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Related Concept Videos

Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview01:13

Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview

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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Infrared (IR) Spectroscopy: Overview01:09

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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.
Different compounds display unique properties due to their...
Ultraviolet and Visible (UV–Vis) Spectroscopy: Overview01:02

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Ultraviolet–visible (UV–visible or UV–Vis) spectroscopy is an analytical technique that investigates the interaction between matter and UV–Vis light within the electromagnetic spectrum. This method is widely used for its versatility, simplicity, and relatively quick data acquisition, making it valuable for both qualitative and quantitative analysis. When UV–Vis radiation passes through a material,  molecules absorb light depending on the energy required for electronic transitions. As a result...
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IR Spectrometers

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...
Applications of IR Spectroscopy: Overview01:11

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The non-destructive nature and ability to provide valuable chemical information make IR spectroscopy a versatile technique with broad applications in various scientific and industrial fields. IR spectroscopy is commonly used to identify and characterize organic and inorganic compounds. It provides information about the functional groups present in a molecule and the bonding between atoms. This helps in the structural elucidation of compounds during organic synthesis, pharmaceutical research,...
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When light passes through a substance, a portion of the light is absorbed while the remaining light is reflected or transmitted. If the molecule absorbs light between the wavelengths of 180–400 nm range, the UV spectrum is obtained, and if it absorbs light in the 400–780 nm wavelength range, the visible spectrum is obtained.     
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Related Experiment Video

Updated: Jun 17, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Near infrared scattering by sunlit terrestrial clouds.

H H Blau1, R P Espinola, E C Reifenstein

  • 1Arthur D. Little, Inc., Cambridge, Massachusetts 02140, USA.

Applied Optics
|January 6, 2010
PubMed
Summary
This summary is machine-generated.

Cloud scattering spectra reveal differences between ice and liquid water clouds in the 1.15- to 3.6-micrometer range. Particle size significantly impacts scattering efficiency and spectral features, aligning with theoretical predictions.

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Area of Science:

  • Atmospheric optics
  • Cloud physics
  • Spectroscopy

Background:

  • Solar radiation scattering by clouds is crucial for Earth's energy balance.
  • Understanding cloud optical properties requires detailed spectral analysis.
  • Previous studies lacked comprehensive data across various cloud types and scattering angles.

Purpose of the Study:

  • To measure absolute intensity spectra of solar radiation scattered by clouds.
  • To investigate the angular dependence of cloud scattering across different wavelengths.
  • To differentiate scattering characteristics of ice and liquid water clouds.

Main Methods:

  • Acquisition of radiance spectra in the 1.15- to 3.6-micrometer region.
  • Measurements as a function of cloud type, altitude, and scattering angle.
  • Analysis of spectral features and scattering efficiency.

Main Results:

  • Scattering efficiency increased significantly with decreasing scattering angle, particularly in strongly absorbing regions (2.6-2.9 µm).
  • Ice clouds exhibited characteristic spectral minima at 1.5, 2.0, and 2.8 µm due to absorption.
  • These minima were absent in liquid-water clouds, despite similar bulk absorption properties.

Conclusions:

  • Particle size is a key factor explaining the observed differences in scattering behavior between ice and liquid water clouds.
  • The findings align with theoretical models of light scattering.
  • Spectral analysis provides valuable insights into cloud microphysical properties.