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Related Concept Videos

Gas Chromatography: Types of Detectors-II01:19

Gas Chromatography: Types of Detectors-II

In gas chromatography, different detectors are employed to meet specific analytical needs. These detectors are often categorized based on their detection mechanisms and the types of compounds they are best suited to analyze. Thermal Conductivity Detectors (TCD), Flame Ionization Detectors (FID), and Electron Capture Detectors (ECD) represent common categories, each with unique operating principles and applications. However, beyond these, several other detectors are designed for more specialized...
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Gas chromatography–mass spectrometry (GC–MS) is the combination of analytical techniques of gas chromatography and mass spectrometry in a single instrument for analyzing a mixture of compounds. The gas chromatograph separates the compounds in the mixture, and the mass spectrometer analyzes each compound separately to determine the molecular masses and molecular structures.
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Gas Chromatography: Types of Detectors-I01:21

Gas Chromatography: Types of Detectors-I

There are different types of detectors used in gas chromatography, each with its own specific properties that make it suitable for detecting certain types of analytes. The most commonly used detectors in GC are thermal conductivity detector (TCD), flame ionization detector (FID), and electron capture detector (ECD).
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Flame Photometry: Overview01:02

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Flame photometry, also known as flame emission spectrometry, is a technique used for the qualitative and quantitative analysis of elements present in a sample using a flame as the source of excitation energy. The concept of flame photometry was realized in the early 1860s by Kirchhoff and Bunsen, who discovered that specific elements emit characteristic radiation when excited in flames. The first instrument developed for this purpose was used to measure sodium (Na) in plant ash using a Bunsen...
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).
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Stable isotope measurements of martian atmospheric CO2 at the Phoenix landing site.

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Quantitative Analysis by Thermogravimetry-Mass Spectrum Analysis for Reactions with Evolved Gases
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Published on: October 29, 2018

Phoenix Mars Mission--the thermal evolved gas analyzer.

John H Hoffman1, Roy C Chaney, Hilton Hammack

  • 1University of Texas at Dallas, Richardson, Texas 75080, USA. jhoffman@utdallas.edu

Journal of the American Society for Mass Spectrometry
|August 22, 2008
PubMed
Summary

The Phoenix spacecraft analyzed Martian soil for water history and organic molecules. Its instruments, including the thermal evolved gas analyzer (TEGA), studied subsurface ice and atmospheric gases.

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Area of Science:

  • Planetary Science
  • Astrobiology
  • Geochemistry

Background:

  • The Phoenix mission aimed to investigate the Martian northern arctic region.
  • Understanding Mars's water history and potential for life is a key scientific goal.

Purpose of the Study:

  • To study the history of water on Mars.
  • To search for organic molecules in the icy subsurface Martian soil.
  • To analyze the composition and isotopic ratios of Martian atmospheric gases.

Main Methods:

  • Utilized the Phoenix lander equipped with an arm and scoop to access subsurface ice.
  • Employed the thermal evolved gas analyzer (TEGA) with eight ovens to heat soil samples.
  • Used a miniature magnetic sector mass spectrometer for gas analysis and isotopic ratio measurements.

Main Results:

  • Successfully landed and collected samples from the Martian northern arctic region.
  • The thermal evolved gas analyzer (TEGA) released gases and decomposition products from soil samples.
  • The mass spectrometer provided data on atmospheric composition and isotopic ratios, including noble gases.

Conclusions:

  • The Phoenix mission provided valuable data on the Martian environment and its potential habitability.
  • Analysis of subsurface ice and atmospheric gases contributes to understanding Mars's past and present conditions.
  • The use of advanced instruments like the mass spectrometer with a gas enrichment cell improved measurement accuracy.