Pin-to-plane self-pulsing discharge in transversal airflow: interaction with a substrate of plasma filaments blown out from the discharge zone

2020 ◽  
Vol 29 (4) ◽  
pp. 045012
Author(s):  
Yu S Akishev ◽  
A A Balakirev ◽  
M E Grushin ◽  
V B Karalnik ◽  
M A Medvedev ◽  
...  
2018 ◽  
Vol 49 (3) ◽  
pp. 251-262
Author(s):  
Vyacheslav Konstantinovich Alatortsev ◽  
Sergei Ivanovich Inshakov ◽  
Ivan Sergeevich Inshakov ◽  
Aleksandr Fedorovich Rozhkov ◽  
Vladimir Vladimirovich Skvortsov ◽  
...  

2020 ◽  
Vol 11 (11) ◽  
pp. 17-27
Author(s):  
Vadim V. VOEVODIN ◽  
◽  
Marina V. SOKOLOVA ◽  
Viktor R. SOLOV’YEV ◽  
Nikolay Yu. LYSOV ◽  
...  

The results from an experimental study of impulse surface discharge occurring in an electrode system containing a dielectric plate are presented. On one of its sides, the plate had a corona-producing electrode made of 50 mm thick copper foil grounded through a current shunt for measuring the discharge current. On its other side, the plate had a high-voltage electrode, to which the voltage from a pulse generator was applied. The article presents the results from measurements of the initial voltage and the sizes of the surface discharge area in air when applying single voltage pulses with different pulse front steepness in the range 0,1–3,4 kV/ms and amplitude in the range 7–15 kV. The measurements were carried out for different dielectric barrier materials with the e values from 2 to 35. The dielectric barrier thickness was 0,9–1,8 mm. The study results have shown that the initial surface discharge ignition voltage depends essentially on the voltage pulse parameters, whereas the barrier characteristics have a weaker effect on this voltage. It has been determined that the discharge has different discharge zone length and different structure depending on the dielectric barrier properties and applied voltage parameters. The streamer zone sizes decrease with increasing the barrier material e value at the same voltage pulse steepness and increase with increasing the steepness for each barrier material. The data obtained for a wide range of external conditions can be used in numerical modeling of discharge.


Soil Research ◽  
2008 ◽  
Vol 46 (1) ◽  
pp. 37 ◽  
Author(s):  
M. R. Sargeant ◽  
C. Tang ◽  
P. W. G. Sale

Landholder observations indicate that the growth of Distichlis spicata in saline discharge sites improves the soil condition. An extensive soil sampling survey was conducted at the Wickepin field site in Western Australia, where D. spicata had been growing for 8 years, to test the hypothesis that this halophytic grass will make improvements in chemical and physical properties of the soil. Soil measurements included saturated hydraulic conductivity, water-stable aggregates, root length and dry weight, electrical conductivity, pH, and soil nitrogen and carbon. Results confirm that marked differences in soil properties occurred under D. spicata. For example, a 12-fold increase in saturated hydraulic conductivity occurred where D. spicata had been growing for 8 years, compared to adjacent control soil where no grass had been growing. There were also improvements in aggregate stability, with the most notable improvements in the top 0.10 m of soil, again with the greatest improvements occurring where 8 years of growth had occurred. Soil nitrogen and carbon increased under the sward, with the biggest increases occurring in the top 0.10 m of soil. Electrical conductivity measurements were more variable, mostly due to the large spatial and temporal variation encountered. However, the findings generally support the proposition that the growth of D. spicata does not lead to an accumulation of salt within the rooting zone.


1986 ◽  
Vol 56 (2) ◽  
pp. 409-423 ◽  
Author(s):  
A. Konnerth ◽  
U. Heinemann ◽  
Y. Yaari

