Electromagnetism
5. Mass Spectrometers and Particle Physics
Learning outcomes
- I can explain the purpose of a mass spectrometer.
- I can describe how electric and magnetic fields separate charged particles.
- I can determine how mass-to-charge ratio affects particle motion.
- I can explain how isotopes can be identified using mass spectrometry.
- I can relate mass spectrometers to modern particle physics research.
Mass Spectrometers and Particle Physics
What Is a Mass Spectrometer?
A mass spectrometer is an instrument used to identify and separate charged particles according to their mass-to-charge ratio.
The mass-to-charge ratio is written:
m/q
or, in mass spectrometry, commonly:
m/z
where z represents the ion's charge number.
Mass spectrometers allow scientists to determine:
- which isotopes are present in a sample
- relative isotope abundances
- atomic and molecular masses
- chemical composition
- properties of unknown substances
- masses and identities of particles produced in physics experiments
The central idea is that electric and magnetic fields can control the motion of charged particles.
Why the Particles Must Be Charged
Electric and magnetic fields exert forces on charged particles.
For an electric field:
F_E = qE
For a moving particle in a magnetic field:
F_B = |q|vB sin θ
A neutral atom or molecule has:
q = 0
so it cannot be controlled directly by these forces in the same way.
Therefore, samples are typically converted into:
ions
before their mass-to-charge ratios are analyzed.
The Basic Stages of Mass Spectrometry
Different mass spectrometers use different designs, but a simplified system may contain:
- Ionization
- Acceleration
- Velocity selection or other ion control
- Deflection/separation
- Detection
- Data analysis
The details vary greatly between modern instruments, but these stages provide a useful model for understanding the physics.
Ionization
The first step is to produce charged particles.
Atoms or molecules may lose or gain electrons.
For example:
X → X⁺ + e⁻
The resulting positive ion can then respond to electric and magnetic fields.
An ion with one missing electron has charge:
q = +e
where:
e = 1.60 × 10⁻¹⁹ C
An ion with two missing electrons has:
q = +2e
The ion's charge is important because mass spectrometry separates particles according to:
m/q
not mass alone.
Acceleration by an Electric Field
Electric fields can accelerate ions.
If an ion of charge magnitude |q| is accelerated from rest through a suitable potential difference V:
|q|V = ½mv²
Therefore:
v = √(2|q|V/m)
This converts electrical potential energy into kinetic energy.
Electric fields are therefore useful for controlling the energy and speed of charged particles.
Example: Accelerating an Ion
A singly charged positive ion is accelerated from rest through:
V = 2000 V
Suppose:
m = 3.32 × 10⁻²⁶ kg
q = 1.60 × 10⁻¹⁹ C
Use:
|q|V = ½mv²
v = √(2|q|V/m)
v = √[(2)(1.60 × 10⁻¹⁹)(2000)/(3.32 × 10⁻²⁶)]
v ≈ 1.39 × 10⁵ m/s
The Velocity Selector
Some classic mass-spectrometer designs use a velocity selector.
A velocity selector contains crossed:
- electric field E
- magnetic field B
The fields are arranged so that the electric and magnetic forces act in opposite directions.
Electric force:
F_E = |q|E
Magnetic force:
F_B = |q|vB
for perpendicular motion.
For an undeflected particle:
F_E = F_B
Therefore:
|q|E = |q|vB
Cancel |q|:
v = E/B
Only particles travelling at this speed pass straight through.
Why a Velocity Selector Is Useful
Suppose different ions enter the magnetic analyzing region with many different speeds.
Their paths would depend on both:
- mass
- charge
- speed
This would make interpretation more difficult.
A velocity selector allows only ions with approximately the same selected speed to continue.
Then differences in trajectory depend mainly on:
mass-to-charge ratio
for a fixed magnetic field.
Magnetic Deflection
After velocity selection, ions may enter another magnetic field.
If the ions enter perpendicular to the field:
F_B = |q|vB
The magnetic force is always perpendicular to the velocity.
Therefore, it acts as a centripetal force.
The ions follow circular paths.
Deriving the Circular Radius
Magnetic force:
F_B = |q|vB
Centripetal force:
F_c = mv²/r
Set them equal:
|q|vB = mv²/r
Cancel one v:
|q|B = mv/r
Rearrange:
r = mv/(|q|B)
This is one of the most important equations for charged-particle motion in a magnetic field.
What Determines the Radius?
