated fuse, and the metallized layer would be evaporated as the crack became long enough to generate disruptive discharge. When the discharge time was less than 150ns, small crack emerged in the fuses due to the current heat, and the metallized layer would be evaporated as the crack became long enough to generate disruptive discharge.

实验结果表明:当熔丝的通流时间大于1.5 ms时,电流热效应产生的机械力使安全膜熔丝的金属层产生微小裂纹,当裂纹达到一定长度,两端发生击穿放电,金属层因蒸发而断开;当熔丝中通过较大的电流时,短时间内(50 ns)的电流热效应使熔丝金属层发生熔化产生裂纹,裂纹两端发生击穿放电,金属层因蒸发而断开。

In the second chapter, we investigate propagations of desynchronous disturbances in synchronized chaotic one-way coupled map lattices. It is well known that spatiotemporally chaotic systems with large gradient couplings may show convective instability under the absolute stability condition of chaos synchronization. This convective instability is the key reason for the effective propagation of control signals.

时空混沌在不同的耦合系数情况下会表现出不同的动力学行为,用驱动实现具有强梯度耦合系数的时空混沌同步时,会观察到在绝对稳定条件下被驱动系统表现出对流不稳定性,这种对流不稳定性是在单个信号驱动下实现混沌同步的关键原因。

Convective-type boundary conditions at interface of vessel walls are used in simulating convective heat transfer in blood vessels.

在血管壁施加第三类边界条件是计算血液与组织间对流换热的一种近似计算方法。

At the same time, we discussed the fittable field of deep convective impressible model comparing with the origional pressible equations.The result is that deep convective impressible model is close to the pressible model and is good to be used to simulate troposphere.

本文首先对中小尺度动力学进行理论探讨,特别是与本文有关的深对流不可压动力学模型,比较它与原始可压运动方程组的联系及其适用范围,表明在对流层的研究中使用浅对流不可压模型是不可行的。

The meso-scale convective cell in squall line causes severe convective wind.

由镶嵌在飑线中的小尺度超级单体造成对流性大风。

On the other hand, when the tropical western Pacific is in a cooling state in spring, convective activities are weakened around the Philippines. In this case, there is an anticyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts westward, thus, the late onset of the SCSM can be caused. Moreover, when the tropical western Pacific is also in a cooling state, convective activities around the Philippines are also weak in summer, since the abrupt northward-shift of the western Pacific subtropical high is not obvious in mid-June and early July and it gradually shifts northward during its northward advance in this case, the East Asian summer monsoon rainband can be maintained in the Yangtze River and the Huaihe River valleys.

相反,当春季热带西太平洋处于冷状态,菲律宾周围对流活动弱,在这种情况下,南海上空对流层下层有反气旋性距平环流,西太平洋副热带高压偏西,从而使得南海夏季风爆发晚;并且,当夏季热带西太平洋也处于冷状态,菲律宾周围对流活动也很弱,在这种情况下,西太平洋副热带高压北进时,在6月中旬或7月初向北突跳并不明显,而是以渐进式向北移动,从而使得东亚季风雨带一直维持在长江流域和淮河流域。

The results show that when the tropical western Pacific is in a warming state in spring, convective activities are intensified around the Philippines. In this case, there is a cyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts eastward, thus, the early onset of the South China Sea summer monsoon can be caused. Moreover, when the tropical western Pacific is also in a warming state, convective activities around the Philippines are also strong in summer, since the western Pacific subtropical high abruptly shifts northward in mid-June and early July during its northward advance in this case, the abrupt northward-shift of the East Asian summer monsoon rainband from South China to the Yangtze River and the Huaihe River valleys is obvious in mid-June and this monsoon rainband again jumps northward from the Yangtze River and the Huaihe River valleys to the Yellow River valley, North China and Northeast China in early July.

分析结果表明:当春季热带西太平洋处于暖状态,菲律宾周围对流活动强,在这种情况下,南海上空对流层下层有气旋性距平环流,西太平洋副热带高压偏东,从而使得南海夏季风爆发早;并且,当夏季热带西太平洋也处于暖状态,菲律宾周围对流活动也很强,在这种情况下,西太平洋副热带高压北进时,在6月中旬和7月初存在明显的突跳,从而使得东亚季风雨带在6月中旬明显由华南北跳到江淮流域,并于7月初由江淮流域北跳到黄河流域、华北和东北地区。

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