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Atomic Absorption Spectroscopy: Instrumentation01:22

Atomic Absorption Spectroscopy: Instrumentation

An atomic absorption spectrophotometer (AAS) comprises several components: a radiation source, an atomizer, a monochromator, and a detector. The radiation source can be a hollow-cathode lamp (HCL) or an electrodeless-discharge lamp (EDL), both of which provide a narrow emission line of the required wavelength. However, some instruments use continuum sources and high-resolution monochromators to achieve a narrow range of radiation.
The atomizer used in AAS can be either a flame atomizer or an...
Inductively Coupled Plasma Atomic Emission Spectroscopy: Instrumentation01:26

Inductively Coupled Plasma Atomic Emission Spectroscopy: Instrumentation

Inductively coupled plasma (ICP) is the common plasma source used in atomic emission spectroscopy (AES), a technique that detects and analyzes various elements in a sample. This method is often called inductively coupled plasma atomic emission spectroscopy (ICP-AES).
There are three main types of inductively coupled plasma atomic emission spectroscopy  (ICP-AES) instruments: sequential, simultaneous multichannel, and Fourier transform instruments, with the latter being less commonly used.
Atomic Emission Spectroscopy: Lab01:29

Atomic Emission Spectroscopy: Lab

AES is a powerful analytical technique, especially effective when used with plasma sources, producing abundant spectra in characteristic emission lines. The Inductively Coupled Plasma (ICP), in particular, yields superior quantitative analytical data due to its high stability, low noise, low background, and minimal interferences under optimal experimental conditions. However, newer air-operated microwave sources are emerging as promising alternatives that could be more cost-effective than...
Atomic Fluorescence Spectroscopy01:29

Atomic Fluorescence Spectroscopy

Atomic fluorescence spectroscopy (AFS) is an analytical technique that involves the electronic transitions of atoms in a flame, furnace, or plasma being excited by electromagnetic (EM) radiation. When these atoms absorb energy, they become excited and subsequently release energy as they return to their original state. This emitted light, or "fluorescence," is observed at a right angle to the incident beam. Both absorption and emission processes transpire at distinct wavelengths, which are...
Atomic Emission Spectroscopy: Overview01:20

Atomic Emission Spectroscopy: Overview

Atomic emission spectroscopy (AES) is an analytical technique used to determine the elemental composition of a sample by analyzing the light emitted from excited atoms. In AES, atoms in a sample are excited to higher energy levels by thermal energy from high-temperature sources, such as plasma, arcs, or sparks. When these excited atoms return to lower energy states, they emit light at specific wavelengths characteristic of each element. The resulting atomic emission spectrum, which consists of...
Atomic Emission Spectroscopy: Instrumentation01:22

Atomic Emission Spectroscopy: Instrumentation

The instrumentation of atomic emission spectrometry (AES) involves various components, including atomization devices that convert samples into gas-phase atoms and ions. There are two main types of atomization devices: continuous and discrete atomizers.  Continuous atomizers, like plasmas and flames, introduce samples in a constant stream, while discrete atomizers inject individual samples using syringes or autosamplers. The most common discrete atomizer is the electrothermal atomizer.

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Updated: Jul 4, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

A fixed frequency aerosol albedometer.

Jonathan E Thompson1, Nick Barta, Danielle Policarpio

  • 1Department of Chemistry, University of Nebraska at Kearney, Kearney, NE 68849, USA. thompsonje@unk.edu

Optics Express
|June 11, 2008
PubMed
Summary
This summary is machine-generated.

A novel method accurately measures aerosol single scatter albedo (omega) using simultaneous extinction and scattering measurements. This technique enhances atmospheric research by providing precise aerosol optical property data.

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Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

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Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions
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Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

Published on: January 7, 2019

Area of Science:

  • Atmospheric Science
  • Aerosol Physics
  • Optical Remote Sensing

Background:

  • Aerosol optical properties are crucial for climate modeling and air quality assessment.
  • Accurate measurement of aerosol single scatter albedo (omega) is essential for understanding aerosol radiative effects.
  • Existing methods often lack simultaneous measurements of extinction and scattering, leading to potential discrepancies.

Purpose of the Study:

  • To develop and validate a new method for measuring aerosol single scatter albedo (omega) at 532 nm.
  • To enable simultaneous measurement of aerosol extinction coefficient (b(ext)) and scattering coefficient (b(scat)) on the same sample volume.
  • To improve the accuracy and reliability of aerosol optical property determination.

Main Methods:

  • Employed cavity ring-down spectroscopy (CRDS) for precise measurement of aerosol extinction coefficient (b(ext)).
  • Utilized an integrating sphere nephelometer for determining aerosol scattering coefficient (b(scat)).
  • Integrated CRDS and nephelometer measurements to achieve simultaneous data acquisition on identical aerosol samples.

Main Results:

  • Developed a novel method for measuring aerosol single scatter albedo (omega) at 532 nm.
  • Achieved simultaneous measurements of extinction and scattering coefficients on the same aerosol sample volume.
  • Established limits of detection of 0.61 Mm⁻¹ for extinction and 2.7 Mm⁻¹ for scattering (3s).

Conclusions:

  • The developed method provides a significant advancement in the accurate measurement of aerosol optical properties.
  • Simultaneous measurements enhance the reliability of single scatter albedo determination.
  • This technique offers improved data for atmospheric models and air quality studies.