From:
r = mv/(|q|B)
we can see:
r ∝ m
Greater mass → larger radius
r ∝ v
Greater speed → larger radius
r ∝ 1/|q|
Greater charge magnitude → smaller radius
r ∝ 1/B
Stronger magnetic field → smaller radius
Mass-to-Charge Ratio
Rearrange:
r = mv/(|q|B)
to obtain:
m/|q| = Br/v
Therefore, if B, r and v are known, the particle's mass-to-charge ratio can be determined.
This is the fundamental measurement made by many forms of mass spectrometry.
Combining with a Velocity Selector
The velocity selector gives:
v = E/B₁
Suppose the analyzing magnetic field is B₂.
Then:
r = mv/(|q|B₂)
Substitute:
v = E/B₁
to obtain:
r = mE/(|q|B₁B₂)
If the same magnetic-field strength B is used in both regions:
r = mE/(|q|B²)
Therefore:
r ∝ m/|q|
when E and B are fixed.
Comparing Two Ions
Suppose two ions:
- have the same charge
- have the same speed
- enter the same magnetic field
Then:
r = mv/(|q|B)
so:
r ∝ m
The heavier ion follows a path with a:
larger radius
The lighter ion follows a path with a:
smaller radius
Example: Two Isotopes
Suppose two singly charged ions are isotopes of the same element.
Ion A:
mass = 20 u
Ion B:
mass = 22 u
Both have the same speed and enter the same magnetic field.
Then:
r_B/r_A = m_B/m_A
r_B/r_A = 22/20
r_B/r_A = 1.10
Therefore, the heavier isotope follows a circular path with a radius about:
10% larger
What Are Isotopes?
Isotopes are atoms of the same element with:
- the same number of protons
- different numbers of neutrons
Therefore, isotopes have:
- the same atomic number
- different mass numbers
For example, carbon includes:
- carbon-12
- carbon-13
- carbon-14
Their different masses allow them to be distinguished using mass spectrometry.
Separating Isotopes
Suppose two isotopes are ionized so that each has charge:
+e
They pass through the same velocity selector.
Therefore, they have the same speed.
They then enter the same magnetic field.
Since:
r = mv/(|q|B)
and v, |q| and B are identical:
r ∝ m
Therefore:
heavier isotope → larger radius
lighter isotope → smaller radius
The ions reach different locations on the detector.
Example: Neon Isotopes
Naturally occurring neon contains several isotopes, particularly:
- neon-20
- neon-21
- neon-22
If these atoms are ionized to the same charge and analyzed under the same conditions, their different masses produce different:
m/q values
They can therefore be detected separately.
The instrument can determine both:
- isotope identity
- relative abundance
Mass Spectrum
The output of a mass spectrometer is often represented as a:
mass spectrum
A mass spectrum plots signal intensity against:
mass-to-charge ratio, m/z
Each peak corresponds to ions with a particular m/z value.
The height or intensity of a peak indicates how much of that ion was detected relative to others.
For isotope measurements, this allows both isotope masses and relative abundances to be determined.
Reading an Isotope Mass Spectrum
Suppose an element produces two major peaks:
m/z = 35
and:
m/z = 37
If the ions are singly charged, these may correspond to isotopes with mass numbers approximately:
35 and 37.
If the peak at 35 is much larger, the isotope with mass 35 is more abundant.
Thus:
peak position → m/z
peak intensity → relative abundance
Relative Atomic Mass
Mass spectrometry can be used to calculate the average relative atomic mass of an element from its isotope abundances.
For example, suppose an element contains:
75% isotope-35
25% isotope-37
Then:
relative atomic mass = (35 × 0.75) + (37 × 0.25)
= 26.25 + 9.25
= 35.5
This explains why many relative atomic masses on the periodic table are not whole numbers.
Example: Isotope Abundance
Suppose an element has:
80% isotope-10
20% isotope-11
Average mass:
= (10 × 0.80) + (11 × 0.20)
= 8.0 + 2.2
= 10.2
Mass spectrometry provides the isotope data needed for calculations like this.
Charge State Matters
Mass spectrometers measure:
mass-to-charge ratio
not simply mass.
Consider an ion with mass:
40 u
and charge:
+1
Its approximate m/z is:
40
But if the same mass carried charge:
+2
its approximate m/z would be:
20
Therefore, charge state must be considered when interpreting mass spectra.
Why m/z Is Used
In practical mass spectrometry, the horizontal axis is usually labelled:
m/z
where:
- m represents ion mass
- z represents charge number
For a singly charged ion:
z = 1
so the m/z value corresponds closely to the ion mass in the conventional units used in mass spectrometry.
