C17- Spectroscopy Flashcards
(18 cards)
What increases the amount of vibration in a covalent bond
Temperature
Two types of bond vibration
Bend
Stretch
What does the amount that a bond bends/stretches depend on
The mass of the atoms in a bond- heavier atoms vibrate slower
Strength of the bond- Stronger bonds vibrate faster
What frequency of IR does a chemical bond absorb
a bond will only absorb the same frequency of IR as the natural frequency of the bond
Greenhouse gases in the atmosphere and IR radiation
Some of the suns radiation is reemitted from earth’s surface in longer wavelnegth IR
Greenhouse gases absorb this longer wavelength IR
Vibrating bonds then re emit the IR as temperature
Applications of IR
Identify and measure pollutants
Remote sensors identify vehicle emissions
monitors localised pollutions
Applications of IR
Breathalysers
Measure compounds inbreath such as ethanol
Can measure strength, as more IR absorbed means higher the reading and strength
Elemental analysis
Using percentage composition data to determine empirical formula
Mass spectroscopy
Use of molecular ion peak from a mass spectrum to determine molecular mass
IR spectroscopy
Use of absorption peaks from IR spectrum to identify bond and functional groups
What does a mass spectrometer detect
The mass to charge ratio of the molecular ion
This gives the molecular mass of the compound
Does not detect radicals
How to find the M+ peak on a mass spectrum
Clear peak at the highest m/z value
Why is there a M+1 peak on a mass spectrum
1.1% of carbon atoms are the carbon 13 isotope
This increases molecular mass by 1
What is fragmentation in a mass spectrum
Molecular ions break down into smaller pieces
What does fragmentation break a molecule into
A positively charged fragment ion
and a radical
Values of a CH2+ and C2H5+ fragment
15
29
Values of a CH2OH+ and a CH3CHOH+ fragment
31
45
The sun porduces mainly UV vsible and IR radiation which is partially refglected bvack to space when it reaches earth
Sme is absorbed by earth surface, heating it up
The earth emits this energy back out as IR
The IR radiation emitted by the earth can be absorbed by gases in the troposphere and become trappped
IR radiation is then re emitted in all directions some back towards earth, causing a heating effect