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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Radical Formation: Homolysis00:54

Radical Formation: Homolysis

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Washing, Drying, and Ignition of Precipitates00:52

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After filtration, the precipitate is washed to remove coprecipitated impurities and any remaining mother liquor. Colloidal precipitates, such as silver chloride, are washed with an electrolyte (such as dilute nitric acid) to prevent the peptization of the precipitate. In the case of slightly soluble precipitates, the wash solution contains a common ion to reduce solubility. Lead sulfate, which is slightly soluble in water, is washed with dilute sulfuric acid. Similarly, wash solutions may be...
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Chain Reactions01:29

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Related Experiment Video

Updated: May 11, 2026

Method for Recording Broadband High Resolution Emission Spectra of Laboratory Lightning Arcs
07:51

Method for Recording Broadband High Resolution Emission Spectra of Laboratory Lightning Arcs

Published on: August 27, 2019

Runaway breakdown and hydrometeors in lightning initiation.

A V Gurevich1, A N Karashtin

  • 1PN Lebedev Physical Institute, Russian Academy of Sciences, Moscow 119991, Russia. alex@lpi.ru

Physical Review Letters
|May 21, 2013
PubMed
Summary

Electric pulse discharges in thunderclouds are initiated by runaway breakdown of air in electric fields, driven by extensive atmospheric showers. This process synchronizes microdischarges, leading to charge reset and ion clusters crucial for lightning leader development.

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Last Updated: May 11, 2026

Method for Recording Broadband High Resolution Emission Spectra of Laboratory Lightning Arcs
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Area of Science:

  • Atmospheric physics
  • Electromagnetism
  • Cloud physics

Background:

  • Negative cloud-to-ground lightning initiation involves unique electric pulse discharges.
  • These pulses differ significantly from conventional streamers or leaders.

Purpose of the Study:

  • To analyze the mechanism behind specific electric pulse discharges observed during lightning initiation.
  • To elucidate the role of runaway breakdown of air in electric fields initiated by extensive atmospheric showers (RB-EAS).

Main Methods:

  • Detailed analysis of electric pulse discharges in thunderclouds.
  • Investigating the influence of extensive atmospheric showers (RB-EAS) on air breakdown.
  • Examining microdischarge synchronization at hydrometeors.

Main Results:

  • Pulse shape is determined by runaway breakdown of air in thundercloud electric fields initiated by extensive atmospheric showers (RB-EAS).
  • High pulse electric current amplitude results from synchronized microdischarges at hydrometeors, triggered by RB-EAS-generated electrons.
  • Specific pulse discharges create ion clusters and a region of high fractal ion conductivity.

Conclusions:

  • Charge reset from hydrometeors to free ions and formation of ion clusters are key outcomes.
  • The developed region of high fractal ion conductivity significantly influences charge transport.
  • Ion charge transport is critical for preconditioning the lightning leader.