For multiply charged ions, the same particle can appear at a smaller m/z value.
Magnetic Field Does Not Change Particle Speed
The magnetic force acts perpendicular to the particle's velocity.
Therefore, a magnetic field acting alone:
- changes velocity direction
- does not change speed
- does not change kinetic energy
This makes magnetic fields especially useful for:
steering and separating particle beams
Electric fields, by contrast, can do work on charged particles and change their kinetic energy.
Electric Fields vs Magnetic Fields in Mass Spectrometry
| Electric Fields | Magnetic Fields |
|---|---|
| Can accelerate ions | Can bend ion trajectories |
| Can change kinetic energy | Acting alone, do not change kinetic energy |
| Force F = qE | Force magnitude F = |
| Used for acceleration and control | Used for deflection and separation |
| Can form part of velocity selector | Can form part of velocity selector |
Together, these fields provide powerful control over charged particles.
Example: Finding the Radius
A singly charged positive ion has:
m = 3.32 × 10⁻²⁶ kg
v = 2.0 × 10⁵ m/s
B = 0.50 T
q = 1.60 × 10⁻¹⁹ C
Use:
r = mv/(|q|B)
r = [(3.32 × 10⁻²⁶)(2.0 × 10⁵)] / [(1.60 × 10⁻¹⁹)(0.50)]
r = 0.083 m
Therefore:
r ≈ 8.3 cm
Example: Finding Mass
An ion travels at:
v = 3.0 × 10⁵ m/s
through:
B = 0.40 T
Its circular path has:
r = 0.20 m
The ion is singly charged:
|q| = 1.60 × 10⁻¹⁹ C
From:
r = mv/(|q|B)
rearrange:
m = |q|Br/v
m = [(1.60 × 10⁻¹⁹)(0.40)(0.20)]/(3.0 × 10⁵)
m ≈ 4.27 × 10⁻²⁶ kg
Example: Finding Mass-to-Charge Ratio
A particle follows a circular path with:
r = 0.15 m
in:
B = 0.80 T
at:
v = 4.0 × 10⁵ m/s
Use:
m/|q| = Br/v
m/|q| = (0.80)(0.15)/(4.0 × 10⁵)
m/|q| = 3.0 × 10⁻⁷ kg/C
Multi-Step Mass Spectrometer Problem
A velocity selector contains:
E = 6.0 × 10⁴ N/C
B₁ = 0.20 T
An ion passes through undeflected.
It then enters a second magnetic field:
B₂ = 0.50 T
and follows a circular path:
r = 0.10 m
The ion has charge:
|q| = 1.60 × 10⁻¹⁹ C
Find the speed
v = E/B₁
v = (6.0 × 10⁴)/(0.20)
v = 3.0 × 10⁵ m/s
Find the mass
Use:
m = |q|B₂r/v
m = [(1.60 × 10⁻¹⁹)(0.50)(0.10)]/(3.0 × 10⁵)
m ≈ 2.67 × 10⁻²⁶ kg
This demonstrates how electric and magnetic fields can be combined to determine an unknown particle mass.
From Mass Spectrometers to Particle Physics
The same principles used in a classroom mass spectrometer are important in particle physics.
Particle physicists need to determine properties such as:
- charge
- momentum
- mass
- energy
- particle identity
Charged particles moving through magnetic fields follow curved trajectories.
By studying these trajectories, scientists can reconstruct important properties of the particles.
Particle Momentum
For a charged particle moving perpendicular to a magnetic field:
r = mv/(|q|B)
For non-relativistic motion:
p = mv
Therefore:
p = |q|Br
More generally, the relationship between momentum and curvature remains fundamental in relativistic particle detectors, with the appropriate relativistic momentum.
Therefore:
large radius → larger momentum for fixed |q| and B
small radius → smaller momentum
Charge Sign from Curvature
Positive and negative particles curve in opposite directions in the same magnetic field.
Therefore, the direction of curvature can reveal the:
sign of the particle's charge
For example, two particles leaving a collision point and curving in opposite directions may carry opposite charges.
This is extremely useful in particle identification.
Particle Detectors
Modern particle detectors can contain:
- tracking detectors
- powerful magnets
- calorimeters
- particle-identification systems
- muon detectors
Tracking detectors record the paths of charged particles.
The magnetic field bends these paths.
