Is the electron avalanche process in a martian dust devil self-quenching?

被引:21
作者
Farrell, W. M. [1 ]
McLain, J. L. [2 ]
Collier, M. R. [1 ]
Keller, J. W. [1 ]
Jackson, T. J. [1 ]
Delory, G. T. [3 ]
机构
[1] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[2] Univ Maryland, College Pk, MD 20742 USA
[3] Univ Calif Berkeley, Berkeley, CA 94720 USA
关键词
Mars; Meteorology; OXIDANT ENHANCEMENT; STORMS; DISCHARGES; FIELDS; MARS;
D O I
10.1016/j.icarus.2015.04.003
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Viking era laboratory experiments show that mixing tribocharged grains in a low pressure CO2 gas can form a discharge that glows, indicating the presence of an excited electron population that persists over many seconds. Based on these early experiments, it has been predicted that martian dust devils and storms may also contain a plasma and new plasma chemical species as a result of dust grain tribo-charging. However, recent results from modeling suggest a contrasting result: that a sustained electron discharge may not be easily established since the increase in gas conductivity would act to short-out the local E-fields and quickly dissipate the charged grains driving the process. In essence, the system was thought to be self-quenching (i.e., turn itself off). In this work, we attempt to reconcile the difference between observation and model via new laboratory measurements. We conclude that in a Mars-like low pressure CO2 atmosphere and expected E-fields, the electron current remains (for the most part) below the expected driving tribo-electric dust currents (similar to 10 mu A/m(2)), thereby making quenching unlikely. Published by Elsevier Inc.
引用
收藏
页码:333 / 337
页数:5
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