
Mass spectrometers
by Chris Woodford. Last updated: June 2, 2011.
Everyone loves a rainbow and most people understand, at least roughly, how they work: raindrops split a beam of white sunlight into rays of colored light, bending the blueish ones more than the reddish ones to make the well-known arc in the sky. Rain, then, is a brilliant method for separating sunlight. Chemists and physicists use a similar method for separating mixtures of substances into their components, turning them into beams of particles and then bending them with electricity and magnetism to make a kind of spectrum of different atoms that are easier to identify. This technique is called mass spectrometry and it was pioneered by British physicist Francis Aston in 1919. Let's take a closer look at how it works!
Photo: Left: A mass spectrometer at Pacific Northwest National Laboratory. Photo by courtesy of US Department of Energy.
What is a mass spectrometer?
Mass spectrometers are much simpler than they look—or sound. Suppose someone gives you a bucketful of atoms of different chemical elements and asks you what's inside. You need to separate out the atoms quickly and efficiently, but how do you do it? Simple! Tip your bucket into a mass spectrometer. It turns the atoms into ions (electrically charged atoms with either too few or too many electrons). Then it separates the ions by passing them first through an electric field, then through a magnetic field, so they fan out into a spectrum. A computerized detector tallies the ions in different parts of the spectrum and you can use this information to figure out what kinds of atoms were originally in your bucket. That's the basic idea, anyway. In reality, it's a bit more complex than this—there's no bucket, for a start!
Photo: A scientist uses a mass spectrometer in the Aeronomy Laboratory, Air Force Geophysics Laboratory (AFGL).
Photo by William W. Magel courtesy of US Air Force and Defense Imagery.