From the curvature, scientists can determine information about:
- momentum
- charge sign
- particle interactions
High-Momentum Particles
From:
p = |q|Br
for a fixed magnetic field and charge magnitude:
larger momentum → larger radius
A very high-momentum particle bends only slightly.
A lower-momentum particle bends more strongly.
Therefore:
straighter-looking track → generally greater momentum
under otherwise comparable conditions.
Particle Collisions
In high-energy particle physics, beams of particles can be accelerated and collided.
The collisions may produce many new particles.
These particles move outward through detectors.
Charged particles curve in magnetic fields.
Neutral particles do not leave curved charged-particle tracks directly, although their presence may be inferred from:
- decay products
- energy deposits
- missing momentum or energy
- other detector signatures
Mass Spectrometry and Particle Detection: The Connection
Traditional mass spectrometry and particle-physics detectors share several fundamental ideas:
| Mass Spectrometry | Particle Physics |
|---|---|
| Ionizes atoms/molecules | Produces or studies subatomic particles |
| Uses electric fields | Uses electric fields for acceleration/control |
| Uses magnetic fields | Uses powerful magnetic fields |
| Measures m/z | Measures charge, momentum and other properties |
| Separates ions | Separates/reconstructs particle trajectories |
| Detects particles | Uses sophisticated particle detectors |
Both rely on the predictable motion of charged particles in electromagnetic fields.
Particle Accelerators
Particle accelerators use electric fields to increase particle energy.
Magnetic fields are then used to:
- steer beams
- bend trajectories
- focus particles
- maintain beam paths
This reflects the same basic distinction seen in mass spectrometry:
electric fields → change particle energy
magnetic fields → control particle direction
Mass Spectrometry in Modern Science
Mass spectrometry has applications far beyond basic isotope identification.
It is used in:
- chemistry
- environmental science
- geology
- astronomy
- medicine
- pharmaceuticals
- forensic science
- materials science
- nuclear physics
- particle physics
Scientists can use mass spectrometric techniques to identify extremely small quantities of substances and make very precise measurements of particle masses.
Dating and Isotope Studies
Mass spectrometers can precisely measure isotope ratios.
These measurements are useful in:
- radiometric dating
- geological studies
- climate reconstruction
- tracing chemical sources
- nuclear research
For example, isotope ratios can reveal information about the origin and history of materials.
Detecting Unknown Substances
Molecules can be ionized and sometimes broken into fragments.
Different fragments have different m/z values.
The resulting pattern can act like a:
molecular fingerprint
Scientists compare the pattern with known data to help identify an unknown substance.
This is widely used in analytical chemistry and forensic science.
Mass Spectrometers vs Particle Accelerators
A mass spectrometer is mainly designed to:
identify or analyze particles according to m/z
A particle accelerator is mainly designed to:
increase particle energy and control particle beams
However, both use many of the same electromagnetic principles.
The technologies therefore overlap strongly in their underlying physics.
Analyzing a Mass Spectrometer Problem
A useful strategy is:
Identify the stage
Is the particle being:
- accelerated?
- velocity-selected?
- magnetically deflected?
Choose the relevant equation
Acceleration:
|q|V = ½mv²
Velocity selector:
v = E/B
Magnetic deflection:
r = mv/(|q|B)
Check the charge
Remember that the device measures:
m/q
not simply m.
Check units
Use:
- kg for mass
- C for charge
- m/s for speed
- T for magnetic flux density
- m for radius
- V for potential difference
Equation Summary
Electric force
F_E = qE
Magnetic force magnitude
F_B = |q|vB sin θ
Magnetic force for perpendicular motion
F_B = |q|vB
Energy gained through a suitable potential difference
|q|V = ½mv²
Velocity selector
v = E/B
Circular radius
r = mv/(|q|B)
Mass-to-charge ratio
m/|q| = Br/v
Momentum from curvature
p = |q|Br
These equations connect the major ideas of charged-particle motion, mass spectrometry and particle detection.
Common Mistakes
Mistake: Saying a mass spectrometer separates particles only according to mass.
It responds to mass-to-charge ratio.
Mistake: Forgetting that particles must be charged.
Electric and magnetic fields require charged particles for direct electromagnetic control.
Mistake: Saying magnetic fields increase particle speed.
A magnetic field acting alone changes direction, not speed.
Mistake: Assuming heavier ions curve more strongly.
For equal q, v and B, heavier ions have a larger radius and therefore curve less sharply.
Mistake: Ignoring ion charge.
