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Comparison of Laser-Extinction and Natural Luminosity Measurements for Soot Probing in Diesel Optical Engines

机译:柴油光学发动机烟灰探测的激光消光和自然发光度测量的比较

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Soot emissions from diesel internal combustion engines are strictly regulated nowadays. Laser extinction measurement (LEM) and natural luminosity (NL) of sooty flames are commonly applied to study soot. LEM measures soot along the laser beam path and it can probe soot regardless of temperature. NL integrates the whole field of view and relies on soot temperature. In this work, a comparison of simultaneously recorded LEM and NL data has been performed in a heavy-duty optical engine. A 685 nm laser beam is used for LEM. The laser was modulated at 63 kHz, which facilitated subtraction of the background NL signal from the raw LEM data. By Beer-Lambert’s law, KL factor can be calculated and used as a metric to describe soot measurements. A compensation of transmitted laser intensity fluctuation and soot deposits on optical windows has been performed in this work. The data compensation successfully reduced the transmitted laser intensity fluctuation and made it possible to study in-cylinder low temperature soot residual. The KL curves were compared with NL curve in this work. In the late cycle the KL curve can successfully show the low temperature soot which is not detected by NL. The KL curve is found to rise about 2 CAD ahead of the corresponding NL curve due to liquid fuel spray disturbance. In this case, LEM is not a suitable method to calculate KL for analyzing the early soot formation if there are liquid phase fuel droplets crossing the probing laser beam.
机译:柴油内燃机的烟灰排放现在是严格调节的。 SOOTAY火焰的激光消光测量(LEM)和天然亮度(NL)通常用于研究烟灰。 lem沿着激光束路径测量烟灰,无论温度如何,都可以探测烟灰。 NL整合整个视野并依赖于烟灰温度。在这项工作中,在重型光学引擎中执行了同时记录的LEM和NL数据的比较。 685nm激光束用于LEM。激光在63 kHz下调制,这促进了从原始LEM数据中的背景NL信号的减法。通过Beer-Lambert的定律,可以计算KL因子并用作指标以描述烟灰测量。在这项工作中,已经在这项工作中进行了透射激光强度波动和烟灰沉积物的补偿。数据补偿成功地降低了透射的激光强度波动,并使其可以研究缸内低温烟灰残留。在这项工作中将KL曲线与NL曲线进行比较。在后期循环中,KL曲线可以成功地显示NL未检测到的低温烟灰。由于液体燃料喷雾干扰,发现KL曲线在相应的NL曲线前提高了约2 cad。在这种情况下,如果存在穿过探测激光束的液相燃料液滴,则lem不是计算用于分析早期烟灰地层的K1的合适方法。

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