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Related Concept Videos

UV–Vis Spectrometers01:14

UV–Vis Spectrometers

The absorbance of UV and visible (UV–visible) radiations is measured using a UV–visible spectrophotometer. Deuterium lamps, which emit UV radiation, and tungsten lamps, which produce radiation in the visible region, are used as light sources in UV–visible spectrophotometers. A monochromator or prism is used for diffraction grating, i.e., to split the incoming radiation into different wavelengths. A system of slits is used to focus the desired wavelength on the sample cell. Samples for...
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.
The ATR process begins by directing a beam...
Spectrophotometry: Introduction01:16

Spectrophotometry: Introduction

Spectrophotometry is the quantitative measurement of the absorption, reflection, diffraction, or transmission of electromagnetic radiation through a material as a function of the intensity and wavelength of the radiation. A spectrophotometer is a device used to measure the change in the radiation intensity caused by its interaction with the material.
The essential components of a spectrophotometer include a source of electromagnetic radiation, a slot for placing a material to be analyzed, and a...
Atomic Absorption Spectroscopy: Interference01:25

Atomic Absorption Spectroscopy: Interference

Interference leads to systematic error in atomic absorption (AA) measurements by enhancing or diminishing the analytical signal or the background. These interferences can be grouped into three main categories: spectral interference, chemical interference, and physical interference.
Spectral interference occurs when signals from other elements or molecules overlap with the analyte signal, falsely elevating or masking the analyte's absorbance. This interference can be corrected using Zeeman,...
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...
Atomic Absorption Spectroscopy: Lab01:21

Atomic Absorption Spectroscopy: Lab

For AAS measurements, samples must be introduced as clear solutions, often requiring extensive preliminary treatment to dissolve materials like soils, animal tissues, and minerals. Common methods for sample preparation include treatment with hot mineral acids, wet ashing, combustion in closed containers, high-temperature ashing, or fusion with reagents.
 Solutions containing organic solvents, such as low-molecular-mass alcohols, esters, or ketones, enhance absorbances by increasing nebulizer...

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Related Experiment Video

Updated: Jun 23, 2026

Measurement of Particle Size Distribution in Turbid Solutions by Dynamic Light Scattering Microscopy
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Measurement of Particle Size Distribution in Turbid Solutions by Dynamic Light Scattering Microscopy

Published on: January 9, 2017

[Decomposing total suspended particle absorption based on the spectral correlation relationship].

Gui-Fen Wang1, Wen-Xi Cao, Ding-Tian Yang

  • 1LED Laboratory, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China. guifenwang@scsio.ac.cn

Guang Pu Xue Yu Guang Pu Fen Xi = Guang Pu
|April 24, 2009
PubMed
Summary

A new model accurately separates phytoplankton and nonalgal particle absorption, crucial for ocean color remote sensing. This method improves phytoplankton absorption retrieval from in situ and satellite data.

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Last Updated: Jun 23, 2026

Measurement of Particle Size Distribution in Turbid Solutions by Dynamic Light Scattering Microscopy
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Measurement of Particle Size Distribution in Turbid Solutions by Dynamic Light Scattering Microscopy

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Performing Spectroscopy on Plasmonic Nanoparticles with Transmission-Based Nomarski-Type Differential Interference Contrast Microscopy

Published on: June 5, 2019

Area of Science:

  • Oceanography
  • Remote Sensing
  • Biogeochemistry

Context:

  • Particulate absorption is key to ocean color.
  • Phytoplankton and nonalgal particles influence total absorption.
  • Accurate separation is needed for biogeochemical studies.

Purpose:

  • Develop a model to partition total particulate absorption into phytoplankton and nonalgal components.
  • Establish spectral relationships for phytoplankton and nonalgal particle absorption.
  • Validate the model using independent measurements.

Summary:

  • A novel model decomposes total particulate absorption spectra using distinct phytoplankton and nonalgal particle relationships.
  • Phytoplankton absorption is modeled quadratically with aph(443), and nonalgal absorption exponentially.
  • The model shows high accuracy (r2 > 0.97) and consistency with in situ measurements.

Impact:

  • Provides an effective tool for local applications in oceanographic research.
  • Eliminates the need for pigment concentration data.
  • Aligns with ocean color satellite sensor bands for broader applicability.