A doubly charged ion behaves differently from a singly charged ion of the same mass.
Mistake: Assuming m/z always equals mass.
This is approximately true for many singly charged ions when conventional mass-spectrometry units are used, but not for multiply charged ions.
Mistake: Confusing peak position with abundance.
Peak position indicates m/z; peak intensity indicates relative signal or abundance under the relevant measurement conditions.
Mistake: Saying all modern mass spectrometers use exactly the same magnetic-sector design.
Many modern instruments use different methods of separating and detecting ions. The magnetic-sector model is especially useful for understanding the underlying charged-particle physics.
Key Terms
Mass spectrometer — instrument used to separate and identify ions according to mass-to-charge ratio.
Mass-to-charge ratio (m/q) — ratio of particle mass to electric charge.
m/z — conventional mass-spectrometry notation for mass-to-charge ratio using the ion's charge number.
Ionization — process of producing charged particles from neutral atoms or molecules.
Ion — electrically charged atom or molecule.
Velocity selector — crossed electric and magnetic fields that allow particles of a selected speed to pass undeflected.
Magnetic deflection — bending of a charged-particle trajectory by a magnetic field.
Isotope — atom of an element with the same proton number but a different neutron number.
Mass spectrum — representation of detected ion signal against m/z.
Relative abundance — amount of one isotope or ion relative to others detected in the sample.
Detector — component that records arriving particles or ions.
Particle accelerator — device using electromagnetic fields to accelerate and control charged particles.
Tracking detector — detector used to reconstruct charged-particle trajectories.
Momentum — quantity related to mass and velocity; for charged-particle curvature in a magnetic field, p = |q|Br for perpendicular motion.
Key Takeaways
- A mass spectrometer analyzes charged particles according to mass-to-charge ratio.
- Neutral atoms or molecules must generally be ionized before electromagnetic analysis.
- Electric fields can accelerate ions and change their kinetic energy.
- Magnetic fields bend charged-particle trajectories.
- A velocity selector can produce particles with a selected speed using v = E/B.
- A particle moving perpendicular to a magnetic field can follow a circular path.
- The radius is r = mv/(|q|B).
- Greater mass produces a larger radius when q, v and B are unchanged.
- Greater charge magnitude produces a smaller radius.
- Stronger magnetic fields produce smaller radii.
- Mass spectrometry can separate isotopes because isotopes have different masses.
- Peak position in a mass spectrum identifies m/z.
- Peak intensity can provide information about relative abundance.
- Isotope abundances can be used to calculate average relative atomic mass.
- Mass spectrometers measure m/z rather than mass alone.
- Multiply charged ions can have much smaller m/z values than singly charged ions of the same mass.
- Magnetic curvature can be used to determine charged-particle momentum.
- Positive and negative particles curve in opposite directions in the same magnetic field.
- Particle accelerators and mass spectrometers use many of the same electromagnetic principles.
- Modern particle physics relies heavily on electromagnetic control and detection of charged particles.
Check Your Understanding
- What is the main purpose of a mass spectrometer?
- Why must particles normally be ionized before they can be analyzed using electric and magnetic fields?
- What is meant by mass-to-charge ratio?
- Describe the main stages of a simplified mass spectrometer.
- Explain how an electric field can accelerate an ion.
- State the energy equation for an ion accelerated from rest through a suitable potential difference.
- Explain how a velocity selector works.
- Derive v = E/B for an undeflected particle.
- Why is selecting particles with the same speed useful before magnetic deflection?
- Explain why a charged particle can follow a circular path in a magnetic field.
- State the equation r = mv/(|q|B) and explain each quantity.
- Two singly charged ions have the same speed in the same magnetic field. Which follows the larger-radius path: the heavier or lighter ion?
- Explain how isotopes can be separated using a mass spectrometer.
- What information does the position of a peak in a mass spectrum provide?
- What information can peak intensity provide?
- An element contains 60% isotope-10 and 40% isotope-11. Calculate its average relative atomic mass.
- A particle has m = 4.0 × 10⁻²⁶ kg, q = 1.60 × 10⁻¹⁹ C, v = 2.0 × 10⁵ m/s and enters a 0.50 T magnetic field perpendicularly. Calculate its circular radius.
- Explain why a +2 ion behaves differently from a +1 ion of the same mass and speed in the same magnetic field.
- Explain how the curvature of a charged-particle track can provide information about its momentum.
- Describe two important connections between mass spectrometry and modern particle-physics research.