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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

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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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In precipitation gravimetry, the precipitating agent should react specifically or selectively with the analyte. While a specific reagent reacts with the analyte alone, a selective reagent can react with a limited number of chemical species.
The obtained precipitate should be either a pure substance of known composition or easily converted to one by a simple process, such as ignition or drying. In addition, the precipitate should be insoluble and easily filterable. In general, filterability...
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Precipitation and Co-precipitation01:17

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Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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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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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Simulating Impacts of Ice Storms on Forest Ecosystems
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Prediction of Lightning Inception by Large Ice Particles and Extensive Air Showers.

Anna Dubinova1, Casper Rutjes1, Ute Ebert1,2

  • 1Centrum Wiskunde & Informatica (CWI), Amsterdam, Netherlands.

Physical Review Letters
|July 17, 2015
PubMed
Summary

Lightning can initiate under specific conditions, requiring an electric field at 15% of breakdown strength, elongated ice particles, and sufficient free electrons. These factors, alongside cosmic ray air showers, can trigger atmospheric discharges.

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Area of Science:

  • Atmospheric Physics
  • Electromagnetism
  • Cloud Microphysics

Background:

  • Understanding the precise conditions for lightning initiation is crucial for atmospheric science and electrical safety.
  • Previous models often simplified the complex interplay of atmospheric electricity, ice particle properties, and cosmic ray interactions.

Purpose of the Study:

  • To determine the minimum conditions required for lightning initiation.
  • To investigate the role of ice particle size, free electron density, and electric fields in triggering atmospheric discharges.

Main Methods:

  • Utilizing computational simulations incorporating the permittivity of ice ε(ω).
  • Modeling atmospheric conditions with specific parameters for electric field strength, ice particle dimensions, and free electron concentrations.
  • Analyzing the influence of cosmic ray air showers on electron density.

Main Results:

  • Lightning can be initiated when the electric field reaches 15% of the breakdown field.
  • Elongated ice particles (6 cm) and a density of 100 free electrons/cm³ are identified as key factors.
  • Simulations indicate that a 3m high and 0.2 km² electric field zone can trigger at least one discharge per minute.

Conclusions:

  • The study provides a specific parameter set for lightning initiation, highlighting the importance of ice particle size distribution.
  • Cosmic ray-induced air showers play a role in achieving the necessary free electron density at high altitudes.
  • Further detailed measurements of ice particle size distribution are recommended to refine lightning prediction models.