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Related Concept Videos

Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

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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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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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Types of Coprecipitation01:10

Types of Coprecipitation

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Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
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Global Climate Change01:50

Global Climate Change

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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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Precipitation of Ions03:11

Precipitation of Ions

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Predicting Precipitation
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Precipitate Formation and Particle Size Control01:16

Precipitate Formation and Particle Size Control

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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.
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Updated: Aug 9, 2025

Production and Measurement of Organic Particulate Matter in the Harvard Environmental Chamber
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Pyrocumulonimbus affect average stratospheric aerosol composition.

J M Katich1,2, E C Apel3, I Bourgeois1,2

  • 1National Oceanic and Atmospheric Administration (NOAA) Chemical Sciences Laboratory (CSL), Boulder, CO, USA.

Science (New York, N.Y.)
|February 23, 2023
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Summary
This summary is machine-generated.

Wildfire-generated pyrocumulonimbus (pyroCb) clouds inject smoke into the stratosphere. These pyroCb contribute significantly to stratospheric aerosols, with potential for dominant future climate impacts.

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Area of Science:

  • Atmospheric Science
  • Climate Science
  • Aerosol Science

Background:

  • Pyrocumulonimbus (pyroCb) clouds, formed by wildfires, inject smoke into the stratosphere.
  • The climate impacts of pyroCb are uncertain due to their episodic nature.

Purpose of the Study:

  • To quantify the contribution of pyroCb smoke to the stratospheric aerosol budget.
  • To understand the long-term influence of pyroCb activity on stratospheric aerosols.

Main Methods:

  • Analysis of 13 years of airborne observations.
  • In situ measurements of pyroCb smoke properties.

Main Results:

  • PyroCb smoke exhibits distinctive and stable aerosol properties.
  • PyroCb contribute 10-25% of black carbon and organic aerosols in the present-day lower stratosphere.
  • Impacts are observed in both Northern and Southern Hemispheres.

Conclusions:

  • PyroCb significantly influence the stratospheric aerosol budget.
  • Increased pyroCb frequency or magnitude in future climates could lead to dominant stratospheric aerosol trends.