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Related Concept Videos

Oxidative Cleavage of Alkenes: Ozonolysis01:46

Oxidative Cleavage of Alkenes: Ozonolysis

In ozonolysis, ozone is used to cleave a carbon–carbon double bond to form aldehydes and ketones, or carboxylic acids, depending on the work-up.
Ozone is a symmetrical bent molecule stabilized by a resonance structure.
UV–Vis Spectroscopy: Woodward–Fieser Rules01:29

UV–Vis Spectroscopy: Woodward–Fieser Rules

UV–Visible absorption spectra of conjugated dienes arise from the lowest energy π → π* transitions. The light-absorbing part of the molecule is called the chromophore, and the substituents directly attached to the chromophore are called auxochromes. A strong correlation exists between the absorption maxima, λmax, and the structure of a conjugated π system. The Woodward–Fieser rules predict the value of λmax for a given structure by adding the contributions...
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There are two ways to determine the amount of heat involved in a chemical change: measure it experimentally, or calculate it from other experimentally determined enthalpy changes. Some reactions are difficult, if not impossible, to investigate and make accurate measurements for experimentally. And even when a reaction is not hard to perform or measure, it is convenient to be able to determine the heat involved in a reaction without having to perform an experiment.
Ostwald’s Dilution Law01:25

Ostwald’s Dilution Law

Consider a binary electrolyte AB with a concentration ‘c’ that reversibly dissociates into its constituent ions. The degree of this dissociation is represented by ⍺. This means that the equilibrium concentration of each ionic species can be expressed as ⍺c. As well as this, the fraction of the electrolyte that remains undissociated at equilibrium is given by (1−⍺). The corresponding equilibrium concentration for this undissociated portion is then calculated as (1−⍺)c. For such solutions,...
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Half-life of a Reaction02:42

Half-life of a Reaction

The half-life of a reaction (t1/2) is the time required for one-half of a given amount of reactant to be consumed. In each succeeding half-life, half of the remaining concentration of the reactant is consumed. For example, during the decomposition of hydrogen peroxide, during the first half-life (from 0.00 hours to 6.00 hours), the concentration of H2O2 decreases from 1.000 M to 0.500 M. During the second half-life (from 6.00 hours to 12.00 hours), the concentration decreases from 0.500 M to...

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Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
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The vanishing ozone weekday/weekend effect.

George T Wolff1, Dennis F Kahlbaum, Jon M Heuss

  • 1Air Improvement Resource, Inc., 47298 Sunnybrook Lane, Suite 103, Novi, MI, 48374, USA. gwolff@airimprovement.com

Journal of the Air & Waste Management Association (1995)
|April 6, 2013
PubMed
Summary

Weekend ozone levels were once higher than weekdays in many cities due to lower precursor emissions. Recent emission controls have largely eliminated this ozone phenomenon, with most areas showing little weekend/weekday difference.

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Area of Science:

  • Environmental Science
  • Atmospheric Chemistry
  • Air Quality Research

Background:

  • Historically, urban areas exhibited higher weekend ozone (O3) concentrations despite lower precursor emissions.
  • This weekend ozone phenomenon was prevalent in the late 1990s, particularly in the Northeast, Midwest, and coastal California.

Purpose of the Study:

  • To analyze the changes in weekday/weekend ozone concentration differences from the late 1990s to the late 2000s.
  • To investigate the impact of evolving ozone precursor emission trends on observed ozone levels.

Main Methods:

  • National analysis of weekday/weekend ozone (O3) data from 1997-1999 and 2008-2010.
  • Comparison of 8-hr maximum O3 concentrations and other O3 metrics across different time periods.
  • Examination of trends in ozone precursor emissions, specifically nitrogen oxides (NOx) and volatile organic compounds (VOCs).

Main Results:

  • The phenomenon of higher weekend O3 concentrations significantly declined between 1997-1999 and 2008-2010.
  • The percentage of sites with higher weekend O3 dropped from ~35% to <5%, while sites with higher weekday O3 increased from 3% to ~27%.
  • Increased VOC/NOx emission ratios, driven by greater NOx reductions, appear to be the primary reason for this shift.

Conclusions:

  • Weekend emission reductions, often linked to motor vehicle use, served as an inadvertent test of ozone control strategies.
  • Implemented emission controls have largely resolved the issue of higher weekend ozone in most urban areas.
  • Current emission control strategies suggest that weekend emission reductions have minimal impact on ozone concentrations in most locations.