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Attenuated total reflectance (ATR) infrared spectroscopy is a powerful analytical technique used to study the composition of materials. It is widely employed in chemistry, materials science, forensic science, and other fields where sample characterization is required. ATR has several advantages over traditional transmission IR spectroscopy, including the requirement of little to no sample preparation and the ability to analyze a wide range of samples.
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When electromagnetic radiation passes through a material, atoms or molecules transition from a lower to a higher energy state by absorbing radiation corresponding to the energy difference between the two states. The absorption of infrared (IR) radiation causes transitions between vibrational energy levels in a molecule. Therefore, IR spectroscopy is a useful analytical tool for determining the molecular structure of molecules.
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IR Spectrometers

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There are two main infrared (IR) spectrophotometers: dispersive IR spectrometers and Fourier transform infrared (FTIR) spectrometers. In a dispersive IR spectrometer, a beam of infrared radiation produced by a hot wire is divided into two parallel equal-intensity beams using mirrors. One beam passes through the sample, while another is a reference beam. The beams then move through the monochromator, which separates the radiations into a continuous spectrum of different frequencies. The...
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In a flame photometer, when a solution like potassium chloride is aspirated into the flame, the solvent evaporates, leaving behind dehydrated salt. This salt dissociates into free gaseous atoms in their ground state. Some of these atoms absorb energy from the flame, leading to their excitation. The excited atoms return to the ground state, emitting photons at characteristic wavelengths. Because only electronic transitions are involved, the resulting emission lines are very narrow. The intensity...
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Atomic Absorption Spectroscopy (AAS) atomizes samples through flame atomization or electrothermal atomization. Flame atomization typically involves a nebulizer and spray chamber assembly to combine the sample with a fuel–oxidant mixture, creating a fine aerosol mist that enters a burner. Typically, the fuel and oxidant are combined in an approximately stoichiometric ratio. However, for atoms that are easily oxidized, a fuel-rich mixture may be more advantageous. Only about 5% of the...
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Volatilization gravimetry is an analytical technique that measures the mass lost due to the volatilization of the substance. This technique is used to estimate the amount of volatile material in a sample. To perform this method, heat a known amount of the sample to a high temperature in a crucible or other suitable vessel. The volatile substance in the sample evaporates, and the vapor is completely expelled from the crucible either by heating the sample or bubbling a stream of inert gas through...
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Artificial cloud test confirms volcanic ash detection using infrared spectral imaging.

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Airborne volcanic ash detection is crucial for aviation safety. A new infrared camera system, Airborne Volcanic Object Imaging Detector (AVOID), has successfully demonstrated remote detection of volcanic ash clouds from a long-range aircraft.

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Area of Science:

  • Earth and Planetary Science
  • Atmospheric Science
  • Aviation Safety

Background:

  • Airborne volcanic ash poses a significant hazard to aviation safety.
  • Current detection methods are insufficient for fine ash particles and visual detection is unreliable.
  • The 2010 Eyjafjallajökull eruption highlighted the need for advanced ash detection systems.

Purpose of the Study:

  • To evaluate the capability of a novel bi-spectral infrared camera system (AVOID) for detecting volcanic ash.
  • To assess the system's performance in detecting and quantifying ash clouds from commercial jet aircraft distances.
  • To demonstrate the feasibility of airborne remote sensing for volcanic ash.

Main Methods:

  • Development and deployment of a bi-spectral, fast-sampling, uncooled infrared camera (AVOID).
  • Conducted an experiment over the Atlantic Ocean using a controlled artificial ash cloud.
  • Utilized a second aircraft for ash dispersal and a third for in-situ measurements with optical particle counters.

Main Results:

  • The AVOID system successfully detected and quantified volcanic ash clouds at distances of 20-70 km.
  • The system identified ash concentrations of approximately 200 μg m⁻³ in a cloud of fine ash (mean radii ~10 μm).
  • Demonstrated successful airborne remote detection of volcanic ash from a long-range flight test.

Conclusions:

  • The AVOID system shows significant promise for the remote detection of airborne volcanic ash.
  • This technology can contribute to keeping airspace open and preventing aircraft groundings during volcanic events.
  • Successful long-range flight tests confirm the viability of this approach for enhanced aviation safety.