Epileptiform activity induced in rat hippocampal slices by lowering extracellular Ca2+ concentration ([Ca2+]o) was studied with extracellular and intracellular recordings. Perfusing the slices with low Ca2+ (less than or equal to 0.2 mM) or EGTA-containing solutions blocked the synaptic responses of hippocampal pyramidal cells (HPCs). Despite the block, spontaneous paroxysms, termed seizurelike events (SLEs), appeared in the CA1 area and then recurred regularly at a stable frequency. Transient hypoxia accelerated their development and increased their frequency. When [Ca2+]o was raised in a stepwise manner, the SLEs disappeared at 0.3 mM. With extracellular recording from the CA1 stratum pyramidale, a SLE was characterized by a large negative shift in the field potential, which lasted for several seconds. During this period a large population of CA1 neurons discharged intensely and often in synchrony, as concluded from the frequent appearance of population spikes. Synchronization, however, was not a necessary precursor for the development of paroxysmal activity, but seemed to be the end result of massive neuronal excitation. The cellular counterpart of a SLE, as revealed by intracellular recording from HPCs in the discharge zone of the paroxysms, was a long-lasting depolarization shift (LDS) of up to 20 mV. This was accompanied by accelerated firing of the neuron. A prolonged after-hyperpolarization succeeded each LDS and arrested cell firing. Brief (approximately 50 ms) bursts were commonly observed before LDS onset. Single electrical stimuli applied focally to the stratum pyramidale or alveus evoked paroxysms identical to the spontaneous SLEs, provided they surpassed a critical threshold intensity. Subthreshold stimuli elicited only small local responses, whereas stimuli of varied suprathreshold intensities evoked the same maximal SLEs. Thus the buildup of a SLE is an all or nothing or a regenerative process, which mobilizes the majority, if not all, of the local neuronal population. Each SLE was followed by absolute and relative refractory periods during which focal stimulation was, respectively, ineffective and less effective in evoking a maximal SLE. In most slices the spontaneous SLEs commenced at a "focus" located in the CA1a subarea (near the subiculum). SLEs evoked by focal stimulation arose near the stimulating electrode. From their site of origin the paroxysmal discharges spread transversely through the entire CA1 area at a mean velocity of 1.74 mm/s. Consequently, the discharge zone of a SLE could encompass for several seconds the entire CA1 area.(ABSTRACT TRUNCATED AT 400 WORDS)


2005 ◽  
Vol 247 (1-3) ◽  
pp. 171-180 ◽  
Author(s):  
G. Méchain ◽  
C.D’Amico ◽  
Y.-B. André ◽  
S. Tzortzakis ◽  
M. Franco ◽  
...  

Water ◽  
2022 ◽  
Vol 14 (2) ◽  
pp. 165
Author(s):  
Alexander I. Malov ◽  
Evgeniya S. Sidkina ◽  
Mikhail V. Mironenko ◽  
Alexey S. Tyshov ◽  
Elena V. Cherkasova

The technogenic impact of the development of the Lomonosov diamond deposit is associated with the discharge of quarry and drainage water into the river, which has a special conservation status. Earlier studies on the composition of bottom sediments showed that there are signs of increased accumulation of heavy metals and radionuclides at wastewater discharge sites. The purpose of this work was to predict changes in the composition of surface water and bottom sediment in the river during the further development of mining operations with brackish and salty water captured by drainage systems, the presence of which was established in the zone of their future influence. For this, a simulation of changes in the composition of the water in the river was carried out using the GEOCHEQ software package by minimizing the free energy of the system using a convex simplex algorithm. It was found that the maximum salinity of surface water can reach 1.51 g/L. In this case, the MPC of Cl−, Na+, SO42−, Mg2+, Sr, V, and U can be exceeded for fishery watercourses. The genetic basis of the accumulation of these components in solutions for mixing was considered. According to the calculations, when about 5000 m3/h of drainage water is discharge d into the river, the mass of precipitated chemical elements will be 56–191 t/h, including up to 2.1 t/h of iron; therefore, accumulation in the discharge zone must be controlled.


Author(s):  
Wouter Tierens ◽  
James R Myra ◽  
Roberto Bilato ◽  
Laurent Colas

Abstract Perkins et al. PRL 2012 [1] reported unexpected power losses during High Harmonic Fast Wave (HHFW) heating and current drive in NSTX. Recently, Tierens et al [2] proposed that these losses may be attributable to surface waves on field-aligned plasma filaments, which carry power along the filaments, to be lost at the endpoints where the filaments intersect the limiters. In this work, we show that there is indeed a resonant loss mechanism associated with the excitation of these surface waves, and derive an analytic expression for the power lost to surface wave modes at each filament.


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