Probing Luminescent Radiation of Positive Streamer in Atmospheric Air: Experiments at Low Temperature

2020 ◽  
Vol 27 (6) ◽  
pp. 1-8
Author(s):  
Yong Yi ◽  
Tohid Shahsavarian ◽  
Wenxi Tang ◽  
Liming Wang ◽  
Fanghui Yin
2019 ◽  
Vol 68 (9) ◽  
pp. 095202
Author(s):  
Jing-Yi Tu ◽  
She Chen ◽  
Feng Wang

The proportion of krypton and xenon in dry air has been measured by a method using distillation and low-temperature gas-chromatography for the isolation of krypton and xenon. The separation has been controlled by the use of radioactive 85 Kr tracer. The krypton content of dry air is 1⋅139 ± 0⋅01 x 10 -6 by volume. The xenon content of dry air is 0⋅086 ± 0⋅001 x 10 -6 by volume.


2018 ◽  
Vol 25 (12) ◽  
pp. 123507 ◽  
Author(s):  
Shuqun Wu ◽  
Wenxin Cheng ◽  
Guowang Huang ◽  
Fei Wu ◽  
Chang Liu ◽  
...  

Some time ago I communicated to the Society the results of an attempt to estimate the amounts of krypton and of xenon in air. The quantities were necessarily minimum estimates, for there is no doubt that both krypton and xenon must evaporate when air evaporates, even if that take place at a very low temperature. Dr. Travers and I guessed at the amounts of neon and helium, and supposed that the amount of helium was one or two parts per million, and that of neon one or two parts per 100,000. This guess is not very far from the truth, as the following account of recent experiments will show. The ingenious method discovered by Sir James Dewar of using cooled cocoanut charcoal as an absorbent for gases has made it easy to carry out the estimation. The process consists in cooling 100 grammes of such charcoal to — 100°, approximately, in a bulb from which all air has been removed by a pump. Such charcoal will absorb about three litres of air; at that temperature neither neon nor helium are absorbed in appreciable quantity, as special experiments showed. Hence on placing the cooled bulb containing the char­coal in communication with a Töpler pump, the uncondensed gases enter the barrel of the pump. On closing the connecting stop-cock, a further quantity of gas accumulates, and is again removed into the pump in the same manner. As the relative volumes of the pump and of the cooled bulb were approxi­mately 4 to 1, after communication had been established four times, only 1/256 of the contents of the bulb were left in it. And as the gas in contact with charcoal exerts a kind of vapour-pressure, inasmuch as the pressure which it gives depends on the temperature as well as on the extent of the surface of charcoal to which it is exposed, it may be assumed that gas escapes from the charcoal on each reduction of pressure, and that the more volatile gases in the bulb should be expelled by the less volatile.


2018 ◽  
Vol 25 (6) ◽  
pp. 2086-2092 ◽  
Author(s):  
Chunjie Wang ◽  
Hongwei Mei ◽  
Wenxi Tang ◽  
Liming Wang

2008 ◽  
Vol 5 (5) ◽  
pp. 482-488 ◽  
Author(s):  
Xing‐Min Shi ◽  
Guan‐Jun Zhang ◽  
Yu‐Kang Yuan ◽  
Yue Ma ◽  
Gui‐Min Xu ◽  
...  

2014 ◽  
Vol 42 (10) ◽  
pp. 2418-2419 ◽  
Author(s):  
Takao Matsumoto ◽  
Koji Kijima ◽  
Yasuji Izawa ◽  
Kiyoto Nishijima

Author(s):  
P.P.K. Smith

Grains of pigeonite, a calcium-poor silicate mineral of the pyroxene group, from the Whin Sill dolerite have been ion-thinned and examined by TEM. The pigeonite is strongly zoned chemically from the composition Wo8En64FS28 in the core to Wo13En34FS53 at the rim. Two phase transformations have occurred during the cooling of this pigeonite:- exsolution of augite, a more calcic pyroxene, and inversion of the pigeonite from the high- temperature C face-centred form to the low-temperature primitive form, with the formation of antiphase boundaries (APB's). Different sequences of these exsolution and inversion reactions, together with different nucleation mechanisms of the augite, have created three distinct microstructures depending on the position in the grain.In the core of the grains small platelets of augite about 0.02μm thick have farmed parallel to the (001) plane (Fig. 1). These are thought to have exsolved by homogeneous nucleation. Subsequently the inversion of the pigeonite has led to the creation of APB's.


Author(s):  
S. Edith Taylor ◽  
Patrick Echlin ◽  
May McKoon ◽  
Thomas L. Hayes

Low temperature x-ray microanalysis (LTXM) of solid biological materials has been documented for Lemna minor L. root tips. This discussion will be limited to a demonstration of LTXM for measuring relative elemental distributions of P,S,Cl and K species within whole cells of tobacco leaves.Mature Wisconsin-38 tobacco was grown in the greenhouse at the University of California, Berkeley and picked daily from the mid-stalk position (leaf #9). The tissue was excised from the right of the mid rib and rapidly frozen in liquid nitrogen slush. It was then placed into an Amray biochamber and maintained at 103K. Fracture faces of the tissue were prepared and carbon-coated in the biochamber. The prepared sample was transferred from the biochamber to the Amray 1000A SEM equipped with a cold stage to maintain low temperatures at 103K. Analyses were performed using a tungsten source with accelerating voltages of 17.5 to 20 KV and beam currents from 1-2nA.


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