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Streamer-to-spark transition initiated by a nanosecond overvoltage pulsed discharge in air

机译:通过空气中的纳秒过压脉冲放电发起的飘带到火花转变

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This study is focused on the streamer-to-spark transition generated by an overvoltage nanosecond pulsed discharge under atmospheric pressure air in order to provide a quantitative insight into plasma-assisted ignition. The discharge is generated in atmospheric pressure air by the application of a positive high voltage pulse of 35 kV to pin-to-pin electrodes and a rise time of 5 ns. The generated discharge consists of a streamer phase with high voltage and high current followed by a spark phase characterized by a low voltage and a decreasing current in several hundreds of nanosecond. During the streamer phase, the gas temperature measured by optical emission spectroscopy related to the second positive system of nitrogen shows an ultra-fast gas heating up to 1200 K at 15 ns after the current rise. This ultra-fast gas heating, due to the quenching of electronically excited species by oxygen molecules, is followed by a quick dissociation of molecules and then the discharge transition to a spark. At this transition, the discharge contracts toward the channel axis and evolves into a highly conducting thin column. The spark phase is characterized by a high degree of ionization of nitrogen and oxygen atoms shown by the electron number density and temperature measured from optical emission spectroscopy measurements of N~+ lines. Schlieren imaging and optical emission spectroscopy techniques provide the time evolution of the spark radius, from which the initial pressure in the spark is estimated. The expansion of the plasma is adiabatic in the early phase. The electronic temperature and density during this phase allows the determination of the isentropic coefficient. The value around 1.2-1.3 is coherent with the high ionization rate of the plasma in the early phase. The results obtained in this study provide a database and the initial conditions for the validation of numerical simulations of the ignition by plasma discharge.
机译:该研究专注于由大气压力空气下的过电压纳秒脉冲放电产生的拖面式过渡,以便提供对等离子体辅助点火的定量洞察。通过在大气压空气中施加35kV的正高电压脉冲以销钉电极和5 ns的上升时间来产生排出。产生的放电由具有高电压和高电流的拖缆相位,然后是由低电压的传感的火花阶段和几百纳秒内的电流降低。在炉阶段期间,通过与氮的第二正系统相关的光发射光谱法测量的气体温度显示出在电流上升后15ns的超快速气体加热至1200k。这种超快气体加热由于氧分子通过电子激发物质淬火,然后是分子的快速解离,然后将放电过渡到火花。在这种过渡时,排放朝向通道轴线并进化成高导电的薄塔。火花阶段的特征在于通过N〜+线的光发射光谱测量测量的电子数密度和温度所示的氮和氧原子的高度电离。 Schlieren成像和光发射光谱技术提供了火花半径的时间演变,从中估计了火花中的初始压力。血浆的膨胀是在早期阶段的绝热。在该阶段期间的电子温度和密度允许确定等熵系数。 1.2-1.3左右的值与早期血浆的高电离速率相干。本研究中获得的结果提供了一种数据库和初始条件,用于通过等离子体放电验证点火的数值模拟。

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